35
REVIEWS Sonochemistry: Environmental Science and Engineering Applications Yusuf G. Adewuyi* North Carolina A and T State University, Department of Chemical Engineering, Greensboro, North Carolina 27411 Sonochemical engineering is a field involving the application of sonic and ultrasonic waves to chemical processing. Sonochemistry enhances or promotes chemical reactions and mass transfer. It offers the potential for shorter reaction cycles, cheaper reagents, and less extreme physical conditions, leading to less expensive and perhaps smaller plants. The amount of things that can be accomplished with sonochemistry is, at this stage, only limited by the minds of those working in this exciting field. Existing literature on sonochemical reacting systems is chemistry- intensive, and applications of this novel means of reaction in environmental remediation and pollution prevention seem almost unlimited. For example, environmental sonochemistry is a rapidly growing area that deals with the destruction of organics in aqueous solutions. However, some theoretical and engineering aspects are not fully understood. This paper reviews the field comprehensively by combining the existing knowledge from chemistry with insights into the pathways and kinetic analysis of environmental sonochemical reacting systems and with challenges for large-scale applications. The review is intended to advance our understanding and outline directions for future research. Contents 1. Introduction 4681 2. Theory 4682 2.1 Fundamentals of Ultrasound 4682 2.2 Factors Affecting Aqueous Sonochemical Processes 4682 2.3 Fundamentals of Sonochemical Reactions 4683 3. Types of Pollutants 4686 4. Prior Literature 4686 4.1 Aromatic Compounds 4686 4.2 Chlorinated Aliphatic Hydrocarbons 4700 4.3 Explosives 4702 4.4 Herbicides and Pesticides 4703 4.5 Organic Dyes 4704 4.6 Organic and Inorganic Gaseous Pollutants 4704 4.7 Organic Sulfur Compounds 4706 4.8 Oxygenates and Alcohols 4706 4.9 Other Organic Compounds 4706 4.10 Other Environmental Applications 4707 5. Discussion 4707 5.1 Reaction Pathways and Kinetics 4708 5.2 Effects of Water Quality 4708 5.3 Sonication Byproducts and Toxicity Effects 4709 5.4 Efficiency and Scale-up Issues 4709 6. Concluding Remarks 4711 7. Literature Cited 4712 1. Introduction When ultrasonic (or sonic) energy at high powers more than 1 / 3 W/cm 2 for water at room temperaturesis applied to a liquid, a “cold boiling” termed cavitation takes place. Simply put, cavitation is the formation, growth, and sudden collapse of bubbles in liquids. 1,2 Ultrasonic vibration reduces the thickness of liquid films, enhances gas transfer, and reduces bubble coa- lescence, which increases the interfacial area for gas transfer. 3-6 For example, the diffusion of liquids through porous media is enhanced by ultrasound. Ultrasound can be used to separate gases because lighter molecules in an ultrasonic field will travel further than heavier ones. Ultrasonic energy is also used to remove contami- nants from air and to break down toxic compounds in water and soil. 6 Nearly half of the 189 hazardous air pollutants (“air toxics”) regulated by the Clean Air Act Amendment (CAAA) of 1990 are volatile organic com- pounds (VOCs). This diverse list includes common solvents or halogenated aliphatic compounds, such as methylene chloride, chloroform, and trichloroethylene, all of which are mineralized by ultrasonic irradiation. 7-14 The term mineralization implies the final products of degradation reactions, which are carbon dioxide, short-chain organic acids, and/or inorganic ions. Ben- zene, well-known for its resistance to the action of strong * Phone: 336-334-7564. Fax: 336-334-7904. E-mail: adewuyi@ ncat.edu. 4681 Ind. Eng. Chem. Res. 2001, 40, 4681-4715 10.1021/ie010096l CCC: $20.00 © 2001 American Chemical Society Published on Web 10/04/2001

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REVIEWS

Sonochemistry: Environmental Science and EngineeringApplications

Yusuf G. Adewuyi*

North Carolina A and T State University, Department of Chemical Engineering,Greensboro, North Carolina 27411

Sonochemical engineering is a field involving the application of sonic and ultrasonic waves tochemical processing. Sonochemistry enhances or promotes chemical reactions and mass transfer.It offers the potential for shorter reaction cycles, cheaper reagents, and less extreme physicalconditions, leading to less expensive and perhaps smaller plants. The amount of things thatcan be accomplished with sonochemistry is, at this stage, only limited by the minds of thoseworking in this exciting field. Existing literature on sonochemical reacting systems is chemistry-intensive, and applications of this novel means of reaction in environmental remediation andpollution prevention seem almost unlimited. For example, environmental sonochemistry is arapidly growing area that deals with the destruction of organics in aqueous solutions. However,some theoretical and engineering aspects are not fully understood. This paper reviews the fieldcomprehensively by combining the existing knowledge from chemistry with insights into thepathways and kinetic analysis of environmental sonochemical reacting systems and withchallenges for large-scale applications. The review is intended to advance our understandingand outline directions for future research.

Contents

1. Introduction 46812. Theory 4682

2.1 Fundamentals of Ultrasound 46822.2 Factors Affecting Aqueous

Sonochemical Processes4682

2.3 Fundamentals of SonochemicalReactions

4683

3. Types of Pollutants 46864. Prior Literature 4686

4.1 Aromatic Compounds 46864.2 Chlorinated Aliphatic

Hydrocarbons4700

4.3 Explosives 47024.4 Herbicides and Pesticides 47034.5 Organic Dyes 47044.6 Organic and Inorganic Gaseous

Pollutants4704

4.7 Organic Sulfur Compounds 47064.8 Oxygenates and Alcohols 47064.9 Other Organic Compounds 4706

4.10 Other EnvironmentalApplications

4707

5. Discussion 47075.1 Reaction Pathways and Kinetics 47085.2 Effects of Water Quality 47085.3 Sonication Byproducts and

Toxicity Effects4709

5.4 Efficiency and Scale-up Issues 4709

6. Concluding Remarks 47117. Literature Cited 4712

1. IntroductionWhen ultrasonic (or sonic) energy at high powers

more than 1/3 W/cm2 for water at room temperaturesisapplied to a liquid, a “cold boiling” termed cavitationtakes place. Simply put, cavitation is the formation,growth, and sudden collapse of bubbles in liquids.1,2

Ultrasonic vibration reduces the thickness of liquidfilms, enhances gas transfer, and reduces bubble coa-lescence, which increases the interfacial area for gastransfer.3-6 For example, the diffusion of liquids throughporous media is enhanced by ultrasound. Ultrasoundcan be used to separate gases because lighter moleculesin an ultrasonic field will travel further than heavierones. Ultrasonic energy is also used to remove contami-nants from air and to break down toxic compounds inwater and soil.6 Nearly half of the 189 hazardous airpollutants (“air toxics”) regulated by the Clean Air ActAmendment (CAAA) of 1990 are volatile organic com-pounds (VOCs). This diverse list includes commonsolvents or halogenated aliphatic compounds, such asmethylene chloride, chloroform, and trichloroethylene,all of which are mineralized by ultrasonic irradiation.7-14 The term mineralization implies the final productsof degradation reactions, which are carbon dioxide,short-chain organic acids, and/or inorganic ions. Ben-zene, well-known for its resistance to the action of strong

* Phone: 336-334-7564.Fax: 336-334-7904.E-mail: [email protected].

4681Ind. Eng. Chem. Res. 2001, 40, 4681-4715

10.1021/ie010096l CCC: $20.00 © 2001 American Chemical SocietyPublished on Web 10/04/2001

oxidants, succumbs under ultrasonication in aqueousmedium.15 Sonochemical oxidation techniques involvethe use of sonic or ultrasonic waves to produce anoxidative environment via cavitation that yields local-ized microbubbles and supercritical regions in theaqueous phase.16 The collapse of these bubbles leads tosurprisingly high local temperatures and pressures.Locally, the high temperature and pressure may reachup to and above 5000 K and 1000 atm, respectively.17,18

These rather extreme conditions are very short-lived buthave shown to result in the generation of highly reactivespecies including hydroxyl (OH•), hydrogen (H•) andhydroperoxyl (HO2

•) radicals, and hydrogen peroxide.19-23

These radicals are capable of initiating or promotingmany fast reduction-oxidation (REDOX) reactions.These reactions with inorganic and organic substratesare fast and often near the diffusion-controlled rate.24-25

Sonochemistry is an example of advanced oxidationprocesses (or AOPs).26,27 As shown in Table 1, AOPs owetheir enhanced reactivity, as least in part to the genera-tion of reactive free radicals, the most important ofwhich is the excited hydroxyl radical (•OH).

A number of studies have documented the role ofsonochemistry in homogeneous and heterogeneouschemistry.28-30 Although the phenomena of sonochem-istry has been recognized for many years and despiteits recent advances, the mechanisms of homogeneousand heterogeneous sonochemistry are not fully under-stood. It is only recently that applications in synthesisand pollution control have prompted interest in indus-trial scale operation.31,32 Thompson and Doraiswamy33

and Moholkar et al.34 recently reviewed the fundamen-tals and science and engineering aspects of ultrasoundand its applications to organic synthesis. Luche28 dis-cusses the use of sonochemistry in organometallicsynthesis, biphasic systems, catalytic reactions, andorganic electrochemistry and the practical consider-ations for process optimization. However, the applica-tions of this novel means of reaction in environmentalremediation and pollution prevention seem almostunlimited. Sonication improves mass transfer and chemi-cal reaction and is expected to reduce or eliminatechemical usage, resulting in minimal sludge and dis-posal problems. This paper reviews the field of envi-ronmental sonochemistry comprehensively by combin-

ing the existing knowledge from chemistry with insightsinto the pathways and kinetic analysis of environmentalsonochemical reacting systems and with challenges forlong-term reliability and economical scaleup.

2. Theory2.1. Fundamentals of Ultrasound. Ultrasound are

waves at frequencies above those within the hearingrange of the average person, i.e., at frequencies above16 kHz (16 000 cycles per second).1,2 Ultrasonic energy(high frequency sound waves) produces an alternatingadiabatic compression and rarefaction of the liquidmedia being irradiated. In the rarefaction part of theultrasonic wave (when the liquid is unduly stretchedor “torn apart”), microbubbles form because of reducedpressure (i.e., sufficiently large negative pressures).These microbubbles contain vaporized liquid or gas thatwas previously dissolved in the liquid. The microbubblescan be either stable about their average size for manycycles or transient when they grow to certain size andviolently collapse or implode during the compressionpart of the wave. The critical size depends on the liquidand the frequency of sound; at 20 kHz, for example, itis roughly 100-170 µm. The implosions are the spec-tacular part of sonochemistry. The energy put into theliquid to create the microvoids is released in this partof the wave, creating high local pressures up to 1000atm and high transitory temperatures up to 5000 K.17-21

This energy-releasing phenomena of the bubble forma-tion and collapse is simply called cavitation or (“coldboiling”), or for the case described above, acousticcavitation.1,35-37 Cavitation can also be achieved bythrottling a valve downstream from a pump. Whenpressure at an orifice or any other mechanical constric-tion falls below the vapor pressure of liquid, cavitationsare generated which then collapse downstream with arecovery of pressure, giving rise to high temperatureand pressure pulses. Cavitation achieved from thismechanism is termed hydrodynamic cavitation.38

2.2. Factors Affecting Aqueous SonochemicalProcesses. Sonochemistry is complicated by the factthat the nature or the physicochemical properties of thesolvent, solute, or gas in the bubble can have dramaticeffect on the cavitational collapse.37 Cavities are morereadily formed when using solvents with high vaporpressure (VP), low viscosity (µ), and low surface tension(σ); however, the intensity of cavitation is benefited byusing solvents of opposite characteristics (i.e., low VP;high µ, σ, and density, F). The intermolecular forces inthe liquid must be overcome in order to form thebubbles. Thus, solvents with high densities, surfacetensions, and viscosities generally have higher thresholdfor cavitation but more harsh conditions once cavitationbegins.35 There are several properties of gases that canaffect sonochemical activities.5 The heat capacity ratio(Cp/Cv) or polytropic ratio (γ) of the gas in the bubbleaffects the amount of heat released and, hence the finaltemperature produced in an adiabatic compression andthe cause of reaction. Assuming adiabatic bubble col-lapse, the maximum temperatures and pressures withinthe collapsed cavitation bubbles (eqs 1 and 2) arepredicted by Noltingk and Nepprias from approximatesolutions of Rayleigh-Plesset equations.39-40

Table 1. Some Advanced Oxidation Technologies

(i) Fenton-Type ReactionsFe2+ + H2O2 f •OH + Fe3+ + OH-

(ii) Ozone-Peroxide-UV SystemsO3 + -OH f O2

- f •OH3O3 + UV (<400 nm) f 2 •OHH2O2 + UV (<400 nm) f 2 •OHH2O2 + O3 f 2•OHH2O2 + O3 + UV f •OH

(iii) Semiconductor Oxides-UV SystemsTiO2 + hv f TiO2 (h+ + e-)H+ + OH- f •OH

(iv) Radiolysis (High-Energy Beams):H2O f e-

aq + H• + •OH + (H2, H2O2, H3O+)

(v) Wet Oxidation (WO) Systems:RH + O2 f R• + HO2

RH + HO2• f R• + H2O2

H2O2 + M f 2 OH•

RH + OH• f R• + H2OR• + O2 f ROO•

ROO• + RH f ROOH + R•

(vi) Sonolysis (Ultrasound)H2O f H• + •OH

Tmax ) To[Pa(γ - 1)Pv

] (1)

4682 Ind. Eng. Chem. Res., Vol. 40, No. 22, 2001

where To ) ambient (experimental) temperature ortemperature of bulk solution, Pv ) pressure in thebubble at its maximum size or the vapor pressure ofthe solution, Pa ) pressure in the bubble at the momentof transient collapse (i.e., acoustic pressure), and γ )polytropic index of the cavity medium.5 As seen fromthese equations, higher temperatures and pressures aregenerated with monatomic gases with higher γ thanthose with polyatomic gases with lower γ. Anotherparameter that affects cavitational collapse is thethermal conductivity of the gas. Although compressionis adiabatic in the sonochemical process, small amountsof heat are transferred to the bulk liquid. A gas withlow thermal conductivity reduces heat dissipation fromcavitation site following adiabatic collapse and shouldfavor higher collapse temperature compared with highthermal conductivity gas. In addition, the gas with thehigher thermal conductivity reduces the temperatureachieved in a collapse. The solubility of the gas in theliquid used is also an important aspect; the more solublethe gas, the more likely it is to diffuse into the cavitationbubble. Dissolved gases form the nuclei for cavitation.Soluble gases should result in the formation of largernumber of cavitation nuclei and extensive bubble col-lapse since these gases are readily forced back to theaqueous phase.

As expected from sonochemical reactions, loweringtemperature increases the rate of reaction unlike mostchemical reacting systems. This is attributed to thelowering of the solvent vapor pressure which increasesthe intensity of cavitation. At low vapor pressure, lessvapor has an opportunity to diffuse into the bubble andthus cushion the cavitational collapse, therefore makingthe implosion more violent. Also, as liquid temperaturedecreases, the amount of gas dissolved increases andthe vapor pressure of the liquid decreases. Very volatilesolvents lead to relatively high pressures in the bubbleand also “cushion” the collapse. In some cases, theincrease of temperature may favor the reaction kineticsto a point and further increase in reaction temperatureleads to a decrease in the reaction rate.41

In the case of a progrssive planar or spherical wave,the acoustic (or sound) intensity (in W m-2) is directlyrelated to acoustic pressure by eq 3:

where F is the density of the fluid (e.g., water) and c isthe speed of sound in the fluid (1500m/s in water). Theacoustic power (W) represents the intensity emitted bya given surface. The term Fc represents the acousticimpedance (Z) of the medium. Values of Z for air, water,benzene, and ethanol are 400, 1.5 × 106, 1.1 × 106, and0.95 × 106, kg m-2 s-1 respectively.28 The literaturepoints to the conclusion that some increase in thepressure of the system should increase the reaction ratedue to the magnified effect of cavitation implosions.However, as pressure increases, the intensity must beincreased to obtain cavitation in the first place. Toomuch pressure reduces the rate of reaction by decreas-ing the frequency or efficiency of bubble formations.37

An increase in ultrasound intensity means an increasein the acoustic amplitude (i.e., Pa). The collapse time,

the temperature, and the pressure on collapse are alldependent on acoustic amplitude; the cavitation bubblecollapse will be more violent at higher acoustic ampli-tudes. An increase in intensity will thus result ingreater sonochemical effects in the collapsing bubble.5,28

The power delivered to a system depends to some extenton the frequency level. In most cases, as the power isincreased, the reaction rate also increases. At a criticalpower level, increasing the power will decrease the rateof reaction.42 Power input to the system is dependenton the amplitude. By increasing the amplitude, thepower is also increased.42,43 Sonochemical activity riseswith increasing intensity to an optimum above whichefficiency falls. According to Raleigh, the main conditionof effective action for ultrasonic cavitation is that thetime of cavity collapse should be smaller than half theultrasonics period (τ < T/2), as shown in eq 4.44,45 For abubble under constant external pressure (hydrostatic)from an initial or maximum radius, Rmax, to some finalradius, the relation is given by

where τ ) time of cavitation bubble collapse, Rmax ) themaximum radius of cavitation bubble, T ) ultrasonicperiod, Ph ) hydrostatic pressure, and F ) density ofliquid.28,44-45

When the acoustic power increases and simulta-neously increases amplitude of vibration, the maximumradius of the cavity bubble also increases, as well as itstime of collapse, τ, and this bubble is not able to collapsewithin time equal half of the period. That is, before thesound field reverses itself, and the rarefaction phasebegins acting on the collapsing bubble.

Frequency has significant effect on the cavitationprocess because it alters the critical size of the cavita-tional bubble.46-51 At very high frequencies, the cavi-tational effect is reduced because either (i) the rarefac-tion cycle of the sound wave produces a negativepressure which is insufficient in its duration and/orintensity to initiate cavitation or (ii) the compressioncycle occurs faster than the time for the microbubble tocollapse. Lower frequency ultrasound produces moreviolent cavitation, leading to higher localized temper-atures and pressures. However, current research indi-cates that in reactions such as oxidations, higherfrequencies may lead to higher reaction rates. This isdue to the fact that higher frequency may actuallyincrease the number of free radicals in the systembecause although cavitation is less violent, there aremore cavitation events and thus more opportunities forthe free radicals to be produced. Francony and Petrierobserved the ultrasonic degradation of carbon tetra-chloride was enhanced and the yield of products fasterwhen using 500 kHz ultrasound compared with 20kHz.48 But at very high frequencies, the cavitationprocess is decreased. Entezari and Kruus studied thesonochemical reaction rate of oxidation of iodide atdifferent temperatures (0-50 °C) and with differentultrasonic horns at low frequency (20 kHz) and with ahigh-frequency (900 kHz) apparatus.50 The resultsshowed that at 900 kHz the rate of oxidation increasedup to 30 °C at lower power levels whereas at 20 kHz,the rate of oxidation decreased with increasing temper-ature.

2.3. Fundamentals of Sonochemical Reactions.The influence of ultrasonic energy on chemical activity

Pmax ) Pv{Pa(γ - 1)Pv

}[γ/γ-1]

(2)

I )Pa

2

2Fc(3)

τ ≈ 0.915Rmax( FPh

)1/2< T

2(4)

Ind. Eng. Chem. Res., Vol. 40, No. 22, 2001 4683

may involve any or all of the following: production ofheat, promotion of mixing (stirring) or mass transfer,promotion of intimate contact between materials, dis-persion of contaminated layers of chemicals, and pro-duction of free-chemical radicals.1-3,52-53 The physicaleffects of ultrasound can enhance the reactivity of acatalyst by enlarging the surface area or accelerate areaction by proper mixing of reagents. The chemicaleffects of ultrasound enhance reaction rates because ofthe formation of highly reactive radical species formedduring cavitation.4,21 Homogeneous sonochemistry ex-amines, mainly in the liquid phase, the activity of theradicals or excited species formed in the bubble gasphase (OH•, H•, X•, C2

•, CN/, etc.) during the violentimplosion and their possible release into the liquid.28

The cavitation event also gives rise to acoustic micros-treaming or formation of miniature eddies that en-hances the mass and heat transfer in the liquid, andalso causes velocity gradients that results in shearforces. In heterogeneous sonochemistry, the mechanicaleffects of cavitation resulting from the erosion action ofmicrojets formed during asymmetric collapse of bubblesat the vicinity of interfaces are also important.28 So far,four theories have been proposed to explain the sono-chemical events: (1) hot-spot theory; (2) “electrical”theory; (3) “plasma discharge” theory, and (4) super-critical theory. These have led to several modes ofreactivity being proposed: pyrolytic decomposition, hy-droxyl radical oxidation, plasma chemistry, and super-critical water oxidation. The “hot-spot” theory suggeststhat a pressure of thousands of atmosphere (up to 1000atm) is generated and a temperature of about 5000 Kresults during the violent collapse of the bubble.17-19

Both Margulis54 and Lepoint55 advocate that the ex-treme conditions associated with fragmentative collapseare due to the intense electrical fields. The “electrical”theory by Margulis suggests that during bubble forma-tion and collapse, enormous electrical field gradients aregenerated and these are sufficiently high to cause bondbreakage and chemical activity.22,54 The “plasma theory”by Lepoint and Mullie also suggests the extreme condi-

tions associated with the fragmentative collapse is dueto intense electrical fields and seems not to involve atrue implosion. They liken the origin of cavitationchemistry to corona-like discharges caused by a frag-mentation process and supported their views by drawingnumerous analogies between sonochemistry and coronachemistry and indicating the formation of microplasmasinside the bubbles.55 The supercritical theory recentlyproposed by Hoffmann56 suggests the existence of alayer in the bubble-solution interface where tempera-ture and pressure may be beyond the critical conditionsof water (647 K, 22.1 MPa) and which may havephysical properties intermediate between those of a gasand a liquid. They showed that supercritical water isobtained during the collapse of cavitation bubblesgenerated sonolytically.

In general, most studies in environmental sonochem-istry have adopted the “hot spot” concepts to explainexperimental results. This theory considers a sonochem-ical reaction as a highly heterogeneous reaction in whichreactive species and heat are produced from a well-defined microreactor, “the bubble of cavitation.21,57 Inthe “structured hot spot” model shown in Figure 1, threeregions for the occurrence of chemical reactions arepostulated: (1) a hot gaseous nucleus; (2) an interfacialregion with radial gradient in temperature and localradical density; and (3) the bulk solution at ambienttemperature. Reactions involving free radicals can occurwithin the collapsing bubble, at the interface of thebubble, and in the surrounding liquid. Within the centerof the bubble, harsh conditions generated on bubblecollapse cause bond breakage and/or the dissociation ofthe water and other vapors and gases, leading to theformation of free radicals or the formation of excitedstates. Solvent and/or substrates suffer homolytic bondbreakage to produce reactive species. The high temper-atures and pressures created during cavitation providethe activation energy required for the bond cleavage.The radicals generated either react with each other toform new molecules and radicals or diffuse into the bulkliquid to serve as oxidants. The second reaction site is

Figure 1. Three reaction zones in the cavitation process.

4684 Ind. Eng. Chem. Res., Vol. 40, No. 22, 2001

the liquid shell immediately surrounding the implodingcavity, which has been estimated to heat up to ap-proximately 2000 K during cavity implosion. In thissolvent layer surrounding the hot bubble, both combus-tion and free-radical reactions (involving •OH derivedfrom the decomposition of H2O) occur.23 Reactions hereare comparable to pyrolysis reactions. Pyrolysis (i.e.,combustion) in the interfacial region is predominant athigh solute concentrations, while at low solute concen-trations, free-radical reactions are likely to predominate.At this interface between the bubble and bulk liquid,surface-active reagents also accumulate and speciesproduced in the bubble first react with chemicals in thebulk liquid. It has been shown that the majority ofdegradation takes place in the bubble-bulk interfaceregion.58,59 The liquid reaction zone was estimated toextend ∼200 nm from the bubble surface and had alifetime of <2 µs.17-19 In the bulk liquid, no primarysonochemical activity takes place although subsequentreactions with ultrasonically generated intermediatesmay occur. A small number of free radicals produced inthe cavities or at the interface may move into the bulk-liquid phase and react with the substrate presenttherein in secondary reactions to form new products.Depending on their physical properties and concentra-tions, molecules present in the medium will be “burned”in close to the bubble or will undergo radical reactions.

For example, reactions R4 and R7 in Table 2 do notoccur in the gaseous phase (where H2O2 is unstable)because of the prevailing high temperatures and pres-sures. Rather, these reactions occur at the relativelycooler interfacial region.

Some of the sonochemical reactions identified in thecavitational events are summarized in Table 2. Theformation of •H and •OH is attributed to the thermaldissociation of water vapor present in the cavities duringthe compression phase (R1). Sonolysis of water alsoproduces H2O2 and hydrogen gas, via hydroxyl radicalsand hydrogen atoms (R2-R7). The presence of oxygenimproves sonochemical activities, but it is not essentialfor water sonolysis, and sonochemical oxidation andreduction can proceed in the presence of any gas.However, in the presence of oxygen acting as a scaven-ger of hydrogen atom (and thus suppressing the recom-bination of •H and •OH), the hydroperoxyl radical (HO2

•)is additionally formed which is an oxidizing agent (R3).This radical causes a number other reactions to occurresulting in the formation of H2O2, O2, O, and H2 asproducts (R4-R9). Thermal dissociation of oxygen mol-ecule may also occur, leading to the generation ofadditional hydroxyl radicals (R38-R39). In the absenceof •OH scavengers, the main product of the sonolysis ofwater is H2O2 (R7). H2O2 can also be produced in an“inert” atmosphere but only at the expense of •OH

Table 2. Proposed Kinetic Mechanisms

A. Water DissociationH2O f H• + •OH R1 •OH + •OH f H2O2 R7 H• + H2O2 f •OH + H2O R13H• + H• f H2 R2 •OH + •OH f H2O + O• R8 H• + H2O2 f H2 + HO2

• R14H• + O2 f HO2

• R3 •OH + •HO2 f H2O + O2 R9 •OH + H2O2 f HO2• + H2O R15

HO2• + HO2

• f H2O2 + O2 R4 O• + O• f O2 R10 •OH + H2 f H2O + H• R16HO2

• + HO2• f H2O + 3/2O2 R5 1/2O2 + 2H• f H2O R11 H2O + •OH f H2O2 + H• R17

H• + HO2• f H2O2 R6 H• + OH• f H2O R12

B. Under N2 AtmosphereAs in R1 Plus

N2 f 2N• R18 NO + NO2 f N2O3 R25 NO + NO f N2O + O R32N• + •OH f NO + H• R19 N2O3 + H2O f 2HNO2 R26 N2O + O• f 2NO (or N2 + O2) R33NO + •OH f HNO2 R20 N• + H• f :NH R27 N2O + N2 f O• R34NO + •OH f NO2 + H• R21 :NH + :NH f N2 + H2 R28 N• + O2 f NO + O• R35NO + H• f N• + •OH R22 N2 + •OH f N2O + H• R29 NO + O f NO2

• R362 NO2(aq) + H2O f HNO2 + HNO3 R23 N2 + O• f N2O (or NO + N•) R30 2NO + O2 f 2NO2 R37NO2 + •OH f HNO3 R24 N• + NO f N2 + O R31

C. Under O2 AtmosphereAs in R1 Plus

O2 f 2O• R38 O• + H2 f •OH + H• R42 O3 + O f 2O2 R46O• + H2O f 2•OH R39 O• + HO2

• f •OH + O2 R43 2HO2• f H2O2 + O2 R47

O• + O2 fO3 R40 O• + H2O2 f •OH + HO2• R44 2•OH f H2O2 R48

H• + O2 f •OH + O• (or HO2•) R41 HO2

• f •OH + O• R45 2•OH f O• + H2O R49

D. Under Ar AtmosphereAs in R1 plus

•OH + •H + M f H2O + M R50 O• + H2O + M f H2O2 + M R55 O• + H2O f 2•OH R602•OH f •O + H2O R51 O2 + H• + M f HO2

• + M R56 Ar f Ar/ R612•OH + M f H2O2 + M R52 •OH + H2O2 f HO2

• + H2O R57 Ar/ + H2O f H2O/ + Ar R622H• + M f H2 + M R53 2HO2

• f H2O2 + O2 R58 H2O/ f H• + •OH R632O• + M f O2 + M R54 HO2

• + H• f H2O + O• R59

E. Under Air AtmospehreAs in B and C Plus

N2 + O2 f 2NO R64 NO2• + O• f NO3 R66 N2O5 + H2O f 2HNO3 R68

N2O• + O• f 2NO R65 NO2 + NO3 f N2O5 R67

F. Under H2 AtmosphereAs in R1 Plus

H2 f H• + H• R69 H2 + •OH f H2O + H• R70

G. Under CO2 AtmosphereAs in R1 Plus

CO2 + •H f CO + •OH R71 O• + O• f O2 R74 CO2 + H• f HCOO• R76CO2 f CO + O• R72 CO + O• f CO2 R75 HCOO• + H• f HCHO + O• R772H• + O• f H2O R73

Ind. Eng. Chem. Res., Vol. 40, No. 22, 2001 4685

radical (R51). Formation of atomic nitrogen and oxygen,nitrogen fixation (with HNO2 as the major acid compo-nent formed) can occur in the cavity.60 Nitrogen mol-ecules inside the cavitation bubble may react at hightemperature with hydroxyl radicals and oxygen atomsto give nitrous oxide and nitrogen oxide by a mechanismanalogous to that in combustion chemistry (R19, R29-R30). N2O is unstable under the high-temperatureconditions of the cavitation bubble and is furtherdecomposed in the gas phase and may be transformedto NO (R33).60 NO may undergo further reactions eitherin the gas-phase of acoustic cavities or free-radicalreactions in the cooler interfacial zone, ultimatelyresulting in the formation of nitrous and nitric acids(R20-R23). Nitrogen fixation is inhibited by H2 and COunder a hydrogen atmosphere; oxidation reactions arealmost completely suppressed owing to the strongreducing ability of •H. The inhibiting effect of CO onnitrogen is as follows. The oxygen formed in the irradi-ated water is used up in the oxidation of the COintroduced into the water with subsequent formationof CO2 (R74). The presence of CO (or CO2 in smallamount) may cause formation of HCHO in the cavita-tion bubble (R75-R76). If CO is introduced with N2 andH2, then HCN and HCHO are major products. HCN,NH3, and HCHO can be formed from solutions saturatedwith N2, CO, and H2.60 Another mechanism suggestedis that in which inert gases penetrating into a cavitycan contribute to the transfer of electron excitation towater or hydrogen molecules.22,44,60 For example, theexcited argon atom (Ar*) can participate in energytransfer reactions, as shown in reactions (R60-R62). Inthe presence of H2, argon also facilitates the formationof ‚H by direct dissociation of H2 within the cavitationbubble.

3. Types of Pollutants

A number of previous studies have examined thetransformation of pollutants by ultrasonic irradiationor combined ultrasound and other advanced oxidationtechniques to organic techniques to organic intermedi-ates with mineralizaton to inorganic ions, CO2, andshort-chain organic acids as final products in somecases. The pollutants studied and other environmentalapplications include:

(1) Aromatic Compounds• Phenol, 2-, 3-, 4- and 2,4-chlorophenols, p-nitrophenol,

and p-nitrophenyl acetate (PNPA)• Benzene, toluene, ethylbenzene, 1,3,5-trimethylben-

zene (mesitylene), xylene, fluoro-, bromo-, iodo- andchlorobenzene, hydroxybenzoic acids, humic acids,nitrobenzene, nitro- and chloro-toluene, and styrene

• Polycyclic aromatic hydrocarbons (PAHs),- anthracene,phenanthrene, pyrene, byphenyl, and dioxin

• Mixtures of chlorophenol and chlorobenzenes(2) Chlorinated Aliphatic Hydrocarbons (CAHs)• Trichloroethylene (TCE) and tetra- or perchloroethyl-

ene (PCE)• Carbon tetrachloride (CCl4), chloroform (CHCl3), dichlo-

romethane (CH2Cl2), and methylene chloride (CH3-Cl)

• 1,1,1-Trichloro and 1,2-dichloroethane• Chloral hydrate• Mixtures of CAHs with phenols, BTEX, or chloroben-

zenes

(3) Explosives• 2,4,6-Trinitrotoluene (TNT)• Cyclotrimethylene-trinitramine (RDX)• HMX (octahydro-1,3,5,7-tetranitro-1,3,5,7-tetrazocine)(4) Herbicides and Pesticides• Herbicides: atracine, alachlor, chlorpropham (isopro-

pyl-3-chlorocarbanilate 3-chloraniline)• Pesticides: pentachlorophenol (PeCP) and pentachlo-

rophenate (PCP), polychlorophenyls (PCBs), par-athion (O5-O-diethylo-p-nitrophenyl-thiophosphate),and phenyltrifluoromethyl ketone (PTMK)

(5) Organic Dyes• Azo dye, remazol black (RB)• Azo dye, naphthol blue black (NBB)(6) Organic and Inorganic Gaseous Pollutants• Greenhouse gasessfluorotrichlormethane (CFC 11),

trifluorotrichloro ethane (CFC 113), nitrous oxide, andcarbon dioxide

• Hydrocarbonssacetylene, methane, ethane, propane• Hydrogen sulfide• Ozone(7) Organic Sulfur Compounds• Carbon disulfide• Di-n-butylsulfide(8) Oxygenates and Alcohols• Methyl tert-butyl ether (MTBE), methanol, and etha-

nol• Mixtures of alcohols and chloromethanes• Mixtures of alcohols (i.e., ethanol), polyvinlpyrrolidone

(PVP), and tetranitromethane (TNM)(9) Other Organic Compounds• Surfactantsstert-octylphenoxy polyethoxyethanol (Tri-

ton X-100), polyoxyethylene alkyl ether (SS 70)• Formic acid and formates• Acetate• Thymine(10) Other Environmental Applications• Industrial wastes of a cyclohexane oxidation unit• Natural groundwater and organic matter• Biological treatment systems: toxicity reduction and

disinfection

4. Prior Literature

Studies involving the use of sonochemical or pho-tosonochemical processes to treat a variety of chemicalcontaminants mostly in aqueous systems are sum-marized in Table 3, highlighting the chemical oxidationschemes and experimental conditions utilized, removaleffectiveness, and intermediates and degradation prod-ucts observed.

4.1. Aromatic Compounds. The ultrasonic degrada-tion of phenol, chlorophenols, and nitrophenols havebeen studied by a number of investigators. The inter-mediates and products of the sonochemical oxidation ofphenol usually include hydroquinone, catechol, p- ando-benzoquinone, 2,5-dioxohexen-3-dioic, muconic, ma-leic, succinic, formic, propanoic, oxalic and acetic acids,and CO2. Berlan et al.61 observed that primary degrada-tion products such as dihydroxybenzenes and quinonesare further degraded upon time into the low molecularcarboxylic acids under mild external conditions (roomtemperature, atmospheric pressure) due to local extremeconditions resulting from cavitation, without the needfor any chemical reagent. Petrier et al.62 found the rateof sonochemical phenol degradation to proceed morerapidly at higher (i.e., 487 kHz) than low (i.e., 20 kHz)frequency with concomitant better release of •OH in the

4686 Ind. Eng. Chem. Res., Vol. 40, No. 22, 2001

Tab

le3.

Stu

die

sU

tili

zin

gS

onoc

hem

ical

and

Ph

otos

onoc

hem

ical

Deg

rad

atio

nof

Aq

ueo

us

Org

anic

and

Inor

gan

icP

ollu

tan

ts

auth

ors

con

tam

inan

tsde

grad

edco

nce

ntr

atio

n

chem

ical

oxid

atio

nsc

hem

eex

peri

men

tal

con

diti

ons

degr

adat

ion

inte

rmed

iate

s/pr

odu

cts

degr

adat

ion

effi

cien

cy/o

ther

resu

lts

orre

mar

ks

Ade

wu

yian

dC

olli

ns,

2001

a,b

carb

ondi

sulf

ide

(CS

2)6.

4-7.

10-

4

M,1

0.5

×10

-4

M,1

3.2-

13.6

×10

-4M

ult

raso

un

d:20

kHz,

14-

50W

tem

p,1-

50°C

;ir

radi

atin

gga

ses,

Air

,Ar,

He,

N2O

;pH

8-11

inai

r:s

ulf

ate

inth

epH

ran

ge8-

11de

grad

atio

nra

tes

inth

eir

radi

atin

gga

ses

isin

the

orde

rH

e>

Air

>N

2O>

Ar

Ali

ppie

tal

.,19

92ca

rbon

tetr

ach

lori

de(C

Cl 4

),ch

loro

form

(CH

Cl 3

)di

chlo

rom

eth

ane

(CH

2Cl 2

),(i

naq

ueo

us

solu

tion

ofK

I)

1.0-

5.0

MC

Cl 4

,1.0

MK

I

ult

raso

un

d(U

S)

(300

W)

tem

p,ro

om,

irra

diat

ion

tim

e,1-

3h

Fre

eio

din

ean

dC

l 2in

the

case

ofC

Cl 4

.HC

lin

ferr

edfr

ompH

decr

ease

.No

Cl 2

form

edw

ith

CH

Cl 2

and

CH

Cl 2

.

5.0

×10

-3

-3.

10-

3(m

oldm

-3 )

free

iodi

ne

yiel

d.

Bar

bier

and

Pet

rier

,19

96

4-n

itro

phen

ol(4

-Np)

0.5

mM

ult

raso

un

d/oz

onat

ion

ult

raso

un

d,20

kHz

(30

W),

500

kHz

(30

W);

O3

con

cen

trat

ion

,1.

72×

10-

4M

at20

kHz,

1.58

×10

-4

Mat

500

kHz

tem

p,20

(2

°C;p

H2;

irra

diat

ing

gas,

O3/

O2

(2-

3%O

3)

4-n

itro

cate

chol

,CO

2u

ltra

sou

nd-

enh

ance

dO

3m

iner

iliz

atio

npo

ten

tial

pote

nti

alof

subs

trat

e

Ber

lan

etal

.,19

94ph

enol

;an

ilin

e;2-

chlo

roph

enol

100

mg/

Lu

ltra

sou

nd

(30

W),

inte

nsi

ty,1

Wcm

-2at

541

kHz

and

27W

cm-

1at

20kH

z

tem

p,27

(2

°C;p

H6;

diss

olve

dga

s,ai

r,O

2,an

dA

r;so

lid

cata

lyst

hyd

roqu

inon

e,ca

tech

ol,

p-be

nzo

quin

one,

oxal

icm

alei

c,ac

etic

,for

mic

and

prop

anoi

cac

ids,

and

CO

2

Tot

alde

grad

atio

naf

ter

100

min

at54

1kH

z,u

nch

ange

dat

20kH

z.M

iner

aliz

atio

nof

phen

olim

prov

edw

ith

Ran

eyn

icke

l.B

hat

nag

aran

dC

heu

ng,

1994

met

hyl

ene

chlo

ride

;ch

loro

form

,CH

Cl 3

;ca

rbon

tetr

ach

lori

de,

CC

l 4;1

,2-d

ich

loro

eth

ane,

DC

A;

1,1,

1-tr

ich

loro

eth

ane,

TC

A;

tric

hlo

roet

hyl

ene

(TC

E);

perc

hlo

roet

hyl

ene

(PC

E)

50-

350

mg/

Laq

ueo

us

solu

tion

sof

VO

Cs

and

mix

ture

s

ult

raso

un

d(2

0kH

z,0.

1kW

/L)

tem

p,25

°C;

pH6-

5,7,

9N

och

lori

nat

edpr

odu

cts

dete

cted

.HC

lin

ferr

edfr

ompH

decr

ease

.

72-

99.9

%de

stru

ctio

nin

20-

40m

in.F

irst

-ord

erde

grad

atio

nki

net

ics

vari

esfr

om0.

021

to0.

046

min

-1 .

Bu

ttn

eret

al.,

1991

met

han

ol-

wat

erm

ixtu

res

0-10

0vo

l.%

CH

3OH

ult

raso

un

d(U

S)

(1-M

Hz,

2W

/cm

2 )

irra

diat

ion

tim

e,10

min

H2,

CH

2O,C

O,C

H4,

C2H

4,C

2H6

un

der

argo

n;C

O2,

CO

,H

CO

OH

,CH

2O,H

2O2,

H2

un

der

oxyg

en

degr

adat

ion

effi

cien

cyn

otex

plic

itly

give

n

Cat

allo

and

Jun

k,19

95ch

lorp

yrif

os,3

,3′,4

,4′-

tetr

ach

loro

azox

yben

zen

e(T

CA

OB

),2-

chlo

robi

phen

yl,

2,4,

8-tr

ich

loro

dibe

nzo

fura

n(T

CD

F),

lin

dan

e,al

drin

,h

exac

hlo

robe

nze

ne

(HC

B),

mix

ture

ofch

lori

nat

edol

efin

s,pa

rafi

ns

and

arom

atic

s

3µg

/mL

ult

raso

un

d(1

.6kW

h)

tem

p,4-

12°C

;so

nic

atio

nti

me,

6-10

hat

5-10

0ps

i.S

parg

edu

nde

rA

rfo

r1

hpr

ior

toru

n.

dech

lori

nat

ion

prod

uct

sde

tect

edfo

ral

lco

mpo

un

ds(e

xcep

tfo

rT

CA

OB

and

TC

DF

)u

nde

rm

inim

also

noc

hem

ical

con

diti

ons

not

expl

icit

lygi

ven

Ch

enet

al.,

1971

phen

ol(P

hO

H),

sew

erw

aste

trea

tmen

tef

flu

ent

Ph

OH

,10

0-70

0m

g/L

,sol

idca

taly

sts,

20-

200

mg

ult

raso

un

d,25

,55

,an

d80

0kH

z;in

ten

sity

,0-

33.3

W/c

m2

tem

p,22

°C;

irra

diat

ing

gas,

air;

cata

lyst

s,V

2O5,

PtO

2,A

g 2O

,Mn

O2,

and

Ru

O2

hyd

roqu

inon

e,ca

tech

olox

idat

ion

proc

eede

dto

war

dco

mpl

etio

nat

the

hig

hfr

equ

ency

Ch

endk

ean

dF

ogle

r,19

83

carb

onte

trac

hlo

ride

(pu

reC

Cl 4

,tw

o-ph

ase

wat

er-

CC

l 4so

luti

on,

satu

rate

dw

ater

solu

tion

inC

Cl 4

)

0-10

0vo

l.%

CC

l 4u

ltra

sou

nd

irra

diat

ion

tim

e,15

min

;pre

ssu

re,

1-20

atm

maj

orpr

odu

cts,

HC

lan

dH

OC

l;m

inor

prod

uct

s,C

2Cl 4

orC

2Cl 6

7.5-

20.0

%C

Cl 4

con

sum

ed

Ind. Eng. Chem. Res., Vol. 40, No. 22, 2001 4687

Tab

le3.

(Con

tin

ued

)

auth

ors

con

tam

inan

tsde

grad

edco

nce

ntr

atio

n

chem

ical

oxid

atio

nsc

hem

eex

peri

men

tal

con

diti

ons

degr

adat

ion

inte

rmed

iate

s/pr

odu

cts

degr

adat

ion

effi

cien

cy/o

ther

resu

lts

orre

mar

ks

Ch

eun

get

al.,

1991

met

hyl

ene

chlo

ride

,car

bon

tetr

ach

lori

de,

1,1,

1-tr

ich

loro

eth

ane,

tric

hlo

roet

hyl

ene

100-

1000

mg/

Laq

ueo

us

solu

tion

s

ult

raso

un

d(2

50W

)te

mp,

15-

20°C

Pro

duct

sn

otex

plic

itly

repo

rted

.HC

lfo

rmat

ion

infe

rred

from

pHdr

op.

Met

hyl

ene

chlo

ride

drop

ped

from

120

to25

ppm

in40

min

.Fir

st-o

rder

rate

con

stan

tof

3.93

×10

-2

min

-1ca

lcu

late

d.C

heu

ng

and

Ku

rup,

1994

flu

orot

rich

loro

met

han

e(C

FC

11),

trif

luor

otri

chlo

roet

han

e(C

FC

113)

50m

g/L

aqu

eou

sso

luti

on

ult

raso

un

d(2

0kH

z),b

atch

reac

tor

(160

W/4

.6W

/mL

),ci

rcu

lati

ng

reac

tor

(CR

),0.

64W

/mL

tem

p,5-

10°C

CR

at5

psig

HC

l,H

For

oth

erac

idic

spec

ies

(in

ferr

edfr

ompH

drop

)

alm

ost

100%

in40

min

for

CR

and

10m

info

rba

tch

reac

tor

Cos

tet

al.,

1993

p-n

itro

phen

ol(i

nth

epr

esen

ceof

com

mon

chem

ical

sof

nat

ura

lwat

er)

10-

5M

ult

raso

un

d(2

0kH

z,50

W)

tem

p,10

°C;

pH5.

5;ir

radi

atio

nm

ediu

m,a

ir

4-n

itro

cate

chol

degr

adat

ion

not

affe

cted

bych

emic

als

ofn

atu

ralw

ater

Dah

i,19

76R

hod

amin

eB

,E.c

oli

E.c

oli,

106 -

107

bact

eria

per

mL

son

ozon

atio

n;

ult

raso

un

d,20

kHz

ozon

e,3.

68-

3.94

mg

min

-1

L-

1

tem

p,18

°C;

pH7.

2;ir

radi

atio

nm

ediu

m,

O2/

O3

not

dete

rmin

edu

ltra

son

ictr

eatm

ent

ofef

flu

ent

from

biol

ogic

alse

wag

ere

duce

dth

est

eril

izat

ion

dose

ofO

3by

50%

and

deco

lora

tion

zero

-ord

erra

teco

nst

ant

ofR

hod

amin

eB

by55

%D

avid

etal

.,19

98ch

lorp

roph

am(i

sopr

opyl

-3-

chlo

roca

rban

ilat

e),

3-ch

loro

anil

ine

0.1

mM

aqu

eou

sso

luti

ons

son

olys

is,p

robe

tran

sdu

cer

(20

&48

2kH

z,40

W)

tem

p,20

°C;

irra

diat

ion

med

ium

,air

3-ch

loro

anil

ine,

HC

OO

H,C

O,C

O2,

Cl-

for

chlo

rpro

pham

;Cl-

,N

O2-

,N

O3-

,CO

,CO

2fo

r3-

chlo

roan

ilin

e

Deg

rada

tion

effi

cien

cyw

as10

0%af

ter

45m

inat

482

kHz

and

60%

at20

kHz.

Eff

icie

nt

elim

inat

ion

ofbo

thco

mpo

un

dsat

482

kHz.

De

Vis

sch

eran

dL

ange

nh

ove

1998

tric

hlo

roet

hyl

ene

(TC

E),

o-ch

loro

phen

ol(o

-CP

),1,

3-di

chlo

ro-2

-pro

pan

ol(D

CP

)

TC

E,3

.34

mM

;o-C

P,

0.36

2an

d0.

724

mM

;D

CP

,0.2

9m

M;H

2O2,

0,1,

10,1

00m

M;

Cu

SO

4,10

,41

mM

ult

raso

un

d(5

18kH

z,18

.2W

)w

ith

/wit

hou

tF

ento

nre

agen

t,h

ydro

gen

pero

xide

(H2O

2)or

orga

nic

pero

xide

s

solu

tion

tem

p,30

°C;

irra

diat

ion

med

ium

,air

not

repo

rted

H2O

2en

han

ced

o-C

Pde

grad

atio

nra

teby

20-

25%

.TC

Ean

dD

CP

un

affe

cted

byH

2O2.

Pre

sen

ceof

t-B

uO

OH

and

t-B

u-O

O-t

-Bu

inh

ibit

edde

grad

atio

n.

De

Vis

sch

eret

al.,

1997

eth

ylbe

nze

ne

(EB

)0.

5-1m

Maq

ueo

us

solu

tion

ult

raso

un

d(5

18(

1kH

z,13

Wpe

r15

0cm

3

solu

tion

)

solu

tion

tem

p,30

(1

°Cbe

nze

ne,

tolu

ene,

styr

ene,

cum

ene

prop

ylbe

nze

ne,

diph

enyl

met

han

e,1,

2-di

phen

ylet

han

e,be

nza

ldeh

yde

acet

oph

enon

e,ph

enyl

acet

ylen

e

Rat

esar

efi

rst-

orde

r.P

yrol

ysis

isan

impo

rtan

tpa

thw

ay.

De

Vis

sch

eret

al.,

1996

ben

zen

e(B

),et

hyl

ben

zen

e(E

B),

styr

ene

(S),

o-ch

loro

tolu

ene

(OC

)

B,3

.38,

1.69

,0.

9,an

d0.

45m

M;E

B,1

,0.

5,an

d0.

33m

M;O

C,

0.68

,0.3

4,0.

17m

M;S

,0.

97,0

.49,

and

0.25

mM

ult

raso

un

d(5

20kH

z)te

mp,

29(

1°C

;pH

7n

otre

port

edfi

rst-

orde

rki

net

icra

tes,

k(m

in-

1 ):

B,0

.027

1;E

B,

0.06

22;O

C,0

.043

1;S

,0.

0446

Dri

jver

set

al.,

1999

tric

hlo

roet

hyl

ene

(TC

E)

chlo

robe

nze

ne

(CB

)m

ixtu

res

ofT

CE

and

CB

TC

E,0

.84,

1.67

,an

d3.

37m

M;C

B,0

86,

1.72

,an

d3.

44m

M

ult

raso

un

d,52

0kH

z(1

4.23

(0.

73W

)te

mp,

29.5

+0.

5°C

;so

luti

onpH

7

prod

uct

sfr

omm

ixtu

reof

TC

Ean

dC

B,

C8H

4Cl 2

,C8H

6,C

l 2,

C8H

5,C

l 3,a

nd

C8H

4Cl 4

.

TC

E,3

.34

to0.

1in

90m

in.

Son

olys

isra

tes

ofT

CE

and

CB

depe

nd

onin

itia

lco

nce

ntr

atio

nof

TC

Ean

dC

B

4688 Ind. Eng. Chem. Res., Vol. 40, No. 22, 2001

Tab

le3.

(Con

tin

ued

)

auth

ors

con

tam

inan

tsde

grad

edco

nce

ntr

atio

n

chem

ical

oxid

atio

nsc

hem

eex

peri

men

tal

con

diti

ons

degr

adat

ion

inte

rmed

iate

s/pr

odu

cts

degr

adat

ion

effi

cien

cy/o

ther

resu

lts

orre

mar

ks

Dri

jver

set

al.,

1998

chlo

robe

nze

ne

1.72

mM

aqu

eou

sso

luti

on.

ult

raso

un

d,52

0kH

z(1

4.23

(0.

73W

,0.0

95W

ml-

1 )

tem

p,29

.5(

0.5

°C;

solu

tion

pH,

4.7,

7,10

;ir

radi

atio

nga

s,A

r,ai

r

met

han

e,ac

etyl

ene,

bute

nyn

e,bu

tadi

yne,

phen

ylac

etyl

ene,

ben

zen

e,n

on-c

hlo

rin

ated

mon

o-an

ddi

cycl

ich

ydro

carb

ons,

chlo

roph

enol

s,C

P(i

nth

epr

esen

ceof

air

only

)

Arg

onac

cele

rate

dde

grad

atio

nra

tes

com

pare

dw

ith

air.

Dri

jver

set

al.,

1996

tric

hlo

roet

hyl

ene

(TC

E)

3.34

mM

aqu

eou

sso

luti

on

ult

raso

un

d,52

0kH

z(0

.095

W/m

L),

20kH

z(0

.43

W/m

L)

tem

p,29

-32

°C;p

H,

4.7,

7,10

;ir

radi

atio

nga

s,ai

r,A

r

C2H

Cl,

C2C

l 2,C

4Cl 2

,C

2Cl 4

,C4H

Cl 3

,C4C

l 4,

C4H

Cl 5

,C4C

l 6

Con

cen

trat

ion

decr

ease

dfr

om3.

34to

0.25

mM

at52

0kH

zan

d3.

34to

0.5

mM

at20

kHz

in60

min

.

D’S

ilvi

aet

al.,

1990

ben

zo[a

}pyr

ene

(B[a

]P,

ben

zo[g

hi]

pery

len

e,co

ron

ene

(PA

Hs)

and

2-ch

loro

dibe

nzo

-p-d

ioxi

n(i

n20

%et

han

ol-

wat

er),

tric

hlo

roet

hyl

ene

(TC

E),

1,1,

1-tr

ich

loro

eth

ane

(TC

A)

PA

Hs,

8.9-

15m

g/L

,pu

reor

nea

tT

CE

and

TC

A

ult

raso

un

d(1

8kH

z,50

W)

PA

Hso

luti

ons

typi

call

yso

nic

ated

for

over

2h

peri

od

PA

Han

dD

ioxi

n,f

ine

carb

onac

eou

sde

posi

ts;

TC

Ean

dT

CA

,bro

wn

poly

mer

icm

ater

ials

B[a

]Pin

20%

aqu

eou

set

han

ol,9

9.1%

,94.

1%an

d22

%de

grad

atio

nra

tes

afte

r60

min

for

init

ial

con

cen

trat

ion

sof

1.1,

8.9

and

21.5

ppm

resp

ecti

vely

,si

gnif

ican

tly

low

erfo

r10

0%et

han

olso

luti

onal

one.

Eil

er,

1994

VO

Cs,

tric

hlo

roth

ylen

e(T

CE

)pr

imar

ily;

BT

EX

,B

enze

ne

(Bz)

;tol

uen

e(T

L);

eth

ylbe

nze

ne

(EB

);xy

len

es(X

L)

TC

E,

1475

-20

00;

Bz,

240-

500;

TL

,8-

11;X

L,

up

to10

0(a

llin

ppb)

CA

VO

Xsy

stem

,se

quen

tial

hyd

rody

nam

icca

vita

tion

(360

W,5

&10

kW)

and

UV

phot

olys

is(l

ow-p

ress

ure

Hg

lam

p,2.

5-10

kW)

H2O

2ad

ded

befo

reth

eca

vita

tion

cham

ber

orga

nic

acid

s,h

alid

es,

CO

2an

dH

2Ore

mov

alef

fici

enci

esgr

eate

rth

an99

.9%

for

TC

Ean

dB

TE

X

En

teza

riet

al.,

1997

carb

ondi

sulf

ide

(CS

2)pu

reC

S2

ult

raso

un

d,90

0kH

z(2

9W

)an

d20

kHz

(49

W)

tem

p,-

50to

+10

°C;

irra

diat

ing

gas,

Ar,

H2,

air,

He,

O2,

CO

2

amor

phou

sca

rbon

and

mon

ocli

nic

sulf

ur

effe

ctof

irra

diat

ing

gas

onra

te,H

e>

H2

>A

ir>

O2,

neg

ligi

ble

rate

at90

0kH

z

Gon

drex

onet

al.,

1999

pen

tach

loro

phen

ol(P

CP

)10

-4

Maq

ueo

us

solu

tion

s

thre

e-st

age

son

och

emic

alre

acto

r(5

00kH

zea

ch,0

-10

0W

)

tem

p,20

(2

°C;s

olu

tion

pH7

No

prod

uct

san

din

term

edia

tes

dete

rmin

ed.

con

vers

ion

rate

su

pto

80%

for

ult

raso

nic

un

its

inse

ries

Gon

zeet

al.,

1999

Sod

ium

pen

tach

loro

phen

ate

(NaP

CP

)as

was

tew

ater

mod

elco

mpo

un

d.B

acte

ria

(vib

rio

fisc

her

i).D

aph

nid

s(D

aph

nia

mag

na)

.

0.1

mM

sequ

enti

alu

ltra

son

ic/

biol

ogic

altr

eatm

ent;

Ele

ctri

cal

gen

erat

or,5

00kH

z,0-

100W

tem

p,20

(2

°Cso

luti

on,

pH6.

8-7.

5;op

erat

ing

wat

tage

,55

-65

W

degr

adat

ion

prod

uct

sn

otre

port

edU

ltra

son

icir

radi

atio

nde

crea

sed

imm

ense

lyth

eto

xici

tyof

NaP

CP

tom

icro

orga

nis

ms

and

cou

ldbe

use

das

preo

xida

tion

step

befo

rebi

olog

ical

trea

tmen

t.G

uti

erre

zan

dH

engl

ein

,19

88

poly

(vin

ylpy

rrol

idon

e)(P

VP

),et

han

ol(E

tOH

)an

dte

tran

itro

met

han

e(T

NM

)in

aqu

eou

sso

luti

on

PV

P,0

-0.

1M

EtO

H,

0-0.

5M

TN

M,4

.5×

10-

3M

and

10-

3M

(in

wat

erpl

us

glyc

ol,

glyc

erin

,or

prop

anol

-2)

ult

raso

un

d(3

00kH

z,2

Wcm

-2 )

irra

diat

ing

med

ium

,Ar

PV

Pan

dE

tOH

,CH

4,C

2H6,

CH

2O,C

H3C

HO

,C

2H6,

CO

,CO

2;T

NM

,C

(NO

2)3-

,NO

2-,

NO

3-,

N2,

CO

,CO

2

Th

ede

com

posi

tion

ofT

NM

ison

eof

the

fast

est

son

och

emic

alre

acti

ons.

Max

imu

mra

tes

ofP

VP

occu

rred

atab

out

0.04

M

Ind. Eng. Chem. Res., Vol. 40, No. 22, 2001 4689

Tab

le3.

(Con

tin

ued

)

auth

ors

con

tam

inan

tsde

grad

edco

nce

ntr

atio

n

chem

ical

oxid

atio

nsc

hem

eex

peri

men

tal

con

diti

ons

degr

adat

ion

inte

rmed

iate

s/pr

odu

cts

degr

adat

ion

effi

cien

cy/o

ther

resu

lts

orre

mar

ks

Gu

tier

rez

etal

.,19

86aq

ueo

us

acet

ate

solu

tion

s0-

0.8

mol

/dm

3

acet

ate

ult

raso

un

d,30

0kH

z(1

6W

)te

mp,

room

(2

°C;

irra

diat

ing

gas,

Ar;

irra

diat

ing

tim

e,30

min

maj

or,s

ucc

inic

,gly

coli

can

dgl

yoxy

lic

acid

,an

dsm

alle

ram

oun

tsof

HC

HO

,CO

2;m

inor

,CH

4

At

acet

ate

con

cen

trat

ion

grea

ter

than

0.4

mol

/dm

3 ,C

O2

and

CO

beca

me

the

pred

omin

ant

prod

uct

sof

son

olys

is.

Ham

lin

etal

.,19

61ca

rbon

tetr

ach

lori

de(C

Cl 4

)an

dch

loro

form

(CH

Cl 3

)in

aqu

eou

ssu

spen

sion

2m

LC

Cl 4

orC

HC

l 3in

20m

LH

2O

ult

raso

nic

gen

erat

or,

med

ical

(15

W,

1mc-

sec,

3W

/cm

2 ),e

lect

ric

(5W

,300

kc/s

)

tem

p,20

°C;

irra

diat

ing

gas,

Ar;

irra

diat

ing

tim

e,15

-18

0m

in

CC

l 4:

CO

2,O

2,C

l 2,

HC

l,C

2Cl 6

,C2C

l 4;

CH

Cl 3

:H

Cl,

C2C

l 6,

C2C

l 4

wit

hC

Cl 4

alon

e(n

ow

ater

),ca

vita

tion

occu

rred

but

ther

ew

asn

ore

acti

on

Har

ada,

1998

carb

ondi

oxid

e(C

O2)

CO

2in

dist

ille

dw

ater

(0.0

-0.

60m

ole

frac

tion

)

ult

raso

un

d(2

00kH

z,20

0W

)te

mp,

5-45

°C;

irra

diat

ion

gas,

Ar,

He,

H2,

N2

gase

ous

prod

uct

s;m

ajor

,CO

,H2;

min

or,

O2

the

decr

easi

ng

rate

for

CO

2fo

llow

edth

eor

der

Ar

>H

eH

2>

N2

Har

tet

al.,

1990

acet

ylen

ein

aqu

eou

sso

luti

ons

0-10

-2

Mu

ltra

sou

nd

quar

tzge

ner

ator

(1M

Hz,

2W/c

m2 )

irra

diat

ing

med

ium

,Ar

H2,

CO

,CH

4,H

CO

OH

,C

H3C

OO

H,H

CH

O,

CH

3CH

O,o

ther

C2-

C8

hyd

roca

rbon

s,in

solu

ble

soot

,C6H

6,st

yren

e,n

aph

thal

ene,

and

phen

ylac

etyl

ene

Pro

duct

ssi

mil

arto

thos

ein

pyro

lysi

san

dco

mbu

stio

n.

Max

imu

mra

teoc

curr

edat

10-

3M

or5

vol%

ofC

2H2

Har

tet

al.,

1990

met

han

e(C

H4)

,eth

ane

(C2H

6)w

ater

con

tain

ing

2-10

0vo

l%C

H4

orC

2H6

inA

r

ult

raso

un

d,30

0kH

z,2

W/c

m2

irra

diat

ion

gas,

Ar

maj

orpr

odu

cts,

hyd

roge

n,a

cety

len

e,et

hyl

ene,

eth

ane;

min

or,C

O,p

ropa

ne,

prop

ene

max

imu

mde

com

posi

tion

occu

rsat

15%

for

met

han

ean

d10

%fo

ret

han

e

Har

tan

dH

engl

ein

,198

8fo

rmic

acid

-w

ater

mix

ture

s0-

30M

aqu

eou

sso

luti

on

ult

raso

un

d(3

00kH

z,2

W/c

m2 )

gas

med

ium

,A

rm

ajor

,H2C

O2,

CO

;m

inor

,oxa

lic

acid

At

15M

HC

OO

H,o

vera

llra

teof

deco

mpo

siti

onis

540

mM

min

-1 .

Har

tan

dH

engl

ein

,19

86

ozon

e(O

3)in

aqu

eou

sso

luti

ons

O3,

353

&62

8m

M,1

.6m

Mu

ltra

sou

nd,

300

kHz

tem

p,33

°C;

irra

diat

ion

gas,

Ar

+O

2/O

3m

ixtu

re

H2O

2fo

rmat

ion

rapi

dde

com

posi

tion

rate

ofoz

one

(3m

M/m

in)

occu

rred

at[O

3])

1m

M

Har

tan

dH

engl

ein

,19

86

nit

rou

sox

ide

(N2O

)w

ater

con

tain

ing

0-10

0vo

l%

N2O

inA

r

ult

raso

un

d,30

0kH

zir

radi

atio

nga

s,A

rN

2,O

2,N

O2-

,N

O3-

max

imu

myi

eld

obta

ined

atA

r/N

2Ovo

l%ra

tio

of85

:15

Har

tan

dH

engl

ein

,19

85

solu

tion

sof

KI

and

sodi

um

form

ate

(HC

O2N

a)in

pure

and

ozon

ized

wat

er

HC

O2-

,0.

001,

0.01

&0.

1M

KI;

0.1

M

ult

raso

un

d,30

0kH

z;O

3,31

.8&

67.4

mM

irra

diat

ing

gas,

Ar,

O2,

and

Ar/

O2

mix

ture

;so

luti

onpH

6.32

-12

.07

KI:

iodi

ne,

H2O

2;H

2al

sofo

rmed

inth

eab

sen

ceof

O2.

HC

O2N

a:H

2O2,

H2,

CO

2an

dox

alat

ein

the

abse

nce

ofO

2;H

2O2

and

CO

2(a

bsen

ceof

O2)

the

yiel

dof

H2O

2w

asab

out

4ti

mes

grea

ter

un

der

Ar/

O2

mix

ture

(70/

30%

)th

anu

nde

rth

epu

rega

ses

Hen

glei

n,

1985

carb

ondi

oxid

e(C

O2)

,n

itro

us

oxid

e(N

2O),

met

han

e(C

H4)

CO

2-N

2O-

CH

4co

nta

inin

gaq

.so

luti

ons

(0.0

.1m

ole

frac

tion

);E

than

ol(0

.05M

);K

I(0

.1M

)

ult

raso

un

d,30

0kH

z(3

.5W

/cm

2 )bu

lkso

luti

onte

mp,

20°C

;ir

radi

atin

gga

s,A

r

CO

2:m

ajor

,CO

;min

or,

HC

OO

H.N

2O:

N2,

nit

rite

,nit

rate

.CH

4:C

2H6,

C3-

and

C4-

hyd

roca

rbon

s,C

O,C

O2,

CH

2O

No

chem

ical

effe

cts

occu

rred

duri

ng

irra

diat

ion

un

der

anat

mos

pher

eof

pure

CO

2,N

2O,o

rC

H4.

Son

och

emis

try

char

acte

rize

dby

ast

ron

gli

nka

gebe

twee

nth

eso

nol

ysis

ofw

ater

and

the

gas.

Hir

aiet

al.,

1996

CF

C-1

13(F

2ClC

-C

Cl 2

F),

HC

FC

-225

ca(F

3C-

CF

2-C

Cl 2

H),

HC

FC

-225

cb(F

2ClC

-C

F2-

CC

lFH

)an

dH

FC

-134

a(F

3C-

CF

2H)

inw

ater

CF

C-1

13,

25-

1000

ppm

;H

CF

C-

225c

a,cb

,100

ppm

;H

FC

-134

a,30

0pp

m

ult

raso

un

d(2

00kH

z,6

W/c

m2 )

irra

diat

ion

med

ium

,Ar,

air

CO

,CO

2,C

l-,F

-C

FC

san

dH

CF

Cs

are

read

ily

deco

mpo

sed

∼CF

C-1

13de

grad

atio

nfa

ster

un

der

argo

nth

anai

r

4690 Ind. Eng. Chem. Res., Vol. 40, No. 22, 2001

Tab

le3.

(Con

tin

ued

)

auth

ors

con

tam

inan

tsde

grad

edco

nce

ntr

atio

n

chem

ical

oxid

atio

nsc

hem

eex

peri

men

tal

con

diti

ons

degr

adat

ion

inte

rmed

iate

s/pr

odu

cts

degr

adat

ion

effi

cien

cy/o

ther

resu

lts

orre

mar

ks

Hu

aet

al.,

1995

p-n

itro

phen

ol(p

-Np)

inaq

ueo

us

solu

tion

100

µMn

ear-

fiel

dac

oust

ical

proc

esso

r(N

AP

),16

and

20kH

z,0-

1775

W

tem

p,22

-25

°C;s

olu

tion

pH4.

5-5.

0;ir

radi

atio

nm

ediu

m,A

r,O

2,m

ixtu

reof

Ar/

O2

4-n

itro

cate

chol

(4-N

C);

oth

erpr

odu

cts

not

repo

rted

her

e

firs

t-or

der

rate

con

stan

tsat

1.4W

/cm

2h

igh

erin

Ar

than

inO

2,k O

2)

5.19

×10

-4

s-1

k Ar

)7.

94×

10-

4s-

1

Hu

aet

al.,

1995

p-n

itro

phen

ylac

etat

e(P

NP

A)

inaq

ueo

us

solu

tion

100

µMim

mer

sion

-pro

beu

ltra

sou

nd

(115

W,9

6W

/cm

2 )

tem

p,25

°Cso

luti

onpH

3-8;

irra

diat

ion

gas,

Kr,

Ar,

He

maj

or,h

ydro

lysi

spr

odu

cts;

min

or,N

O2-

,NO

3-h

ydro

lysi

sra

teco

nst

ants

vari

esfr

om9.

10-

5to

3.8

×10

-4

s-1 ,

depe

ndi

ng

ondi

ssol

ved

gas,

acce

lera

ted

byu

ltra

sou

nd

Hu

aan

dH

offm

ann

1996

carb

onte

trac

hlo

ride

(CC

l 4)

and

p-n

itro

phen

ol(p

-Np)

+C

Cl 4

inw

ater

wit

h/w

ith

out

satu

rati

onw

ith

Ozo

ne

(O3)

CC

l 4,1

.95

×10

-4

and

1.95

×10

-5

mol

L-

1 ;p-

Np,

100

µM

ult

raso

un

d(2

0kH

z,13

5or

112.

5W

/cm

2 )

solu

tion

pH11

.8;

irra

diat

ion

gas,

Ar

CC

l 4:

C2C

l 4,

C2C

l 6,C

l-,

HO

Cl,

p-N

p;4-

nit

roca

tech

ol(4

-NC

)

CC

l 4:

90%

and

99%

redu

ctio

naf

ter

12an

d90

min

,res

pect

ivel

y;n

otaf

fect

edby

O3.

Deg

rada

tion

ofp-

Np

enh

ance

dsi

gnif

ican

tly

byC

Cl 4

and

4-n

itro

cate

chol

accu

mu

lati

onm

inim

ized

Hu

ng

etal

.,20

00n

itro

ben

zen

e(N

B)

25µM

ult

raso

un

d(U

S)/

Fe°

.US

,20

kHz

(139

W/L

);F

e°,0

-88

g/L

tem

p,15

(2

°C;i

nit

ialp

H6

inte

rmed

iate

s:w

ith

US

,o-

,p-,

m-n

itro

phen

olan

d4-

nit

roca

tech

ol;

wit

hF

e°,n

itro

ben

zen

e,an

ilin

e

com

bin

atio

nof

ult

raso

un

dan

dF

e°h

adsy

ner

gist

icef

fect

onth

ere

duct

ion

ofn

itro

ben

zen

e

Hu

ng

and

Hof

fman

n,

1998

carb

onte

trac

hlo

ride

(CC

l 4)

0.1

mM

ult

raso

un

d(U

S)/

Fe°

.US

,20

kHz

(62

W/2

85L

);F

e°,

0-24

.49

g/L

(pow

der)

0-42

g/L

(tu

rnin

gs)

tem

p,15

°C;

irra

diat

ion

gas,

Ar;

init

ial

pH7

inte

rmed

iate

s:U

S/F

e°,

C2C

l 4an

dC

2Cl 6

;Fe°

(on

ly),

CH

Cl 3

,an

dC

H2C

l 2

com

bin

edU

S/F

e°sy

stem

had

apo

siti

vesy

ner

gist

icef

fect

onC

Cl 4

deh

alog

enat

ion

Inaz

uet

al.,

1993

tric

hlo

roet

hyl

ene

(TC

E),

tetr

ach

loro

eth

ylen

e(P

CE

),1,

1,1-

tric

hlo

roet

han

e(T

CA

),ch

loro

form

(CH

Cl 3

),ca

rbon

tetr

ach

lori

de(C

Cl 4

)

10pp

mu

ltra

sou

nd

gen

erat

or/b

ariu

mti

tan

ate

osci

llat

or(2

00kH

z,6

W/c

m2 )

irra

diat

ion

gas,

Ar,

O2,

orai

r

inai

ror

O2,

Cl-

,H2,

CO

2,n

egli

gibl

eC

O;i

nar

gon

,Cl-

,H2,

CO

,CO

2

Ove

r75

%in

itia

lam

oun

tde

com

pose

din

10m

in.

Ord

erof

degr

adat

ion

rate

s:in

argo

n,T

CE

>T

CA

>P

CE

;in

air,

CC

l 4>

CH

Cl 3

Inga

leet

al.,

1995

refr

acto

ryco

mpo

nen

tin

the

indu

stri

alw

aste

ofa

cycl

ohex

ane

oxid

atio

nu

nit

CO

D,1

000

mg

dm-

3se

quen

tial

son

icat

ion

/wet

oxid

atio

n(S

ON

IWO

);u

ltra

son

iccl

ean

ing

bath

(40

kHz,

150/

300W

)

son

icat

ion

at30

and

50°C

wit

hC

uS

O4

(6.2

10-

4

cata

lyst

for

1h

;WO

,250

°C,

0.69

MP

a

form

atio

nof

acet

icac

idas

bypr

odu

cth

ybri

dsy

stem

mor

eef

fect

ive

than

son

icat

ion

-66

%in

CO

Dre

duct

ion

(147

3to

499

mg

dm-

3 )vs

36%

(153

3to

980)

for

Cu

2+

syst

em

Joh

nst

onan

dH

ocki

ng,

1993

pen

tach

loro

phen

ol(P

CP

),3-

chlo

robi

phen

yl(3

-CB

),4-

chlo

roph

enol

(4-C

P),

2,4-

dich

loro

phen

ol(D

CP

)

PC

P,2

.4×

10-

4M

;3-C

B,

10-

4M

;4-

CP

,7×

10-

3

M;D

CP

,2×

10-

3M

sim

ult

aneo

us

UV

(Hg

bulb

-100

W,

7000

W/c

m2 /

ult

raso

un

d(2

0kH

z,47

5W

)/ph

otoc

atal

ytic

(TiO

2)tr

eatm

ent

tem

p,35

(2

°C;T

iO2:

surf

ace

area

,55

(10

m2 /

g;am

oun

t,0.

2%W

/Wca

taly

st/

solu

tion

PC

P:

chlo

ride

Son

icat

ion

ofU

V-i

rrad

iate

dca

taly

stso

luti

onsi

gnif

ican

tly

impr

oved

rate

s.

Kan

gan

dH

offm

ann

,19

98

met

hyl

tert

-bu

tyle

ther

(MT

BE

)0.

01-

1.0

mM

sim

ult

aneo

us

son

olys

is/

ozon

atio

n,

ult

raso

un

d(2

05kH

z,20

0W

L-

1 ),

[O3]

o)

0.26

-0.

34µM

tem

p,20

°C;

solu

tion

pH6.

6-6.

8;ir

radi

atio

nga

s,O

2/O

3;ir

rad.

tim

e,0-

60m

in

tert

-bu

tylf

orm

ate

(8%

),te

rt-b

uty

lalc

ohol

(5%

),m

eth

ylac

etat

e(3

%),

acet

one

(12%

)

the

pres

ence

ofO

3ac

cele

rate

dM

TB

Ede

grad

atio

nra

tes

subs

tan

tial

ly,e

nh

ance

men

tby

1.5-

3.9

depe

ndi

ng

on[M

TB

E] o

Ind. Eng. Chem. Res., Vol. 40, No. 22, 2001 4691

Tab

le3.

(Con

tin

ued

)

auth

ors

con

tam

inan

tsde

grad

edco

nce

ntr

atio

n

chem

ical

oxid

atio

nsc

hem

eex

peri

men

tal

con

diti

ons

degr

adat

ion

inte

rmed

iate

s/pr

odu

cts

degr

adat

ion

effi

cien

cy/o

ther

resu

lts

orre

mar

ks

Kh

enok

han

dL

apin

skay

a,19

56

ben

zen

e(B

z),t

olu

ene

(TL

),ph

enol

(Ph

OH

)(s

atu

rate

daq

ueo

us

solu

tion

)

Bx,

2.4,

5.0

&10

.2×

10-

4M

;P

hO

H,0

.01,

0.08

&0.

32M

ult

raso

un

d,43

5kc

tem

p,40

°CB

z&

TL

,HC

HO

,ph

enol

ich

ydro

xyls

HC

HO

yiel

dsin

crea

sed

wit

hin

itia

lcon

cen

trat

ion

ofB

zor

TL

and

tim

e

Koi

ke,1

992

alco

hol

-w

ater

mix

ture

s,C

H3O

H,C

2H5O

H,

n-C

3H7O

H,i

-C

3H7O

H

10-

80vo

l%so

nic

atio

nba

th(S

B),

50kH

z,12

0W

argo

nbu

bble

dfo

r15

min

befo

reso

nic

atio

n

typi

calp

rodu

cts,

CH

4,C

2H6,

C3H

6,C

2H4,

C2H

2

orde

rof

yiel

dfo

rC

H4

was

C2H

5OH

>C

H3O

H>

i-C

3H7O

H∼

n-C

3H7O

H

Kos

zalk

aet

al.,

1992

syn

thet

icca

rbon

tetr

ach

lori

deC

Cl 4

),co

nta

min

ated

wat

er

13.6

-15

.8pp

mu

ltra

son

icpr

obe

(475

W)

(son

icat

ion

at25

0W

),u

nkn

own

chem

ical

agen

t

tem

p,25

-35

°C;p

ress

ure

,15

-45

psig

;ir

radi

atio

n,a

ir,A

r,H

2;ir

rad.

tim

e,0-

5m

in

inte

rmed

iate

s,ch

loro

form

,di

chlo

rom

eth

ane,

chlo

rom

eth

ane;

fin

alpr

odu

cts,

met

han

e,ch

lori

ne/

chlo

ride

CC

l 4re

duce

dfr

om13

.6to

1.71

ppm

(g90

%de

stru

ctio

n)

byso

nol

ysis

,15

.8pp

mto

<0.

5pp

bw

ith

son

olys

ispl

us

chem

ical

agen

t.K

otro

nar

ouet

al.,

1992

para

thio

n(O

,O-d

ieth

ylO

-p-n

itro

phen

ylth

ioph

osph

ate)

satu

rate

daq

ueo

us

para

thio

nso

luti

on(8

2µM

)

ult

raso

un

d(2

0kH

z,75

Wcm

-2 )

tem

p,30

°C;

solu

tion

pH6.

0;fi

nal

pHaf

ter

2h

son

icat

ion

,3.7

p-n

itro

phen

ol(p

-Np)

,S

O42-

,PO

42-,o

xala

te(C

2O42-

),N

O2-

,NO

3-

init

ialp

arat

hio

nw

asde

grad

ede

2h

sin

ce[S

O42-

] ow

asor

igin

ally

equ

al82

µM

Kot

ron

arou

etal

.,19

91p-

nit

roph

enol

(p-N

p)in

oxyg

enat

edaq

ueo

us

solu

tion

s

100

µMu

ltra

sou

nd

(20

kHz,

84W

)te

mp,

30°C

solu

tion

pH2.

12;

irra

diat

ion

gas,

air

NO

2-,N

O3-

,p-

ben

zoqu

inon

e(p

-BQ

),h

ydro

quin

one,

4-n

itro

cate

chol

,fo

rmat

e(H

CO

2-),

oxal

ate

firs

t-or

der

rate

con

stan

tsde

crea

sed

from

3.67

×10

-4 s

-1

(pH

o5)

to2.

10-

4

s-1

(pH

o8)

.

Kot

ron

arou

etal

.,19

92h

ydro

gen

sulf

ide

(H2S

)(S

[-II

])

[H2S

]+

[HS

-]

+[S

2-])

92,1

00an

d20

µMpr

obe

ult

raso

un

d(2

0kH

z,∼7

5W

/cm

2or

∼85W

)

tem

p,25

°Cso

luti

onpH

10.6

-7.

4;ir

radi

atio

nga

s,ai

r

sulf

ate

(SO

42-),

sulf

ite

(SO

32-),

thio

sulf

ate

(S2O

32-)

inth

em

ole

rati

o2.

2:2.

7:1

resp

ecti

vely

S(-

II)

com

plet

ely

oxid

ized

inle

ssth

an30

min

Kru

ger

etal

.,19

99n

atu

ralg

rou

ndw

ater

con

tain

ing

mai

nly

1,2-

dich

loro

eth

ane

(1,2

-DC

A)

350

µg/L

ult

raso

un

d[3

61kH

z(6

0W

),62

0kH

z(7

5W

),an

d10

86kH

z(1

05W

)

tem

p,22

-31

°C;s

olu

tion

pH6.

2-7;

irra

diat

ion

gas,

air

chlo

ride

com

plet

ede

stru

ctio

nw

ith

in60

min

Ku

etal

.,19

972-

chlo

roph

enol

(2-C

P)

inaq

ueo

us

solu

tion

1.26

×10

-4

Mpr

obe

ult

raso

un

d(2

0kH

z,0-

550

W);

inte

nsi

ty,

38.1

W/c

m2

tem

p,17

-60

°C;p

H3,

5,7,

9,an

d10

;ir

rad.

gas,

air,

O2,

N2

chlo

roh

ydro

quin

one,

cate

chol

,ch

lori

deat

pH11

,bu

tgl

yoxi

lic

acid

also

dete

cted

atpH

3

appa

ren

tps

eudo

firs

t-or

der

rate

con

stan

tra

nge

dfr

om3.

3to

1.5

×10

-3

inth

epH

ran

ge3-

11at

24(

°C

Lin

etal

.,19

962-

chlo

roph

enol

(2-C

P)

10an

d10

0m

g/L

ult

raso

un

d(2

0kH

z,16

0W

)/H

2O2

(200

mg/

L)

proc

ess

tem

p,25

°C;

pH3,

7,11

;ca

taly

st,

FeS

O4

not

expl

icit

lygi

ven

;to

talo

rgan

icca

rbon

(TO

C)

mon

itor

ed

2-C

Pde

com

posi

tion

was

99%

,62%

,an

d15

%at

pH3,

7,an

d11

,res

pect

ivel

y,at

350

min

,an

dw

asen

han

ced

byF

eSO

4as

cata

lyst

.L

inet

al.,

1996

2-ch

loro

phen

ol(2

-CP

)10

0m

g/L

ult

raso

un

d(2

0kH

z,0,

125,

and

160

W)/

H2O

2(0

,10

0,20

0,an

d50

0m

g/L

)pr

oces

s

tem

p,25

°C;

solu

tion

pH3,

5,7,

9,11

not

expl

icit

lygi

ven

;to

talp

rgan

icca

rbon

(TO

C)

mon

itor

ed

H2O

2im

prov

ed2-

CP

deco

mpo

siti

on,5

7%ov

erth

eco

ntr

olw

ith

500

mg/

LH

2O2

Lu

r′e,

1962

phen

ol(P

hO

H),

ben

zen

eP

hO

H,

25-

300

mg/

L;

Bz,

200-

500

mg/

L

ult

raso

un

d,80

0kc

/s,1

500

W;

Inte

nsi

ty,4

-7

W/c

m2

(350

mL

solu

tion

)

solu

tion

tem

p,40

-60

°C;

trea

tmen

tti

me,

40m

into

5h

.

Ph

OH

:ca

tech

ol,

pyro

gall

ol,o

-qu

inon

e;B

z;ph

enol

,pyr

ogal

lol,

cate

chol

,for

mal

deh

yde

Pro

lon

ged

trea

tmen

tre

sult

edin

rapi

dox

idat

ion

ofca

tech

olto

mu

con

icac

id.

Mea

det

al.,

1975

thym

ine

(aer

ated

aqu

eou

sso

luti

ons)

10-

3 -2

×10

-2

Mu

ltra

sou

nd

(447

.5(

0.6

kHz,

5W

cm-

2 )

solu

tion

tem

p,25

°Cci

s-an

dtr

ans-

5,6-

dih

ydro

xy-5

,6-

dih

ydro

thym

ine,

5-h

ydro

xym

eth

ylu

raci

lan

du

rea

Ava

lue

of1.

8(

0.3

×10

-5

Mm

in-

1w

asob

tain

edfo

rth

eze

ro-

orde

rra

teco

nst

ant.

4692 Ind. Eng. Chem. Res., Vol. 40, No. 22, 2001

Tab

le3.

(Con

tin

ued

)

auth

ors

con

tam

inan

tsde

grad

edco

nce

ntr

atio

n

chem

ical

oxid

atio

nsc

hem

eex

peri

men

tal

con

diti

ons

degr

adat

ion

inte

rmed

iate

s/pr

odu

cts

degr

adat

ion

effi

cien

cy/o

ther

resu

lts

orre

mar

ks

Nag

ata

etal

.,19

96m

onoh

ydro

xybe

nzo

icac

id(H

BA

);3,

4-di

hyd

roxy

ben

zoic

acid

(3,4

-DH

BA

);ga

llic

or3,

4,5-

trih

ydro

xybe

nzo

icac

id(G

A);

tan

nic

acid

(TA

);h

um

icac

id(H

A)

100

µM/L

ult

raso

un

d,20

0kH

z,20

0W

tem

p,25

°C;

irra

diat

ing

gas,

air

&A

r

only

CH

Cl 3

mea

sure

dR

ates

ofth

eH

BA

sw

ere

fast

erin

Ar

than

inai

rbu

tra

tes

ofT

Aan

dH

Aw

ere

fast

erin

air.

Nag

ata

etal

.,20

002-

,3-,

&4-

chlo

roph

enol

(CP

OH

),pe

nta

chlo

roph

enol

(PC

P)

100

µM/L

ult

raso

un

d,20

0kH

z,20

0W

irra

diat

ing

gas,

air

&A

r,pr

esen

ceof

Fe(

II)

chlo

ride

Deg

rada

tion

ofC

PO

Hs

and

PC

Pw

ere

alm

ost

100%

un

der

Ar

and

80-

90%

un

der

air

afte

r1

h.

Ols

onan

dB

arbi

er,

1994

fulv

icac

id(F

A)

and

nat

ura

lly

colo

red

grou

ndw

ater

(NC

G)

FA

,10

mg/

LT

OC

;NC

G,

con

tain

s2.

5-3.

0m

g/L

(dis

solv

edor

gan

icca

rbon

)

son

olys

is/

ozon

olys

is(s

onoz

one

proc

ess)

;u

ltra

sou

nd,

55W

,20

kHz

tem

p,25

°C;

grou

ndw

ater

pH8.

6;ir

radi

atin

gga

s,2.

1%O

3in

O2

(3.2

mg/

min

)

CO

291

%T

OC

rem

oved

asC

O2

(fro

mF

A)

afte

r60

min

.S

onoz

one

ism

ore

effe

ctiv

eth

anoz

one

oru

ltra

sou

nd

alon

e

Oko

uch

iet

al.,

1992

phen

ol(P

hO

H)

100

ppm

(mg/

dm3 )

ult

raso

nic

gen

erat

or(2

00W

;19

.5,5

0,20

0,an

d60

0kH

z)

tem

p,25

°C;

cata

lyst

,Fe2

+,

Mn

O2

irra

diat

ing

gas,

Air

,O2,

N2,

He

cate

chol

,hyd

roqu

inon

ede

grad

atio

nra

tes

incr

ease

din

the

orde

rO

2>

air

>H

e,N

2an

den

han

ced

byca

taly

stO

rzec

how

ska

etal

.,19

95ca

rbon

tetr

ach

lori

de(C

Cl 4

),ch

loro

form

(CH

Cl 3

),tr

ich

loro

eth

ylen

e(T

CE

),ch

loro

ben

zen

e(C

B),

poly

chlo

robi

phen

ols

(PC

Bs)

Tri

ton

X-1

00(T

X)

CC

l 4,4

0pp

m;

CH

Cl 3

,37

ppm

;TC

E,3

7pp

m;C

B,9

4pp

m;P

CB

,55

ppm

;TX

,1%

aq.s

oln

.

ult

raso

un

d(2

0kH

z);c

up

hor

n,

100

W;h

orn

prob

e,12

0W

solu

tion

tem

p,27

-40

°C;

deio

niz

edan

dta

pw

ater

(pH

6.3-

8.37

);so

nic

atio

nti

me,

up

to60

min

.

chlo

ride

and

form

ate

ion

s;ch

lori

de:

CC

l 4,2

.80

ppm

;CH

Cl 3

,4.5

5pp

m;

TC

E,2

.80

ppm

;CB

,0.

50pp

m;P

CB

,0.3

0pp

m;T

X,0

.30

ppm

;fo

rmat

e,<

1.00

ppm

for

each

At

20m

in,t

he

pHde

crea

sed

by2.

3u

nit

sfo

rC

Cl 4

solu

tion

s.

Pet

rier

etal

.,19

92pe

nta

chlo

roph

enat

e(P

CP

)10

-4

Mu

ltra

son

icdi

sktr

ansd

uce

r(5

30kH

z,20

W)

tem

p,24

(1

°C;p

H7;

irra

diat

ion

gas,

Ar,

air,

O2

CO

2,(C

Oin

Ar

only

),C

l-,N

O2-

,an

dN

O3-

fast

clea

vage

ofth

eC

-C

lbo

nd,

rele

asin

gC

l-an

dm

iner

aliz

atio

nof

PC

Pto

CO

2in

100

min

ute

s

Pet

rier

etal

.,19

94(a

)ph

enol

(Ph

OH

)0.

05-

10m

Mu

ltra

sou

nd

(30

W):

disk

tran

sdu

cer,

487

kHz

tita

niu

mpr

obe,

20kH

z

tem

p,25

°C;

irra

diat

ion

gas,

air

CO

2as

the

only

gase

ous

prod

uct

,h

ydro

quin

one

(HQ

),ca

tech

ol(C

C)

ben

zoqu

inon

e(B

Q)

rate

isde

pen

den

ton

[Ph

OH

] 0w

ith

max

imu

mva

lue

reac

hin

gli

mit

sof

:11

.6×

10-

6M

min

-1

(for

487

kHz)

and

1.84

×10

-6

Mm

in-

1(f

or20

kHz)

Pet

rier

etal

.,19

96at

razi

ne

(AT

Z),

pen

tach

loro

phen

ol(P

CP

)A

TZ

,0.1

mM

;P

CP

,0.1

mM

ult

raso

un

d:im

mer

sion

prob

e,20

kHz,

18.5

W;

ult

raso

nic

emit

ter,

500

kHz,

18.5

W

tem

p,20

°C;

pH7

(for

PC

P);

diss

olve

dga

s,ai

r;ir

radi

atio

nti

me,

AT

Z12

0m

in,P

CP

180

min

AT

Z:

deal

kyla

tion

prod

uct

sof

atra

zin

e,C

O2,

chlo

ride

;PC

P:

chlo

ride

the

degr

adat

ion

proc

eede

d7.

8ti

mes

(for

AT

Z)

and

4.8

tim

es(f

orP

CP

)m

ore

rapi

dly

at50

0kH

zth

anat

20kH

z

Pet

rier

etal

.,19

94(b

)ch

loro

form

(CH

Cl 3

),di

chlo

rom

eth

ane

(CH

2Cl 2

),ca

rbon

tetr

ach

lori

de(C

Cl 4

),an

ddi

lute

mix

ture

sof

CC

l 4in

met

han

ol(M

eOH

),bu

tan

ol(B

uO

H),

and

1,2-

Eth

aned

iol

[Et(

OH

) 2]

MeO

H:

1%C

Cl 4

;Bu

OH

:0.

5%C

Cl 4

;E

t(O

H) 2

:0.

02an

d0.

05%

CC

l 4

ult

raso

un

d(3

0W),

Vib

race

llem

itte

r,20

kHz;

Un

dati

mIr

radi

atio

nsy

stem

,500

kHz

irra

diat

ion

gas,

O2

and

argo

n

acid

icde

grad

atio

npr

odu

cts

dete

cted

wit

hâ-

carb

olin

e(1

0-4 -

10-

5

M)

espe

cial

lyfo

rso

luti

ons

ofC

Cl 4

inal

coh

ol

chlo

rom

eth

anes

exte

nsi

vely

deco

mpo

sed

MeO

Han

dB

uO

Hre

mai

ned

stab

le,b

ut

Et(

OH

) 2ox

idiz

ed

Ind. Eng. Chem. Res., Vol. 40, No. 22, 2001 4693

Tab

le3.

(Con

tin

ued

)

auth

ors

con

tam

inan

tsde

grad

edco

nce

ntr

atio

n

chem

ical

oxid

atio

nsc

hem

eex

peri

men

tal

con

diti

ons

degr

adat

ion

inte

rmed

iate

s/pr

odu

cts

degr

adat

ion

effi

cien

cy/o

ther

resu

lts

orre

mar

ks

Pet

rier

etal

.,19

98aq

ueo

us

solu

tion

sof

chlo

robe

nze

ne

(CIB

Z),

4-ch

loro

phen

ol(4

-CIP

h),

1,2-

dich

loro

ben

zen

e(1

,2-D

CB

),1,

3-di

chlo

robe

nze

ne

(1,3

-DC

B),

1,4-

dich

loro

ben

zen

e(1

,4-D

CB

),1,

3,5-

tric

hlo

robe

nze

ne,

(1,3

,5-T

CB

),1-

chlo

ron

aph

thal

ene

(1-C

N)

and

mix

ture

ofC

IBZ

and

CIP

h

CIB

Zan

dC

IPH

,0.5

mM

;1,

2-D

CB

,0.4

mM

1,3-

DC

B,

0.05

mM

;1,

4-D

CB

,0.2

mM

;1,

3,5-

TC

B,

0.02

mM

;1-C

N,

0.04

mM

ult

raso

un

d(3

0W

),di

sktr

ansd

uce

r(5

00kH

z),t

itan

ium

prob

e(2

0kH

z)

tem

p,20

°C;

wat

ereq

uil

ibra

ted

air

CIB

Z:

Cl-

,CO

,CO

2,C

2H2;

4-C

IPH

:C

l-,a

nd

hyd

roxl

ated

inte

rmed

iate

s(h

ydro

quin

one,

4-ch

loro

cate

chol

,etc

.)

Ch

loro

arom

atic

hyd

roca

rbon

syi

elde

dg

89%

Cl-

aspr

odu

ctin

150

min

.For

the

mix

ture

,CIB

Zde

grad

esbe

fore

4-C

IPH

(100

vs30

0m

in).

1,2-

DC

B,

1,3-

DC

B,1

,4-D

CB

,1,

3,5-

TC

B,a

nd

1-C

Nm

ore

effi

cien

tly

dest

roye

d.

Pet

rier

and

Fra

nco

ny,

1997

phen

ol(P

h),

carb

onte

trac

hlo

ride

(CC

l 4)

Ph

,10-

3

mol

/L;C

Cl 4

,4-

4.6

×10

-4

mol

/L

ult

raso

un

d(3

0W

),ti

tan

ium

hor

n,2

0kH

;pi

ezo-

elec

tric

disk

,200

,500

and

800

kH

tem

p,20

°C;

solu

tion

pH2;

O2-

satu

rate

dso

luti

ons

Ph

hyd

roqu

inon

e,ca

tech

ol;C

Cl 4

:C

l-,a

nd

CO

2

degr

adat

ion

rate

sfo

rC

Cl 4

incr

ease

wit

hfr

equ

ency

,bu

tm

axim

um

for

Ph

OH

at20

0kH

z

Ph

ull

etal

.,19

97ba

cter

ialc

ells

(E.c

oli)

676

bact

eria

lco

lon

ies

per

cm3

(1/1

0di

luti

on)

ult

raso

un

d(U

S)

and/

orch

lori

nat

ion

.US

,20

kHz

(8W

cm-

2 )&

800

kHz

(15

Wcm

-2 )

;ch

lori

nat

ion

,0.

01-

30pp

m

tem

p,20

°C;

son

icat

ion

tim

e,1,

2,5,

10,o

r20

min

dead

bact

eria

lcel

lsu

ltra

sou

nd

ampl

ifie

dth

ebi

ocid

alef

fect

san

dre

duce

dth

eam

oun

tof

chlo

rin

ere

quir

edfo

rdi

sin

fect

ion

Pop

aan

dIo

nes

u,1

992

chlo

rom

eth

anes

inaq

ueo

us

med

ia(C

H2C

l 2/H

2O,

CH

Cl 3

/H2O

,CC

l 4/H

2O)

1.5

cm3

sam

ples

(ch

loro

-m

eth

ane)

in98

.5cm

3H

2O

ult

raso

un

d,1

meg

acyc

les/

s,58

4W

tem

p,25

°C;

irra

diat

ion

gas,

argo

n;p

H6

C2H

2Cl 4

,C2H

Cl 5

,C

2Cl 6

the

son

olyt

icre

acti

onfa

irly

obey

sze

ro-o

rder

kin

etic

s.T

he

rate

con

stan

tsw

ere

1.73

×10

-7 ,

2.22

×10

-7 ,

and

2.78

×10

-7

Ms-

1fo

rC

Cl 4

,C

HC

l 3,a

nd

CH

2Cl 2

,re

spec

tive

ly.

Pri

ceet

al.,

1994

chlo

robe

nze

ne

(CB

),1,

4-di

chlo

robe

nze

ne,

(1,4

-DC

B),

nap

hth

alen

e(N

T),

anth

race

ne

(AN

),py

ren

e(P

R)

satu

rate

dso

luti

ons

(M):

CB

,4.1

×10

-3 ;

DC

B,

6.2

×10

-5 ;

NT

,2.

36×

10-

4 ;A

N,2

.30

×10

-7 ;

PR

,6.4

×10

-7

hor

nu

ltra

sou

nd

(22

kHz)

,in

ten

siti

es(W

/cm

2 ),1

3.5,

11.7

,20.

9,an

d38

.9

tem

p,20

°C(a

mbi

ent)

;so

luti

on,p

H5.

48-

4.50

(not

con

trol

led

bybu

ffer

)

not

expl

icit

lyre

port

edA

t20

.9W

/cm

2 ,th

era

teco

nst

ants

for

1,4-

DC

B,N

T,

AN

,an

dP

Rar

e0.

038,

0.01

5,0.

033,

and

0.01

6(m

in-

1 ),r

espe

ctiv

ely,

and

0.02

2fo

rC

Bat

23.9

W/c

m2

Raj

anet

al.,

1998

a,b

wat

er-K

I-C

Cl 4

syst

em(K

I-w

ater

solu

tion

satu

rate

dw

ith

CC

l 4)

1%,1

6.6%

,an

d25

%K

Iso

luti

ons

con

tain

ing

5.2

×10

-3

MC

Cl 4

hor

nu

ltra

sou

nd

(25

kHz)

tem

p,34

°C;

irra

diat

ion

gase

s,ai

r,N

2,O

2

I 2,C

l 2,C

l,H

OC

l,H

Cl,

CO

2,an

dO

2

Mod

elde

velo

ped

pred

icte

dw

ellt

he

rate

sob

serv

edfo

rC

Cl 4

susp

ensi

onin

KI

solu

tion

.

Rei

nh

art

etal

.,19

96tr

ich

loro

eth

ylen

e(T

CE

)5-

20pp

mso

nol

ysis

/ze

rova

len

tF

e.U

S:

20kH

z,90

&18

0W

;iro

n(F

e),

1&3

g/L

tem

p,25

°C;

irra

diat

ion

gas,

N2

not

expl

icit

lyre

port

edC

l-in

ferr

edco

mbi

ned

son

olys

is/F

era

tes

was

3ti

mes

that

ofF

eal

one

Sak

aiet

al.,

1977

chlo

ralh

ydra

te(C

H)

0.1

Min

aqu

eou

sso

luti

ons

ult

raso

un

d(2

9an

d40

0kH

z);

pow

erou

tpu

t,0.

5W

/cm

tem

p,30

°C;s

olu

tion

satu

rate

dw

ith

air

and

mix

ture

s(2

0/80

and

2/98

)of

O2

and

N2

chlo

ride

ion

(Cl-

)ki

net

icra

teex

pres

sion

obta

ined

for

the

form

atio

nof

HC

lagr

eed

wit

hex

peri

men

talr

esu

lt

4694 Ind. Eng. Chem. Res., Vol. 40, No. 22, 2001

Tab

le3.

(Con

tin

ued

)

auth

ors

con

tam

inan

tsde

grad

edco

nce

ntr

atio

n

chem

ical

oxid

atio

nsc

hem

eex

peri

men

tal

con

diti

ons

degr

adat

ion

inte

rmed

iate

s/pr

odu

cts

degr

adat

ion

effi

cien

cy/o

ther

resu

lts

orre

mar

ks

Seh

gala

nd

Wan

g,19

81th

ymin

e(T

HY

)0.

1m

Mu

ltra

sou

nd

(1-

7W

cm2 )

tem

p,20

-70

°C;a

erat

ion

med

ium

,air

not

dete

rmin

edA

tan

aera

tion

rate

of50

mL

/min

at34

°C,[

TH

Y]

isre

duce

dto

hal

fin

30m

in.

Ser

pon

eet

al.,

1994

2-,3

-,an

d4-

chlo

roph

enol

s(2

-CP

OH

,3-C

PO

H,a

nd

4-C

PO

H)

4-C

PO

H,7

5.1

µM;3

-CP

OH

,77

.8µM

;2-

CP

OH

,83.

1µM

hor

nu

ltra

sou

nd

(20

kHz,

49.5

W,5

2.1

W/c

m2 )

tem

p,33

(2

°C;a

ireq

uil

ibra

ted;

nat

ura

lsol

uti

onpH

:4-

CP

OH

,5.1

;3-

CP

OH

,5.4

;2-

CP

OH

,5.7

4-C

PO

H,h

ydro

quin

one

(HQ

),4-

chlo

rore

sorc

inol

(4C

R),

4-ch

loro

cate

chol

(4-C

C);

3-C

PO

H,C

l-,

chlo

roh

ydro

quin

one

(CH

Q),

4-3-

CC

,ca

rbon

aceo

us

spec

ies;

C-

CP

OH

,CH

Q,3

-C

C,

cate

chol

(CC

)

tota

ldeg

rada

tion

in10

hfo

r2-

CP

OH

and

3-C

PO

Han

d15

hfo

r4-

CP

OH

wit

hra

tes

[4.8

(0.

4,4.

4(

0.5,

and

3.3

+0.

2]×

10-

3m

in-

1 ,re

spec

tive

ly.

Ser

pon

eet

al.,

1992

phen

ol(P

hO

H)

and

inte

rmed

iate

s,ca

tech

ol(C

C)

hyd

roqu

inon

e(H

Q),

p-be

nzo

quin

one

(BQ

)

Ph

OH

,75

µM(p

H12

),68

µM(p

H3)

and

51µM

(pH

5.7)

;HQ

,44

µM,p

H3;

BQ

,43

µM,

pH3;

CC

,54

µM,p

H3

imm

ersi

onh

orn

ult

raso

un

d20

0kH

z,25

,50,

or75

W/c

m2

30(

2°C

;pH

3,5.

4,5.

7,12

;op

ento

air

Ph

OH

,app

eara

nce

(in

9h)

and

subs

equ

ent

disa

ppea

ran

ceof

CC

,H

Qan

dB

QB

Q,H

Q+

un

iden

tifi

edsp

ecie

sH

Q,B

Q+

un

iden

tifi

edsp

ecie

s

At

pH12

,nei

ther

HQ

,CC

orB

Cw

ere

dete

cted

from

the

inso

nat

ion

ofP

hO

Hsi

nce

they

wer

eu

nst

able

.C

O2

cou

ldn

otbe

dete

cted

.

Sie

rka,

1985

trin

itro

tolu

ene

(TN

T)

and

cycl

otri

met

hyl

ene

-tr

init

ram

ine

(RD

X)

70/3

0m

g/L

TN

T/R

DX

;aq

ueo

us

solu

tion

s

ult

raso

un

d(5

-50

Wat

852-

863

kHz,

60.6

-1,

007

kHz)

/ozo

ne

(72.

91m

gO

3/m

in)

tem

p,25

-59

°C;p

H5.

84-

10.0

not

expl

icit

lyde

term

ined

ult

raso

un

din

hib

ited

kin

etic

sat

hig

hte

mp

and

pHdu

eto

radi

cal-

radi

cal

exti

ngu

ish

men

tre

acti

on

Sie

rka

and

Am

y,19

85h

um

icac

id(H

A)

solu

tion

un

know

nco

nce

ntr

atio

nu

ltra

viol

et/

ult

raso

un

d/O

3;U

S,4

0kH

z,30

0W

;UV

lam

p,25

3.7

nm

;O3,

4.3

mg/

L(2

min

),21

.6m

g/L

(10

min

)an

d43

.2m

g/L

(20

min

)

irra

diat

ing

gas,

O3/

O2;

pHo

4.0,

7.1,

and

10.0

trih

alom

eth

anes

form

atio

npo

ten

tial

(TH

MF

P),

and

non

vola

tile

tota

lor

gan

icca

rbon

(NV

TO

C)

mon

itor

edas

bypr

odu

cts

O3-

US

-U

Vsy

stem

prov

edto

bem

ost

effe

ctiv

ere

acti

onco

ndi

tion

s,fo

llow

edby

O3-

UV

,O3

alon

e,an

dO

3-U

S,p

rovi

din

g93

%,

86%

,75%

,an

d71

%re

duct

ion

inT

HM

FP

leve

ls,

resp

ecti

vely

,in

20m

in.

Sou

daga

ran

dS

aman

t,19

95

tolu

ene

(T),

nit

roto

luen

e(N

T),

O-c

hlo

roto

luen

e(O

-T

),O

-p-x

ylen

e,m

esit

ylen

e(1

,3,5

-tr

imet

hyl

ben

zen

e(M

TB

),an

dis

opro

pyl-

tert

-bu

tylb

enze

ne

(IP

B,T

BB

)

mix

ture

of20

mm

olof

KM

nO

4;an

d10

mm

olof

aryl

alka

ne

in50

cm3

wat

er

KM

nO

4;u

ltra

son

iccl

ean

er(2

3kH

z,12

0W)

tem

p,30

-35

°CT

,ben

zoic

acid

;O-

Tan

dM

TB

,co

rres

pon

din

gca

rbox

ylic

acid

s

Tst

udi

edin

deta

ilam

ong

the

aryl

alka

nes

.Th

eop

tim

alti

me

for

oxid

atio

nof

Tw

as3

h.K

Mn

O4

acce

lera

tes

oxid

atio

nin

the

pres

ence

ofu

ltra

sou

nd.

Spu

rloc

ket

al.,

and

Rei

fnei

der

1970

,197

1

carb

onte

trac

hlo

ride

(CC

l 4);

di-n

-bu

tyls

ulf

ide

(R2S

)

satu

rate

daq

ueo

us

solu

tion

ofC

Cl 4

ult

raso

un

d,28

0-80

0kH

zat

5-11

W/c

m2 )

tem

p,20

°C;

irra

diat

ion

gase

s,O

2an

dA

r

CC

l 4,C

O,C

O2,

HO

Cl,

and

hex

ach

loro

eth

ane

(C2C

l 6)

(in

AR

only

);M

inor

,R2S

O2,

RS

O3H

,bu

tyri

cac

id,C

O,C

2H4,

C2H

2,an

dC

H4

irra

diat

ion

ofpr

odu

cts

R2

SO

and

R2S

O2

yiel

ded

RS

O3H

aspr

inci

palp

rodu

cton

lyat

800

kHz

Sto

cket

al.,

2000

azo

dye,

nap

hth

albl

ue

blac

k(N

BB

)50

(5

µMso

nol

ysis

/ph

otoc

atal

ysis

;U

S,6

40kH

z,25

0W

;TiO

2(P

.25)

,1g/

L

tem

p,20

(5

°CN

BB

inte

rmed

iate

sm

iner

iliz

edto

inor

gan

icsp

ecie

s

Deg

rada

tion

rate

for

son

olys

isw

asab

out

2ti

mes

fast

erth

anth

atof

phot

ocat

alys

is.

Su

zuki

etal

.,20

00su

rfac

tan

t,po

lyox

yeth

ylen

e-al

kyl

eth

er(S

S-7

0)

100

ppm

in10

00m

Laq

ueo

us

sam

ple

ult

raso

un

d/ph

otoc

atal

ysis

,20

0kH

z/20

0W

,T

iO2/

Hg

lam

p(2

53.7

nm

/20W

)

tem

p,25

°C;

irra

diat

ion

gas,

air;

irra

d.ti

me,

60m

in

not

expl

icit

lyde

term

ined

TO

Cm

onit

ored

sign

ific

ant

enh

ance

men

tin

the

phot

ocat

alyt

icre

acti

onob

serv

edw

hen

com

bin

edw

ith

US

irra

diat

ion

Ind. Eng. Chem. Res., Vol. 40, No. 22, 2001 4695

Tab

le3.

(Con

tin

ued

)

auth

ors

con

tam

inan

tsde

grad

edco

nce

ntr

atio

n

chem

ical

oxid

atio

nsc

hem

eex

peri

men

tal

con

diti

ons

degr

adat

ion

inte

rmed

iate

s/pr

odu

cts

degr

adat

ion

effi

cien

cy/o

ther

resu

lts

orre

mar

ks

Tak

izaw

aet

al.,

1996

phen

ol(P

h),

2-n

aph

thol

(2-N

ph),

4-m

eth

ylph

enol

(4-m

Ph

),ca

tech

ol(C

C),

reso

rcin

ol(R

S),

3-te

rt-b

uty

l-4-

hyd

roxy

anis

ole

(3-t

b-4-

HA

N),

3-m

eth

yl-4

-hyd

roxy

anis

ole

(3-m

-4-H

AN

)

8.0

×10

-3

Min

wat

eran

dw

ater

-et

han

olm

ixtu

re(1

:1V

/V,1

00m

L)

ult

raso

un

d(2

00kH

z)te

mp,

25°C

;ir

radi

atio

nti

me,

12-

18h

;ir

radi

atio

nga

s,O

2

Ph

,CC

,hyd

roqu

inon

e(H

Q);

4-m

pH4-

met

hyl

cate

chol

;4-

HA

N,h

ydro

quin

one;

2-N

pH2,

3-di

hyd

ron

aph

thol

;C

Can

dR

S,p

yrog

allo

l;3-

tb-4

-HA

N,

tert

-bu

tyl-

HQ

;3-

m-4

-HA

N,m

etyh

lHQ

Hyd

roxy

late

dpr

odu

cts

yiel

dsra

nge

dfr

om15

%to

Ph

and

4-H

AN

hav

eth

eh

igh

est

yiel

dsof

prod

uct

s,P

h30

%C

Can

d26

%H

Qin

12h

;4-

HA

N,5

0%H

Qin

12h

.

Tau

ber

etal

.,20

004-

nit

roph

enol

10-

3

mol

/dm

3u

ltra

sou

nd,

321

kHz,

170

W/k

gir

radi

atio

nga

s,A

r;pH

4&

10

pH10

,4-n

itro

cate

chol

,h

ydro

quin

one

+be

nzo

quin

one,

nit

rite

;pH

4,pr

odu

cts

atpH

10+

phen

ol,n

itra

te,C

O,

CO

2,H

2

ther

mol

ysis

prod

uct

sob

serv

edat

low

pHco

mpa

red

wit

hO

H-i

ndu

ced

reac

tion

sat

hig

hpH

.

Th

eron

etal

.,19

99ph

enyl

trif

luor

omet

hyl

keto

ne

(PT

MK

)aq

.sol

uti

on16

0µm

ol/L

TiO

2ph

otoc

atal

ysis

and/

oru

ltra

sou

nd

(US

);T

iO2,

3.5

g/L

;US

,30

&51

5kH

z,16

W

tem

p,29

3K

;pH

6-6.

5(n

atu

ral

wat

er)

CF

3CO

OH

and

hyd

roxl

ated

PT

MK

the

amou

nt

ofC

F3C

OO

Hw

as8

tim

eslo

wer

inso

nic

ated

solu

tion

sth

anin

UV

-irr

adia

ted

TiO

2su

spen

sion

atbo

thfr

equ

enci

es

Th

oma

etal

.,19

98be

nze

ne

(Bz)

,tol

uen

e(T

)4,

40,a

nd

80m

g/L

;Bz,

51-

1030

µM;

T,4

3.5-

870

µM

nea

r-fi

eld

acou

stic

proc

esso

r(N

AP

),20

0-80

0W

,16

-20

kHz,

1.3

W/m

L-

1

air

orO

2sa

tura

ted

solu

tion

s

not

repo

rted

rate

con

stan

tsfo

r4

to80

mg/

Lso

luti

ons;

Bz,

0.01

-0.

003

min

-1 ;

T,0

.028

-0.

004

min

-1

Toy

etal

.,19

901,

1,1-

tric

hlo

roet

han

e(C

Cl 3

CH

3,or

TC

A)

3.6

and

2500

ppm

cup-

hor

nu

ltra

sou

nd

(20

kHz)

/Hg/

Xe

lam

p(2

00W

)[p

hot

olys

isan

d/or

son

olys

is]

tem

p,am

bien

t;pH

3ch

lori

de(C

l-)

deco

mpo

siti

onm

ore

exte

nsi

vew

ith

com

bin

edph

otol

ysis

and

son

olys

is(p

hot

oson

olys

is)

than

each

only

Toy

etal

.,19

921,

1,1-

tric

hlo

roet

han

e(C

Cl 3

CH

3or

TC

A)

1.06

and

10pp

mim

mer

sion

hor

nu

ltra

sou

nd

(475

W,2

0kH

z)

tem

p,am

bien

t;op

ento

atm

osph

ere

chlo

ride

(Cl-

)di

sapp

eara

nce

ofT

CA

was

91.4

in18

min

.

Tra

bels

iet

al.,

1996

phen

ol89

-10

0m

g/L

son

olys

is,S

S(2

0an

d50

0kH

z,20

W)/

elec

trol

ysis

,ES

(cu

rren

tde

nsi

ty)

68A

/m2 )

[son

oele

ctro

-ox

idat

ion

(SE

O)]

tem

p,27

(2

°C;s

olu

tion

satu

rate

dw

ith

air

for

20m

in

mal

eic

acid

(MA

),ox

alic

acid

(OA

),m

uco

nic

acid

(MC

A),

p-be

nzo

quin

one

(BQ

),h

ydro

quin

one

(HQ

),ca

tech

ol(C

C),

CO

2

At

20kH

z,5%

con

vers

ion

wit

hso

nol

ysis

alon

eco

mpa

red

wit

h75

5fo

rS

EO

in10

min

.SE

O’s

con

vers

ion

is95

%at

500

kHz

in10

min

and

100%

in60

min

.H

Q,C

C,a

nd

BQ

disa

ppea

raf

ter

2h

at54

0kH

zV

inod

gopa

let

al.,

1998

azo

dye,

rem

azol

blac

kB

(RB

)33

µMu

ltra

sou

nd

(640

kHz,

240

W)

tem

p,am

bien

t;u

nde

rco

nst

ant

bubb

lin

gof

O2

oxal

ate

(C2O

42-)

RB

disa

ppea

red

in90

min

wit

hra

teco

nst

ant

of2.

10-

2m

in-

1an

d60

%m

iner

aliz

atio

nac

hie

ved

in6

h.

Wea

vers

and

Hof

fman

n,

1998

ozon

ein

aqu

eou

sso

luti

ons

85(

5to

245

(3

µMO

3sa

tura

ted

solu

tion

s

ult

raso

un

ddi

rect

prob

e,20

kHz;

263

WL

-1

ult

raso

nic

tran

sdu

cer,

500

kHz,

96W

L-

1

tem

p,23

(3

°C;i

rrad

iati

ng

gas,

O2/

O3

mix

ture

;pH

2

not

expl

icit

lyde

term

ined

firs

t-or

der

degr

adat

ion

rate

con

stan

tsar

e0.

84an

d0.

66m

in-

1 ,re

spec

tive

ly,a

t20

kHz

and

500

kHz

at[O

3]o

)24

5µM

4696 Ind. Eng. Chem. Res., Vol. 40, No. 22, 2001

solution in the former case. Okouchi et al.63 observedthe degradation of phenol in less than 100 min toproceed with pseudo first-order rate and the additionof Fe2+ and MnO2 to increase the rates in aqueoussolutions. Serpone et al.64 noticed the disappearance ofphenol at the initial concentration range of ∼30 to 70µM to follow a zero-order kinetics with k ) 0.08 µM/min at [phenol]initial ) 51 µM and pH 5.7 and slower atan alkaline pH of 12. They also observed three principalintermediate species formed at pH 3 (catechol, hydro-quinone (HQ), p-benzoquinone (BG)), only catechol (CC)and HQ at natural pH 5.4-5.7, and no intermediatesdetected at pH 12. The mechanism is given as

For a constant phenol concentration, the rate of loss ofphenol as a function of sonocation time was foundlinearly related to the sonocation power, P, accordingto

At low concentrations of phenol, k2 [•OH] > k4[phenol],and at low constant P, the rate follows first-orderkinetics; at high concentration, where k2 [•OH] ,k4[phenol], the rate follows zero-order kinetics at con-stant P. However, contrary to the zero-order kineticbehavior observed at 25 and 50 W/cm2, the sono-oxidation of phenol was found to be only first-order at75 W/cm2. Over a pH range of 3-9, Lur’e et al.65 foundthe decomposition of phenol to be practically indepen-dent of pH. Chen et al.66 also found that at highconcentrations ([PhOH] > 300 ppm) the conversion waszero-order and become first-order at very low concentra-tion (<100 ppm). The rate was also found to be negli-gible at low frequency and the oxidation proceededtoward completion at high frequency. Trabelsi et al.67

investigated the oxidation of phenol in a screenedreactor with ultrasound alone at 20 kHz and withultrasound associated with electrolysis. They found thatthe electrochemical oxidation of phenol in NaCl mediacombined with sonication at 20 kHz resulted in 75%conversion of the initial phenol within 10 min and ledto the formation of toxic p-quinone. At a higher fre-quency of 500 kHz, a conversion of 95% was obtainedT

able

3.(C

onti

nu

ed)

auth

ors

con

tam

inan

tsde

grad

edco

nce

ntr

atio

n

chem

ical

oxid

atio

nsc

hem

eex

peri

men

tal

con

diti

ons

degr

adat

ion

inte

rmed

iate

s/pr

odu

cts

degr

adat

ion

effi

cien

cy/o

ther

resu

lts

orre

mar

ks

Wh

eat

and

Tu

meo

,199

7po

lycy

clic

arom

atic

hyd

roca

rbon

s(P

AH

S),

phen

anth

ren

e(P

A),

biph

enyl

(BP

)

PA

orB

P,0

.39

mg/

310

mL

wat

er

ult

raso

un

d(1

47W

/cm

2 )te

mp,

21-

27°C

;air

flow

reac

tor,

100

mL

/min

(ope

nto

atm

osph

ere)

PA

,ph

enan

thre

ne

diol

;B

P,o

rth

o,m

eta,

and

para

-1,1

biph

enol

s

the

toxi

city

ofre

acti

onpr

odu

cts

rem

ain

sto

bede

term

ined

.

Wu

etal

.,19

92ca

rbon

tetr

ach

lori

de(C

Cl 4

)0.

53,1

.6,8

,an

d13

0pm

prob

eu

ltra

sou

nd

(20

kHz,

27W

/cm

2 )te

mp,

20-

60°C

;pH

3-9;

pow

erin

ten

sity

,1-

22W

/cm

2 ;ir

radi

atin

gga

s,ai

r

not

expl

icit

lyre

port

edgr

eate

rth

an99

%de

stru

ctio

nef

fici

enci

esin

6m

inw

ith

anav

erag

efi

rst-

orde

rra

teco

nst

ant

of0.

7m

in-

1at

25°C

Zh

ang

and

Hu

a,20

00po

lych

lori

nat

edbi

phen

yls

(PC

Bs)

,2-c

hlo

robi

phen

yl(2

-PC

B),

4-ch

loro

biph

enyl

(4-P

CB

),2,

4,5-

chlo

robi

phen

yl(2

,4,5

-PC

B)

2-P

CB

,4.6

µM;4

-PC

B,

5.4

µM;

2,4,

5-P

CB

,7.6

×10

-2

µM

prob

eu

ltra

sou

nd

(PU

S),

20kH

zfo

ral

lPC

Bs;

also

at20

5,35

8,61

8,an

d10

71kH

zfo

r2-

PC

Bon

ly

tem

p,15

°C;

pow

erin

ten

sity

,30

.8W

/cm

2 ;ir

radi

atin

gga

s,A

r

biph

enyl

,eth

ylbe

nze

ne,

diet

hyl

biph

enyl

,di

buty

lbip

hen

yl,

phen

ol,p

ropy

lph

enol

,di

-ter

t-bu

tylp

hen

ol,

chlo

ride

pseu

do-f

irst

-ord

erra

teco

nst

ants

at20

kHz/

30.8

Wcm

-2

(s-

1 )ar

e:2-

PC

B,2

.1×

10-

3(

2.8

×10

-5 ;

4-P

CB

,1.

10-

3(

3.4

×10

-5 ;

2,4,

5-P

CB

,2.6

×10

-3

(9.

10-

5

H2O + ))) 798k1

k-1

•OH + H• (5)

•OH 98k2 1/2H2O2 (6)

•H 98k3 1/2H2 (7)

•OH + phenol 98k4

products (8)

Rate )k1k4[phenol]

k2[•OH] + k4[phenol]

(10)

Ind. Eng. Chem. Res., Vol. 40, No. 22, 2001 4697

within the same treatment time with acetic and chlo-rocrylic acids as final products of degradation. However,sonoelectrooxidation at high frequency allowed totaldegradation in 20 min with no toxic aromatic intermedi-ates. They also observed that high frequency ultrasoundenhanced mass transfer substantially up to 70-fold themass transfer by diffusion, and without ultrasounddimerization of phenol radicals yielded polymeric specieswhich built on the electrodes and passivated them.

The sono-oxidation intermediates and products of 2-,3-, and 4-chlorophenols (2-,3-,4-CPOH) and 2,4-dichlo-rophenol (2,4-DCP) in air equilibrated media generallyinclude chlorohydroquinone (CHQs), catechols (CC),chlorocatechols, chlororesorcinols (CRSs), and chlorides.In addition, 2,4-dichlorophenol has been found to pro-duce some 2- and 4-chlorophenols as intermediates. Themajor mechanism of oxidation for these chlorophenolsis a radical attack similar to equations for phenol (eqs5-9).64 Serpone et al.68 obtained CHQ as the majorintermediate for both 2-CPOH and 3-CPOH sonolysis,with a small quantity of catechol (CC) in the case of2-CPOH. By contrast, the principal intermediate for4-CPOH was found to be HQ with a small amount of4-CRS. Ku et al.69 in the sono-oxidation of 2-CPOH withoxygen purging at various solution pH levels identifiedCHQ, CC and glycoxilic acid as intermediates at pH 3but only CHQ and CC at pH 11. Lin et al.70 found thatthe combination of ultrasound with H2O2 increased theefficiency of 2-CPOH decomposition significantly. Withthe ultrasound/H2O2 process, they observed that withpH controlled at 3, the rate of 2-CPOH decomposition(i.e., 99%) was enhanced up to 6.6-fold and TOC removal(i.e., 63%) up to 9.8-fold compared with values at pHcontrolled at 11. The variations in decomposition ratesat the different pH values were attributed to the pKavalue of 8.49 for 2-CPOH at 25 °C. The 2-CPOH isalmost completely in the ionic form when the pH exceedsthe pKa value of 8.49 but exists in molecular form whenpH < pKa, the fraction in molecular state increasingwith pH drop. In ionic state, 2-CPOH does not vaporizeinto the cavitation bubbles, and oxidation reactionoccurs with OH radicals outside the bubble film. How-ever, in the molecular state, reactions occur by boththermal cleavage inside the bubble and oxidation withOH radicals outside, leading to more effective decom-position. Lin et al.71 also studied the effect of H2O2concentration on decomposition. It was shown that themore the H2O2 that was added, the greater the degrada-tion efficiency. In a particular study with 500 mg/L ofH2O2 and initial 2-CPOH concentration of 100 mg/L,they observed, after a reaction time of 30 min, animprovement as great as 57% over the control, i.e.,without H2O2 addition. The result was attributed toincrease in OH radicals generated on addition of H2O2.However, the increase in degradation rates was notsignificant between the additions of 200 and 500 mg/LH2O2, suggesting the concentration saturation of OHradicals at the 200 mg/L level. Petrier et al.72 studiedthe sonochemical degradation of 4CPOH and concludedthat the release of end products (i.e., Cl-) and formationof hydroxylated intermediates (HQ, CC) were evidenceof a two-step reaction involving OH radicals withsubstrate in the liquid layer surrounding the cavitationbubble. The dechlorination yields were also found to behigher at 500 kHz (using undatim ultrasonic source)than with the common 20 kHz ultrasonic probe. Thedechlorination rates for 4-chloro-3,5-dimethyl-phenol

were found to be approximately 2 orders of magnitudelower than that of 2,4-chlorophenol (2,4-DCP), and thiswas attributed to the fact that the formation of aryneintermediates is blocked by the ortho methyl groups.73

Nagata et al.74 found the first-order ultrasonic degrada-tion rates of 2-, 3-, and 4-chlorophenol to be faster underargon atmosphere compared to air atmosphere. With 0.1mM initial concentrations, the rates for 2-CPOH,3-CPOH, and 4-CPOH were 6.0, 7.2, and 7.0 µM min-1,respectively, in argon compared to 5.0, 6.6, and 4.5 µMmin-1 in air atmosphere. The rate was even faster for3-CPOH (k ) 20.0 µM min-1) with an initial concentra-tion of 1 mM in argon atmosphere. The faster degrada-tion of 3-CP compared to 2-CP and 4-CP was attributedto the fact that with 3-CP, there are three points ofsimultaneous ortho and para orientation to Cl and OHgroups where, due to the electrophilic character of OH,OH radical addition would easily occur. Johnston andHocking75 investigated the photocatalytic and photolyticdegradation of 2,4-DCP with and without sonication.They found that the use of sonication (1 × 10-3 M, 2,4-DCP, or 0.2% or 0.05% TiO2) in photolysis resulted inthe enhancement of chloride release rate by a factor of4 compared with that of UV irradiation only.

The main sonooxidation products of p-nitrophenol (p-Np) are nitrates (NO2

-), nitrates (NO3-), short-chain

carboxylic acids, formic acid (or formate, HCO2-), acetic

acid (or acetate), and oxalic acid (or oxalate) withintermediates such as 4-nitrocatechol (4-NP), hydro-quinone, and benzoquinone. Kotronarou et al.76 andHoffmann et al.58 found that in the presence of ultra-sound, p-nitrophenol solutions was denitrated to yieldNO2

- and NO3- by two independent mechanisms: (a)

via the gas-phase reaction, which takes place in purewater, and (b) from the decay of p-NP molecules. It wasshown that while NO3

- did not interfere with thesonochemical reactions of p-NP, NO2

- appeared to affectthe decay of p-nitrophenol and the formation of 4-ni-trocatechol (4-NP). Ultrasonic irradiation of a solutioncontaining 100 µM p-NP and 100 µM NaNO2 was foundto result in a slower disappearance of p-NP (k1 ) 2.0 ×10-4 s-1) when compared to a kinetic run in the absenceof NO2

- (k1 ) 3.67 × 10-4 s-1). On the basis of theproducts and kinetic observations, it was concluded thatthe degradation of p-NP involved high-temperaturereactions of p-NP in the interfacial region of cavitationbubbles and that the main pathway was carbon-nitrogen bond cleavage with hydroxyl radical reactionproviding a secondary reaction channel. Hua et al.77

studied the sonochemical degradation of p-NP usinghigh-power ultrasonic system (parallel-plate near fieldacoustical processor, NAP, with 0-1775W) in the pres-ence of argon (Ar) and oxygen (O2) in order to investigatethe effect of power per area. They found pseudo-first-order constant for p-NP degradation in the presence ofpure O2, (k2 ) 5.19 × 10-4s-1) was lower than that inthe presence of pure Ar, (kAr ) 7.94 × 10-4s-1). Thehighest degradation rate was in the presence of Ar/O2(4:1 v/v) mixtures (kAr/O2 ) 1.20 × 10-3s-1) at the sameintensity of 1.4 W/cm2. Cost et al.78 also studied thesonochemical reactions of p-NP in solutions containingparticulate matter, phosphate (total ions: HPO4

2- +H2PO4

-, and a pH 6.8), bicarbonate (HCO3- ions, and

pH 8), and humic acid and in solutions from lake water(natural water). They also observed first-order rateconstants, kobs, for p-NP of 4.4 × 10-4 in deionized waterand 3.4-3.2 × 10-4 s-1 in water with bicarbonate

4698 Ind. Eng. Chem. Res., Vol. 40, No. 22, 2001

concentration: 10-4 e [HCO3-] e 10-2 M. They found

the degradation rate was unaffected by chemicals ofnatural water. They rationalized the results by indicat-ing that for pollutants such as p-NP which decay viathermal reactions near the interface or inside of cavi-tating bubbles, the high-temperature denitration reac-tions in this case are not significantly affected bycommon chemicals of natural waters. Barbier andPetrier79 investigated the ultrasonic degradation andminerilization of 4-nitrophenol (4-NP) at two ferquencies(20 kHz and 500 kHz) and in water saturated withoxygen or an oxygen-ozone gas mixture. They found thecoupling of ultrasound and O3 increased the potentialof ozonation to mineralize 4-NP degradation products.At low pH (pH 2), where the ozone auto-decompositionradical pathway is suppressed, they observed 4-NPmineralization at 500 kHz was 1.8 times faster than at20 kHz for the same O3 consumption and attributed theenhanced rate to increased O3 utilization occurring atthe higher frequency. Tauber et al.80 found the sonolyticdegradation of 4-nitrophenol (4-NP) in argon-saturatedaqueous solution (321 kHz) was fully due to OH-radical-induced reactions at pH 10, where 4-nitrophenol isdeprotonated (pKa ) 7.1) and nonvolatile 4-nitrophe-nolate predominates. At pH 4 and with the neutral formof 4-nitrophenol, oxidative-pyrolytic degradation pre-dominated, resulting in large yields of CO, CO2, and H2.

Takizawa et al.81 sonicated various phenolic com-pounds in aqueous media (water and water-ethanol) at215 °C for 12-18 h. using 200 kHz ultrasound in thepresence of oxygen and isolated various hydroxylatedphenols as products of ultrasonic oxidation (Table 3).They also identified catechol and hydroquinone as theoxidation products of phenol. They postulated the fol-lowing mechanism for the production of hydroquinonefrom phenol: The phenolic benzene ring was attackedby the hydroxyl radical produced in water sonochemi-cally. The attack took place at the carbon attached tothe methoxy group at the p-position of phenolic hydroxygroup and the methoxy group was eliminated withhydrogen radical to give hydroquinone and methanol.Hua et al.56 observed that ultrasonic irradiation acceler-ated the rate of hydrolysis of p-nitrophenyl acetate (p-NPA) in aqueous solution by 2 orders of magnitude overthe pH range of 3-8 compared to the same hydrolysisunder ambient conditions at 25 °C. The first-order rateconstants were independent of pH and ionic strength.They explained their observations by considering theexistence of transient supercritical water (SCW) aroundthe collapsing cavitation bubbles during sonolysis as animportant factor in the acceleration of chemical reac-tions due to higher concentration of OH- at the hotbubble interface resulting from higher ion product, Kw,of supercritical water.

The main chemical degradation intermediates andproducts from benzene usually include phenol, catechol(CC), hydroquinone (HQ), p- and o-benzoquinone (p- ando- BQ), 1,2,3-trihydroxybenzene, maleic and muconicacid, formalaldehyde, and acetylene.82-85 Chlorobenzenetransforms into 4-chlorophenol, chlorophenol, 4-chloro-catechol, hydroquinone, benzene, butenyne, butadiyne,nonchlorinated mono- and dicyclic hydrocarbons, CH4,and C2H2 upon ultrasonic irradiation in air-saturatedsolutions.84 De Visscher et al.82 investigated the sono-chemical degradation of monocyclic aromatic com-pounds, benzene, ethylbenzene, styrene, and o-chloro-toluene, in aqueous solutions and found the first-order

reactions to be dependent on initial concentrations ofthe substrates and the sonication time. Pyrolysis isexpected to be the main reaction path for the degrada-tion of polar compounds. De Visscher et al.83 analyzedthe reaction products of the sonochemical degradationof ethylbenzene in aqueous solutions and found themto be typical of high-temperature pyrolysis reactions.The reaction rates were also found to be first-order.Unlike ethylbenzene, both pyrolysis and radical attackappear to be important pathways of benzene andchlorobenzene degradations. Drijvers et al.84 observedthat chlorobenzene was mainly degraded thermally andthat the first-order degradation rates for the sonolysiswas not influenced by the pH of the aqueous solutionwhile saturating the solution with argon instead of airaccelerated the degradation. It was also suggested thatchlorophenol (CP), the only oxygen-containing interme-diate detected, was not formed directly by the reactionof OH radicals with chlorobenzene but resulted from theaddition of oxygen to chlorophenyl radicals in theinterface since chlorobenzene could not break down inthe bulk solution itself. Price et al.86 obtained a first-order rate constant of 0.055 min-1 and 0.08 min-1,respectively, for the sonication of chlorobenzene (CB)and 1,4-dichlorobenzene (1,4-DCB) at about 39 Wcm-2

and observed that 1,4-DCB was totally consumed after40-50 min. For a given intensity (i.e., 20.9 W/cm2), thereaction rate of 1,4-DCB was found to be faster com-pared with those of CB, naphthalene (NT), anthracene(AN), and pyrene (PR). Drijvers et al.85 compared thesonolysis at 520 kHz (9.4 or 0.063 Wml-1) and 25 °C offour monohalogenated benzenes, fluorobenzene (FB),chlorobenzene (CB), bromobenzene (BB), and iodoben-zene (IB), at different initial concentrations, 0.5, 1, and2 mM. They found all four to degrade by similarmechanisms and the sonolysis rates to depend on initialconcentrations. Petrier et al.72 also studied the sonochem-ical degradation of chlorobenzene (CB). On the basis ofthe chloride ion evolution, the low level of hydroxylatedintermediates, and the formation of gaseous stableproducts (CO2, CO, C2H2), they suggested a thermaldegradation inside the cavitation bubble as the prefer-ential reaction pathway, with C2H2 formed by ther-molytic ring cleavage. The formation of brown carbon-aceous particles was attributed to soot formation underpyrolytic conditions, phenyl radical combination, orC2H2 reactions at high temperatures. For a mixture ofthe hydrophobic CB and the hydrophilic 4-CPOH at 0.5mM each, CB decayed first, and the 4-CPOH transfor-mation started only when CB reached a low level (0.02mM). The results also indicated that the presence ofhydrophobic compound with high vapor pressure (Hen-ry’s law constant, H, for CB ) 3.77 × 10-3 atm.m3mol-1)hinders efficiently the degradation of hydrophilic com-pound with less vapor pressure (H ) 2.4 × 10-3

atm.m3mol-1) or the less volatile solute, 4-CPOH.Khenokh and Lapinskaya87 observed that the oxidativeprocesses arising from the ultrasonic irradiations ofbenzene and toluene in aqueous solutions resulted inthe destruction of the six-membered ring compounds,with the formation of formaldehyde and other simulta-neous reactions leading to the formation of phenol.Thoma et al.88 studied the sonochemical treatment ofbenzene and toluene in water using a parallel plate nearfield acoustic processor (NAP). They found the magne-tostrictive system to be capable of degrading bothcontaminants in a continuous stirred tank reactor

Ind. Eng. Chem. Res., Vol. 40, No. 22, 2001 4699

configuration with the rate constant inversely propor-tional to the target pollutant concentration. They alsoobserved that the apparent first-order rate constantincreased approximately linearly with the power input(measured from the wall) to the system.

Hung et al.89 found the rate of reduction of nitroben-zene by Feo enhanced in the presence of ultrasound(US). For example, the first-order rate constant for theultrasonic degradation of nitrobenzene in the absenceof Feo was found to be 1.8 × 10-3 min-1 compared to7.8 × 10-3 min-1 in the presence of 70 g/L Feo. Theydescribed the overall rate of nitrobenzene disappearanceby the linear relation:

where kus, kFeo, and k′ are, respectively, the first-orderdegradation rate constants for sonolysis, reduction byFeo, and the synergistic kinetic effect achieved bycombining the two systems. They also obtained thefollowing relation from eq 11:

where ksec, kp ) xoka, xo, and ka are the average second-order rate constant for the reaction between the Feo

surface sites or the reaction intermediates and ni-trobenzene, a zero-order rate constant that increaseswith added [Feo], the initial activated Feo surface beforethe application of ultrasound, and a proportionality (dx/dt ) kax, x ) surface area of Feo at time t), respectively.They attributed the faster degradation rates in thecombined US/Feo system to several causes. These in-clude the indirect chemical effects associated with thecontinuous ultrasonic cleaning and activation of the Feo

surface, the accelerated rates of mass transport result-ing from the turbulent effects of cavitation, and theacidity produced by H+ released from HNO3, a productof sonolysis of nitrobenzene and water. The intermedi-ates such as 4-nitrocatechol and benzoquinone usuallyobserved when Feo is used for reduction were negligiblein the combined US/Feo system. They also found thesonolytic degradation of aniline to be a first-orderreaction with apparent rate constant of 2.4 × 10-3 min-1

at 20 kHz and 139 WL-1 with or without Feo.Soudagar and Samant90 evaluated the ultrasound-

catalyzed oxidation of various aryl alkanes (eg., toluene,nitro- and o-chloro-toluene, p-xylene) to the correspond-ing aryl carboxylic acids using aqueous KMnO4 underheterogeneous conditions and optimized parameterssuch as quantity of KMnO4, stirring rate and reactiontime. It was shown that heterogeneous oxidation ofunsubstituted aryl alkanes was significantly acceleratedusing aqueous KMnO4 at ambient temperatures and inthe presence of ultrasound. While under optimizedconditions o-chlorotoluene and mesitylene (1,3,5-tri-methylbenzene) were effectively converted into thecorresponding carboxylic acids, isopropyl benzene andtert-butyl benzene did not undergo oxidation and wererecovered unreacted. Nagata et al.91 investigated theaqueous sonochemical degradation of hydroxybenzoicacids such as monohydroxbenzoic acids (HBAs), 3,4-dihydroxybenzoic acid (3,4-DHBA), 3,4,5-trihydroxyben-zoic acid (gallic acid, GA), tannic acid (TA), and humic

acids (HA) under air or argon atmosphere. They foundthe pseudo-first-order constants for 2-HBA, 3-HBA, and4-HBA to be 3.0 × 10-2, 4.9 × 10-2 and 5.1 × 10-2 min-1,respectively, under Ar and 2.7 × 10-2, 3.4 × 10-,2 and3.1 × 10-2 min-1 under air. However, the rate constantsof GA and TA were higher under air irradiation (5.5 ×10-2 and 16.4 × 10-2 min-1) compared with irradiationunder Ar (2.6 × 10-2 and 6.4 × 10-2 min-1). The rateconstant for 3,4-DHBA was the same under bothatmospheres (1.9 × 10-2 min-1). The decomposition of3-HBA was almost completely quenched in the presenceof t-BuOH at a concentration of 0.1 mM. They arguedthat the sonolytic degradation of the HBA under Aratmosphere proceeded mainly via reactions with OHradicals in the bulk solution. Whereas under air oxygenmolecules contributed to the decomposition of the poly-hydroxybenzoic acids at the interface, thermal decom-position in cavitation bubbles or interfacial regionsplayed a negligible role in both atmospheres. They alsosuggested that the participation of oxygen moleculesaccounted for the faster decomposition rates of GA andTA in air, the rates in air facilitated with an increasingnumber of OH groups (kTA > kGA) as expected withoxidation of phenolic compounds with oxygen. D-Silvaet al.92 observed the rapid destruction of polycyclicaromatic hydrocarbons (PAHs) and dioxin when solu-tions of benzo[a]pyrene (B[a]P), benzo[ghi]perylene,coronene, or 2-chlorodibenzo-p-dioxin in 20% ethanol-water at approximately 10-15 ppm levels were sub-jected to high-intensity sonication. It was shown thatthe sonolytic decomposition of PAH and dioxin wasaccompanied by the formation of a black carbonaceousresidues. It was also shown that the effect of ultrasoundon a 100% ethanol solution of B[a]P was not as pro-nounced as in water-ethanol mixture.

4.2. Chlorinated Aliphatic Hydrocarbons (CAHs).The sonochemical reactivity of chlorinated hydrocarbonsin aqueous solutions is attributed to their volatility andtheir low solubility in water, properties facilitating theirconcentration in the cavitation bubbles resulting inrapid decomposition by high temperature and highpressure. The sonication of 15 mL of neat chlorinatedsolvents 1,1,1-trichloroethane (TCA) and trichloroeth-ylene (TCE) produced a yellow color (presumably dueto elemental chlorine) in 10 min and in 2 h produced abrown suspension indicating the solvents have polym-erized due the treatment.92 Inazu et al.93 found thataqueous solutions of trichloroethylene (TCE), tetrachlo-roethylene (PCE), 1,1,1-trichloroethane (1,1,1-TCA),chloroform (CHCl3), and carbon tetrachloride (CCl4)decomposed rapidly to chloride anions (Cl-), hydrogen,carbon monoxide, and carbon dioxide by ultrasonicirradiation in the presence of argon, O2, or air. Theysuggested that the main reactions were thermal decom-position or combustion in cavitation bubbles and notreactions by OH radicals or H atom. It was also shownthat the main products of TCE degradation productsunder Ar were Cl-, CO, and H2. The minor products ofthe decomposition under Ar were CO2, CH4, C2H4, anda trace amount of dichloroethylene. Under the sonica-tion of O2 or air, considerable amount of CO2 evolved,and no CO was observed. Drijvers et al.94 identified thefollowing volatile products of TCE sonication at 50kHz: chloroacetylene (C2HCl), dichloroacetylene (C2Cl2),dichlorodiacetylene (C4Cl2), tetrachloroethylene (C2Cl4),two isomers of trichlorobutenyne (C4HCl3), tetrachlo-robutenyne (C4Cl4), pentachlorobutadiene (C4HCl5), and

-d[NB]

dt) kus[NB] + kFeo[NB] + k′[NB] )

(kUS + kFeo + k′)[NB] (11)

-ln[ [NB][NB]o] ) (kus + kFeo)t + 1

2kseckpt

2 (12)

4700 Ind. Eng. Chem. Res., Vol. 40, No. 22, 2001

hexachlorobutadiene (C4Cl6). It was also shown that thedegradation rate of TCE was more energetically efficientat 520 kHz than at 20 kHz. Reinhart et al.95 studiedthe combined effects of sonication and zerovalent ironon the destruction rate of TCE and found ultrasound toincrease the rate significantly. For example, they ob-tained first-order rate constants, k (hr-1), of 0.0147,0.0218, and 0.0426, respectively, for ultrasound alone,iron alone (3 g/L), and the combined system, respec-tively.

The main intermediates of the sonication of theaqueous carbon tetrachloride (CCl4) are tetrachloro-ethylene (C2Cl4) and hexachloroethane (C2Cl6) withtrace amounts of dichlorocarbene, dichlromethane,trichloroethylene, tetrachloroethane, pentachloroethane,hexachloropropene, hexachlorobutadiene, and chloro-form, and the final products are usually chlorine,chlorides (or HCl), chlorohydric acid, hypochlorous acid(HOCl), CO, and CO2.96-100 Jennings et al.97 investi-gated the sonochemical reactions of CCl4-H2O mixturesin an argon atmosphere and compared results withthose of CHCl3-H2O mixtures. They observed cavitationwhen CCl4 was sonicated alone, but there was noreaction. In the presence of as little as 1 mL H2O per100 mL of CCl4, reaction ensued, and the total inorganicchlorine yield was found not to be significantly sensitiveto large changes in the CCl4 to H2O ratios. The observedproducts from the CCl4 reaction included: CO2, O2, Cl2,HCl, C2Cl6, and C2Cl4 compared with products ofCHCl3: HCl, C2Cl6, and C2Cl4. Hua and Hoffman99

studied the sonolytic destruction of aqueous CCl4 in theabsence or presence of ozone (O3). The observed first-order degradation rates in argon-saturated aqueoussolutions were 3.3 × 10-3 and 3.9 × 10-3 s-1 with CCl4initial concentration of 1.95 × 10-4 and 1.95 × 10-5 molL-1, respectively. It was shown that the presence of O3did not affect the degradation rate significantly butinhibited the accumulation of C2Cl4 and C2Cl6 interme-diates. However, sonication of p-nitrophenol in Ar-saturation aqueous solution in the presence of CCl4resulted in the degradation rate enhancement of p-NPby a factor of 4.5 compared to sonication without CCl4and the reduction of 4-nitrocatechol, an aromatic deg-radation product. The improvement in rate and mini-mization of 4-nitrocatechol formation were shown to bedue to the presence of HOCl, a product of CCl4 sonolysis.

Koszalka et al.100 obtained 98% reduction of CCl4 inthe presence of H2, air, or Ar and observed the ultrasonicdestruction to be an exponential process. It was shownthat the initial reaction products: chloroform, dichlo-romethane, and chloromethane were further degradedto methane and chlorine/chloride. Total halogen analy-ses of unreacted and reacted CCl4-contaminated samplesalso confirmed Cl balance, indicating that CCl4 was notvolatilized or masked by the chemistry of the process.Wu et al.7 studied the destruction of CCl4 under dis-solved air and varied process parameters such as pH,irradiation, time, steady-state temperatures, and ultra-sonic intensity. It was shown that CCl4 destruction ratewas significantly affected by the intensity of the ultra-sonic energy, the rate increasing proportionally to theintensity. However, the addition of H2O2 as an oxidantwith or without ultrasonic irradiation was also foundto have negligible effect upon the rate. This was at-tributed to the predominance of the thermal dissociationreaction in the cavitation holes under supercriticalconditions compared to the bulk-liquid-phase reactions

involving CCl4 and oxidants such as OH radicals. Thebulk-liquid rate constants (e.g., 107 M-1 min-1) werefound to be about several times smaller than those inthe cavities (e.g., 1012 M-1 min-1). On the basis of adetailed chemical reaction mechanism and assuming abatch reactor, they described the destruction of CCl4 inwater by the following differential equations usingsecond-order rate constants and concentrations in thebulk-liquid phase and cavity respectively:

where M is any collision partner and kc is the systemadjustment coefficient, which is a function of bubbleconcentration, bubble radius concentration, mixing ex-tent of the system, etc. The results of this modelformulation via a series of elementary reactions werefound to be in general in agreement with experimentaldata. They obtained the value of kc to be constant at2.5 × 10-11 by fitting experimental data to the model,assuming constant vessel size, steady-state tempera-ture, and power. Hung and Hoffmann101 investigatedthe degradation of CCl4 by combined ultrasound (US)and iron (Feo) in Ar-saturated solutions and observed a40-fold enhancement in overall rate for the coupledsystem compared with US alone. The first-order ultra-sonic rate constant for CCl4 was 0.107 min-1 at 62 W(20 kHz) in 285 mL solution, whereas the apparent rateconstant in the presence of Feo was found to depend onthe total surface area of elemental iron as follows:

where kus ) 0.107 min-1, kFeo ) 0.105 L m-2 min-1, andAFeo is the reactive surface area of Feo in units of m2/L.Rajan et al.102,103 investigated experimentally and bymodeling of the water-KI-CCl4 system and attributedthe significant increase in oxidation rates observed ina suspension of CCl4 liquid in KI solution to the releaseof Cl2, Cl, and HOCl, which act as a separate source ofreactants to yield I2. They used a complex mathematicalmodel that included detailed kinetics of CCl4 to predictthe extent of degradation of dissolved CCl4 and the largeenhancements in the rate of oxidation of aqueous iodineion (I-) in the presence of CCl4. A similar study of theCCl4/KI (1.0 M solution) system by Alippi et al.9 foundthe yield of free iodine to increase linearly with soni-cation time.

Petrier et al.104 studied the sonolysis of chloromethaneand their dilute mixtures in alcohols under saturationwith Ar or O2 and found the zero-order rate constantsto be greater in Ar atmosphere. Since the sonochemicalcleavage of the alcohols were found to be weak, theinitial step in the transformation (faster in Ar) wasattributed to the C-Cl cleavage, in constrast to thereaction in water, where sonochemical cleavage of thesolvent plays a major role. They also explained that thesonolysis, probably in the cavitation bubble of CCl4 andwhich was more efficient in alcohols than in the purestate, could result from the preferential vaporization ofthis apolar molecule into a bubble formed in a hydrogen-bonded structured liquid. Toy et al.12,13 investigated the

-d[CCl4]dt

) kI[OH][CCl4] + kII[H][CCl4] +

kIII[HO2][CCl4] + kIV[O][CCl4] (13)

d[CCl4]dt

) kckv[CCl4][M] (14)

kobs ) (kus + kFeoAFeo) min-1 (15)

Ind. Eng. Chem. Res., Vol. 40, No. 22, 2001 4701

decomposition of aqueous 1,1,1-trichloroethane (1,1,1-TCA) under sonolysis, photolysis, and the synergisticcombination of the two and reported more extensivedecomposition with combined photolysis and sonolysis(photosonolysis) than UV photolysis or sonolysis alone.It was also shown that TCA (CCl3CH3) decomposed intogases, VOCs, and ionic species, and as the volume ofthe same concentration was increased, the sonolysisdigestion efficiency decreased. Cheung et al.8 examinedthe sonochemical destruction of methylene chloride(CH3Cl), TCA, TCE, and CCl4 and attributed the rapiddecrease of reactor solution pH in all cases to theprobable formation of HCl from the chlorinated reac-tants with the hydrogen source being water. Bhatnagarand Cheung10 studied the kinetic behavior of individualVOCs in the presence of other VOCs by sonicatingmixtures of (1) two chloromethanes (CH3Cl + CCl4) and(2) CH2Cl2, CCl4 (C1 compounds) + 1,1,1-TCA (C2compound). The first-order rate constants for the com-pounds were essentially unchanged by the presence ofother reacting species. Petrier and Francony105 com-pared the decomposition rates of CCl4 and phenol atdifferent frequencies (20-800 kHz) and observed thatirrespective of frequency, it was easier to decompose thehydrophobic and volatile CCl4 than the hydrophilicphenol with a low vapor pressure. For the phenol, theyfound that degradation proceeded faster at 200 kHz andthat the addition of an excess of 1-butanol (10-foldphenol initial concentration), used to scavenge hydroxylradicals totally inhibited the reaction. The rate ofdisappearance of CCl4 on the other hand was found toincrease slightly with increase in frequency, and theaddition of 1-butanol (10-fold CCl4 initial concentration)did not affect the rate of CCl4 destruction. It was alsoshown that both phenol degradation and H2O2 forma-tion involving reactions with OH radical at the interfaceincreased with frequency reaching an optimal value at200 kHz. Drijvers et al.106 investigated the mutualinfluence of TCE and chlorobenzene by sonicating diluteaqueous mixtures of the two volatile organic compoundsand found the sonolysis rates to depend strongly on theinitial concentration of TCE and CB. The presence ofCB was found to lower the sonolysis rate of TCE, whilethe sonolysis rate of CB (with initial concentration 3.44mM) was enhanced by the presence of 0.84 mM TCE.They attributed the different effects of both volatileorganics on each other’s sonolysis to the difference inreaction rate of TCE and CB with the radicals formedduring sonolysis. They suggested that the effect of TCEon the sonolysis rate of CB (i.e., the lowering of the γvalue of the gas present in the cavitation bubble andconsequently the temperature during collapse) wascompensated by an increased indirect degradation of CBby radicals formed out of TCE.

De Visscher and Van Langelove107 explored the influ-ence of Fenton-type oxidants on the aqueous sonochemi-cal degradation of trichloroethylene (TCE), o-chlorophe-nol (o-CP), and 1,3-dichloro-2-propanol (DCP). It wasshown that di-tert-butyl peroxide inhibited the sonolysisof both TCE and CP by scavenging OH radicals and bylowering the maximum temperature generated duringa cavitation event. However, 10 mM tert-butyl hydro-peroxide had no considerable effect on the sonochemicaldegradation of TCE but inhibited completely the deg-radation of o-CP. The effect of TCE was interpreted tomean that the amount of tert-butyl hydroperoxide in thecavitation bubbles (where TCE is degraded) was too low

to change the conditions of a cavitation event signifi-cantly. The effect on o-CP indicated that tert-butylhyroperoxide scavenged OH radicals without producingany radicals that entered the liquid phase where oxida-tion was expected to occur. Unlike the less polar, organicperoxides, the presence of H2O2 did not affect thedegradation of TCE and DCP but enhanced the degra-dation of o-CP on the order of 20-25%. The degradationof both o-CP and DCP (with low Henry’s constant) areexpected to occur by radical attack. Hence, they at-tributed the low reactivity of DCP toward OH to thelack of aromatic rings on which the radicals can addand to the presence of Cl atoms on DCP that could leadto electronic repulsion toward the OH radical. They alsoobserved that in the presence of H2O2 and copper ions,the sonochemical degradation of o-CP is the sum of theeffect of the ultrasound and the chemical oxidation effectand likened the overall degradation mechanisms tosonochemical switching effect. That is, sonication in-duces a specific reactivity and silent chemical, andsonochemical degradations follow separate paths. TheCAV-OX has been shown to degrade TCE and BTEXin contaminated groundwater with efficiencies betterthan 99.9% when varied principal opearting parameterssuch as H2O2 dose, pH, and flow rate are used.14 Theprocess involves the use of sequential hydrodynamiccavitation and direct UV photolysis of H2O2 to generatehydroxyl and hydroperoxyl radicals. Orzechowska etal.108 monitered and compared the chloride releasetendencies of CCl4, CHCl3, TCE, aromatic chloro com-pounds (e.g., CB, polyaromatic chloro compounds, PCBs,4,4′- and 3,3′-dichlorobiphenyl) and TritonX-100 (a sur-factant) upon sonication and found that CB and PCBsdid not release Cl- as readily as did CCl4, CHCl3, andTCE. They attributed the results to possible hydroxy-lation reactions at an open position of aromatic ring,i.e., oxidation of PCBs and CB by OH radical withoutdehalogenation. The presence of humic substances wasalso found not to affect Cl- yields. Catallo and Junk109

studied the sonochemical transformation of hazardouschlorinated chemicals and a mixture of chlorinatedolefins, paraffins, and aromatics from a Louisianasuperfund site (LSS) and observed dechlorination viaaryl C-Cl bond heterolysis and hydroxylation reactionsto be the main reaction pathways. Dechlorination and/or other transformations were observed for chlorinatedalkanes (e.g., CCl4) 2,4-dichlorophenol, chlorpyrifos, andlindane (hexachlorocyclohexane, γ-isomer) and a forrange of chlorinated aromatic and aliphatic chemicalsin the LSS mixture. The herbicide byproducts, chlorpy-rifos, 3,3′,4,4-tetrachloroazoxybenzene (TCAOB), andtrichlorodibenzofuran (TCDF), were not dechlorinated.However, TCAOB appeared to deoxygenate sonochemi-cally to the 3,3′,4,4 tetrachloroazobenzene. Sakai et al.110

studied the sonochemical degradation of aqueous solu-tions of chloral hydrate (CCl3CH(OH)2 or simply CH)and found the rate to be proportional to the square ofoxygen concentration at low concentrations, while atrelatively high concentration, the rate is independentof the oxygen concentration. They also found the reac-tion rate to be proportional to the square root of theconcentration of chloral hydrate and to the intensity ofthe ultrasound regardless of the concentration of oxygengas dissolved in the solutions.

4.3. Explosives. Sierka111 investigated the treatmentof aqueous solutions of trinitrotoluene (TNT) and cy-clotrimethylene-trinitramine (RDX) in the weight ratio

4702 Ind. Eng. Chem. Res., Vol. 40, No. 22, 2001

of 70:30 (typical of munitions wastewater) at 25-59 °Cusing a combination of ozone and ultrasound in the pHrange of 5.84-10.00. They demonstrated the synergisticeffects of both ozone and ultrasound. While the maxi-mum destruction of both TOC and TNT was observedat 859 kHz and 50W, experiments performed withoutO3 at these same conditions resulted in no TNT or TOCremovals. The increased removal with O3/ultrasoundsystems was explained partially by the increased tem-perature in the reactor. While at 25 °C, the TNTdestroyed after 60 min of ozonation was 23%; 99% wasdestroyed when temperature averaged 59 °C. Removalrates of both TNT and TOC increased directly withincreases in reaction temperature and initial pH. How-ever, it was shown that at solution pH values main-tained in excess of 9.6, the combination of high pH andtemperature was not beneficial. This was attributed tothe fact that ultrasound inhibited kinetics at hightemperatures and pH by promoting radical-radicalextinguishment reaction. But ultrasound was also shownto have an additional benefit potential in that it can actas a catalyst by enhancing the autodecomposition of O3to free radicals once the ozone has been dissolved in theaqueous phase. Sonolysis was evident in the degrada-tion of residues of the military explosives TNT (2,4,6-trinitrotoluene) and HMX (octahydro-1,3,5,7-tetranitro-1,3,5,7-tetrazocine), as indicated by release of nitrate(NO3

-) during treatment.73 Hoffmann and co-work-ers16,58 112 investigated the sonochemical degradation ofTNT at 20 and 500 kHz to acetate, formate, glycolate,oxalate, CO2, NO2

-, and NO3- as products with 1,3,5-

trinitrobenzene as intermediate and found the overalldegradation rate to follow an apparent first-order ratelaw. The overall reaction stoichiometry for the autooxidation of TNT was found to be:

where ))) denotes ultrasonic irradiation. They foundTNT degradation to be more efficient at 500 kHz than20 kHz, irrespective of the background gas. The first-order kinetic rates vary by a factor up to 3, dependingon the nature of dissolved gases and also on theultrasonic frequency: kO2 ) 1.67 × 10-5 s-1, kAr ) 4.50× 10-5 s-1, and kO2/O3 ) 5.50 × 10-5 s-1 (with 99/1 vol% O2/O3 mixture as cavitating gases) at 20 kHz com-pared with kO2 ) 2.00 × 10-5 s-1, kAr ) 7.17 × 10-5 s-1,and kO2/O3 ) 8.50 × 10-4 s-1 at 500 kHz.

4.4. Herbicides and Pesticides. The sonolysis of thesystemic herbicide, chlorpropham (isopropyl-3-chloro-carbanilate) in air equilibrated aqueous solutions leadto the formation of hydroxylated products and 3-chlo-roaniline as intermediates, and subsequent mineraliza-tion of intermediates to Cl-, NO2

-, NO3-, CO, and CO2.

David et al.113 observed that the ultrasonic treatmentof chlorpropham at 482 and 20 kHz led to a highlydrastic degradation with the initial rate at the highfrequency (13.0 × 10-8 M s-1), much higher than thatat the low frequency (4.2 × 10-8 M s-1). They alsonoticed a complete degradation after 45 min at 482 kHzcompared with 1/3 of chlorpropham remaining after 60min at 20 kHz. It was also shown that the yield of Cl-

was about 98% after 80 min at 482 kHz, indicating theC-Cl bond cleavage is a major primary process. Twopathways deduced to be involved in the transformation,the oxidation by OH• and pyrolysis near the cavitation

bubbles. The formation of hydrated products (e.g.,3-chlorohydroquinone) indicated the involvement of thehydroxyl radical in the degradation of chloropropham.Petrier et al.114 investigated the ultrasonic degradationof atrazine, CIET [2,4-diamino-6-chloro-N-ethhyl-N′-(1-methylethyl)-1,3,5 triazine] and pentachlorophenol (PCP)at 500 kHz and 20 kHz and demonstrated in both casesthat degradations were more efficient and complete atthe higher frequency. Sonochemical degradation ofatrazine resulted in dealkylation product: CIAT [2,4-diamino-6-chloro-N-(1-methylethyl)-1,3,5 triazine],CEAT[2,4-diamino-6-chloro-N-ethyl-1,3,5 triazine], andCAAT[2,4-diamino-6-chloro-1,3,5- triazine], which aretypical oxidation products of atrazine from degradationby ozone, Fentons reagent, or TiO2 photocatalysis. Longirradiation times (3 h) resulted in the formation of CO2(13% of initial atrazine) and chloride. They observed fastreactions for PeCP (10-4 M aqueous solution at pH 7)at both frequencies, yielding 98% of the theoreticalamount of chloride and 20% theoretical carbon as CO2recovered after 180 min for the reaction conducted at500 kHz. However, the addition of n-pentanol (10 mM)inhibited completely both atrazine and PeCP degrada-tion at high and low frequency, suggesting reactionswith OH• radicals escaping from the cavitation bubble.Koshkinen et al.115 found the sonochemical degradationof atrazine to be slower than that of alachlor (70-fold)at 20 kHz at the same concentration (e.g., 3.1 µmol/L)and temperature (30 °C). The first-order rate constantsand extrapolated half-lives were 8.01 × 10-3 min-1 and86 min and 2.1 × 10-3 min-1 and 330 min for alachlorand atrazine, respectively. They also attributed thedecomposition of both atrazine and alachlor to theattack by hydroxyl free radicals. Nagata et al.74 foundthe aqueous sonochemical degradation of 0.1 mM pen-tachlorophenol (PeCP) to be faster under argon atmo-sphere compared with air atmosphere (first-order rateconstant of 6.4 vs 4.5 µM min-1).

Gondrexon et al.116 studied the sonochemical degra-dation of PeCP in a three-stage, continuous flow,laboratory-scale ultrasonic reactor and obtained a con-version up to 80%. Johnston and Hocking75 investigatedthe photocatalytic and photolytic degradation of PeCP(2.4 × 10-4 M solution) with and without sonication.They observed the initial rate of chloride formation dueto photocatalysis using TiO2 to be about 2.7 times fasterwith sonication than without. In the absence of sonica-tion, the percent degradation measured by Cl- releasereached a value of 40% after 50 min, beyond whichcontinued irradiation up to 200 min did not significantlyaffect increase in degradation. In contrast, combinedsonication, UV, and photolysis resulted in a rapid initialdegradation, with near quantitative release of chlorideafter 120 min. They attributed their observation topossible poisoning of catalyst active sites during pho-todegradation by inert intermediates formed but whichare removed from active sites by sonication, allowingfurther degradation or decrease in pH during photolysis,leading to significant decrease in a photochemicaldegradation process. Petrier et al.117 also studied thesonochemical degradation of pentachlorophenate (PCP)at 530 kHz in aqueous solutions saturated with air,oxygen, or argon and observed the degradation and theresulting toxicity decrease to be faster under argonbubbling (PCP disappeared in 50 min) than under airor oxygen. The ultrasonic degradation of PCP was alsoattributed to a rapid cleavage of carbon-chlorine bond

C7H5(NO2)3 + 9O2 98)))))

7CO2 + H2O + 3H+ + 3NO3- (16)

Ind. Eng. Chem. Res., Vol. 40, No. 22, 2001 4703

to release Cl- (90% chlorine recovered as Cl- in 150min). This was followed by degradation to CO2 in air-or oxygen-saturated solutions (or CO in argon-saturatedsolutions) and nitrite and nitrate in solutions aeratedwith air or oxygen. They also postulated that becauseof the high temperature inside the cavitation bubble,the formation of CO in the presence of argon was dueto reactions of the type:

Wheat and Tumeo118 studied the aqueous sonolysis oftwo polycyclic aromatic hydrocarbons or PAH’s (phenan-threne and biphenyl), and the results obtained suggestpolychlorinated biphenyls (PCB’s) may be susceptibleto hydroxyl radical substitution reactions under thevigorous reaction conditions supplied by high-intensityultrasound. The principal products of biphenyl reactionidentified through mass spectral analysis were [1,1-biphen]-2-ol, [1,1-biphen]-3-ol and [1,1-biphen]-4-ol, andthe principal products of phenanthrene appeared to bedi-hydroxy substituted phenanthrene. The phenolicproducts produced from these hydrophobic compoundswere considered consistent with a free radical attackby hydroxyl free radicals (OH•) on the hydrocarbonskeleton. Zhang and Hua119 also observed that poly-chlorinated biphenyls (2-, 4-, and 2,4,5-chlorobiphenyls)dechlorinated rapidly to chloride ion during sonolysisat 20 kHz with 99% destruction of 2-PCB, 4-PCB, and2,4,5-PCB in 36, 47, and 29 min, respectively. Thechloride recovery ratio defined as [Cl-] /([M]i - [M]f) ×n, where n is the number of chlorine atoms per cogenerin each sample and [M]i and [M]f are initial and finalconcentrations of parent compound (i.e., mol/L PCB),were 77%, 79%, and 70%, respectively, for 2-PCB,4-PCB, and 2,4,5-PCB, respectively. They also identifiedproducts such as biphenyl, toluene, ethylbenzene, phe-nol, trichlorophenol, hexenyldiphenol, and other phenols(Table 3). They investigated the role of aqueous hydroxylradical in the decomposition of 2-PCB at 205, 358, 618,and 1071 kHz. It was shown that ultrasonic irradiationwas optimal at 358 kHz but chloride recovery wasoptimal at 1071 kHz. They proposed that both ther-molysis and free radical attack are important pathwaysof PCB destruction but that free radical attack (espe-cially •OH) in the aqueous phase played a more signifi-cant role at 358 kHz than at other three frequencies.Johnston and Hocking75 investigated the photo catalytic/photolytic degradation of PCB isomer 3-chlorobiphenylat 75 ppm level (4 × 10-4 M) by monitoring the chlorideformation. TiO2 (0.2% w/w) and 30 mL aliquots weresubjected to UV irradiation and to combined UV/ultrasound irradiation. They found a linear rate ofappearance of chloride with time for both conditions,but rates with sonication were approximately 3 timesgreater that without sonication, and they attributed theenhanced rates partially to the highly hydrophobicnature (i.e., low solubility) of substrate. They alsoattributed the significant increase in degradation ratesand efficiency of the concurrent UV/ultrasonic irradia-tion to cavitational effects, bulk, and localized masstransport effects and sonochemical reactions.

Kotronarou et al.120 showed that the sonolysis ofparathion (o,o-diethyl o-p-nitro phenyl thiophosphate)led to its transformation to sulfate, nitrate, nitrite,phosphate, oxalate and p-nitrophenol, p-NP (parathion

hydrolysis product) with complete degradation in e2 h.They proposed that parathion transformation proceededvia thermal decomposition in the hot interfacial regionof the collapsing bubbles with secondary reactions with•OH radicals. Theron et al.121 determined the removalrates of phenyltrifluoromethyl ketone (160 µmol L-1

PTMK) by sonolysis at 30 and 515 kHz, by UV-irradiated TiO2 (Degussa P25 and Rhodia), and bysimultaneous photocatalysis and ultrasonic irradiations.The PTMK first-order removal rate constant was foundto be 14 times greater at the higher frequency comparedwith that at the lower frequency at the same energylevel and 2.5 times higher when synthesized RhodiaTiO2 was used instead of Degussa P25. The amount oftrifluoroacetic acid (CF3COOH or TFA), an undesirableand stable product of TiO2-treated CF3-containing pol-lutants, was about 8 times lower in sonicated solutionsthan in UV-irradiated suspensions, for both frequencies.

4.5. Organic Dyes. Vinodgopal et al.122 studied thesonochemical degradation of a reactive black dye (Azodye, Remazol Black B or RB) at high frequency (640kHz) in O2-saturated aqueous solution. They foundsonolysis as a feasible method to achieve both decolori-zation and 65% degradation of the dye in 6 h asmeasured by the decrease in the in total organic content.The pseudo-first-order rate constant for the disappear-ance of the dye was determined to be 2.9 × 10-2min-1.They also observed that degradation stopped far shortof completion when performed in an aqueous solutionof about 2% tert-butyl alcohol, an excellent OH radicalscavenger, and attributed the conversion of the dye tooxalate (C2O4

2-) to •OH radical-initiated oxidative deg-radation. They also compared photocatalytic and radi-olytic methods of degradation to sonolysis. Their resultssuggested that sonochemical degradation rates of Azodyes were substantially faster and led to better destruc-tion of the dye compared to photocatalysis. Stock et al.123

investigated the degradation of an azo dye, naphtholblue black (NBB), using sequential combination of high-frequency sonolysis and photocatalysis in four differentconfigurations: (1) sonolysis only, (2) photocatalysisonly, (3) simultaneous sonolysis and photocatalysis, and(4) sequential sonolysis and photocatalysis. They ob-served that for individual techniques, sonolysis waseffective for inducing faster degradation of the parentdye, while TiO2 photocatalysis was effective for promot-ing degradation. For example, photocatalysis was re-sponsible for 68% conversion compared to 35% forsonolysis after 12 h. It was also shown that the first-order rate was enhanced by the combined systems(simultaneous and sequential). For example, pseudo-first-order rate constant was 1.83 × 10-2 min-1 for thecombined case compared with 1.04 × 10-2 min-1 forsonolysis or 0.56 × 10-2 min-1 for photocatalytic experi-ments.

4.6. Organic and Inorganic Gaseous Pollutants.Cheung and Kurup124 investigated the sonochemicaldestruction of fluorotrichloromethane (CFC11) and tri-fluorotrichloroethane (CFC113) in dilute aqueous solu-tions in a batch and circulating reactor. They found therates to be fairly rapid with less than 5% of the originalCFC’s undergoing volatilization and the bulk of materialdestroyed in the liquid phase. In these preliminarystudies, they also observed the rates to be slightly higherat 5 °C than at 10 °C and rapid drops in pH (initial valueof 7.4 to about 5.4), indicating the formation of acidicspecies. Hirai et al.125 evaluated a number of CFC’s and

CO2 + Ar f CO + O + Ar and

CO2 + •H f CO + •OH

4704 Ind. Eng. Chem. Res., Vol. 40, No. 22, 2001

HFC’s and found them to be readily decomposedsonochemically with high efficiency to inorganic prod-ucts (CO, CO2, Cl-, F-). It was also shown that CFC-113 decomposed faster under argon atmosphere (withhigher CP/Cv ratio) than air atmosphere and that itsdecomposition rate was not significantly affected by theaddition of tert-butyl alcohol (tert-BuOH), a knowneffective OH radical scavenger. Hart and Henglein126

studied the sonochemistry of Ar/N2O mixtures and thepure gases in aqueous solutions at high frequency, 300kHz, and observed products of decomposition of N2O tobe N2, O2, NO2

- (or HNO2), and small amount of NO3-

(or HNO3). It was also observed that the maximum yieldof decomposition occurred at an Ar/N2O vol % ratio of85:15. However, the rate of N2O decomposition was verylow when water was sonicated under pure nitrous oxide,as expected with a triatomic gas. The yield of HNO2 wasmuch higher than observed in the irradiation of waterunder air and under mixtures of nitrogen and argon,and this was attributed to the decomposition of N2O ofthe type: 3N2O + H2O f 2HNO2 + 2N2. Henglein127

studied the ultrasonic irradiation of water under argonatmosphere containing small amounts of CO2, N2O andCH4. They observed no chemical effects in the irradia-tion under atmosphere of pure CO2, N2O, or CH4.However, they showed that sonochemistry in an argonatmosphere containing small amount of any of thepolyatomic gases was characterized by a strong linkagebetween the sonolysis of water and the added gas. Themain products of the sonolysis of CO2 were CO andsmall amount of formic acid, about 30 times smallerthan CO yield. The main products of N2O sonolysis wereN2, NO2

- and NO3- in this study.127 In the N2O-Ar

containing solutions, they observed the yields of theproducts NO2

- and NO3- were about 10 times greater

than the amounts formed in the ultrasonic irradiationof aerated water and greater than the amounts in waterirradiated in the presence of both N2O and O2. Hara-da128 investigated the sonolysis of CO2 dissolved inwater (0.0-0.6 mole fraction CO2 in water) at 5-45 °Cusing an ultrasonic generator (200 kHz, 200 W) and Ar,He, H2, and N2 as the irradiating gases. While irradia-tion of ultrasound had hardly any sonochemical effectunder CO2 atmosphere, the most favorable atmospherefor reducing was CO2-Ar mixture with 0.03 molefraction of CO2 in gas phase, a concentration consideredan equal mixture of CO2 and Ar in water because CO2is more soluble than Ar. The amount of CO2 in CO2-Ar was found to decrease to about half at 5 °C, and thedecreasing rate for CO2 followed the order Ar > He >H2 > N2. They also observed that dissolved CO2 wasdeoxidized to carbon monoxide (CO2 f CO + O) bysonolysis and showed that the hydrogen carbonate orbicarbonate ion (HCO3

-) played an important rolecompared to the carbonate ion (CO3

2-). Since hydrogenis also obtained from the solvent (water) and both COand H2 are fuel gases, which also react to produce C1compounds such as methanol, they proposed sonicationas a useful and potential technique to reduce CO2 andproduce fuel.

The main oxidation products of the methane-contain-ing solutions were oxygen-containing gases such as CO,CO2, and compounds with oxygen, such as C2H4, C2H6,and C3 and C4 compounds, and the production of largeamounts of H2. Hart et al.129 also identified H2, C2H2,C2H4, and C2H6 as major products and C3-C4 hydro-carbons (e.g., propane, propene, 2-methylpropane, n-

butane, 1-butene, 2-methyl,1-butane and butadiene) andCO as other products of CH4 sonolysis under argonatmosphere. They found the products for the sonolysisof the C2H6 to be the same as CH4 except that they wereproduced in higher yields. Hart et al.130 also observedthe sonochemical degradation of acetylene to be rapid(90% consumption of C2H2 at time g 80 min) withformation of large products. In addition to small gasmolecules such as CO and CH4, various hydrocarbonswith intermediate C atom numbers, such as benzeneand other C6H6 isomers, high C atom numbers such asnaphthalene are formed.

Kotronarous et al.131 found the ultrasonic irradiationof H2S or S(-II), [[S(-II) ) [H2S] + [HS-] + [S2-]]solutions to result in rapid oxidation and the formationof sulfate (SO4

2-), sulfite (SO32-), and thiosulfate (S2O3

2-)as products at pH g 10 with the initial mole ratio of2.2:2.7:1, respectively. They also found oxidation of S(-II) at pH 10 to be zero order with respect to [S(-II)]with the zero-order rate constant, kO, dependent oninitial concentration of S(-II) and increasing linearlywith [S(-II)]O up to [S(-II)]O = 450µM (where kO = 12µM min-1) and remaining constant thereafter. However,at low pH e 8.5 (e.g., pH 7.4), the rate of ultrasonicoxidation of S(-II) was first order with respect to [S(-II)], the rate of oxidation increased with a decrease inpH, and measured concentrations of SO4

2-, SO32-, and

S2O32- could not account for the total observed decrease

in S(-II), especially at the short sonication times. Thediscrepancy between the [Sox] measured and the [Sox]expected was attributed to the formation of sulfur (S8)that was not analytically measured but increased theturbidity of the solution. The apparent zero-orderdependence on [S(-II)] suggested that the rate-deter-mining step (or the main pathway) in the overallreaction was the reaction of HS- and the oxidationintermediates with •OH radical in the liquid phase asit diffused out of the cavitation bubble (HS- + •OH fHSOH-) and the observed decrease in the zero-orderrate constant at the pH > 10 was attributed partly tothe dissociation of •OH in the alkaline solutions andsince the oxide radical ion (•O-) reacts more slowly withthe same substrate than •OH according to the reaction:•OH +OH- S O•- + H2O, where the forward rate, kf )1.2 × 1010m-1s-1 and the backward rate, kb ) 9.3 ×107s-1. At pH e 8.5, thermal decomposition of H2Swithin or near collapsing cavitation bubbles was con-sidered the important reaction pathway. Kotronarouand Hoffmann132 also developed a comprehensive aque-ous-phase mechanism for the free-radical chemistry ofthe S(-II) + ‚OH + O2 system and used the mechanismto successfully model the oxidation of S(-II) at 20 kHzand 75 W/cm2 and at pH g 10, assuming a continuousand uniform ‚OH (3.5 µM/min) input into the solutionfrom the imploding cavitation bubbles.

When water was irradiated with ultrasound under anatmosphere containing O2 and O3, an extremely rapiddecomposition of O3 was found to take place, leading toa yield of H2O2 up to a factor of 6 higher than in watercontaining oxygen only.133 Weaver and Hoffmann3 in-vestigated the sonolytic degradation of O3 aqueoussolutions at pH 2 using both closed and open continuousflow systems and the mass transfer mechanisms occur-ring in sonolytic ozonation and their effects on chemicalreactivity. They found the sonochemical degradation ofO3 to follow apparent first-order kinetics with typicalrate constants of 0.84 ( 0.07 and 0.66 ( 0.08 min-1,

Ind. Eng. Chem. Res., Vol. 40, No. 22, 2001 4705

respectively, at 20 and 500 kHz and an initial O3concentration of 245 ( 3 µM. It was also shown thatboth the sonochemical degradation of O3 and theincrease in O2/O3 gas flow rate enhanced mass transferat 20 kHz. This effect was attributed partially toturbulence induced by acoustic streaming.

4.7. Organic Sulfur Compounds. Spurlock andReifsneider96,134 investigated the ultrasonic irradiationof diakyl sulfides at 20 °C using 280-, 610-, and 800-kHz transducers and 5-11 W/cm2 intensities underoxygen and argon atmospheres and in suspensions inpure water and in saturated aqueous solutions of CCl4.The principal products of the irradiation of 0.06 Maqueous suspension of di-n-butyl sulfide (R2S) at 800kHz and 9.4w/cm2 were di-n-butyl sulfoxide (R2SO) andn-butyl sulfonic acid (RSO3H) in the yield ratios of 85/15 and 80/10 in O2 and Ar, respectively. Minor productsobserved included di-n-butyl sulfone (R2SO2), butyricacid, carbon monoxide, ethylene, acetylene, and meth-ane.

Entezari et al.135 sonicated 50 mL of pure carbondisulfide (CS2) at 20, 50, and 900 kHz frequencies underthe atmosphere of different gases (Ar, H2, Air, He, O2,CO2) in a temperature range of -50 to +10 °C. Theyobserved that ultrasonic sonication at 900 and 50 kHz(up to 4 h) led to no visible or chemical changes due tothe sonication while irradiation of CS2 at 20 kHzfrequency resulted in the formation of heterogeneousmixture of amorphous carbon and monoclinic sulfur. Thedissociation of CS2 was proposed to be due to theextreme conditions resulting from the collapse of thecavity bubbles, the low thermal conductivity of CS2ensuring the high-temperature persisted long enoughto result in the breakage of the C-S bond to formelemental carbon and sulfur. The dissociation rate wasalso found to be rapid and efficient at lower tempera-tures and higher intensities but at the same power(49W) and under helium and hydrogen gas than underair, argon, or oxygen. The fact that the sonochemicalactivity was higher in He than in Ar (with lower heatconductivity) was attributed to other properties of gases,especially solubility. Adewuyi and Collins136,137 studiedthe kinetics of the sonochemical degradation of aqueouscarbon disulfide in a batch reactor at 20 kHz and theeffects of process parameters (e.g., concentration, tem-perature, ultrasonic intensity) on the degradation pro-cess. They found the reaction rate to be zero-order inthe temperature range 20-50 °C and first-order at lowertemperature. The zero-order rate constant for thedegradation at 20 °C, at 14 W, and in air was 2.27 ×10-5 min-1. At the same initial concentrations andtemperature of 20 °C and in the presence of air, thedegradation rate of CS2 at 50 W (39.47 W/m2) was morethan 2 times that at 14 W (11.04 W/m2). The rate ofsonochemical degradation of CS2 in the presence of thedifferent gases was on the order of He > Air > N2O >Ar; the rate with helium was found to be about 3 timesthat of argon. They found the formation of sulfate as aproduct to be enhanced at the lower pH and also atlower temperatures when solutions from experimentsin the pH range 8-11 and temperatures 5-50 °C wereanalyzed.

4.8. Oxygenates and Alcohols. Kang and Hoff-mann138 studied the sonolysis, ozonolysis and the com-bined sonolysis/ozonation of methyl tert-butyl ether(MTBE) in the concentration range of 0.01-1.0 mM anddemonstrated that the addition of O3 to the influent O2

gas ([O3]0 ) 0.26-0.34 mM in solution) accelerated thedegradation of MTBE by a factor of 1.5-3.9, dependingon the initial concentration of MTBE. The sonochemicalfirst-order degradation rate constant for the loss ofMTBE was found to increase from 4.1 × 10-4 at[MTBE]0 ) 1.0 mM (90% conversion in 93 min) to 8.5× 10-4s-1 as the concentration of MTBE decreases to0.01 mM (90% conversion in 45 min). The O3-ultrasoundsystem was shown to effectively degrade the MTBE intoinnocuous and biodegradable products with tert-butylformate (TBF), tert-butyl alcohol (TBA), methyl acetate(MA), and acetone identified as primary intermediatesand byproducts of the degradation reaction. Acetone,which was formed from the oxidation of TBF (degrada-tion rate constant, kTBF ) 1.87 × 10-3s-1) and TBA, wasfound as the intermediate product with the highest yield(12%). Using measured values of MTBE and TBF rateconstants, a reaction mechanism involving tree parallelpathways: (1) direct pyrolytic decomposition of MTBE,(2) direct reaction of MTBE with O3, and (3) reaction ofMTBE with •OH radical were proposed and used toobtain the following kinetic rate expression:

where kpyr, kI, kII, and kIII are the pseudo-first-order rateconstant for the direct pyrolysis, thermal degradationleading to O-CH3 bond breakage, direct reaction withozone, and other direct routes to products formation,respectively.

Koike139 studied the sonolysis of alcohol-water mix-tures using CH3OH, C2H5OH, n-C3H7OH, and i-C3H7-OH and found each mixture to form gaseous products,including CH4, C2H6, C2H4, C2H2, and C3H6. Koike139

found the product yields to increase to a maximum atalcohol composition of about 20 vol % in the watersolution and to decrease thereafter for each of thealcohol-water mixture. Buttner et al.140 studied thesonolysis of water-methanol mixtures under argon andoxygen and obtained similar results. With increasingmethanol concentration the product yields first in-creased as methanol is a reactant and decreased withincreasing concentration leading to a maximum in theyields versus composition curves. In solutions containingmore than 80% methanol, they observed almost nochemical reactions. They detected typical pyrolysis andcombustion products of methanol (H2, CH2O, CO, CH4,and traces of C2H4 and C2H2 under argon, and CO2, CO,HCOOH, CH2O, H2O2 and traces of H2 under oxygen).Gutierrez and Henglein141 compared the sonolysis ofaqueous solutions of ethanol (as volatile and solublesolute), poly(vinylpyrrolidine) PVP (as nonvolatile sol-ute), and tetranitromethane TNM (as volatile andalmost insoluble solute) under Ar irradiation (at 300kHz and 2W/cm2). They explained the formation ofproducts in all three cases (such as CH4, C2H4, C2H6,CO, and CO2 from ethanol and PVP; and NO2

-, NO3-,

N2, CO, CO2 from TNM) in terms of pyrolysis in or closeto the cavitation bubbles.

4.9. Other Organic Compounds. Suzuki et al.142

examined the effect of ultrasound (200 kHz, 200W) at298 K on the degradation rate of the surfactant, poly-oxyethylene-alkyl ether (C14H29O(CH2CH2)7H), underthree different conditions: ultrasonic irradiation only(sonoprocess), photocatalytic reaction using TiO2 (0.25

-d[MTBE]

dt) (kpyr + kI + kII + kIII)[MTBE] )

ko[MTBE] (17)

4706 Ind. Eng. Chem. Res., Vol. 40, No. 22, 2001

g/mL of P25) and low-pressure mercury (20W, 253.7 nm)lamp (photoprocess), and the combination of the twoprocesses (photosonoprocess). They observed the decom-position rate in the photosonoprocess was faster thanthe photoprocess or sonoprocess alone. A significantacceleration in the degradation of TOC was also ob-served when stirring speed was increased from 100 to500 rpm. The significantly enhanced rate in the pho-tosonoprocess compared to the sonoprocess alone wasattributed to the redispersion of the agglomeratedcatalyst particles under ultrasonic irradiation. They alsosuccessfully separated solid catalyst particles agglomer-ated by ultrasonic irradiation at 28 kHz in the presenceof glass beads.

Hart and Henglein143 evaluated the sonolysis ofmixtures of formic acid and water at concentrations of0-30 M. The main reaction products under an argonatmosphere were H2, CO2, CO, and very small amountsof oxalic acid. Hart and Henglein144 also studied theirradiation of aqueous solutions of potassium iodide andsodium formate under the atmosphere of argon, oxygenand argon-oxygen mixtures of varying composition. Thesono products of formate solutions were H2O2 and CO2in the presence of O2 and H2, CO2, and oxalate in theabsence of O2. Gutierrez et al.145 found the products ofsonolysis of acetate to include succinic acid (as a productof attack of OH radicals on acetate), glyoxylic andglycolic acids, smaller amounts of HCHO, CO, and CO2,and CH4 as a minor product.

Thymine (Thy) was found to degrade sonochemicallyin aqueous solutions at 450 kHz into six products: cis-and trans-5, 6-dihydroxy-dihydrothymine (cis- and trans-thymine glycols), 5-hydroxymethyluraacid, urea, andpossibly N-formyl-N′-pyruvelurea plus an unidentifiedproduct.41 Mead et al.146 also found the degradation tovary linearly with sonication time with a zero-order rateconstant of 1.8 ( 0.3 × 10-5 M.min-1. Sehgal andWang41 found that at an aeration rate of 50 mL/min andat 34 °C, the concentration of thymine is reduced to halfits value in 30 min, implying that an average of 3 ×10-8mol or 1.8 × 1016 molecules of Thy reacted persecond per liter. The studies also indicated there was achange in kinetics of reaction of Thy from first to zeroorder as temperature of solution changed from 0 to 50°C, and they suggested that the sono reaction took placein the bubble-liquid interphase.

4.10. Other Environmental Applications. Ingaleet al.147 investigated the degradation of a refractorycomponent in the industrial waste of a cyclohexeneoxidation unit using a hybrid system, namely, sonicationfollowed by catalytic wet oxidation (SONIWO). It wasshown that sonication in the presence of CuSO4 ascatalyst resulted in an accelerated degradation of theunknown compound which was refractory to wet oxida-tion at 225 °C compared with sonication without acatalyst.

Kruger148 investigated the sonolysis of natural ground-water containing 1,2-didhloroethane (1,2-DCA) as themain organic contaminants (350 µg/L), and trichlo-romethane, cis-1,2-dichloroethane, trichloroethane andtetrachloroeathane, trichloroethene, tetrachloroethenein trace amounts (total of ∼85 µg/L), and Fe (3-17 mg/L) and Mn (0.4-0.9 mg/L) as the main inorganicproducts. They observed almost complete destruction of1,2-DCA in all cases after 60 min and pseudo-first-order

rate constants of 0.062, 0.063, and 0.044 min-1, for thesonication at 361, 620, and 1086 kHz respectively at105W.

Olson and Barbier149 studied the effectiveness of the“sonozone” process (i.e., combined ultrasound ozonolysis)in degrading refractory electrolytes such as humicmaterials using purified fulvic acid, FA (as a substrate)and naturally colored groundwater sample with pH 8.6.The combined system was found to significantly en-hance TOC removal and mineralization rates. Sierkaand Amy150 also studied the singular and combinedeffects of ultraviolet (UV) light and ultrasound (US) onthe ozone (O3) oxidation of humic substances, the mostimportant of the trihalomethane (THM) precursors.They found that the combination of O3-US-UV provedto be the most effective reaction condition, followed byO3-UV, O3 alone, and O3-US, providing 93%, 86%,75%, and 71% reduction in trihalomethane formationpotential (THMFP) levels, respectively, in the reactiontime of 20 min.

Gonze et al.151 investigated the use of the ultrasonicprocess as a preoxidation step before a classical biologi-cal treatment used for further mineralization. Theysimultaneously monitored the toxicity for sodium pen-tachlorophenate solution (NaPCP) on marine bacteria(Vibrio fischeri) and on daphnids (Daphniamagna), andthe biodegradability of the pollutant solution duringultrasonic irradiation at 500 kHz. The pollution degra-dation was found to follow an apparent first-orderkinetic:

i.e., the disappearance rate is proportional to the powerdensity applied, and the kinetic pseudo first-order rateconstant, kth (m3 J-1) is representative of ultrasonicefficiency. In general, they demonstrated that ultrasonicirradiation decreased the toxicity of NaPCP and couldbe considered a preoxidation step without which theNaPCP could not be degraded by activated sludge forup to 28 days.

Dahi152 studied the ozonation process with and with-out simultaneous sonication at 20 kHz in regard to thedisinfections of microorganism (Escherichia coli) andoxidation of organic (e.g., Rhodamine B). The ultrasonictreatment was found to intensify the action of ozone inthe oxidation of chemicals and in the inactivation ofmicroorganisms. The enhanced performance of thesimultaneous sonozonation process was attributed to (1)sonochemical degradation of O3, causing augmentationof activities of free radicals in water, and (2) increasein the aeration parameter (kLa value) and intensifiedmass transfer resulting from sonication. Phull et al.153

reported the biocidal effects of ultrasound alone (at 20-25 kHz and 800 kHz) or in conjunction with chlorineon microorganisms. Ultrasound was found to signifi-cantly amplify the biocidal effects of normal chlorinationand to reduce the amount of chlorine required fordisinfections.

5. Discussion

As reviewed above, the results of most studies seemto demonstrate that while ultrasound is effective indegrading pollutants, total mineralization is difficult toobtain with ultrasound alone, in particular, with recal-

[NaPCP] ) [NaPCP]o exp(-kth

Pth

Vt) (18)

Ind. Eng. Chem. Res., Vol. 40, No. 22, 2001 4707

citrant pollutants or mixtures of pollutants. Moreover,where the final products are determined to be carbondioxide, short-chain organic acids, and/or inorganic ions,the time scale and the dissipated power necessary toobtain the complete minerilization of the hazardouspollutants are currently not economically or practicallyacceptable. Combinations of ultrasound with otheradvanced oxidation processes (AOPs) or conventionalbiological processes are found to be effective in degrad-ing some recalcitrant compounds; however, the econom-ics are poorly understood. This section discusses someof the problems related to sonochemical reaction kinet-ics, byproducts, and ecological effects and to technical-scale application and implementation of the ultrasoundfor water treatment and the need to address them.

5.1. Reaction Pathways and Kinetics. In general,three distinct pathways have been determined in thesonochemical degradation of chemical compounds. Theseinclude oxidation by hydroxyl radicals, pyrolytic decom-position, and supercritical water oxidation.58 The ultra-sonic degradation of organic compounds in dilute aque-ous solutions depends to a large extent on the natureof the organic material. The specific nature of thesaturating gas also influences the relative proportionof the pyrolytic or free radical steps. Hydrophobic andvolatile organic compounds tend to partition into thecollapsing cavitation bubbles and degrade mainly bydirect thermal decomposition leading to the formationof combustion byproducts. The sonochemical oxidationof polar organics (e.g., phenol) is slow compared to thatof nonpolar, volatile organics such as CCl4.56,58 Hydro-philic and less volatile or nonvolatile compounds de-grade to form oxidation or reduction byproducts byreacting with hydroxyl radicals or hydrogen atomsdiffusing out of the cavitation bubbles. Thermal de-struction processes are not considered important fornonvolatile substrates because they do not partitionappreciably into the bubbles. The efficiency with whicha solute reacts with hydroxyl radicals generated inultrasonic reaction mixtures is related to its hydropho-bicity; the greater the hydrophobicity is, the moreefficient the solute can act a radical scavenger.154 Thetime scales of treatment in simple batch reactorsreported in the literature are generally in the range ofminutes to hours for complete degradation. Most inves-tigators have observed the kinetics of sono degradationof pollutants to be first- or zero-order. For pollutantswith first-order degradation rates, the first-order rateconstants tend to decrease as the initial substrateconcentrations increase.112,131 In contrast, for pollutantsdisplaying zero-order substrate disappearance, the rateconstants increase as the initial substrate concentrationincreases. A change in reaction order from zero-order(at high initial substrate concentration) to first-order(at lower initial substrate concentration) has also beenobserved.66 The change in rate constants with initialsubstrate concentration is ascribed to radical scaveng-ing/recombination, i.e., a combination of a first orderthermal destruction processes and a zero order reactionwith hydroxyl radicals.112,131 Sehgal and Wang41 ob-served change in reaction order from first to zero astemperature increased. Cost et al.78 indicated that zero-order kinetics are typical of hydroxyl radical reactionssince the free radicals are generated at constant rateunder ultrasonic irradiation and suggested the slowdegradation of humic acid occurred mainly by radicalattack.

Generally, improvements in technology are needed tooxidize organics especially polar compounds more ef-ficiently. If degradation rates can be enhanced, reactiontimes will be reduced for equivalent final contaminantconcentrations, translating to reduction in reactor sizes.Consequently, the cost of application of this technologyto industrial or field-scale projects would be significantlyreduced. The manipulation of macroscopic parametershas been shown to lead to enhancement of cavitationchemistry as the number of cavitation bubbles andchemical events at each bubble are varied. Hoffmannand co-workers77 optimized the degradation rates ofaqueous-phase organic compounds with acoustical pro-cessors by adjusting the energy density, energy inten-sity, and the nature and properties of the saturatinggas in solution. They observed that the first-orderdegradation rates increase as the energy density andintensity increased to a saturation value. Continuousgassing conditions also induce a greater number ofcavitation events in homogeneous systems and assistcavitation in heterogeneous systems.28 Susuki et al.155

investigated the influence of aeration, bubble distribu-tion, and frequency on the degradation rate of surfactantSS-70 (initial concentration, 50 ppm; critical micelleconcentration, 52.2 ppm) at 298°K using cylindrical-type(26 kHz) and disk-type (100 kHz, 300 kHz) ultrasonictransducers and showed that the degradation rates wereenhanced by aeration (i.e., aeration bubbles generated)and the shape of the reactors used. It is also well-knownthat ultrasonic degradation of phenolic compoundsinvolve •OH radical attack, and hence, the use of high-frequency ultrasound (e.g., 500 kHz) has proven to bemore advantageous compared with low-frequency ul-trasound. Higher ultrasonic frequencies are more favor-able for the generation of hydroxyl radicals possibly dueto faster production rates.46,48-50 Weaver et al.156 ex-amined the first-order sono degradation kinetics of threesimilar aromatic compounds, nitrobenzene (NB), 4-ni-tophenol (4-NP), and 4-chlorophenol (4-CP), by ultra-sound at frequencies of 20 and 500 kHz. They found thatin the 20 kHz reactor, NB degraded the fastest and 4-NPthe slowest, but in the 500 kHz reactor, 4-CP was thefastest while 4-NP was the most resistant to sonolyticdestruction. They attributed the results to the greaterdegree of vapor-phase pyrolysis at the lower frequencydue to high temperatures achieved during bubble col-lapse, while higher frequency favored ‚OH production.Using 20 kHz ultrasound, large salt-induced enhance-ments in oxidation/destruction rates have been ob-served: 6-fold for chlorobenzene, 7-fold for p-ethylphe-nol, and 3-fold for phenol oxidation, in sodium chloridesolutions (0, 0.17, 0.67, and 1.38 mol/L).59 The enhance-ment was ascribed to the fact that the presence of thesalt increased the residence of the aromatice compoundsin or at the surface of the cavitation bubbles. The rateof the sonochemical degradation of 3-chlorophenol wasenhanced 2.4 times by the addition of appropriateamount of Fe(II) concentrations (e.g., 1 mM). Theenhancement was attributed to the probable regenera-tion of OH radicals from H2O2, which would otherwiseformed from recombination of OH radicals and contrib-uted to lesser degradation.74 More such inexpensiveapproaches for improving process efficiency should beinvestigated in the future to make sonochemical oxida-tion an economically viable remediation technology.

5.2. Effects of Water Quality. This section discusseshow measures of water quality (i.e., matrix components)

4708 Ind. Eng. Chem. Res., Vol. 40, No. 22, 2001

such as alkalinity, particulate matter (dissolved organicand inorganic), and mixtures of compounds affect therates of sono-reactions. Sonchemical oxidation reactionslike other AOPs should generally be inhibited by highalkalinity usually resulting from the presence of largeconcentrations of radical scavengers such as bicarbon-ates and carbonates. This significantly reduces processefficiency. However, Cost et al.78 observed that addedalkalinity did not affect the rates of destruction ofp-nitrophenol (p-Np) or p-nitrocatechol by ultrasound.According to models on bubble nucleation in liquids,suspended particles are expected to affect cavitation,and hence, the rates of ultrasonic degradation of pol-lutants because of the formation and stabilization of gasbubbles in the crevices of the particles. Large particlesmight be expected to decrease the rate because of soundattenuation. Fine particles containing gas- and vapor-filled crevices might enhance the rate by providingadditional nuclei for bubble formation.157 However,Kotronarou112 investigated the effect of large sandparticles (500 µm average) and fine particles (7 nmaverage) on the sonication of sulfide oxidation andobserved no significant effect for the sizes and concen-trations studied. Cost et al.78 also noted that particulatematter (sea sand or Fe2O3 particle) did not significantlyaffect the degradation rate of p-Np. Orzechowska etal.108 observed that the presence of humic substancesdid not affect Cl- yields in the sonication of aqueouschlorinated hydrocarbons. However, Taylor et al.158

found the presence of fulvic acid (FA) to significantlyinhibit the sonochemical degradation of PAHs (in theconcentration range of 0.1-0.5 µM) at 20 kHz (600W)and at 20 °C. In the presence of approximately 50 µMFA, the first-order rate constants (k, s-1) of anthracene,phenanthrene, and pyrene decreased by factors of 3.7(0.015 vs 0.0041), 3.3 (0.006 vs 0.0018), and 2.3 (0.006vs 0.0026), respectively.

Multicomponent waste streams are more realisticmatrices to consider for practical treatment situations.Hua and Hoffmann99 found that sonication of a mixtureof CCl4 and p-NP resulted in the enhancement of p-NPdegradation, demonstrating that ultrasound is notlimited to single-solute solutions. They also found thatthe effect of CCl4 in a mixed waste stream was particu-larly interesting in that it released a residual oxidant,which could continue to attack other refractory mol-ecules in solution after the ultrasonic irradiation washalted. Drijvers et al.106 also showed that volatileorganic compounds could strongly affect each other’ssonolysis rates. However, as indicated earlier, thepresence of hydrophobic compound CB hindered thedegradation of hydrophilic compound, 4-CPOH.72 Zhangand Hua159 found moderate decreases in degradationefficiency when a mixture containing 10µM chloropicrin(CCl3NO2 or CP), 10µM trichloroacetonitrile (C2Cl3N orTCA), and 0.5 mM bromobenzene (BB) was sonicatedat both 20 kHz (30.8 Wcm-2) and 358 kHz in a complexaqueous matrix (i.e., river water) compared to reagentgrade water. Differences in rate constants observedduring sonication of the mixture and individual com-pounds were also minimal. The first-order rate con-stants at 20 kHz for TCA, CP, and BB were, respec-tively, 4.7 × 10-2 ( 6.5 × 10-4, 5.3 × 10-2 ( 4.4 × 10-4,and 4.4 × 10-2 ( 7.5 × 10-4 min-1 when sonicatedindividually. The rates were 4.4 × 10-2 ( 7.2 × 10-4,5.0 × 10-2 ( 8.8 × 10-4, and 4.1 × 10-2 ( 9.1 × 10-4

min-1 in a mixture. Since both industrial waste streams

and contaminated waters (surface and groundwater)generally contain a wide array of both pollutant andnonpollutant chemicals, more studies on the effects ofwater quality on sonochemical oxidation rates areneeded to advance our understanding.

5.3. Sonication Byproducts and Toxicity Effects.If ultrasound is to be used in the destruction of hazard-ous wastes on an industrial scale, the associated reac-tions must be ecologically acceptable. Hence, the toxicityof the reaction products obtained from sonochemicaltreatments is a factor that should be considered priorto subsequent utilization of treated water. In moststudies so far, the toxicity of the reaction productsproduced by treatment remains to be determined.Special attention must be paid to the types of productsformed and their toxicity and resistance to furtherultrasonic cleavage or other secondary treatments. Totalorganic carbon (TOC) analysis is one method that hasbeen used extensively to determine quantitativelywhether the sono degradation of the organic compoundresults in complete minerilization to the relativelyharmless CO2 (g) or some product that presents toxicfeatures. However, TOC analyses do not give the entirepicture with respect to toxicity because a given hazard-ous substance may also degrade to carbon deposits135

or be converted into other benign substrates that areacceptable end-products. A quick minerilization of anorganic contaminant should be the goal to minimize thesurvival time of toxic intermediates. The use of ultra-sound in combination with other advanced oxidationprocesses or conventional biological processes has beenfound to be effective in reducing toxicity. For example,Gonze et al.151 demonstrated that ultrasonic irradiationwhen used as a pretreatment step decreased the toxicityof sodium pentachlorophenol (NaPCP) solution im-mensely allowing degradation by biological activatedsludge process. Other possible ways include the couplingof H2O2, O3, or UV photocatalysis and solution chemistrymodification to enhance the efficiency of free radicalgeneration through cavitation. Hoffmann and col-leagues138 demonstrated that the combination of ultra-sound with ozonation or other AOPs effectively degradedrecalcitrant pollutants such as MTBE into innocuousand biodegradable products. Trabelsi et al.67 showedthat the combination of electrochemistry and high-frequency sonication allowed a total degradation ofphenol within 20 min with no production of toxicaromatic intermediates. It appears that using a combi-native AOP approach is certainly a positive step towardachieving quick minerilization and more such studiesshould be considered in future efforts to address andmitigate the byproduct toxicity problems.

5.4. Efficiency and Scaleup Issues. The ultrasonicsystem transforms electrical power into vibrational orultrasonic energy, i.e., mechanical energy.31-32 160-161

This mechanical energy is then transmitted into thesonicated reaction medium. The efficiency of the energytransformation depends not only on the equipment itselfbut also on the ultrasonication conditions. Therefore,the amount of acoustic energy delivered into the liquidmedium cannot be measured solely by measuring theamount of electrical energy expended to produce themechanical vibration. Sonolysis is relatively inefficientwith respect to total input energy. This is because partof the total energy input is lost to produce heat andanother part produces cavitation. But not all of thecavitational energy produces chemical and physical

Ind. Eng. Chem. Res., Vol. 40, No. 22, 2001 4709

effects. Some energy is consumed in sound re-emission(i.e., harmonics and sub-harmonics).32,57 The low ef-ficiency of the conversion sequence electrical energy facoustic energy f chemical effects may preclude the useof this method as a primary treatment. As illustratedby Kotronarou et al.,131 the limitation of sonolysis forthe control of H2S and other trace contaminants inwater is that it is relatively inefficient with respect tothe energy input. Their calculations indicated only asmall portion of the total energy supplied to the systemresulted in “useful” free-radical reactions. The energytransformation losses within the system are shown inFigure 2. At each stage in the transmission of power,there is an inefficiency whereby sonochemical benefitis lost to heat or sound. Hence, it can be appreciatedthat the determination of an energy balance is not easy.The sonochemical yield (SY ) measured effect/inputpower (W)) is measured in moles of products generatedper second. Despite the difficulty in ascertaining ac-curate energy balance, “SY” is defined in general thisway similar to the definition of “photochemicalyield”.31,32,162 Hence, the acoustical power transferredto the reaction mixture is less than the overall powerinput into the power generators (i.e., the power drawnfrom the wall supply). The challenge is to harness theseenergy losses to useful purposes, e.g., pollution treat-ment. In addition to knowledge of the characteristics ofthe reaction mixtures and kinetics of reaction, effectivescaleup procedure is necessary and requires that allparameters affecting cavitation efficiency be studiedwell, properly quantified and optimized.

The majority of the reported studies to date employedlaboratory-scale piezoelectric probe (0.25-0.5 in.) batchreactors with small volumes (20-200 mL) for ultrasonicdegradation of pollutants45,160 The probe type reactoris widely used due to its ability to deliver high poweroutput and the ease of operation to give optimumperformance at different amplitudes. However, Kotron-arou and Hoffmann111,132 found that the same energyinput dispersed over a broader area resulted in asignificant enhancement in reaction rate and energyutilization efficiency. It was also shown that sonolysisreactors with larger radiating surfaces are more energyefficient the direct immersion probe reactor, which hasa small (1 cm2) radiating surface. In addition to the low-energy utilization efficiency, the probe type reactor

system is also not an optimal reactor configuration forthe efficient generation of transient cavitation for twoother reasons. First, sonication efficiency is reduced dueto blanketing effect caused by intense generation ofcavitation bubbles at the tip. Second, the probe typetransducer tips have relatively short life before thetitanium tip requires replacement. For these reasons,the application of direct probe sonolysis to specialapplications such as groundwater remediation or pre-treatment of industrial hazardous wastes is not eco-nomically feasible. In their studies of H2S ultrasonicoxidation, Hoffmann and co-workers131,132 found a directlinear relationship between the applied power at a fixedfrequency and the observed rate of loss of S(-II),indicating a continuous-flow stirred-tank probe reactorcould attain significant conversion efficiencies. Theirinitial tests indicated that the use of large high-poweredsonicators in the CSTR mode could result in viabledegradation efficiencies. Hua et al.77 found that a near-field acoustical processor or NAP (where liquid flowsbetween two high intensity vibrating plates) was moreefficient than a probe reactor for the degradation ofp-nitrophenol. They observed that NAP provided about1.5 times the power per unit volume of the probe reactorbut resulted in 19 times more p-nitrophenol destructionper kilojoule energy imparted on the system. It was alsoshown that the G value for the probe reactor is ap-proximately 1 order of magnitude less than that in theNAP, although the degradation rate constants were thesame magnitude. The G value is an efficiency measureused in radiation chemistry and for each species inneutral water is defined as the number of moleculesundergoing reaction for each 100 eV electrical energytransferred.25 The NAP parallel-plate reactor allows fora lower sound intensity but a higher acoustical powerper unit volume than those of the conventional probe-type reactor. However, limited work has been reportedon the NAP and tank reactors, and comparison of theirperformance data with the probe reactor are scarce.Gondrexon et al.116 observed a conversion rate forpentachlorophenol (PCP) up to 80% using a three-stagelaboratory-scale sonochemical reactor (each equippedwith 500 kHz piezoelectric disk) and operating in thecontinuous flow mode. Operation in continuous-flowmode also has the advantage of short residence time,especially for pollutants that are degraded quickly.

Figure 2. Energy conversion in sonochemical processes.

4710 Ind. Eng. Chem. Res., Vol. 40, No. 22, 2001

However, as they indicated, the scaleup of such anexperimental system would not be easy, and a lot oftechnical problems remain to be overcome. But increas-ing commercial interest in sonochemical processesshould reduce cost in the very near future. Problemsrelated to technical-scale application and implementa-tion of sonochemical steps into conventional watertreatments must be considered in future investiga-tions.31,32,160

6. Concluding Remarks

Ultrasonic irradiation shows promise and has thepotential for use in environmental remediation due theproduction of high concentrations of oxidizing speciessuch as •OH and H2O2 in solution and localized transienthigh temperatures and pressures. In terms of conven-ience and simplicity of operation, sonolysis could proveto be economically competitive and far superior to manyalternative approaches. These include high-temperaturecatalytic combustion or incineration, activated carbonor zeolite adsorption, supercritical fluid extraction oroxidation, substrate-specific biodegradation, membraneseparation, electron-beam irradiation, UV-photolytic,and other chemical degradation methods.26,163-164 Someof these techniques are cost-intensive and requiretransference of the target molecule from an aqueousphase. Biodegradation provides a promising method forenvironmental remediation. However, currently avail-able processes are slow and produce unpredictableresults. Aerobic biological oxidation is also limited whenthe feed is either recalcitrant to bidegradation, orinhibitory or toxic to the bioculture.164 The sonochemicalapproach also has the advantage of being adaptable tomixed solid-liquid wastes. Ultrasonic degradation isseveral times (about 10 000-fold) faster than naturalaerobic oxidation, for example.115 Also, sonochemicaldegradation occurs over wide range concentrations(varying by order of magnitude), unlike certain biologi-cal systems that are inhibited by relatively low sub-strate concentrations. In a recent economic analysis ofa dilute p-nitrophenol aqueous waste treatment, the costof sonochemical oxidation was found to be comparableto that of incineration.77 The relative efficiency ofultrasound in terms of p-nitrophenol degraded per literof water was also shown to be far superior to conven-tional UV-photolytic degradation.58 Calculated G valueefficiencies from the literature also indicate sonochemi-cal systems are competitive with other AOPs such asUV photocatalysis and supercritical water oxida-tion.87,163,165 Sonolysis does not require the addition ofchemical additives to achieve viable degradation rates.However, some chemicals may be utilized as an effectivesonolytic catalyst for reactions involving ‚OH radical forexample.

As obvious from the degradation products in Table 3,complete mineralization of recalcitrant pollutant isdifficult to obtain at reasonable rates with ultrasoundalone. Because the efficiency of electrical-to-sound-to-thermal conversion is poor, even faster decompositionis needed to carry out the oxidation at the commerciallevel. Moreover, other barriers remain to the large-scaleimplementation of this technology for pollution degra-dation. The economics are poorly understood. Thescaleup of sonochemical reactors remains problematicbecause few studies have been done to determine whichmeasures of reactor efficiency correlates best withpollutant destruction rates. Several studies have noted

the change in biodegradability of a waste subjected toprior chemical oxidation.164 Integration of destructiveprocesses for recalcitrant or inhibiting contaminantconversion is advantageous conceptually. However,substantial research efforts are needed to developefficient processes through coupling of biological ap-proaches with chemical and physical treatments. Thedesign key for such a coupled system lies in choosingprocesses that complement each other and leads to asynergistic effect. Sonochemical oxidation technologiesare most advantageously used in combination with otheradvanced oxidation processes and/or biological treat-ment.

Ultrasound has other environmental science andengineering applications. Low permeability geomateri-als such as clay or silt are difficult to remediate becauseof low transport rates and high adsorption potential. Ithas been shown that ultrasonic vibrations enhanceremoval of volatile organic compounds (VOCs) andliquid contaminants from low permeability geologicformations that have been pneumatically or hydrauli-cally fractured.166 Mukherjee et al.167 and Liu et al.168

also showed that sonication could be used as a pretreat-ment step to improve the release of organic matterassociated with the particulate phase into the solubleaqueous phase enhancing its bioavailability during theanaerobic biodegradation of aquatic sediments. Also, inthe desorption of phenol from activated carbon andpolymeric resin, Rege et al.169 found sonication at 40kHz and 1.44 MHz to significantly increase desorptionrates, and the rates were also favored by decreasedtemperature, aerated medium, and increased ultrasonicintensity. They also found desorption rates in theabsence of ultrasound was limited by pore diffusion,whereas those under ultrasonic irradiations were lim-ited by surface reaction. The improvement in desorptionrates were attributed to an enhancement in diffusionaltransport due to the acoustic microstreaming causedwithin the pores.

The amount of things that can be accomplished withsonochemistry is, at this stage, only limited by theminds of those working in this exciting field. It is awhole new field of research that is growing very fast,with exciting prospect for any researcher. The reviewof the environmental aspects of sonochemistry high-lighting remediation processes, reaction pathways, andkinetic studies presented here indicates a large scopefor further experimental and theoretical investigationson all aspects of this important medium of reaction.More research and developmental studies, both experi-mental and theoretical and encompassing kinetics,reaction mechanisms, reactor design, and energy con-servation, are needed to improve reliability and mini-mize costs for scale-up and long-term use.170-172 De-staillat et al.173 demonstrated the effectiveness of a novelpilot-plant scale sonochemical reactor (UES 4000CPilotstation) recently developed for large-scale reme-diation applications. A budget analysis of this system(612 kHz, 3 kW) indicated that nearly one-third of theapplied power is converted into sonochemical activity.It is hoped that this review has stimulated thinkingbeyond the cases presented and should spur futureengineering-based research in the continued use ofsonochemical oxidation as an environmentally benignprocess for the removal of inorganic and organic speciesfrom industrial wastewater streams and remediation ofcontaminants in subsurface environments.

Ind. Eng. Chem. Res., Vol. 40, No. 22, 2001 4711

Acknowledgment

The author thanks Air Force Office of ScientificResearch (Grant. No. F.49620-95-1-0541) and Depart-ment of Energy (Grant No. DE-FC04-90AL66158) forfinancial support.

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Received for review January 30, 2001Revised manuscript received July 18, 2001

Accepted August 13, 2001

IE010096L

Ind. Eng. Chem. Res., Vol. 40, No. 22, 2001 4715