Porous Structure of Waste f Ly Ashes and Their Chemical Modifications

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    .Powder Technology 123 2002 5358

    www.elsevier.comrlocaterpowtec

    Porous structure of waste fly ashes and their chemical modifications

    Z. Sarbak), M. Kramer-Wachowiak

    Faculty of Chemistry, Adam Mickiewicz Uniersity, Grunwaldzka 6, 60-780 Poznan, Poland

    Received 1 December 2000; received in revised form 1 March 2001; accepted 6 July 2001

    Abstract

    Changes in the porous structure of fly ashes ZS-13 subjected to chemical treatment with solutions of NaOH, NaOH rNH HCO ,4 3

    EDTA, and HCl are examined. The initial material with 3 m2rg surface area and 0.01 cm3rg pore volume after modification revealed an

    increased surface area and pore volume. The greatest increase in the surface area equal to 105 m 2rg was noted for the sample treated

    with HCl, while the greatest increase in pore volume equal to 0.18 cm3rg was obtained for the sample treated with EDTA. In the

    modified products, meso- and macropores prevail, although in the sample treated with HCl, the presence of a small contribution of

    micropores was detected. All the modifications, except that treated with HCl, were found to contain slit-shaped macropores. In the sample .treated with HCl, the pores were in the shape of nonparallel plates. A study by scanning electron microscopy SEM allowed a detailed

    determination of the shape of the isles and agglomerates. Chemical treatment of the initial fly ashes resulted in a transformation of the

    ball-shaped agglomerations into different products characterised by specific size and shape of particles. q2002 Elsevier Science B.V. All

    rights reserved.

    Keywords: Fly ashes; Chemical treatment; BET; Pore size; Pore volume; SEM

    1. Introduction

    Fly ashes are waste products of coal combustion in

    electric and thermal power plants. The ashes are capturedelectrostatically in electrofilters or mechanically by cy-

    clones and then they are deposited directly into ponds or

    landfills, where they can become hazardous to the environ-w xment 1 .

    Fly ashes are oxides whose composition depends on the

    type of coal subjected to combustion and the combustion

    conditions. The main components of ashes are mineralsw xsuch as kaolinite, mullite, quartz, calcite, and pyrite 2 .

    High contents of silicates and aluminasilicates suggest

    their susceptibility to transformation into zeolite-like crys-w xtalline materials as a result of chemical treatment 3 6 . It

    is also expected that the obtained materials may be effi-w xcient adsorbents of environmental pollutants 7 .

    The aim of the present study is to determine changes in

    the surface area and porous structure of fly ashes from .Konin Power Plants Poland firing brown coal and their

    chemical modifications with different chemical agents.

    )

    Corresponding author. .E-mail address:[email protected] Z. Sarbak .

    2. Experimental

    The study was performed on fly ash denoted by the

    symbol ZS-13 from the Konin Power Plant combustingbrown coal.

    2.1. Modification of fly ashes

    Twenty grams of fly ash from the Konin Power Plant

    was mixed with 160 cm3 3.5 M solution of NaOH and

    heated in a water bath under reflux at 90100 8C for 24 h,

    and then filtered off and washed with distilled water until

    pHs 7. The obtained material was dried at 120 8C for

    12 h.

    The same procedure was applied to obtain other modifi-

    cations of ashes using 160 cm3 3.5 M solution of NaOH

    and 0.015 molar equivalent of NH HCO , 200 cm3 2.5 M4 3solution of HCl, and 0.05 molar equivalent of EDTA in

    100 cm3 of water.

    2.2. Chemical analysis

    Chemical analysis was performed on a solution ob-

    tained after melting the sample in a Philips type PW 2400

    fluorescence X-ray spectrometer.

    0032-5910r02r$ - see front matter q2002 Elsevier Science B.V. All rights reserved.

    .P II: S 0 0 3 2 -5 9 1 0 0 1 0 0 4 3 1 -4

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    Table 1

    Chemical composition of ZS-13 fly ashes

    .Component Content wt.%

    SiO 27.372Al O 6.632 3Fe O 3.752 3TiO 0.962MgO 8.23

    CaO 34.48

    Na O 1.082K O 0.412

    2.3. X-ray diffraction studies

    Diffractograms of the starting material and the obtained

    modifications were made on a TUR M-62 diffractometer .using CuK radiation and Ni filter ls 1.5418 A .a

    2.4. Infrared spectroscopy studies

    The studies were performed on a Perkin-Elmer Model

    180 spectrometer within the range of 1800400 cmy1,

    using a 1.5-mg sample mixed with 200 mg of KBr andpressed into a thin transparent tablet.

    ( )2.5. Scanning electron microscopy SEM

    Microscopic observations were made using a Philips

    type SEM 515 scanning electron microscope at the acceler-

    ating voltage 15 kV. At the first stage, a suspension of the

    samples was made and the smear was covered with a thin

    film of gold in the atmosphere of argon, in Balzers type

    SCD 050 evaporator.

    2.6. Surface area and pore characterisation

    To determine the surface area, specific volume, and

    mean pore radius, the samples were first degassed at 350

    8C and then subject to N adsorption using BET method.2The study was performed using a Sorptometer ASAP 2010

    made by Micromeritics.

    3. Results and discussion

    Results of the chemical analyses of the initial fly ash

    ZS-13 are shown in Table 1.

    Table 2The effect of chemical modifications of ZS-13 fly ashes on the pore

    properties and surface area

    Chemical BET surface Mean pore Pore volume2 3 . . .treatment area m rg radius A cm rg

    None 3 34 0.01

    NaOH 59 48 0.14

    NaOHr 60 43 0.13

    NH HCO4 3EDTA 60 50 0.18

    HCl 105 17 0.10

    Fig. 1. Pore volume distribution as a function of the pore radius for fly

    ash ZS-13.

    According to the calculations carried out from chemical

    analyses, the molar ratio of SiO rAl O was equal to2 2 3 . 7.02, whereas that of SiO q Al O r Ca q MgO q2 2 3

    .Fe O was equal to 0.62, which indicates that the ashes2 3belong to the calciumsilica class.

    Modification of the ash with the solutions mentioned

    above brings a change in many textural parameters. Table

    2 gives the pore and surface area characteristics of the

    chemically amended fly ash. In all instances, the surface

    area of the chemically amended fly ash is greater than in

    Fig. 2. Pore volume distribution as a function of the pore radius for fly

    ash ZS-13 modified with NaOH solution.

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    Fig. 3. Pore volume distribution as a function of the pore radius for fly

    ash ZS-13 modified with NaOHrNH HCO solution.4 3

    .the unmodified ash ZS-13 . The greatest increase in the

    surface area is observed for the ashes subjected to the

    modification by hydrochloric acid. This modification also

    resulted in the lowest mean pore radius, which is about

    twice as small as that of the initial ash. Chemical modifica-

    tion by the other solutions leads to a smaller increase in

    the mean pore radius. A more dramatic influence of chemi-

    cal modification is a large increase, 10-fold or even greater,

    in the pore volume. The greatest pore volume increase was

    noted for the sample modified by the EDTA solution. For

    Fig. 4. Pore volume distribution as a function of the pore radius for fly

    ash ZS-13 modified with EDTA solution.

    Fig. 5. Pore volume distribution as a function of the pore radius for fly

    ash ZS-13 modified with HCl solution.

    this sample, the pore radius was also the largest. The

    sample ZS-13 HCl showing the greatest surface area was

    characterised by the smallest mean pore radius and the

    smallest pore volume of all chemically modified samples.

    This means that the sample has a much greater amount of

    micropores than the other modifications.

    A low surface area and small pore volume of the initial

    ash at a relatively large mean pore radius indicates thepresence of meso- pore radius between 10 and 250 A, 10

    . .As 1 nm and macropores pore radius exceeding 250 Aw xaccording to IUPAC 8 classification. This supposition is

    . .Fig. 6. Nitrogen adsorption x and desorption o isotherms for fly ash

    ZS-13.

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    . .Fig. 7. Nitrogen adsorption x and desorption o isotherms for fly ash

    ZS-13 modified with NaOH solution.

    confirmed by the dependence of the volume of the ad- .sorbed nitrogen versus the pore radius Figs. 1 5 . In this

    modification, the dominant pores have a radius of 20 A. Asimilar conclusion has been drawn on the initial prepara-

    tion ZS-13, in which mesopores of the radius 20 A occurin abundance. The samples obtained as a result of modifi-

    cation with the solutions NaOH and NaOHrNH HCO4 3have the maximum contribution of pores of the radii 20

    and 100 A. In the sample modified with EDTA, themaximum contribution of the mesopores of the radii 20

    and 35 A was established.In our opinion, a greater surface area and volume of

    pores in the samples modified with NaOH solution is

    . .Fig. 8. Nitrogen adsorption x and desorption o isotherms for fly ash

    ZS-13 modified with NaOHrNH HCO solution.4 3

    . .Fig. 9. Nitrogen adsorption x and desorption o isotherms for fly ash

    ZS-13 modified with EDTA solution.

    mainly a consequence of conversion of fly ashes into

    zeolite-like structures. A similar conclusion follows fromw xthe study by Howden 9 , who reported that the treatment

    .of kaolinite a component of fly ashes with this solution

    results in the formation of zeolite structures. The increase

    in the parameters discussed upon the treatment with HCl

    and EDTA solutions is related to the process of dealumina-

    tion. The course of this process in the case of syntheticw xsilicaalumina was described by Scherzer 10 .

    The isotherm of nitrogen adsorption obtained for the .initial ash ZS-13 Fig. 6 can be classified as type II in the

    w xIUPAC 8 classification. This kind of isotherm corre-

    . .Fig. 10. Nitrogen adsorption x and desorption o isotherms for fly ash

    ZS-13 modified with HCl solution.

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    sponds to the situation when at relatively low pressures, a

    monolayer of nitrogen is formed, and at relatively high

    pressures, a nitrogen multilayer is formed. This character

    of the isotherm is typical of macroporous materials. The

    small surface area and low pore volume at a relatively

    large mean pore radius indicates that the fly ash tested has

    a macroporous structure. The fact that the hysteresis loop

    begins at relatively low pressures also implies a small

    contribution of micropores. The hysteresis loop can beclassified as H3 type, which means the overwhelming

    w xpresence of slit-shaped pores 11 .

    The adsorption isotherms and hysteresis loops obtained

    for the samples modified with NaOH and NaOHrNH 4 .HCO Figs. 7 and 8 are similar and can be classified as3

    types II and H3, respectively. For the sample modified .with EDTA Fig. 9 , the shape of the isotherm is similar

    .type II , but the hysteresis loop, although also of type H3,

    is much broader. A different character of the nitrogen

    adsorption isotherm is observed for the sample ZS-13 HCl

    .Fig. 10 . Its adsorption significantly increases at relativelylow pressure, which means that the number of micropores

    in this sample is much higher than in the sample ZS-13.

    . . . .Fig. 11. Scanning electron micrographs of a fly ashes ZS-13 modified with: b NaOH solution, c and d NaOHrNH HCO solution, e HCl solution4 3 .and f EDTA solution.

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    The isotherm can be classified as type I with an admixture

    of type II, which corresponds to microporous adsorbents,

    e.g. zeolite-like crystalline solids, containing some macro-

    pores. The hysteresis loop looks like type H4 characteristic

    of the adsorbents with the pores formed by nonparallelw xplates 11 . A comparison of our results concerning the

    surface area and porous structure of the material studied

    with literature data is impossible because of the lack of the

    latter.SEM observations proved the presence of well-devel-

    oped particles in the shape of rather smooth balls of the

    diameter of 24 mm and sometimes even 7 mm, in the .initial fly ashes Fig. 11a . Moreover, the occurrence of

    scarce agglomerates of amorphous particles, of approxi-

    mately 46 mm in size, was noted.

    After exposure to a solution of sodium hydroxide, the

    smooth balls become objects of deformed ball-like shape .Fig. 11b , sizes 45 or 1012 mm, with numerous plates

    on the surface, which testifies to the occurrence of crys-

    tallisation. Individual particles were found with well-devel-

    oped smooth walls. In the background, there were numer-

    ous small particles of the size about 5 mm, as well as a

    number of short fibres of about 3 mm in length. Exposition

    of the fly ashes to solutions of sodium hydroxide and .sodium bicarbonate Fig. 11c and d causes a transforma-

    tion of the ball-shaped agglomerations into large particles

    of the size of 1012 mm, with well-developed plates on

    the surface.

    The effect of HCl brings about a transformation of the

    majority of ball-shaped particles into agglomerations of .undefined shape Fig. 11e . The observations also revealed

    a formation of a single crystal in the form of a rod of the

    size 7=15 mm. When EDTA was used for chemical

    .modification of the ashes, SEM Fig. 11f shows that onlyscarce ball-shaped particles remained, while the majority

    were transformed into numerous pillars of the size 6=1.2mm and individual cubic crystals with rounded edge 3=3

    .mm .

    As follows from the above data, each of the procedures

    of chemical modification, transforms the fly ashes ZS-13

    into a different product characterised by specific shape and

    size of particles. It should be emphasised that the fly ashes

    differ depending on the kind of combusted coal and com-

    bustion conditions. Therefore, a comparison of selected

    texture parameters seems pointless.

    4. Conclusions

    Chemical treatment of the initial fly ashes ZS-13 char-

    acterised by 3 m2rg surface and 0.01 cm3rg pore volume

    leads to an increase in their surface area and pore volume.

    The greatest pore volume of 0.18 cm3rg occurs for the

    sample treated with the EDTA solution, whereas the great-

    est surface area of 105 m2rg was observed for HCl

    modification. The sample ZS-13 HCl reveals a relatively

    large contribution of micropores when compared to the

    initial fly ashes but do not occur in the other samples. The

    shape of the adsorption isotherms and hysteresis loop

    suggests that the sample ZS-13 contains mainly slit-shaped

    macropores. Similar pores were found in the other samples

    except ZS-13 HCl, in which micro- and macropores of the

    shape of nonparallel plates were found.

    The modification with solutions of NaOH, NaOHrNH HCO , and EDTA leads to obtaining of new materials4 3characterised by greater surface area than that of the initial

    fly ashes, which is of about 60 m2rg.

    According to the results of the SEM study, the sample

    ZS-13 reveals the presence of well-developed particles in

    the shape of smooth balls of a diameter of 24 mm, which

    under the influence of NaOH treatment, undergo deforma-

    tion and numerous plates and short fibres appear on their

    surface. The chemical treatment with NaOHrNH HCO4 3solution leads to the appearance of large particles of the

    size of 1012 mm with well-developed plates. The modifi-

    cation with EDTA leads to a transformation of the ball-

    shaped particles into numerous pillars. The treatment with

    HCl resulted in the appearance of agglomerations of unde-

    fined shape.

    In the aspect of future application of these materials as

    adsorbents, catalysts, or their supports, it seems that all the

    above-described modifications can find appropriate use

    This conclusion is justified by the facts that chemical

    modifications of the ashes have led to a significant in-

    crease in the surface area, mean pore size, and transforma-

    tion of ball-shaped structure of the initial ash ZS-13 into

    crystalline structures observable under a scanning electron

    microscope.

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