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ALGINATE BASED ENCAPSULATION OF MICROBIAL GRANULES AS A PROTECTIVE MEANS TO REDUCE STRESS DURING ANAEROBIC DIGESTION Karlien Springael Student number: 01405489 Promotor(s): Prof. dr. ir. Nico Boon, Dr. ir. Jo De Vrieze Tutor: Eng. Cindy Ka Y Law Master’s Dissertation submitted to Ghent University in partial fulfilment of the requirements for the degree of Master of Science in Bioscience Engineering: Cell and Gene Biotechnology Academiejaar: 2018 - 2019

ALGINATE BASED ENCAPSULATION OF MICROBIAL GRANULES …€¦ · alginate based encapsulation of microbial granules as a protective means to reduce stress during anaerobic digestion

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Page 1: ALGINATE BASED ENCAPSULATION OF MICROBIAL GRANULES …€¦ · alginate based encapsulation of microbial granules as a protective means to reduce stress during anaerobic digestion

ALGINATE BASED ENCAPSULATION

OF MICROBIAL GRANULES AS A

PROTECTIVE MEANS TO REDUCE

STRESS DURING ANAEROBIC

DIGESTION

Karlien Springael Student number: 01405489

Promotor(s): Prof. dr. ir. Nico Boon, Dr. ir. Jo De Vrieze

Tutor: Eng. Cindy Ka Y Law

Master’s Dissertation submitted to Ghent University in partial fulfilment of the requirements for the

degree of Master of Science in Bioscience Engineering: Cell and Gene Biotechnology

Academiejaar: 2018 - 2019

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De auteur en de promotoren geven de toelating deze scriptie voor consultatie beschikbaar te stellen en delen van de scriptie te kopiëren voor persoonlijk gebruik. Elk ander gebruik valt onder de beperkingen van het auteursrecht, in het bijzonder met betrekking tot de verplichting de bron uitdrukkelijk te vermelden bij het aanhalen van resultaten uit deze scriptie.” “The author and the promotors give the permission to use this thesis for consultation and to copy parts of it for personal use. Every other use is subject to copyright laws, more specifically the source must be extensively specified when using the results from this thesis.”

Ghent, 7th June, 2018

The promotors, The tutor, The author,

Prof. dr. ir. Nico Boon Eng. Cindy Ka Y Law Karlien Springael

Dr. ir. Jo De Vrieze

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ACKNOWLEDGEMENT - DANKWOORD

Met pijn in het hart neem ik na 5 jaar afscheid van het prachtige Boerekot, waar ik onvergetelijke

momenten heb beleefd en vrienden voor het leven heb gemaakt. Het laatste jaar, hét thesisjaar, was

er eentje met veel ups, maar ook wel met een paar stevige downs. Overgestroomde reactoren, kapotte

gastellers, gaslekken, … ze zijn allemaal de revue gepasseerd. Toch was het een jaar waarin ik enorm

veel heb bijgeleerd en dat ik bijgevolg met veel trots kan afsluiten.

Eerst en vooral wil ik Jo De Vrieze bedanken voor al de tijd die hij, ondanks zijn drukke agenda, voor

mij heeft vrijgemaakt. Zijn vindingrijkheid, positieve ingesteldheid en kritische kijk op de zaken hebben

er mee voor gezorgd dat ik deze thesis uiteindelijk mooi kan afronden. Ook Cindy wil ik in het bijzonder

bedanken omdat ik altijd op haar kon rekenen en omdat ze altijd met veel enthousiasme voor me klaar

stond. Ook wil ik mijn promotor Prof. dr. Ir. Nico Boon bedanken die mij de kans heeft gegeven om

mijn thesisonderzoek hier bij CMET uit te voeren.

Bedankt ook aan het hele CMET-team voor het creëren van een amicale werksfeer in een leuke

omgeving. Als ik vragen had, stond er altijd wel iemand klaar in het labo om me met de glimlach verder

te helpen. Wie ik in dit dankwoord ook zeker niet mag vergeten, zijn de mensen die in de K32 stonden

en er steeds weer voor zorgden dat ik elke dag met plezier naar het labo kwam.

Tot slot wil ik mijn mama en papa danken omdat ze er steeds weer stonden om me door de moeilijkere

periodes te helpen. Als ik in de vijf jaar al eens een dipje had, zorgden zij er telkens voor dat ik de moed

er inhield en doorbeet. Ook mijn beste vriendinnen en mijn vriend moet ik danken voor hun

vriendschap en geduld. En om af te sluiten wil ook nog Dominique danken voor haar zeer

gewaardeerde Engelse taaltips en -adviezen.

En zoals Madeleine Ferron zo mooi zei:

‘Pour réussir il ne suffit pas de continuer, il faut toujours se dépasser’

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CONTENT LITERATURE STUDY ........................................................................................................................... 1

1 Anaerobic digestion ......................................................................................................................... 1

1.1 Introduction ............................................................................................................................. 1

1.2 Anaerobic digestion process ................................................................................................... 1

1.3 Microbial population ............................................................................................................... 2

1.3.1 Hydrolytic-acidogenic bacteria ........................................................................................ 2

1.3.2 Acetogenic bacteria ......................................................................................................... 3

1.3.3 Methanogenic archaea .................................................................................................... 3

1.4 Different types of waste streams ............................................................................................ 4

1.4.1 Industrial waste streams ................................................................................................. 4

1.4.2 Manure ............................................................................................................................ 5

1.4.3 Energy crops and agricultural waste ............................................................................... 5

1.4.4 Municipal waste .............................................................................................................. 5

1.5 Control of anaerobic digestion ................................................................................................ 5

1.5.1 Effect of pH ...................................................................................................................... 5

1.5.2 Effect of temperature ...................................................................................................... 6

1.5.3 Effect of organic loading rate .......................................................................................... 6

1.5.4 Essential growth factors .................................................................................................. 6

1.6 Inhibitors of the anaerobic digestion process ......................................................................... 7

1.6.1 Sulfate and sulfide ........................................................................................................... 7

1.6.2 Long chain fatty acids ...................................................................................................... 8

1.6.3 Ammonium and ammonia ............................................................................................... 8

1.6.4 Salt ................................................................................................................................... 9

1.6.5 Trace elements ................................................................................................................ 9

2 Anaerobic granulation technology ................................................................................................ 10

2.1 Introduction ........................................................................................................................... 10

2.2 Anaerobic granulation reactor technologies ......................................................................... 10

2.2.1 Continuous stirred tank reactor (CSTR) ......................................................................... 10

2.2.2 Upflow anaerobic sludge blanket reactor (UASB) ......................................................... 11

2.2.3 Expanded granular sludge bed reactor (EGSB) .............................................................. 12

2.2.4 Internal circulation reactor (IC) ..................................................................................... 12

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2.3 Anaerobic granulation theories ............................................................................................. 13

2.3.1 Structural models .......................................................................................................... 13

2.3.2 Thermodynamic models ................................................................................................ 16

2.3.3 Proton translocation dehydration theory ..................................................................... 17

2.4 Parameters influencing anaerobic granulation ..................................................................... 18

2.4.1 Reactor temperature ..................................................................................................... 18

2.4.2 Reactor pH ..................................................................................................................... 18

2.4.3 Characteristics of seed sludge ....................................................................................... 18

2.4.4 Upflow velocity and hydraulic retention time............................................................... 19

2.4.5 Organic loading rate ...................................................................................................... 19

2.4.6 Wastewater composition/characteristics of substrate ................................................. 19

2.4.7 Addition of natural and synthetic polymers .................................................................. 20

2.4.8 Addition of cations ........................................................................................................ 20

MATERIAL AND METHODS .......................................................................................................... 21

1 Experimental approach ................................................................................................................. 21

2 Experimental set-up and operation .............................................................................................. 22

2.1 Reactor set-up ....................................................................................................................... 22

2.2 Feedstock............................................................................................................................... 23

2.2.1 Start-up .......................................................................................................................... 23

2.2.2 Experiment 1 ................................................................................................................. 23

2.2.3 Experiment 2 ................................................................................................................. 23

2.2.4 Experiment 3 ................................................................................................................. 23

2.3 Sludge inoculum .................................................................................................................... 24

2.3.1 Start-up .......................................................................................................................... 25

2.3.2 Experiment 1 ................................................................................................................. 25

2.3.3 Experiment 2 ................................................................................................................. 25

2.3.4 Experiment 3 ................................................................................................................. 25

2.4 Volumetric methane production and methane yield ............................................................ 26

3 Analytical techniques .................................................................................................................... 26

3.1 Total Kjeldahl nitrogen .......................................................................................................... 26

3.2 total ammonia nitrogen ........................................................................................................ 27

3.3 Total suspended solids and volatile suspended solids .......................................................... 27

3.4 Total solids and volatile solids ............................................................................................... 28

3.5 pH .......................................................................................................................................... 28

3.6 Chemical oxygen demand ..................................................................................................... 29

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3.7 Biogas composition ............................................................................................................... 29

3.8 Volatile fatty acids ................................................................................................................. 29

3.9 Cations ................................................................................................................................... 30

3.10 Anions .................................................................................................................................... 30

4 Biochemical methane potential (BMP) test .................................................................................. 30

5 Batch tests ..................................................................................................................................... 31

5.1 Shear stress batch test .......................................................................................................... 31

5.2 Potassium and phosphate batch test .................................................................................... 32

RESULTS ............................................................................................................................................. 33

1 Characterization of inoculum ........................................................................................................ 33

2 Characterization of molasse .......................................................................................................... 33

3 Start-up .......................................................................................................................................... 34

4 Reactor experiments ..................................................................................................................... 36

4.1 Disintegration of the alginate matrix .................................................................................... 36

4.1 pH .......................................................................................................................................... 38

4.2 Volatile fatty acids ................................................................................................................. 39

4.3 Volumetric methane production ........................................................................................... 40

4.4 Methane yield ....................................................................................................................... 42

4.5 Cations ................................................................................................................................... 43

5 Biochemical methane potential (BMP) test .................................................................................. 44

6 Batch test ....................................................................................................................................... 45

6.1 Shear stress batch test .......................................................................................................... 45

6.2 Potassium and phosphate batch test .................................................................................... 45

DISCUSSION ...................................................................................................................................... 47

1 Disintegration of the alginate matrix ............................................................................................ 47

1.1 Disintegration due to degradation by the microbial biomass ............................................... 48

1.2 High concentrations of Na+ cause swelling and consequently disintegration ...................... 48

1.3 Shear stress accelerates the disintegration as a result of microbial degradation ................ 49

2 Characteristics of the encapsulated sludge ................................................................................... 50

2.1 pH of the encapsulated sludge .............................................................................................. 50

2.2 Methane production of the encapsulated sludge ................................................................. 51

2.3 Elevated Ca2+ levels in the reactor containing the encapsulated sludge ............................... 52

CONCLUSION AND FUTURE PERSPECTIVES ............................................................................. 55

BIBLIOGRAPHY ................................................................................................................................. 57

APPENDIX 1: ANION AND CATION COMPOSITION OF SYNTHETIC MEDIUM 1 AND 2 .................... 67

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APPENDIX 2: CALCULATIONS OF COD OF ALGINATE ....................................................................... 69

APPENDIX 3: CATION CONCENTRATIONS OF THE THREE EXPERIMENTS ......................................... 71

APPENDIX 4: REPLICATES SHEAR STRESS BATCH TEST ...................................................................... 73

APPENDIX 5: REPLICATES POTASSIUM AND PHOSPHATE BATCH TEST ............................................ 79

APPENDIX 6: COMPARISON BETWEEN SHEAR STRESS BATCH TEST AND POTASSIUM PHOSPHATE

BATCH TEST ........................................................................................................................................... 83

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TABLE OF ABBREVIATIONS

AD Anaerobic digestion

BMP Biomethane potential

CMC Carboxymethylcellulose

COD Carbon oxygen demand

CSTR Continuous stirred tank reactor

DLVO Derjaguin-Landau-Verwey-Overbeek

DS Degree of substitution

ECP Extracellular polymers

EGSB Expanded granular sludge bed

FA Free ammonia

FID Flame ionization detector

G Guluronate

HRT Hydraulic retention time

IC Internal circulation

IC Ion chromatograph

LCFA Long chain fatty acids

M Mannuronate

MSW Municipal solid waste

OHPA Obligatory H2-producing acetogenic bacteria

OLR Organic loading rate

Rpm Rounds per minute

SAB Syntrophic acetogenic bacteria

SAOB Syntrophic acetate oxidizing bacteria

SEM-EDS Scanning electron microscopy - energy dispersive microscopy

SMA Specific methanogenic activity

SRB Sulphate reducing bacteria

SRT Solid retention time

STP Standard temperature and pressure

TAN Total ammonia nitrogen

TKN Total Kjeldahl nitrogen

TS Total solids

TSS Total suspended solids

UASB Upflow anaerobic sludge blanket

VFA Volatile fatty acids

VS Volatile solids

VSS Volatile suspended solids

WWTP Wastewater treatment plant

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ABSTRACT Emerging bio-refineries produce organic compounds from renewable raw materials, such as sugar beet

and energy crops, associated with the production of enormous quantities of toxic wastewaters.

However, the treatment of these wastewater via anaerobic digestion (AD) is complex. Anaerobic

digestion, especially methanogenesis, is very sensitive to different types of stress, such as salt stress,

fluctuations in pH, temperature and organic loading rate, and too high concentrations of, for example,

ammonium, sulfate and trace elements. When granular AD systems experience stress, the microbial

granules start to disintegrate, associated with the wash-out of these granules. Therefore, a new

approach of ‘granule engineering’ is applied in this thesis, in which the microbial granules are

encapsulated in an alginate matrix. If the microbial granules start to disintegrate, due to stress, the

matrix keeps the biomass close together, ensuring good settling properties and, consequently,

preventing wash-out of the granules. In this way, a robust and stress-tolerant AD process is created. In

this study, the stability of the alginate matrix to encapsulate granular sludge for the resistance towards

stress was investigated.

Two UASB reactors were run under steady state while different experiments were conducted. One

reactor contained alginate encapsulated granular sludge, while the other reactor, containing natural

granular sludge, served as a control. In the first experiment, molasse was used as influent, which

contained high concentrations of PO43-. After 10 days, the entire alginate matrix was broken down. In

the second experiment, a synthetic medium with low concentrations of PO43- and without carbon

source was used as influent. In the reactor that contained the encapsulated granular sludge, biogas

was produced, which indicated that the microbial biomass was able to degrade the alginate matrix. In

the last experiment, in which the same synthetic medium with carbon-source was used, four different

methods of encapsulation were tested, to slow down or to prevent the disintegration of the matrix.

The different methods consisted of the encapsulation with 1.3% and 1.8% alginate, the encapsulation

with a 1.3% alginate matrix mixed with glucose and the encapsulation with 0.5% alginate mixed with

carboxymethylcellulose. However, none of the methods slowed down or prevented the disintegration

of the alginate matrix.

From the aforementioned experiments, the overall performance of the encapsulated granular sludge

was also tested in terms of pH, VFA concentrations and biogas production. At the start of each

experiment, a pH drop was observed in the reactor containing the encapsulated granular sludge,

accompanied by an increase in VFA concentration. This may be explained by the longer lag-phase of

the methanogenic archaea compared to the hydrolytic, acidogenic and acetogenic bacteria. The lag-

phase also affected the methane production of the reactor containing the encapsulated sludge, which,

therefore, lags behind the control reactor. After the biomass was adapted, similar amounts of methane

production were observed among both reactors.

At the same time, the stability of the alginate matrix was tested in terms of shear stress and high PO43-

and K+ concentrations. From these batch experiments, it can be concluded that shear stress accelerates

the disintegration of the alginate matrix as a result of microbial degradation, but does not have an

effect on the stability of the alginate matrix alone. In addition, PO43- anions and K+ cations also had no

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effect, but Na+, originating from Na2HPO4, did have a great influence on the disintegration of the

alginate matrix. High concentrations of Na+ (> 100 mg/L) first cause swelling of the matrix and

consequently disintegration.

In summary, encapsulation of anaerobic granular sludge by an alginate matrix as a protective means

to reduce stress, didn’t prevent the production of biogas. However, during the AD process, the matrix

wasn’t stable enough. Therefore, future research must establish how the stability of the alginate matrix

can be increased or must consider other encapsulation matrices.

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SAMENVATTING In de nieuwste bio-raffinaderijen worden organische verbindingen aangemaakt uit hernieuwbare

grondstoffen, zoals suikerbieten en energiegewassen, waarbij enorme hoeveelheden afvalwaters

worden geproduceerd. De behandeling van dit afvalwater via anaerobe vergisting (AD - anaerobic

digestion) is echter complex. Anaerobe vergisting, met name methanogenese, is bijzonder gevoelig

voor een hele rist stressoren, waaronder zoutstress, schommelingen qua pH, temperatuur en

organische belasting, evenals te hoge concentraties van bijvoorbeeld ammonium, sulfaat en

sporenelementen. Wanneer de AD van granulair slib stress ondervindt, kunnen de microbiële granules

desintegreren, met als gevolg de uitspoeling van die granules. Daarom wordt een nieuwe benadering

van 'granule engineering' toegepast, waarbij de microbiële granules worden ingekapseld in een

alginaatmatrix. Wanneer als gevolg van stress de microbiële granules gaan desintegreren, weet de

matrix de biomassa bij elkaar te houden. Dat staat dan weer garant voor goede

bezinkingseigenschappen dat de uitspoeling van de granules voorkomt. Op deze manier wordt een

robuust en tolerant AD-proces gecreëerd. In deze studie werd de stabiliteit van de alginaatmatrix voor

het inkapselen van granulair slib in het kader van de stressbestendigheid onderzocht.

Er werden verschillende experimenten uitgevoerd in twee steady-state UASB-reactoren. In de ene

reactor zat ingekapseld granulair slib terwijl de andere, de controlereactor, natuurlijk granulair slib

bevatte. In het eerste experiment werd als influent molasse met hoge concentraties PO43- gebruikt. Na

10 dagen was de hele alginaatmatrix afgebroken. In het tweede experiment werd als influent een

synthetisch medium met lage PO43--concentraties zonder koolstofbron gebruikt. In de reactor met het

ingekapselde granulair slib werd biogas geproduceerd; wat aantoonde dat de microbiële biomassa in

staat was om de alginaatmatrix af te breken en dus als koolstofbron te gebruiken. In het laatste

experiment, waarbij hetzelfde synthetische medium met koolstofbron werd gebruikt, werden vier

verschillende inkapselingsmethoden getest om de desintegratie van de matrix te vertragen of te

verhinderen. De verschillende methoden bestonden uit de inkapseling met 1,3% en 1,8% alginaat, de

inkapseling met een 1,3% alginaatmatrix gemengd met glucose en de inkapseling met 0,5% alginaat

gemengd met carboxymethylcellulose. Geen van deze methoden vertraagde of verhinderde echter de

desintegratie van de alginaatmatrix.

Tijdens bovengenoemde experimenten werden tevens de algemene prestaties van het ingekapselde

granulair slib getest wat betreft pH, VVZ-concentraties en biogasproductie. Bij aanvang van elk

experiment werd in de reactor met het ingekapselde granulair slib een daling van de pH-waarde

waargenomen, die gepaard ging met een toename van de VVZ-concentratie. Dit kan worden verklaard

door de langere lag-fase van de methanogene archaea in vergelijking met de hydrolytische, acidogene

en acetogene bacteriën. De lag-fase had ook een impact op de methaanproductie van de reactor met

het ingekapselde slib, dat bijgevolg achter liep op de controlereactor. Nadat de biomassa zich had

aangepast, kon worden vastgesteld dat in beide reactoren vergelijkbare hoeveelheden methaan

werden geproduceerd.

Tegelijkertijd werd de stabiliteit van de alginaatmatrix getest op schuifspanning en hoge PO43- en K+

concentraties. Uit deze reeks experimenten kan worden geconcludeerd dat schuifspanning de

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desintegratie van de alginaatmatrix versnelt als gevolg van microbiële afbraak, maar geen impact heeft

op de stabiliteit van de alginaatmatrix op zich. Daarnaast hadden PO43- anionen en K+ kationen ook

geen invloed, maar Na+, afkomstig van Na2HPO4, had wel een grote impact op de desintegratie van de

alginaatmatrix. Hoge Na+ concentraties (> 100 mg/L) leiden eerst tot het zwellen van de matrix en

vervolgens tot desintegratie.

Samengevat, kan worden gesteld dat wanneer granulair slib als bescherming tegen stress in een

alginaatmatrix wordt ingekapseld, de biogasproductie niet wordt gehinderd. Wel werd aangetoond

dat de alginaatmatrix tijdens het AD-proces niet voldoende stabiel was. Bijgevolg moet verder

onderzoek aantonen hoe de stabiliteit van de alginaatmatrix naar een hoger niveau kan worden getild

of moeten andere inkapselingsmatrices worden overwogen.

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INTRODUCTION Concern for climate and the environment has become an integral part of our current society as the

numerous marches and youth strikes in Europe and around the globe have shown. The most recent

Intergovernmental Panel on Climate Change (IPCC) report ‘Global Warming of 1.5°C’ highlights the

urgency to reduce greenhouse gas emissions if the increase in global temperature is to be limited to

1.5°C. To meet this demand, it is imperative to reduce our dependency on fossil fuels and to cut down

on the amount of greenhouse gas emission society generates. Replacing fossil fuel energy with

renewable energy or bioenergy has become more urgent than ever. Many processes can provide

bioenergy while simultaneously ensuring that pollution control objectives are attained. One important

process in that particular context is anaerobic digestion (AD). Anaerobic digestion is an efficient and

environmentally sustainable technology that has three main advantages. Firstly, AD uses sludge

produced during the treatment of municipal wastewater, thereby reducing the amount of sludge that

needs to be disposed of. Secondly, AD is a sustainable way to bioprocess industrial wastewaters

generated by, for example, the food-processing industry and breweries, and the agricultural

wastewaters from intensive confinement farming and convert them into a valuable product. Finally,

AD provides bioenergy in the form of biogas, which is a mixture of mainly CH4 and CO2, without

releasing any gases into the atmosphere, thereby reducing overall emissions. Although methane is a

low-value product, biogas is catalytically converted to syngas (H2, CO), which can be used to produce

liquid fuel through conventional chemical manufacturing processes. In addition, methane can be

converted to other useful products such as methanol for use in the production of biodiesel. However,

AD also comes with a number of disadvantages attached. The significant capital investment that is

required and the considerable operational costs mean that it is unlikely to be viable as a single source

of renewable energy and should be regarded as part of an integrated system. Furthermore, anaerobic

digestion plants generate traffic. To minimize the impact on the environment caused by that traffic

and the nuisance for the neighborhood, the location of these plants should be chosen carefully. Finally,

AD requires pre-treatment of the feedstock and post-treatment of the effluent and biogas. Despite

these disadvantages, AD still has an important role to play in the fight against climate change and in

our efforts to create a better world for all (Angenent et al., 2004; Appels et al., 2008a; Dinsdale et al.,

2007; Jossen et al., 2019; Monnet, 2003).

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1

LITERATURE STUDY

1 ANAEROBIC DIGESTION

1.1 INTRODUCTION Anaerobic digestion (AD) is a process in which the degradation of organic substances by

microorganisms under anaerobic conditions takes place, which eventually leads to the production of

microbial biomass and biogas. The AD has several advantages e.g., low sludge production, low energy

consumption, no aeration requirements, and the biogas produced can be used as a source of

renewable energy (Chen et al., 2008; McHugh et al., 2003). Due to these advantages, this process is

already successfully being used in the treatment of agricultural, industrial and municipal waste. Up to

10% of organic waste in several European countries, is treated by means of AD (Li et al., 2011). The

microbial population involved can be divided into different groups, each with its own specific function.

These groups differ widely from each other in terms of physiology, nutritional needs, growth kinetics

and sensitivity towards environmental conditions. Minor fluctuations in operational parameters, e.g.,

temperature and pH, can unbalance the microbial population and can lead to process failure. This poor

operational stability still prevents AD from being widely used without any complications (Chen et al.,

2008).

1.2 ANAEROBIC DIGESTION PROCESS Anaerobic digestion includes four stages (Figure 1). The first stage is called hydrolysis in which insoluble

organic material and macromolecules, e.g., polysaccharides, proteins, nucleic acids and lipids are

degraded into smaller soluble organic components (Appels et al., 2008a). This stage occurs due to

extracellular hydrolytic enzymes that are produced and excreted by the hydrolytic bacterial population

(Parkin & Owen, 1986). Because hydrolysis plays a major role during AD, this step may become the

rate limiting step (Molino et al., 2013). The substances produced are further split during acidogenesis

or the fermentative stage. In this second stage, volatile fatty acids (VFA), alcohols and organic acids

are formed by acidogenic or fermentative bacteria along with ammonia (NH3), H2, CO2, H2S and other

by-products. The third stage is acetogenesis, and is carried out by acetogenic bacteria. During this

stage, acetic acid, as well as H2 and CO2 are mainly produced. However, the partial pressure of H2 in

the mixture mainly determines the equilibrium state of this conversion (Appels et al., 2008a; Hattori,

2008). If for example the partial pressure of H2 gas exceeds a certain threshold1, the production of

methane (CH4) is inhibited, and the concentration of VFA will increase. Finally, in the last stage, CH4 is

produced during so-called methanogenesis. The formation of CH4 can be carried out by two groups of

methanogenic archaea. The first group of methanogens, the acetoclastic methanogens, cleave acetate

to generate CO2 and CH4, while the second group, the hydrogenotrophic methanogens, produce CH4

from the reduction of CO2 using H2 gas as electron donor (Parkin & Owen, 1986).

1 Sterling Jr. et al.reported normal H2 gas concentrations in digester biogas ranging from 6 to 20 Pa. On the contrary, De Vrieze reports H2 concentration values ranging 0.1 Pa to 101 Pa.

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2

Figure 1 - Subsequent steps in the anaerobic digestion process

1.3 MICROBIAL POPULATION As already mentioned in 1.2, the microbial population participating in the AD process consists of three

trophic groups, namely the hydrolytic-acidogenic bacteria, the acetogenic bacteria and the

methanogenic archaea. The composition of these three groups may differ depending on the type of

feedstock, on the one hand, and the process temperature, on the other hand. The operational

temperature varies between psychrophilic (<20°C), mesophilic (30-38°C) or thermophilic temperature

(50-60°C) (Ziganshin et al., 2013). The first group only depends on acetogens and methanogens in

terms of H2 scavenging, while the acetogenic bacteria and methanogenic archaea are strictly

dependent on each other. Acetogenic bacteria act as H2 donor, while methanogenic archaea act as H2

acceptor. Thus, process failure leading to inhibition of methanogenesis also affects acetogenic

bacteria. Therefore they are often referred to as the methanogenic association or consortium (De

Vrieze, 2019; Michihiko & Tomonori, 1982).

1.3.1 HYDROLYTIC-ACIDOGENIC BACTERIA The first step, which is also the rate-limiting step of AD, is hydrolysis. Microorganisms that are involved

in this step mainly belong to the Firmicutes, Bacteroidetes and Proteobacteria phyla (De Vrieze, 2014).

To increase the rate of hydrolysis and the overall efficiency of the AD process, knowledge of the

microbial ecology during this step is of great importance (Wang et al., 2010). It is known that similar

bacteria that are involved in hydrolysis are responsible for acidogenesis. However, energy is yielded,

and bacteria grow rather by the acidogenesis of monomers than the hydrolyzation of polymers, which

still results in hydrolysis remaining the rate-limiting step.

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As already mentioned, during this second step, VFA are produced with a very high conversion rate.

Nevertheless, the maximum concentration of organic acids attained reaches a threshold of 20 – 30 g/L.

Higher concentrations can inhibit hydrolysis as well as acidogenesis. (De Vrieze, 2019).

1.3.2 ACETOGENIC BACTERIA Acetogenic bacteria are very diverse, although many of the bacteria belong to the class Clostridia.

These bacteria convert the intermediary products, formed during the acidogenesis step, into acetate,

H2 and CO2. If H2 accumulates, significant H2 pressure can occur, which results in the inhibition of

acetogenic bacteria and the loss of acetate production. However, methanogenic archaea use H2 in their

pathway, meaning that, in a properly functioning AD process, significant H2 pressure does not occur,

and the formation of CH4 and CO2 can proceed undisturbedly (Gerardi et al., 2008).

Acetogenic bacteria mainly consist of three groups, i.e., the homoacetogenic or syntrophic acetate

oxidizing bacteria (SAOB), the syntrophic acetogenic bacteria (SAB), also called obligatory H2-producing

acetogenic bacteria (OHPA) and sulfate reducing bacteria (SRB).

The first group, the SAOB, cooperate with the hydrogenotrophic archaea. These SAOB convert acetate

to CO2 with the production of H2. This reaction is endergonic (ΔG0 = 104,6 kJ/mol) and is extremely

unfavorable at standard conditions. However, if there exists a sink for H2, the reaction becomes

exergonic (ΔG0 = - 135,6 kJ/mol), and can, therefore, proceed if H2-consuming hydrogenotrophic

archaea eliminate H2 gas. In sum, these bacteria and archaea depend on one another since the bacteria

require H2 scavengers and the archaea require H2 suppliers. (Gerardi et al., 2008; Hattori, 2008).

The second group are SAB, which convert VFA into acetate and H2. Like SAOB, they need the

partnership of H2-scavenging hydrogenotrophic methanogens to maintain their metabolic activity.

Most of the SAB that oxidize propionate belong to the Syntrophobacterales order and the

Peptococcaceae family and the ones that oxidize butyrate mainly belong to the Syntrophomonadaceae

family (De Vrieze, 2014).

The last group are SRB. These bacteria, such as Desulfovibrio desulfuricans, use acetate, H2 and VFA as

electron donor and sulfate as electron acceptor to form sulfide, which can influence acetogenesis.

Under low acetate concentration, the SRB obtain H2 and acetate more easily than methane-forming

archaea, which causes competition between SRB and the methanogenic archaea (Chen et al., 2014;

Gerardi et al., 2008; Hilton & Archer, 1988).

1.3.3 METHANOGENIC ARCHAEA The final step of AD is carried out by the methanogenic archaea. These methane-forming

microorganisms are classified as Archaea, which possess several unique characteristics that are not

found in Eubacteria, such as a non-rigid cell wall, unique lipids in the cell membrane, specialized

coenzymes and a substrate degradation that produces CH4 as waste. These clusters of archaea can be

split into three groups by means of three different pathways. The first group covers the acetoclastic

methanogens, which cleave acetate directly to methane and CO2. Two genera of methanogens,

Methanosarcina and Methanosaeta, are known to operate this biochemical process. The second group

contains the hydrogenotrophic methanogens, which reduce CO2 to CH4 using H2 as electron donor. The

third, and last, group are the methylotrophs, which can use reduced one-carbon compounds such as

methanol or methane as carbon source (De Vrieze, 2014; Gerardi et al., 2008; Hattori, 2008).

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1.4 DIFFERENT TYPES OF WASTE STREAMS Organic waste can occur as solid or liquid material and require a different treatment in AD plants.

Before the different waste streams are digested, they can undergo a pre-treatment step. This step

removes non-biodegradable materials, which take up unnecessary space, provides a uniform small

particle size feedstock for efficient digestions, protects the equipment of the wastewater treatment

plant (WWTP) against physical damage and removes materials, which may decrease the quality of the

digestate. Various types of pre-treatment exist, depending on the kind of waste stream and whether

the waste is solid or liquid. An example of a pre-treatment step of municipal solid waste (MSW) is the

use of a hammermill to reduce the size of the waste particles. Another way to pre-treat MSW is manual

sorting to remove large and unrelated materials (Monnet, 2003). Solid waste streams, such as crop

residues, lignocellulosic sources, and paper have a total solid content of more than 15% and are treated

via solid-state AD. Liquid waste streams, such as liquid wastes from industrial areas, animal manure

and sewage sludge contain less than 15% total solid content, and are treated via the so called liquid

AD (Brown et al., 2012).

1.4.1 INDUSTRIAL WASTE STREAMS Organic industrial waste can exist in a liquid or solid form, and both can be suitable for AD. Industrial

waste streams can be subdivided into waste streams of the food industry, the paper and pulp industry,

and textile industry (Chen et al., 2008). Waste from the food industry contains high-value organic

matter, which makes these waste streams suitable for AD (Rinzema et al., 1988). Food industry sludge

of a WWTP in Bahadurgarh in India, for example, contains about 360 g organic carbon/kg sludge (Garg

et al., 2012). However, these waste streams contain several inhibitors. Wastewater from processed

seafood, for example, has a very high salt content2. High levels of salt can cause an osmotic shock to

the bacterial cells, which causes dehydration, and consequently inhibits AD (Rinzema et al., 1988).

Waste streams of the paper and pulp industry contain high carbon oxygen demand (COD)

concentrations, which makes AD of these waste streams very favorable. However, sulfide is produced

during the Sulfite process3, which is a common inhibitor during AD of these waste streams. The removal

of sulfide can be achieved by sulfur bacteria, which convert sulfide ions to elemental sulfur as a pre-

treatment of the paper industry waste stream (Buisman et al., 1991). Next to sulfide, these waste

streams also contain long chain fatty acids (LCFA), which inhibit the acetoclastic methanogens. Finally,

the presence of halogenated compounds produced during the bleaching process are also possible

inhibitors of the AD process (Hanaki et al., 1981; Koster & Cramer, 1987).

Textile wastewaters have a high chemical complexity, because of the variety of fibers, dyes and process

aids. Components of textile wastewaters, such as dye, dyeing auxiliaries, and surfactants, are inhibitors

of methanogenesis, which makes it very difficult to treat these wastewaters (Chen et al., 2008;

Vandevivere et al., 1998).

2 Kilcast & Angus reports salt concentrations in processed seafood ranging from 1% up to even 30% 3The Sulfite process is a chemical process for the manufacturing of paper pulp.

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1.4.2 MANURE Because of the high amounts of manure produced each year, treatment of this waste stream is one of

the most current applications of AD (Monnet, 2003). Manure has a high nitrogen content (Appels et

al., 2011; Ward et al., 2008). However, the ammonia concentration in animal waste is often too high,

due to the presence of ammonia in manure itself, and due to the conversion of proteins and urea to

ammonia during AD. This can lead to the inhibition of anaerobic digesters. Manure is therefore often

co-digested with other waste streams (Chen et al., 2008; Hashimoto, 1986; Zeeman et al., 1985).

The use of manure in AD has several advantages. One of them is the obtained odorless digestate, which

can be used as a fertilizer. This digestate can then be used on the land to enrich the soil without odor

nuisance (Monnet, 2003). An additional advantage of AD is the controlled release of CH4. The storage

of manure can lead to uncontrolled CH4 emissions, which contribute to global warming effects.

Controlled AD prevents this uncontrolled CH4 release (Appels et al., 2011; Moller et al., 2004a, 2004b).

1.4.3 ENERGY CROPS AND AGRICULTURAL WASTE Crop residues, such as unused stalk, straw, vegetable waste and specially grown energy crops e.g.,

maize, beet and wheat, can also be used to produce biogas. Both crop residues and energy crops have

a high lignocellulosic content. The AD process can degrade cellulose up to 80%, which makes the AD

process of green waste economically beneficial. However, lignin forms a problem, because of its high

non-degradable rigid structure (Appels et al., 2011; Ress et al., 1998). These waste streams can

therefore often only be processed after chemical or physical pre-treatment, which increases the

processing costs (Monnet, 2003).

1.4.4 MUNICIPAL WASTE Municipal waste contains about 60% of organic material, which makes this waste stream very suitable

for AD. However, municipal waste needs to be sorted first to obtain a clean biodegradable fraction.

Sometimes an additional pre-sorting step is applied, necessary for the removal of heavy metals, which

unfortunately increases the treatment costs of AD. Municipal waste has a high content of protein-

containing materials. Ammonia is produced during the degradation of these materials, which can have

an inhibitory effect on the process if the concentrations are too high. (Appels et al., 2011; Ward et al.,

2008).

1.5 CONTROL OF ANAEROBIC DIGESTION Control of the operational parameters of the AD process is essential. Several operational parameters,

e.g., pH, temperature, organic loading rate (OLR) and added nutrients need to be controlled during the

process to optimize the microbial activity to obtain the maximum production of biogas.

1.5.1 EFFECT OF PH The optimal pH range for acidogenesis differs from the pH range for methanogenesis. Acidogenic

bacteria are more or less insensitive to the pH within a range of 4.5 to 9, while methanogenic archaea

can operate only in a pH range of 6.8 to 7.2 (De Vrieze, 2019; Mudrack & Kunst, 1986; Rajeshwari et

al., 2000). The optimal pH range for both groups is situated between 6.8 and 7.5. During AD, acidogenic

bacteria produce VFA, which can reduce the pH of the process. This acidification is countered by the

activity of the methanogenic archaea that produce products, such as CO2, ammonia and bicarbonate.

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These three components act as a buffer to neutralize the effect of VFA and consequently keep the pH

at a near to constant value (Appels et al., 2008a; Turovskiy IS, 2006).

1.5.2 EFFECT OF TEMPERATURE The operating temperature of AD varies from very low temperatures (15°C), which is called

psychrophilic digestion, to higher temperatures (70°C), which is called hyperthermophilic digestion (De

Vrieze, 2014; Gerardi et al., 2008; Lier, 1995). Most AD systems operate under mesophilic conditions

(30-38°C) or thermophilic conditions (50-60°C) (Buhr & Andrews, 1976). Thermophilic digestion shows

several advantages in comparison with mesophilic digestion, e.g. a more efficient destruction rate of

organic solids, a greater resistance to pathogenic organisms and a higher gas production. Nevertheless,

the use of thermophilic temperatures also suffers from several disadvantages, e.g. a lack of process

stability related to high propionate concentrations and higher sensitivity to environmental changes

(Kim et al., 2006; Kim et al., 2002).

Independent of the advantages of thermophilic conditions, the optimum digestion temperature

depends on the type of waste stream used during AD and on the type of digesters. In addition, the

operating temperature needs to be as constant as possible to sustain the microbial composition in the

digester and consequently to maintain a high biogas production rate (Monnet, 2003).

1.5.3 EFFECT OF ORGANIC LOADING RATE The organic loading rate (OLR) is defined as the amount of COD applied in the AD system, per liter, per

day. During the start-up of a reactor, the OLR need to be increased gradually. If the system is fed above

its sustainable OLR, slow-growing methanogenic archaea can’t convert acetate and H2 fast enough to

CH4 and CO2 anymore, which results in the accumulation of VFA, a decrease in pH and, consequently,

a decrease in methanogenic activity and, thus, in lower biogas production. In conclusion, monitoring

the parameters of an AD process, such as pH, biogas production and VFA composition is crucial to

obtain an efficient AD process with stable biogas production (Appels et al., 2008a; Chen et al., 2008;

De Vrieze, 2014; Monnet, 2003).

1.5.4 ESSENTIAL GROWTH FACTORS Essential growth factors can be divided into macronutrients and micronutrients or trace elements. All

these elements are essential in at least one metabolic pathway in AD. It is of utmost importance that

nutrient limitations should be avoided to maintain biogas production (De Vrieze, 2014; Hutnan et al.,

2013; Vintiloiu et al., 2012).

1.5.4.1 MACRONUTRIENTS

Macronutrients, such as carbon, nitrogen, phosphorus and sulfur play an important role in the growth

and metabolism of anaerobic microorganisms (Pobeheim et al., 2010). The C:N ratio, for example,

represents the ratio of the mass of carbon to the mass of nitrogen present in the feedstock.

Microorganisms consume carbohydrates 25-30 times faster than nitrogen. To fulfil this requirement,

and to obtain the maximum yield of biogas, sufficient carbohydrates in the feedstock are needed.

Waste streams that are high in nitrogen and low in carbohydrate can be combined with waste streams

that are carbohydrate-rich (Gashaw, 2014).

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1.5.4.2 MICRONUTRIENTS

The elements B, Co, Cr, Cu, Fe, Mn, Mo, Ni, Se and W are the most important micronutrients or trace

elements needed for optimum growth during AD. Although these trace elements need to be present

in very low concentrations, the lack of these nutrients can have an adverse effect on microbial growth

and performance (De Vrieze, 2014; Feng et al., 2010; Rajeshwari et al., 2000).

The correct dosages of these trace elements can have a positive impact on the process, such as a better

stabilization of the digester, more degradation of organic matter, lower VFA concentrations and

consequently a higher biogas production (Yaw et al., 2016).

The most important microorganisms in the AD process are the methane forming archaea, because they

avoid accumulation of VFA. The methanogenic archaea have very high internal concentrations of Fe,

Ni and Co. Some waste streams don’t contain sufficient concentrations of these three trace elements

to meet the required quantities for the methanogens. Such waste streams have to be supplemented

with these trace elements as a pre-treatment. This unfortunately increases the operation costs. An

inexpensive solution to nutrient limitation is co-digestion with nutrient-rich substrates (Rajeshwari et

al., 2000; Yaw et al., 2016).

1.6 INHIBITORS OF THE ANAEROBIC DIGESTION PROCESS Several substances can inhibit the AD process. The reason why AD is so easily inhibited is because it is

a very vulnerable process with different groups of microorganisms who have their own optimal living

conditions. To obtain the most efficient process conditions, each group of microorganisms needs to

function as best as possible, and a well-balanced system needs to be maintained.

1.6.1 SULFATE AND SULFIDE Different waste streams from the paper industry, the sugar industry and edible oil refineries may

contain high levels of sulfate. During AD of these waste streams, SRB convert this sulfate into sulfide.

However, if the sulfate levels in the waste streams become too high, methane production can be

inhibited by the activity of SRB, and, thus, inhibition of the AD process may occur. This inhibition can

take place on two different levels (Colleran et al., 1995; De Vrieze, 2014).

The first inhibition is caused by substrate competition between the SRB, on the one hand, and the

methanogenic archaea and acetogenic bacteria, on the other hand. While reducing sulfate to sulfide,

the SRB use acetate and H2 as electron donor, which are also the substrates of SAOB and methanogenic

archaea. In addition, when the concentrations of H2 and acetate are low, SRB can use VFA as electron

acceptor. This shows the competition towards SAB, which also use VFA as substrate (Chen et al., 2014;

Hilton & Archer, 1988).

The second inhibition is due to the formation of sulfides, which are highly reactive, corrosive and toxic

to microorganisms, plants, animals and also humans (Colleran et al., 1995). Toxicity of sulfides present

in AD is pH dependent, since only the unionized hydrogen sulfide form can pass through the cell

membrane. Therefore, the extent to which sulfide is toxic or not, depends on the characteristics of the

sludge (Hulshoff Pol et al., 1998; Speece, 1983). Once in the cytoplasm of bacterial cells, sulfide

denatures the native proteins through formation of sulfide and disulfide, cross-linked between

polypeptide chains. Sulfide can also interfere with the assimilatory metabolism of sulfur and it may

also affect the intracellular pH (Chen et al., 2008; Hulshoff Pol et al., 1998; Siles et al., 2010). The

abovementioned consequences reduce the rate of methanogenesis and consequently biogas

production. Therefore, excessive levels of sulfate in waste streams need to be avoided, for example

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through dilution of the waste stream or pre-treatment, such as bioaugmentation, air stripping and

chemical precipitation. However, pre-treatment increases the operational costs (Chen et al., 2014;

Chen et al., 2008; Zhang & Angelidaki, 2015).

1.6.2 LONG CHAIN FATTY ACIDS Long Chain Fatty Acids (LCFAs) are fatty acids with aliphatic tails of 13 to 21 carbons. The LCFA arise

from the hydrolyzation of lipids to glycerol and LCFA. The LCFAs are further converted to H2 and acetate

by SAB and finally to CH4 and CO2 by methanogens. Accumulation of LCFA can inhibit the activity of

syntrophic acetogens and methanogens by the adsorption of LCFA onto the microbial surface, which

limits the transport of nutrients into the cell (Hwu et al., 1998; Pereira et al., 2005). However, LCFA

inhibition is reversible, which can be explained by two hypotheses. The first hypothesis is the

phenotypic adaptation of the existing bacterial community to higher concentrations of LCFA after a lag

phase, which is called physiological acclimatization. The second hypothesis is called population

adaptation and explains the reversible inhibition by a shift towards the enrichment of specific and

better adapted LCFA-degraders. The research Palatsi et al. conducted into these two hypotheses in

2010 indicated that the observed adaptation process can be attributed to the physiological hypothesis

(Palatsi et al., 2010; Pereira et al., 2004).

1.6.3 AMMONIUM AND AMMONIA Ammonia is the end-product of AD of proteins, urea and nucleic acids, and is an essential nutrient for

the growth of microorganisms. However, if the ammonia concentration is too high, it will inhibit the

process. Total ammonia nitrogen (TAN) contains two forms of nitrogen; free ammonia (FA) or

unionized ammonia (NH3) and ionized ammonia or ammonium (NH4+). The FA is the active compound

in AD inhibition, because FA can permeate the cell membrane more rapidly than ammonium (Rajagopal

et al., 2013; Siles et al., 2010). Once in the cell of the methanogens, some FA can be converted to

ammonium, due to the difference between the extracellular and intracellular pH. This process requires

the absorption of protons (H+) using a K+ antiporter, which results in a proton imbalance, potassium

deficiency, a change in intracellular pH and an increase in maintenance energy requirements.

Ammonium can also inhibit the methane synthesizing enzyme directly, which results in less serious

consequences (Chen et al., 2014; Chen et al., 2008).

The concentration of ammonia increases as the temperature increases. This is because of two main

reasons. The first reason is that ammonia is produced during hydrolysis by the degradation of

nitrogenous organic materials and the higher the temperature, the higher the metabolic rate of the

microorganisms, and hence, the higher the hydrolysis rate. The second reason can be derived from the

following equation:

𝑁𝐻3 (𝐹𝐴) = 𝑇𝐴𝑁 ∗ (1 + 10−𝑝𝐻

10−(0,09018+

2729,92𝑇(𝐾)

)−1

From this, it is clear that an increase in temperature will lead to an increase in FA concentration. This

equation also shows the relationship between the FA and the pH (Rajagopal et al., 2013; Sung & Liu,

2003). The pH can also affect the ammonia concentration. In aqueous solutions, there is a chemical

balance between FA and ammonium. If the pH value increases, the amount of FA will also increase,

and the biogas production will decrease. For example, an increase in pH from 7 to 8 will actually lead

to an eight-fold increase in the FA concentration (Chen et al., 2014).

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Acclimation is another factor that influences the degree of ammonia inhibition. Methanogens can

acclimate to high concentrations of ammonia, making them more tolerant towards ammonia stress

(Sung & Liu, 2003).

1.6.4 SALT Different waste streams, such as wastewater from food processing industries and chemical industries,

can contain salt concentrations, possibly inhibiting the AD process. Addition of salt is possible during

industrial processing for pH adjustment, which results in waste streams with a very high salt

concentration. However, if the salt concentration reaches a certain threshold, it can be toxic or

inhibitory to the activity of the microorganisms present in the AD. This inhibition can mostly be

attributed to cations, e.g., Na+, K+, Mg2+ and Ca2+, which are the most common cations in AD (Appels

et al., 2008b; Chen et al., 2008).

Sodium concentrations of more than 8800 mg Na+/L are strongly inhibitory to methanogenic archaea.

Excessive levels of Na+ lower the maximum specific growth rate and the yield of acetoclastic

methanogens, while increasing their specific decay rate. However, the presence of a Na+ concentration

of 350 mg Na+/L is beneficial for methanogenic archaea, because the formation of ATP and NADH

requires a low concentration of Na+ (Appels et al., 2008b; Rinzema et al., 1988).

Potassium shows optimal concentrations similar to Na+. If the concentration is below 400 mg K+/L, the

AD process is enhanced. However, if the concentration exceeds 5850 mg K+/L, 50% of the acetate

utilizing methanogens is inhibited. High concentrations of K+ can lead to a passive influx of K+ ions,

thereby neutralizing the membrane potential. Potassium also extracts metals that were bound to

exchangeable sites in the sludge. This subsequently leads to the removal of essential metals, such as

Cu, Zn, Ni, Mo and Co from the activated sludge, which, in the end, is responsible for the low activity

of the methanogenic population (Appels et al., 2008b; Chen & Cheng, 2007; Chen et al., 2008). The

performance of AD improves with increasing concentration of Ca2+ and reaches a maximum at the

concentration of 3 g Ca2+/L. Higher concentrations of more than 5–7 Ca2+ g/L induces an adverse impact

on the performance of AD (Ahn et al., 2006). Methanogens can also adapt to the increasing salt

concentrations. Continuous exposure of methanogenic archaea leads to a higher tolerance towards

higher Na+ levels (Feijoo et al., 1995).

1.6.5 TRACE ELEMENTS As already mentioned in 1.5.4.2, excessive concentrations of trace elements or micronutrients can

have an adverse impact on the growth and activity of the microbial community. However, the toxicity

of these trace elements towards the microbial community is independent of the total metal

concentration in the digester, but rather depends on the concentration of free metals in the sludge (A.

Lawrence & McCarty, 1965; Mueller & Steiner, 1992). It is known that active, inactive and dead biomass

can bind heavy metals, which consequently results in the accumulation of high levels of heavy metals

(Kuyucak & Volesky, 1988). Acidogens are less susceptible to high concentrations of trace elements.

Hence, the decrease in biogas production and the accumulation of VFA in the reactor can indicate the

presence of toxic levels of heavy metals. However, heavy metals may affect the production of acetate

and butyrate in different ways. In 1993, Lin showed that an increase in concentration of mixed metals

induced an increase in the production of butyrate, but a decrease in the production of acetate and vice

versa (Lin, 1993). Sulfides, derived from the conversion of sulfate to sulfide by SRB, can precipitate

with heavy metals, leading to a reduced effect of toxic heavy metals. The precipitation of heavy metals

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with sulfides may occur over a wide pH range. At neutral pH, many heavy metals also precipitate as

hydroxide. Chen et al. evaluated the toxicity of heavy metals during AD and reported different

inhibiting concentrations, ranging from 70 to 400 mg/L for Cu, 200 to 600 mg/L for Zn and 10 to 2000

mg/L for Ni (A. Lawrence & McCarty, 1965; Lin & Chen, 1999; Mueller & Steiner, 1992; Tiwari et al.,

2006).

2 ANAEROBIC GRANULATION TECHNOLOGY

2.1 INTRODUCTION The anaerobic granular sludge bed technology has become more and more popular in industrial

wastewater treatment, because it has several benefits in comparison with systems that use non-

granular dispersed sludge. Non-granular sludge has a loose structure, and can only be partially

separated from the liquid fraction after it has settled, while granular sludge has a clear and visible

granular shape, which can be separated completely from the liquid fraction. Several advantages of

granular sludge over non-granular sludge will be listed. First, granular sludge settles much faster than

non-granular sludge, which makes granular sludge less susceptible to the wash out of biomass during

start-up. Another advantage is that methanogens in granular sludge are more tolerant to oxygen. This

group of archaea is surrounded by facultative anaerobic bacteria that utilize incoming oxygen before

it can reach the core of the granules, which predominantly consist of methanogens. In addition,

granular sludge is less sensitive to substrate inhibition, compared with non-granular sludge. Finally,

substrate conversion to intermediates and the transfer of intermediates for further degradation is

enhanced in granular sludge, because of the clustering of various bacterial groups in a small area

(Baloch, 2011).

2.2 ANAEROBIC GRANULATION REACTOR TECHNOLOGIES As already mentioned in the introduction of AD, anaerobic treatment shows many advantages over

aerobic processes, e.g., low levels of excess sludge production, less space requirements, no

requirement for aeration and the production of biogas. Because of these advantages, a tremendous

increase in AD of waste was experienced in the last decades, which made the development of

anaerobic reactor technologies indispensable. Upflow anaerobic sludge blanket (UASB) reactor designs

and expanded granular sludge bed (EGSB) reactor designs represent the main proportion of anaerobic

reactor technologies, especially for the treatment of liquid waste streams. For more solid waste

streams, other reactor technologies, such as continuous stirred tank reactor (CSTR) and internal

circulation (IC), can be the choice of preference.

2.2.1 CONTINUOUS STIRRED TANK REACTOR (CSTR) A CSTR consists of one big vessel with a mixer inside that mechanically agitates the reactor to keep the

active anaerobic sludge in suspension. Due to this mixing, it is assumed that there exists no

concentration gradient in the vessel. The feedstock is entering the reactor at the top of the vessel with

the same rate as the outgoing substrate effluent that is leaving the reactor at the bottom of the vessel

(Figure 2). However, in some cases, the feedstock enters at the bottom of the vessel, while the

outgoing effluent leaves the reactor at the top of the vessel. In these two systems, the retention time

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of the anaerobic biomass, i.e. solid retention time (SRT), equals the hydraulic retention time (HRT)

(Cunningham et al., 2010; Kaparaju et al., 2008; Karim et al., 2005). This type of reactor can bear

organic loading rates ranging from 3 to maximum 10 kg COD/m3/d and is typically used for solid rich

waste streams, such as manure and energy crops (De Vrieze, 2014; Pycke et al., 2011; Sundberg et al.,

2013).

2.2.2 UPFLOW ANAEROBIC SLUDGE BLANKET REACTOR (UASB) A UASB reactor consists of one single vessel, and is typically used for low to medium strength

wastewaters. The inlet of the wastewater is situated at the bottom, which makes the upward flow

(about 1.0 m/h upflow velocity) through an anaerobic granular sludge bed possible. The granules are

formed due to the natural aggregation of the microbial community in flocs and granules, on the one

hand, and the combination of the upflow mode with shear, on the other hand. The maintenance of

this sludge bed is possibly through the accumulation of incoming suspended solids and bacterial

growth on these solids. When the wastewater passes this bed, it comes in close contact with the

granular microbial community, which enables degradation of organic matter. These granules have

good settling properties, which avoids the wash-out of biomass. The treated effluent leaves through

an outlet at the top of the reactor, as does the produced biogas. This produced biogas causes hydraulic

turbulence in the sludge bed, which provides an adequate mixing within the system and, therefore,

eliminates mechanical mixing. This mixing provides a better contact between biomass and organics in

the ingoing wastewater (De Vrieze, 2019; McHugh et al., 2003). Another advantage of this reactor

technology is the application of a higher OLR (up to 20 kg COD/m3/d) in comparison with aerobic

systems. Hence less reactor volume and space are required, which reduces the operational costs

(Frankin, 2001; Seghezzo et al., 1998). The SRT is much higher than the HRT of the wastewater, which

gives the biomass sufficient time to grow. Finally, the reactor consists of a three-phase separator, also

called gas-liquid-solids separator, which separates the three phases occurring in the reactor (Fout!

Verwijzingsbron niet gevonden., left) (Bal AS, 2001; De Vrieze, 2019; McHugh et al., 2003).

Figure 2 – Schematic overview of a CSTR

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2.2.3 EXPANDED GRANULAR SLUDGE BED REACTOR (EGSB) Although UASB set-ups are frequently used in industry, this reactor type still struggles with some

problems. First of all, internal mixing was not optimal in a pilot-scale UASB reactor operating at

temperatures ranging from 4 to 20°C (Man et al., 1986). This leads to the creation of dead zones and,

thus, to a reduction in the treatment efficiency. Nevertheless, the use of higher upflow velocities (6 –

15 m/h) in EGSB reactors has solved this problem. These velocities can be obtained either by effluent

recirculation and/or tall narrow reactor design. The increased upflow liquid velocity expands the

granular sludge bed, eliminating dead zones, and increases hydraulic mixing, providing a better

biomass-substrate contact. Compared to UASB reactors, higher OLR up to 30 kg COD/m3/d can be

applied in EGSB systems. Consequently, biogas production is higher. This also improves hydraulic

mixing, which again enhances reactor performance and stability. The EGSB reactor is particularly

suitable for the treatment of low-strength wastewaters containing low levels of COD. Low substrate

levels lead to a lower biogas production rate and, consequently, to a lower mixing intensity. However,

the increased upflow liquid velocities compensate for this lower mixing intensity, making digestion of

low-strength wastewaters possible, due to the improved biomass-substrate contact. A drawback of

this reactor technology is that the granules tend to be washed out of the sludge bed (McHugh et al.,

2003; Seghezzo et al., 1998) (Fout! Verwijzingsbron niet gevonden., right).

2.2.4 INTERNAL CIRCULATION REACTOR The internal circulation (IC) reactor is developed by the Dutch company Paques, and has evolved from

the UASB and the EGSB reactors. The IC reactor consists of two inter-connected UASB compartments

on top of each other. First, the industrial wastewater enters at the bottom of the reactor, and is mixed

with the granular anaerobic biomass in the mixing section. Just above the mixing section, organic

components are converted into methane in the first expanded sludge bed. The produced biogas is

separated from the effluent in the lower phase separator and is, together with water, collected via the

riser pipe in the gas/liquid separator on top of the reactor. Biogas leaves the system and water returns

through the downer pipe into the mixing section where it is mixed with the incoming influent. This is

Figure 3 – Schematic overview of a UASB reactor (left) and an EGSB reactor (right)

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where the name ‘internal circulation reactor’ comes from. In the upper compartment of the reactor,

the effluent is polished a second time in the second expanded sludge bed and biogas is collected in the

upper phase separator. The effluent leaves the system and biogas and water are again separated at

the top of the reactor (Driessen, 2016; PAQUES, n.d.). Due to the internal circulation, incoming influent

is diluted resulting in the potential application of high OLR, up to 30 kg COD/ m3/d. The production of

biogas occurring in two phase separators permits the use of a very high upflow, ranging from 20 to

even 30 m/h. Any biomass lost from the first compartment of the reactor is retained in the upper

section. This facilitates sludge retention within the system and, accordingly, facilitates the use of high

OLR. On the other hand, the effluent in the upper phase separator has a low OLR, which aids the very

efficient separation of biogas, biomass granules and treated effluent (De Vrieze, 2019; McHugh et al.,

2003) (Figure 4).

2.3 ANAEROBIC GRANULATION THEORIES

2.3.1 STRUCTURAL MODELS During anaerobic granulation, both biological and microbiological factors are involved. To understand

the microbiological characteristics of UASB granules and the interactions between different bacteria

and archaea, some structural models for anaerobic granulation were developed (Liu et al., 2003).

2.3.1.1 INERT NUCLEI MODEL

The inert nuclei model for anaerobic granulation was initially proposed in 1980 by Lettinga et al. This

process is initiated by microorganisms that attach themselves to the particle surface of inert

microparticles with a lower specific gravity than the gravity of the biomass present in the reactor. In

this way, the initial biofilm is formed and embryonic granules are created which can further develop

through the continued growth of the attached micro-organisms under given operation conditions

Figure 4 – Schematic overview of an IC reactor

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(Figure 5). Addition of inert matter is effective in the initiation of the formation of anaerobic granules

(Lettinga et al., 1980; Liu et al., 2003; Yoda et al., 1989).

2.3.1.2 SELECTION PRESSURE MODEL

The selection pressure theory explains the effects of liquid upflow velocity on anaerobic granulation.

If the liquid upflow velocity is high (high selection pressure), light and dispersed sludge tends to be

washed out, while heavier components can remain in the reactor. If a low liquid upflow velocity is

applied (low selection pressure), growth will take place, mainly as dispersed biomass, which gives rise

to the formation of a bulking type of sludge. This model suggests that the formation of microbial

aggregation may be an effective protection strategy against these high selection pressures in terms of

upflow velocity (Hulshoff Pol et al., 2004; Liu & Tay, 2002; Liu et al., 2003).

2.3.1.3 MULTI-VALENCE POSITIVE ION-BONDING MODEL

At normal pH values, microbial surfaces are negatively charged. If two surfaces are either both

positively charged or negatively charged, there exists a free energy barrier between them, which acts

as a repulsive force. By introducing multi-valence positive ions, such as Al3+, Ca2+, Fe2+ and Mg2+ the

electrostatic repulsive force between different bacteria is reduced. Another advantage of introducing

positively charged ions is the formation of multi-valent bridges between negatively charged groups on

cell surfaces, which stimulates aggregations of microbial cells (Figure 6). The rate of sludge granulation

during the start-up of a UASB reactor is enhanced by Ca2+ concentrations in the waste stream ranging

from 80 – 150 mg/L (Alibhai & Forster, 1986). However, another study reports optimal Ca2+

concentrations ranging from 150 – 300 mg/L (Yu et al., 2001). The difference in optimum ranges

indicates that the actual effect of Ca2+ on granule formation still needs to be understood. Higher

concentrations (< 600 mg/L) of Ca2+ may be detrimental to the granules because of the formation of

CaCO3, which can precipitate and may block the intragranular pores, leading to severe mass transfer

limitations (Liu et al., 2003; Mahoney et al., 1987; Tiwari et al., 2006; Yu et al., 2001).

Figure 5 – Inert nuclei model

Figure 6 – Multi-valence positive ion-bonding model

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The multi-valent positive ions may promote sludge granulation by bonding with extracellular polymers

(ECP). There exists a high affinity between Ca2+ and ECP, which implies that the initial structure of the

microbial community can form through a ECP – Ca2+ – ECP bridge or cell – Ca2+ – cell linkage (Liu et al.,

2002, 2003).

2.3.1.4 CAPETOWN’S MODEL

It is assumed that Methanobacterium strain AZ produces ECP. The Methanobacterium strain AZ is an

archaeon that utilizes H2 as its sole energy source and can produce all its amino acids, except for the

essential amino acid, cysteine. Under high H2 partial pressure and limited concentrations of cysteine,

several amino acids would be over-secreted. The over-secretion induces ECP formation.

Methanobacterium strain AZ and other bacteria and archaea get stuck in, leading to granulation

initiation. In the Capetown’s model, the overproduction of ECPs is considered a key step for initiating

anaerobic granulation (Liu et al., 2002, 2003).

2.3.1.5 SPAGHETTI MODEL

The first step in the spaghetti model is the formation of precursors. These precursors can consist of

very small aggregates of Methanosaeta, originated by the turbulence generated by the gas production,

or they can consist of the attachment of Methanosaeta to finely dispersed mater. Next, additional

filamentous Methanosaeta will attach to these precursors, which can form a three-dimensional

network through a branched growth process. Other micro-organisms, such as Methanosarcina, can

easily be entrapped in this network, forming a denser aggregate due to microbial growth, whereby the

granules are more spherically shaped, due to the hydraulic shear stress of the upflowing liquid and

biogas. In this model, the formation of structured aggregates is a crucial step in the overall granulation

process (Liu et al., 2003; Tay et al., 2000).

2.3.1.6 SYNTROPHIC MICROCOLONY MODEL

Many different species are involved in biodegradation of organic waste, which makes anaerobic

digestion a very complex process. To make a process as energy-efficient as possible, these species live

in a close synergistic relationship where different products, such as H2 gas and other intermediates,

can be easily transported from cell to cell. Hirsch suggested in 1984 that this close coexistence

eventually leads to the formation of stable microcolonies or consortia, i.e., initial granules (Hirsch,

1984).

2.3.1.7 MULTI-LAYER MODEL

In 1990, MacLeod was the first to create a multi-layer model to explain the formation of granules (Guiot

et al., 1992; MacLeod et al., 1990). According to this model, a granule is made up of 3 different layers.

The first, and innermost, layer consists of methanogenic archaea producing biogas, and this layer is

necessary for the development of the granule. On this nucleus, a second layer is attached, which

contains H2-producing acetogenic bacteria. In a next step, hydrolytic-acidogenic bacteria adhere to this

small aggregate forming the outermost and third layer of the granule. Unlike the model of MacLeod,

Rocheleau et al. showed in 1999 that the center of a UASB granule didn’t contain any living archaea or

bacteria. This can be explained by the accumulation of metabolically inactive, decaying biomass and

inorganic materials in the center of the granule (Figure 7). Other research conducted into the microbial

structure of anaerobic granules also showed a multi-layer model with in the center a granule nucleus

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that didn’t contain any trace of life. Therefore, the model of Rocheleau is more generally accepted

than the model of MacLeod (Hulshoff Pol et al., 2004; Liu et al., 2003; Rocheleau et al., 1999).

2.3.2 THERMODYNAMIC MODELS When two bacteria approach each other, they both experience physico-chemical interactions in terms

of repulsive electrostatic force, attractive van der Waals force, and repulsive hydration interaction

(Parsegian & Rand, 1991). These interactions not only occur between two cell walls, but can also occur

between a cell wall and a microparticle surface. To understand the present physico-chemical

interactions, some thermodynamic models have been developed (Liu et al., 2002).

2.3.2.1 SECONDARY MINIMUM ADHESION MODEL

The secondary minimum adhesion model is explained with the help of the Derjaguin-Landau-Verwey-

Overbeek (DLVO) free energy curve (Figure 8). The DLVO theory describes the force between two

charged surfaces over a distance of more than 1 nm through a liquid medium. This force combines the

effect of Van der Waals interactions and electrostatic repulsions. The initial adhesion between two cell

walls or between a cell wall and a microparticle surface takes place in the secondary minimum of the

DLVO curve. Because of the small Gibbs energy (∆G < 0) of the secondary minimum and because of the

separation distance and a remaining thin water film between the two adhering surfaces, the adhesion

in this minimum is reversible. However, if a micro-organism can reach the primary minimum (∆G <<<

0), short-range interaction forces can be applied and, subsequently, irreversible adhesion occurs. After

irreversible adhesion, colonization starts. The cells start to divide and start producing ECP. According

to the spaghetti model, micro-organisms are trapped in this biofilm structure, and granules are formed

(Costerton et al., 1990; Hulshoff Pol et al., 2004; Liu et al., 2003).

Figure 7 – Multi-layer model of Rocheleau

Figure 8 – General DLVO curve illustrating the main features of this interaction

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2.3.2.2 LOCAL DEHYDRATION AND HYDROPHOBIC INTERACTION MODEL

Under normal culture pH conditions, the cell walls of micro-organisms are hydrated. The thin water

film between two bacteria, prevents them from approaching one another, because of the strong

repulsive hydration interactions. Local dehydration of surfaces that are a short distance apart is a pre-

requisite for bacteria adhesion, because two bacteria will only adhere irreversibly, if both bacterial

surfaces are strongly hydrophobic. This indicates that hydrophobicity and hydrophilicity of microbial

surfaces are important factors in irreversible adhesion (Rouxhet & Mozes, 1990a; Wilschut & Hoekstra,

1984). Because of their hydrophilic surface character, most hydrolytic-acidogenic bacteria are situated

on the outer layer of granules, while methanogens and acetogens, because of their hydrophobic

surface character, are situated in the inner layers of the granules. This explains why hydrolytic-

acidogenic bacteria are most often located in the outer layer of anaerobic granules (Daffonchio et al.,

1995; Liu et al., 2003).

2.3.2.3 SURFACE TENSION MODEL

In general, hydrophilic microorganisms that have a high surface tension tend to form aggregates in

bulk solutions with a low surface tension, while hydrophobic microorganisms that have a low surface

tension tend to form aggregates in bulk solution with a high surface tension. Microorganisms in UASB

reactors may grow in loose association, in multi-layered granules or in mixed conglomerates,

depending on the liquid surface tension present in the reactor (Grootaerd et al., 1997; Thaveesri et al.,

1995). As already mentioned in 2.3.2.2, most hydrolytic and acidogenic bacteria are hydrophilic, while

most of the acetogens and methanogens appear to be hydrophobic. Granulation at low surface

tensions gives rise to granules with hydrolytic and acidogenic bacteria around a acidogenic-

methanogenic association. In contrast to granules formed in high surface tension solution, this type of

granule is less susceptible to adhesion to gas bubbles and subsequent wash-out, and ensures a more

stable reactor performance (Hulshoff Pol et al., 2004; Liu et al., 2002, 2003; Tay et al., 2000).

2.3.3 PROTON TRANSLOCATION DEHYDRATION THEORY The proton translocation dehydration theory was proposed based on the proton translocation activity

on bacterial membrane surfaces. This granulation hypothesis consists of four steps. The first step is the

dehydration of bacterial surfaces. Bacterial surfaces are negatively charged, and are therefore

surrounded by water molecules in aqueous solutions. However, if wastewater is fed into a reactor that

first contained tap water and sludge, the hydrolytic and acidogenic bacteria start to degrade complex

organic compounds, coupled with the activation of electron transport. This electron transport

consequently activates proton pumps on the membranes of these bacteria, which can cause surface

protonation. The existing proton gradient across the surface membranes can break hydrogen bonds

between negatively charged groups on the cell wall and water molecules, and can also partly neutralize

the negatively charged surface of the bacteria, inducing dehydration of the bacterial surfaces. The

second step is called the embryonic granule formation. In this step, proton pumps of acetogens and

methanogens are also activated, causing their membrane surfaces to become dehydrated. Hydrolytic

bacteria, acidogens, acetogens and methanogens may adhere to each other due to external hydraulic

forces and weakened hydration repulsion. This leads to the formation of embryonic granules whose

adhesion is further strengthened by the continued dehydration of the bacterial and archaeal surfaces.

Next, embryonic granules will grow into maturated granules in the third step, which is called granule

maturation. The microorganisms within the embryonic granule continue growing, while other

dispersed bacteria and archaea in the medium can adhere to the granule. The microbial biomass in the

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granules is efficiently organized, depending on the orientation of intermediate metabolite

transference. The last step is post-maturation. Due to the activity of proton pumps in mature granules,

the bacterial surfaces remain hydrophobic, which is principally responsible for maintaining the mature

granules. In addition, ECP is produced in the mature granules which protects granules against shear

stress and attachment to gas bubbles (Hulshoff Pol et al., 2004; Liu et al., 2002, 2003).

2.4 PARAMETERS INFLUENCING ANAEROBIC GRANULATION A UASB system can be initiated using existing granules, which can be assessed in terms of VSS/TSS

content, specific methanogenic activity (SMA) and the ability to settle. However, granular sludge is

expensive (220 – 300 €/ton) and the availability is limited. Unfortunately, formation of anaerobic

granules requires 2 to 8 months, so enhanced and fast production of anaerobic granules is essential

and strongly recommended. Therefore, knowledge of the major factors influencing the granulation

process is of great importance.

2.4.1 REACTOR TEMPERATURE AD is operated under mesophilic conditions (30-38°C) or thermophilic conditions (50-60°C). However,

temperature can have a great impact on the performance of anaerobic granules. Generally, UASB

reactors filled with granular sludge operate under mesophilic conditions with an optimum

temperature of 35°C. Careful temperature control at mesophilic conditions is still necessary, because

mesophilic granules are sensitive to sudden temperature changes, leading to disintegration of the

granules. In addition, the higher the temperature above 38°C, the higher the chances of sludge wash-

out and the higher the risk of decreasing COD removal efficiency. Temperatures lower than 30°C can

inhibit growth of methanogens (Fang & Lau, 1996; Lepisto & Rintala, 1999; Tiwari et al., 2006).

2.4.2 REACTOR PH As already mentioned in section 1.5.1, acidogens are more or less insensitive to the pH within a broad

range (4.5 – 9), while methanogens prefer a more neutral environment. The optimal pH for AD ranges

between 6.8 and 7.5. However, the strength of anaerobic granules decreases with an increase in pH

ranging from 8.5 – 11 or a decrease in pH ranging from 5 – 3. By contrast, the strength of the granules

remains unchanged when the pH ranges from 5.5 to 8. In conclusion, the stability of the granule

structure is enhanced in a slightly acid environment, which can be explained by the proton

translocation dehydration theory (Liu et al., 2003; Tay et al., 2000).

2.4.3 CHARACTERISTICS OF SEED SLUDGE In theory, any medium can be used as seed sludge to start a UASB reactor, as long as the seed sludge

contains the proper microbial community for AD. However, the quality of the applied seed sludge

mainly depends on two factors: the chance of being washed out and the composition of the seed

sludge. Two types of sludge wash-out were distinguished. The first type is sludge bed erosion wash-

out, which is the selective wash-out based on the difference in ability to settle. The second type is

sludge bed expansion. When using lighter, more diluted sewage sludge in the treatment of medium

strength wastewater, wash-out occurs due to the expansion of the sludge bed as a result of increased

hydraulic and gas loading rate. The latter can be avoided when choosing heavier and more

concentrated sewage sludge (De Zeeuw, 1988). Research on the composition of sludge used for

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granulation showed that granulation with syntrophic and methanogenic enriched consortia as

precursor proceeded more rapidly than when using acidogenic flocs as precursor. In other words, some

microbial species would enhance and speed up the granulation process, while other species are less

competent in forming aggregates. In conclusion, manipulation of the composition of the seed sludge

can be beneficial for UASB start-up (El-Mamouni et al., 1997; Hulshoff Pol et al., 1983; Liu et al., 2003).

2.4.4 UPFLOW VELOCITY AND HYDRAULIC RETENTION TIME High upflow liquid velocity (1m/h) in a UASB reactor is associated with a short HRT, which is favorable

for the granulation-process. The effect of a high upflow liquid velocity can be explained by the selection

pressure theory. In fact, granulation enhances the settling velocity of the granules, which reduces

wash-out of granular sludge. However, the effect of reducing the specific wash-out rate of smaller

particles is not assured (Hulshoff Pol et al., 1988). A high liquid upflow velocity also has a significant

positive effect on the mean granule size. Increasing granule size promotes increasing settling velocity,

although some authors have reported that settling velocity seems to be independent from the

diameter of the particles (Arcand et al., 1994; Beeftink & van den Heuvel, 1988). In conclusion, a short

HRT combined with a high upflow velocity ensures that microorganisms unable to form granules are

washed out and, accordingly, that sludge granulation is promoted (Hulshoff Pol et al., 1988).

2.4.5 ORGANIC LOADING RATE The OLR is one of the most important operating parameters in the anaerobic granulation process. It

has been demonstrated that a gradual increase of the OLR during start-up enhances the granulation

process. However, different OLR values need be considered to maximize the granulation velocity, but

still maintain process stability (De Zeeuw, 1988; Fang & Chui, 1993; Hulshoff Pol, 1989). An OLR that is

too high can have several disadvantages for the granulation process. Firstly, it may inhibit

methanogenic activity, causing an accumulation of VFA and, thus, a decrease in pH. As already

mentioned in 2.4.2, a pH that is too low, weakens the strength of the granules, causing them to

disintegrate. The second disadvantage is the increased biogas production rate. This can cause serious

hydrodynamic turbulence, which may be the cause of the seed sludge to wash out from the reactor. A

third and last disadvantage of an OLR that is too high is the increased growth rate. According to the

Monod kinetic, OLR is proportional to the growth rate and high growth rates reduce the strength of

the three-dimensional structure of the microbial community (Liu et al., 2003; Morvai et al., 1992;

Quarmby & Forster, 1995).

2.4.6 WASTEWATER COMPOSITION/CHARACTERISTICS OF SUBSTRATE The composition of the waste stream fed into the reactor can influence the formation, composition

and structure of anaerobic granules. Substrate can be distinguished as high-energy and low-energy

feed, depending on the free energy of oxidation of organics. Rather simple carbohydrate sources are

categorized as high-energy carbohydrate feed, and can promote the growth of hydrolytic and

acidogenic bacteria and the production of ECP. However, the more complex the substrate composition,

the wider the diversity of methanogenic sub-populations. During research on the principles of start-up

and operations of anaerobic systems, Hickey et al. found in 1991 that wastewater containing 10%

sucrose and 90% VFA mixture created granular and flocculent sludge that could not be effectively

separated. By contrast, the use of acidified wastewater gave rise to the formation of a rather

voluminous type of sludge (R. F. Hickey et al., 1991). From this, it can be concluded that the formation

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and microstructure of the granules depend on the characteristics and, thus, on the complexity of the

applied substrate (Chen & Lun, 1993; Liu et al., 2003; Wu, 1991).

2.4.7 ADDITION OF NATURAL AND SYNTHETIC POLYMERS According to some structural granulation models, the development of granules from non-granular

sludge is initiated by the microbial attachment on nuclei or biocarriers. The enhancement of the

granulation process can happen in two ways. The first way is the use of synthetic or natural polymers

to imitate the function of ECP, which promotes microbial agglomeration. Similarly, other polymers can

be used to facilitate the granulation process in a UASB start-up (Wang et al., 2005). El-Mamouni et al.

demonstrated in 1998 that the granulation rate in a chitosan containing reactor was 2.5 times higher

than in a reactor to which no polymers were added, while the SMA remained unchanged. However,

synthetic polymers have several disadvantages, such as inhibitory effect on substrate transfer to

granules, they are less safe for the environment and are not biodegradable. Therefore, research also

focuses on natural polymers, such as bio-flocculants (El-Mamouni et al., 1998; Wang et al., 2005). A

second way to enhance granulation is to use synthetic or natural polymers as inert nuclei or biocarrier.

The addition of inert particles, such as zeolite, improved the formation of granules. Also adding water-

absorbing polymers seemed to promote the granulation rate. It can be concluded that the presence of

synthetic or natural polymers can assist anaerobic granulation (Hulshoff Pol, 1989; Imai, 1997; Liu et

al., 2003).

2.4.8 ADDITION OF CATIONS To a certain extent, the addition of cations, such as Ca2+, Mg2+, Fe2+ and Al3+, can have a positive effect

on the formation of granules. As already mentioned in section 2.3.1.3, adding Ca2+ in concentrations

ranging from 80 – 150 mg/L or 150 – 300 mg/L can stimulate granule formation in several ways. The

first way can be explained by the secondary minimum adhesion model. The DLVO curve shows that

when two negatively charged bacterial cells approach each other, both particles will experience

electrical repulsion, preventing one particle adhering to another. Calcium will bind to the negatively

charged surfaces, thereby neutralizing the charges on the bacterial surfaces. This will lead to a decrease

in electrical repulsion and the adhesion between two cells will be facilitated (Rouxhet & Mozes, 1990b).

Another possible way to enhance anaerobic granulation is the binding between Ca2+ and ECP. As

already mentioned in 2.3.1.3, according to the multi-valence positive ion-bonding model, ECP can bind

to Ca2+ and form a ECP – Ca2+ – ECP bridge, which can serve as the initial structure of growing granules

(Forster & Lewin, 1972; Rudd et al., 1984). The last way of improving the granulation rate ties in with

the proton translocation dehydration theory. Calcium can aid the breakdown of hydrogen bonds

between bacterial cells and, consequently, the neutralization of negatively charged surfaces of the

microorganisms. In other words, Ca2+ can help in inducing dehydration of bacterial cell surfaces (Tay

et al., 2000). Important to raise is that high Ca2+ concentrations of over 600 mg/L may be detrimental,

because of the precipitation of CaCO3 in the granules themselves, which may block intragranular pores,

leading to severe mass transfer limitation and higher ash content in granules and, consequently, to a

lower SMA (Langerak et al., 2000; Yu et al., 2001). If the precipitation occurs outside of the granules,

CaCO3 can provide inert support for bacterial attachment. This leads to granules containing high

amounts of ash accompanied by a relatively high SMA (Kettunen & Rintala, 1998; Liu et al., 2003; Tiwari

et al., 2006).

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MATERIAL AND METHODS

1 EXPERIMENTAL APPROACH Three different experiments were performed. During each experiment, two UASB reactors were

operated under steady state. One reactor (reactor A) was inoculated with alginate (1.3%) encapsulated

anaerobic granular sludge, while the other reactor (control reactor) was inoculated with non-

encapsulated anaerobic granular sludge. A different type of influent was used for every experiment to

test the effect of the applied influent on the alginate matrix. During the first experiment (1), molasse

was used as influent. In the second experiment (2), a synthetic medium, without C-source (synthetic

medium 1) was composed and fed to the reactor, while in the last experiment a synthetic medium with

C- source (synthetic medium 2) was applied as feed for the reactors. During the last experiment,

different variations regarding the encapsulation matrix were evaluated. These variations could be

divided into four parts. The first variation was the encapsulation with 1.3% alginate (3a). The second

variation was the encapsulation with 1.3% alginate, mixed with glucose (3b). The third variation

contained the encapsulation with a concentration of 1.8% alginate, instead of 1.3% (3c), and the last

variation contained an encapsulation matrix, made of 0.5% alginate and carboxymethylcellulose

(CMC)(3d). The main difference between molasse and the synthetic medium was the amount of PO43-

. Table 1 gives an overview of the three conducted experiments.

Before the start of the experiments, both reactors were run for 54 days to let the microbial biomass

adapt to the environment. During this start-up period, reactor A was inoculated with 1.3% alginate

encapsulated granular sludge, while the control reactor was inoculated with non-encapsulated

granular sludge and the influent that was used, was molasse.

Table 1 - Overview of the start-up and the three different experiments

Encapsulation matrix Type of influent Duration (days)

Start-up

1.3% alginate Molasse 54

Experiment 1

1.3% alginate Molasse 15

Experiment 2

1.3% alginate Synthetic medium 1 12

Experiment 3

a 1.3% alginate Synthetic medium 2 9 b 1.3% alginate + D-glucose Synthetic medium 2 8 c 1.8% alginate Synthetic medium 2 11 d Carboxymethylcellulose (CMC) + alginate Synthetic medium 2 15

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2 EXPERIMENTAL SET-UP AND OPERATION

2.1 REACTOR SET-UP During the entire experiment, two identical UASB

set-ups were used with a volume of 2L. Both

reactors were inoculated with anaerobic granular

sludge at a concentration of 447.93 g sludge/2L

reactor, obtained from the Alpro manufactory in

Wevelgem. The sludge of one of the two reactors

(reactor A) was encapsulated in an alginate matrix.

At the bottom of each reactor a marble was placed,

to restrict the loss of sludge. Both reactors were

attached with two clamps to a tripod and were

placed in a spill box. The influent from the influent

vessel was pumped into each reactor at the bottom,

through PVC tubing, with the help of a peristaltic

pump (ProMinent®, flow rate reactor A 22.7

mL/min, control reactor 20.0 mL/min). A timer was

used to control the amount of influent entering the

reactors to ensure this was the same in both

reactors. The effluent, leaving the system at the top

of both reactors, ended up, via PVC tubing, in the

effluent vessels standing in the spill box. The loop

system at the top of each reactor prevented oxygen

from entering the reactors via the effluent tubing.

The recirculation of the sludge through both

reactors was accomplished using a recirculation pump, Leroy Somer Varmeca, that pumped at a

constantly flowrate to obtain the desired upflow velocity of 1m/h. Each reactor was sealed with the

help of a rubber plug that was pierced with a plastic pipette. One end of the pipette came out inside

of the reactor and the other end of the pipette was connected to PVC tubing, outside of the reactor.

Through this tubing, gas could flow out of the reactors and could enter the gas counter. After the

amount of gas was measured, gas was led, via tubing, to an exhaust system. Gas samples were

collected using a syringe with a needle. Between the rubber plug and the gas counter, a serum flask

was connected to the tubing to protect the gas counter from potential incoming liquid. The gas counter

existed of two parts. The first part was a U-shaped tube, connected with the reactors, filled with

mineral oil. However, there was still a headspace of approximately 13 mL left for the gas to enter the

tube. When the gas eventually entered the tube, the mineral oil was being pushed upwards by the gas,

until it reached the eye of a detector, which was the second part of the gas counter. The gas counter

gave a click, and simultaneously released the incoming gas via a tubing to the exhaust system. Knowing

the amount of clicks and knowing the volume of the headspace in the U-shaped tube, the amount of

biogas produced could be calculated. However, only in experiment 2 the gas counters were used to

calculate the amount of biogas produced. Due to gas leaks and failure of the gas counters, the amount

of biogas produced in experiment 1 and 3 were calculated theoretically with the help of the COD

measurements. It should also be noted that the gas counter was an in-house system, which is therefore

not commercially available. Figure 9 gives a picture of the experimental set-up of the control reactor.

Figure 9 - Experimental set-up of the UASB

reactor

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2.2 FEEDSTOCK During the start-up, both reactors were fed with molasses for 54 days, after which they were shut

down for 45 days. After 45 days, both reactors were again fed with molasse for a period of 12 days, to

get them working again. After these 12 days, the first experiment took place in which both reactors

were fed with molasse during 15 days. In the second experiment, the molasses influent from

experiment 1 was replaced by a synthetic medium without glucose, which was fed to the reactors for

12 days. In the last experiment, both reactors were fed with a synthetic medium with glucose. During

each experiment, every Monday, Wednesday and Friday, fresh influent was made and fed to the

reactors. At the start of each experiment, the microbial biomass of both reactors was mixed to ensure

the same microbial community in both reactors. After mixing, half of the sludge was added to the

control reactor, while the other half was used again to make fresh encapsulated alginate beads, which

were, thereafter, added to reactor A.

2.2.1 START-UP During the start-up, both UASB reactors were fed with molasse, obtained from AVEBE in the

Netherlands, which contained 453.48 g COD/kg molasse. The applied OLR was 5 g COD/L/d. To obtain

this OLR, 22.05 g molasses was diluted in 1 L of water4. However, at the initiation of the experiments,

the sludge needed to adapt to the novel feedstock5 and the environment. Therefore, the OLR may not

be too high, which made an OLR of 1 g COD/L/d suitable at the start. Every week, the OLR was increased

with 1 g COD/L/d, until after 5 weeks the desired OLR of 5 g COD/L/d was reached. The OLR was

increased by the adjustment of the amount of incoming influent, which was increased from 200 mL/d

to 1000 mL/d in steps of 200 mL/week.

2.2.2 EXPERIMENT 1 During the first experiment, the same molasse was used as feedstock as during the start-up. By diluting

the molasse 45 times, an OLR of 5 g COD/L/d could be applied immediately.

2.2.3 EXPERIMENT 2 In the second experiment, a synthetic medium was made, which contained a buffer solution, a

macronutrient solution and a trace element solution. No C-source was added to the synthetic medium.

The reason to change from molasse to this medium, was to obtain a lower amount of PO43- in the

reactor. The exact composition of the synthetic medium can be found in Table 2, under the name of

‘Synthetic medium 1’. The anion and cation composition are calculated theoretically and can be found

in Appendix 1 (Table 12).

2.2.4 EXPERIMENT 3 In the last experiment, the same synthetic medium as in 2.2.3 was used, but this time with the addition

of a C-source, in particular D-glucose. Because the sludge was already adapted to the environment

during the start-up, there was no need to slightly increase the OLR, and immediately an OLR of 2.5 g

COD/L/d was applied. To obtain 2.5 g COD/L/d, the influent vessel should contain 2.35 D-glucose/L.

The reason why 2.5 g COD/L/d was applied and not 5 g COD/L/d was the following. Glucose is the

4 Diluting 22.05 g molasse in 1L water corresponds to a dilution factor of 45 5 The sludge came from the Alpro manufactory in Wevelgem, which was stored in a cold room of 4°C

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easiest carbon source for microorganisms to degrade. It would be degraded very fast and possible

acidification could occur, because the acetogenic bacteria couldn’t degrade the produced VFA fast

enough with accumulation of VFA as result. Adding 2.5 g COD/L/d instead of 5 g COD/L/d reduces this

risk. The composition of this medium is listed in Table 2 under the name ‘Synthetic medium 2’.

Table 2 - Composition of synthetic medium 1 (without C-source) and synthetic medium 2 (with C-

source)

Synthetic medium 1 Synthetic medium 2

Carbon source (g/L)

D-glucose 0 2.35

Buffer (g/L)

KH2PO4 0.07 0.07 K2HPO4 0.09 0.09 NaHCO3 0.84 0.84 KHCO3 1.00 1.00 K2HPO4.3H2O 0.11 0.11

Macronutrients (g/L)

CaCl2.2H2O 0.2 0.2 MgCl2.6H2O 0.1 0.1 Fe2(SO4)3 0.1 0.1 NH4Cl 0.5 0.5

Trace elements solution (μg/L)

NiSO4.6H2O 500 500 MnCl2.4 H2O 500 500 FeSO4.7H2O 500 500 ZnSO4.7H2O 100 100 H3BO3 100 100 Na2MoO4.2H2O 50 50 CoCl2.6H2O 50 50 CuSO4.5H2O 5 5

(Aiyuk & Verstraete, 2004; Vrieze et al., 2013)

2.3 SLUDGE INOCULUM Both reactors were inoculated with anaerobic granular sludge derived from the Alpro manufactory.

The volatile suspended solids (VSS) content of the sludge was 44.65 g VSS/kg sludge, while the desired

amount of VSS in the reactors was 10 g VSS/L. Therefore, to each reactor, 447.93 g sludge was added.

However, at the beginning of each experiment, the sludge of reactor A was encapsulated in an alginate

matrix.

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2.3.1 START-UP During the start-up, the sludge of reactor A was encapsulated in a 1.3% (w/v) alginate matrix. First,

73.52 g of CaCl2.2H2O was added to 1 L of distilled water to make a 0.5 M CaCl2 buffer (7.3% (w/v) CaCl2

solution). Next, 447.93 g of sludge was added to 552.07 mL tap water to obtain 20 g VSS/L6. To this

solution, 15 g of sodium alginate was added to obtain a final concentration of 1.5% sodium alginate or

1.3% alginate. After mixing with a magnetic stirrer, the alginate beads were formed with the help of a

micropipette of 1 mL and dripped in the CaCl2 buffer7. Reactor A had a volume of 2 L, thus adding a

suspension of 1 L alginate beads with a content of 20 g VSS/L and 1 L of tap water to a reactor volume

of 2 L, made a final reactor content of 10 g VSS/L.

2.3.2 EXPERIMENT 1 In the first experiment, the encapsulation of the sludge was done in the exact same way as in section

2.3.1.

2.3.3 EXPERIMENT 2 In the second experiment, the encapsulation of the sludge was done in the exact same way as in section

2.3.1.

2.3.4 EXPERIMENT 3 In the third and last experiment, four different variations on the encapsulation of the granules were

tested. It should be noted that at the start of experiment 3, each reactor contained only 368 g sludge,

in contrast to the 447.93 g sludge at the beginning of experiment 1. In the first part of experiment 3,

the encapsulation of the sludge was conducted in the same way as in 2.3.1. The second part of the

experiment contained the first variation. Alginate beads were prepared in the same way as during the

start-up. However, before dripping the sodium alginate-sludge solution into the CaCl2 buffer, 5 g/L of

D-glucose was added to this solution. The hypothesis of the addition of glucose was to give the

microorganisms an initial and easy to degrade C-source to avoid the degradation of the alginate matrix

by the biomass. After a certain moment, channels are made in the beads, which can deliver glucose

from the influent to the granules, which eliminates the need of degrading the alginate matrix. Before

the encapsulation started, 87 g fresh granular sludge was added to each reactor to obtain 447.93 g

sludge per reactor again. In the third part of the experiment, again alginate encapsulated granular

sludge was applied, but this time with an alginate concentration of 1.8% instead of 1.3%. Due to some

sludge losses during the production of the alginate beads of the second part, each reactor contained

415 g of sludge instead of 447.93 g sludge. In the last part, an article of Youngsukkasem et al., 2012

was called upon to create an encapsulation matrix with a concentration of 0.5% alginate and 2.6% of

CMC. First the sludge was suspended in a 2.6% (w/v) CaCl2 solution, containing 2.6% CMC, with a

volume ratio of digesting sludge to CaCl2 and CMC solution of about 1:18. The degree of substitution

(DS) of the CMC was 0.9 and was added to increase the viscosity. This solution was further dropped

into a 0.6% sodium alginate (i.e. 0.5% alginate) solution containing 0.1% (v/v) Tween 20 to improve the

permeability of the encapsulation matrix. The resulting solution was stirred. After stirring, the beads

6 Alginate beads with a VSS content of 20 g VSS/L ensures a more concentrated biomass per bead. 7 Alginate is a polymer, which can crosslink with divalent cations, such as Ca2+, to form a gel. 8 448 g sludge and 52 mL water were added to 500 mL of CaCl2 and CMC solution. This will give an end concentration in the reactor of 10 g VSS/L

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were washed with distilled water and allowed to harden in a 1.3% (w/v) CaCl2 solution for 20 minutes.

Before the encapsulation of the last part of experiment 3 started, 58 g of fresh granular sludge was

added to each reactor to obtain 447.93 g sludge per reactor again.

2.4 VOLUMETRIC METHANE PRODUCTION AND METHANE YIELD The volumetric methane production in mL CH4/L/d and the methane yield in % were calculated for

each experiment. In the second experiment, the amount of methane gas produced was determined

with the help of the gas counters. In experiment 1 and 3 the amount of methane gas produced was

calculated theoretically, without the use of gas counters, by multiplying the consumed COD with

350mL CH4 per gram of COD9. The methane yield was calculated for experiment 1 and 3 by dividing the

consumed COD per day by the actual added COD per day, not the theoretical added COD. No methane

yields were calculated for experiment 2. This can be explained as follows. Both influent vessels didn’t

contain any COD, because no carbon source was added to the synthetic medium. Therefore, the added

COD per day equals zero. If the methane yield is calculated, one need to divide by the added COD,

which is zero and division by zero is undefined.

3 ANALYTICAL TECHNIQUES

3.1 TOTAL KJELDAHL NITROGEN The total Kjeldahl nitrogen (TKN) was analyzed according to Standard methods (4500-Norg B; APHA,

1992). The total organic nitrogen was determined as the difference between TKN and the total

ammonium nitrogen (TAN). Following equation is used to calculate the total organic nitrogen present

in the sample:

𝑂𝑟𝑔­𝑁 (𝑚𝑔 𝑁/𝐿) = 𝑇𝐾𝑁 − 𝑇𝐴𝑁

First, sample preparation for the TKN analysis need to be done. One mL (whether or not diluted)

sample was added to 19 mL of distilled water and placed in a Kjeldahl tube. This was done in triplicate.

The dilution was necessary to obtain a concentration between 9 and 250 mg NH4+-N/L in the tube.

Next to the samples, also three blanks, filled with 20 mL of distilled water, were analyzed. Subsequently

10 mL of sulfuric acid and one Kjeldahl tablet was added to each tube. A Kjeldahl tablet contained 5 g

K2SO4, 0.50 g CuSO4.5H2O/tablet. After preparation of the samples, the tubes were preheated in the

destruction block (150°C) to convert all the nitrogen to ammonia. Next, the temperature was increased

up to 400°C and samples were digested for 2 hours at this temperature. After 2 hours, samples were

cooled down and distillation could take place in the distillation apparatus (Gerhardt, Vadopest 30S,

Königswinter, Germany). The samples were placed in the left side of the machine and a recipient with

20 mL of a boric acid indicator with a pH of 5.3, was placed in the right side of the machine. Ammonia

was distilled, condensed and further dissolved in the boric acid solution with indicator. After

distillation, the samples were titrated with HCl with the help of an automatic titration unit

9 The consumption of 1 g COD yields 350 mL CH4

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(Metrohm,719S Titero, Herisau, Switzerland) to determine the total amount of NH3 present in the

sample. The following equation was used to determine mg TKN-N per liter of sample:

𝑇𝐾𝑁 (𝑚𝑔 𝑁/𝐿) =(𝐴 − 𝐵) ∗ 𝑇 ∗ 14.001 ∗ 1000 ∗ 𝑓

𝑉𝑠𝑎𝑚𝑝𝑙𝑒

A: volume HCI titrated for the sample (mL)

B: volume HCI titrated for the blank (mL)

F: dilution factor

T: titer of the HCI solution (0.02 N or adapted)

Vsample: volume of the sample in mL (mL)

3.2 TOTAL AMMONIA NITROGEN The total ammonia nitrogen (TAN) was measured to determine, together with the TKN, the total

amount of organic nitrogen. Three sample replicates and three blanks were prepared. One mL of

sample was added to 9 mL of distilled water and placed in a Kjeldahl tube. The three blanks contained

20 mL of distilled water. Samples were diluted to obtain a concentration between 5 and 300 mg NH4+-

N/L in the tube. Subsequently, 0.4 g of MgO was added to each sample. After the sample preparation,

samples were placed one by one in the left side of the distillation apparatus (Gerhardt, Vadopest 30S,

Königswinter, Germany) and a recipient with 20 mL of a boric acid indicator with a pH of 5.3, was

placed in the right side of the machine. After distillation, the samples were titrated with HCl with the

help of an automatic titration unit (Metrohm,719S Titero, Herisau, Switzerland) to determine the total

amount of NH3 present in the sample. The following equation was used to determine mg TAN-N per

liter of sample:

𝑇𝐴𝑁 (𝑚𝑔 𝑁/𝐿) =(𝐴 − 𝐵) ∗ 𝑇 ∗ 14.001 ∗ 1000 ∗ 𝑓

𝑉𝑠𝑎𝑚𝑝𝑙𝑒

A: volume HCI titrated for the sample (mL)

B: volume HCI titrated for the blank (mL)

F: dilution factor

T: titer of the HCI solution (0.02 N or adapted)

Vsample: volume of the sample in mL (mL)

3.3 TOTAL SUSPENDED SOLIDS AND VOLATILE SUSPENDED SOLIDS Solids analyses were performed by centrifugation of a known sample volume and by weighing the

difference between the pellet before and after drying at 105°C (TSS) and incinerating at 550°C (VSS).

The total suspended solids (TSS) are the solid residues (both organic and inorganic fraction) left in a

vessel after separation from the aqueous phase by means of centrifugation. The volatile suspended

solids (VSS) represent the amount of organic material, present in the sample. First, a crucible was

placed in the oven (Memmert, Schwabach, Germany) at 103-105°C for 1 hour. Next, the crucible was

cooled down in the desiccator, after which the initial dried crucible was weighed (A). The sample was

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placed in a falcon tube, which was centrifugated during 10 minutes at 7830 g. The supernatant was

poured away, and the pellet was washed with distilled water, after which it was again centrifugated.

The supernatant was again poured away, and the pellet was transferred to the crucible. After weighing

the filled crucible (B), the sample was evaporated by placing it overnight, in the oven at 103-105°C.

The crucible was cooled down to balance temperature and was again weighed (C). Subsequently, the

crucible was placed in the muffle oven (Nabertherm, GmbH, Lilienthal, Germany) at 550°C for at least

1.5 hours to analyze the VSS. The sample was again cooled down in the desiccator and was again

weighed (D). The following equations were used to determine the amount of TSS and VSS in the

sample:

𝑚𝑔 𝑇𝑜𝑡𝑎𝑙 𝑠𝑢𝑝𝑠𝑒𝑛𝑑𝑒𝑑 𝑠𝑜𝑙𝑖𝑑𝑠 (𝑇𝑆𝑆)

𝐿=

(𝐶 − 𝐴) ∗ 106

𝑠𝑎𝑚𝑝𝑙𝑒 𝑣𝑜𝑙𝑢𝑚𝑒 (𝑚𝐿)

𝑚𝑔 𝑣𝑜𝑙𝑎𝑡𝑖𝑙𝑒 𝑠𝑢𝑝𝑠𝑒𝑛𝑑𝑒𝑑 𝑠𝑜𝑙𝑖𝑑𝑠 (𝑉𝑆𝑆)

𝐿=

(𝐶 − 𝐷) ∗ 106

𝑠𝑎𝑚𝑝𝑙𝑒 𝑣𝑜𝑙𝑢𝑚𝑒 (𝑚𝐿)

3.4 TOTAL SOLIDS AND VOLATILE SOLIDS The total solids (TS) represent the total dry matter content present in the sample, both the organic as

the inorganic fraction, while the volatile solids (VS) only represent the organic fraction of the sample.

The same method that was used for the TSS and VSS measurement, was used for the TS and VS

measurement. However, there was no need for centrifugation of the samples, as both soluble and

suspended materials were included. The following equations were used to determine the amount of

TS and VS in the sample:

% 𝑡𝑜𝑡𝑎𝑙 𝑠𝑜𝑙𝑖𝑑𝑠 (𝑇𝑆) = (𝐶 − 𝐴) ∗ 100

𝐵 − 𝐴

% 𝑣𝑜𝑙𝑎𝑡𝑖𝑙𝑒 𝑠𝑜𝑙𝑖𝑑𝑠 (𝑉𝑆) = (𝐶 − 𝐷) ∗ 100

𝐵 − 𝐴

3.5 PH On Monday, Wednesday and Friday, when fresh medium was made, the pH of the effluent in the

reactors was also measured. This was done with the Consort C5010 pH probe. At the beginning of

every week, the pH probe was calibrated. The calibration was accomplished with the help of three

standard calibration buffers with a pH of respectively 4, 7 and 9.

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3.6 CHEMICAL OXYGEN DEMAND The chemical oxygen demand (COD) is the amount of oxygen required to oxidize organic carbon

completely to CO2 by chemical means. The COD of the fresh made influent, the old influent and the

effluent in the vessel were analyzed with Nanocolor® kits (CODE; Macherey-Nagel). Depending on the

COD density in the concerned samples, Nanocolor tubes with different concentration ranges were

chosen (COD15000: 1-15 g O2/L, COD1500: 100-1500 mg/L, COD160: 15-160 mg/L, COD40: 2-40mg/L).

First, the samples were added to the Nanocolor tubes. Next, the Nanocolor tubes (with the addition of

the samples) were put in a destruction block with a temperature of 148°C, for 2 hours. After heating,

the tubes were shaken and were cooled for 30 minutes. The COD content was determined with the

help of the Nanocolor 500D spectrophotometer (Machery-Nagel, Nanocolor 500D, Düren, Germany).

3.7 BIOGAS COMPOSITION The composition of the biogas produced by the two reactors, i.e., CH4, CO2, H2 and H2S, was analyzed

with a Compact GC (Global Analyzer Solutions, Breda, The Netherlands), equipped with a Molsieve 5A

pre-column and Porabond column (CH4, O2, H2 and N2), and a Rt-Q-bond pre-column and Rt-QS-bond

column (CO2, N2O and H2S). Concentrations of gases were determined by means of a thermal

conductivity detector. The LOQ (Limit Of Quantification) for each gas is around 0.05% (500 ppm). The

analysis of the biogas compounds was carried out by three methods. Each method measured one of

the three compounds. The first method measured CH4, N2, O2 and H2, the second method measured

CO2 and N2O, and the last method was responsible for the amount of H2S. A gas sample of 10 mL was

taken with a syringe, and was placed on a rubber stopper to avoid mixing of biogas with the air. During

every method, approximately 2 mL of gas was injected in the Compact GC, after which the amount of

each compound could be read of the computer screen.

3.8 VOLATILE FATTY ACIDS The volatile fatty acids (VFA) (C2-C8) analysis was performed according to Andersen et al., 2014. The

C2-C8 fatty acids (including isoforms C4-C6) were measured by gas chromatography (GC-2014,

Shimadzu®, The Netherlands) with a DB-FFAP 123-3232 column (30m x 0.32 mm x 0.25 µm; Agilent,

Belgium) and a flame ionization detector (FID). Two mL of sample was conditioned with 0.500 mL 50

% H2SO4, 0.4 g of NaCl and 0.400 mL 2-methyl hexanoic acid as internal standard for further extraction

with diethyl ether. The prepared sample (1 µL) was injected at 280°C with a split ratio of 60 and a purge

flow of 3 mL/min. The oven temperature increased by 6°C/min from 110°C to 158°C and by 8°C/min

from 158°C to 175°C where it was kept for 1 minute. The FID had a temperature of 220°C. The carrier

gas was nitrogen gas at a flow rate of 2.49 mL/min. The detection limit of acetate was 30 mg/L, of

propionate 10 mg/L and of the other fatty acids 2 mg/L. The upper detection limit was 1000 mg/L.

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3.9 CATIONS Na+, NH4

+, K+, Mg2+ and Ca2+ were determined on a 761 Compact Ion Chromatograph (IC) (Metrohm,

Switzerland), equipped with a conductivity detector. Ten mL of the samples were first centrifugated at

17 090 g for 10 minutes. The supernatant was filtered with a 0.20 μm filter. The filtered samples were

diluted 50x by adding 500 μL of the filtered samples to 9.5 mL of MQ water. The dilution was necessary,

because the detection limit of the IC ranged from 2 to 100 mg cation/L. The obtained samples were

placed in the autosampler of the IC. The IC contained a silica gel with carboxyl groups (stationary

phase), which retains the different cations during a determined period (retention time). Next, cations

are eluted from the column by the eluent (mobile phase). Cations are quantified based on conductivity

by means of a calibration curve.

3.10 ANIONS Cl-, NO3

-, PO43- and SO4

2- were determined on a 761 Compact Ion Chromatograph (IC) (Metrohm,

Switzerland), equipped with a conductivity detector. Ten mL of the samples were first centrifugated at

17 090 g for 10 minutes. The supernatant was filtered with a 0.45 μm filter. The filtered samples were

diluted 40x by adding 250 μL of the filtered samples to 9.750 mL of MQ water. The dilution was

necessary, because the detection limit of the IC ranged from 0.5 to 100 mg anion/L. The obtained

samples were placed in the autosampler of the IC. The IC contained a silica gel with carboxyl groups

(stationary phase), which retains the different cations during a determined period (retention time).

Next, cations are eluted from the column by the eluent (mobile phase). Cations are quantified based

on conductivity by means of a calibration curve.

4 BIOCHEMICAL METHANE POTENTIAL (BMP) TEST Biochemical methane potential (BMP) tests were performed in batch reactors, each with a working

volume of 80 mL and a headspace of 40 mL. The experiment was operated for 20 days under mesophilic

conditions (34°C). The inoculum consisted of anaerobic granular sludge. The test contained 6 serum

flasks. To three flasks, a specific amount of 1.3% alginate encapsulated anaerobic granular sludge was

added to obtain a final VS concentration of 10 g VSS/L. To the other remaining three flasks, a specific

amount of non-encapsulated anaerobic granular sludge was added, also to obtain a final concentration

of 10 g VSS/L. Next, molasse was added with a substrate to inoculum ratio of 0.5 g COD/g VSS. Finally,

tap water was added to acquire a total liquid volume of 80 mL in each bottle. After inoculum and

substrate addition, the serum flasks were sealed to avoid air intrusion, and connected to air-tight gas

columns by means of an air-tight needle. These gas columns were placed in a water bath containing a

solution of distilled water and HCl at pH < 4.3 to avoid CO2 in the biogas from dissolving. The serum

flasks were incubated in a linear shaking water bath (Grant, GLS Aqua 18 Plus, Shepreth, England) at

the chosen temperature. Volumetric biogas production was evaluated by means of water

displacement in the gas columns. Figure 10 shows a schematic overview of the BMP set-up. Biogas

production was measured on daily basis for 20 days, until the biogas production didn’t change anymore

for more than 3 days. Biogas volumes were reported at standard temperature (273 K) and pressure

(101 325 Pa) (STP) conditions. Biogas composition was evaluated at the end of the experiment with

the compact GC. The volumetric gas production of methane was expressed as the volume of methane

per liter per day (mL CH4/L/d).

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5 BATCH TESTS

5.1 SHEAR STRESS BATCH TEST A batch test was performed to test whether the alginate matrix was resistant towards shear stress,

present in the reactor. This test also gave information about the degradation of the alginate matrix by

the microorganisms in the granules. The batch test contained 32 serum flasks. The first 18 serum flasks

contained 10 g VSS/L of 1.3% alginate encapsulated anaerobic granular sludge. The other 18 flasks

were filled with 1.3% alginate beads that didn’t contain any sludge, but only tap water. To imitate

reactor conditions in the flasks, each flask was filled with effluent of the reactors of experiment 1, with

molasse as influent. The ion concentration of the effluent can be found in Table 3. Nine of the 18 serum

flasks, containing the alginate encapsulated sludge, and nine of the 18 serum flasks, containing

aqueous alginate beads, were placed on a shaker (120 rpm) for 14 days to imitate the shear stress in

the reactor. Table 4 shows an overview of the set-up of the batch test. On day 0, 3, 7, 11 and 14, the

content of each of the serum flasks was placed individually on a grid of 1 cm2 to see whether the beads

decreased in size or not. After taking a photograph, the flasks were again filled with the same beads

and effluent as they contained before. Figure 11 shows the difference between the sludge containing

alginate beads (left) and the water containing alginate beads (right), placed on a mm grid with a total

surface of 0.25 cm2.

Table 3 – Cation concentrations in mg/L of the effluent that was added to the serum flasks of the

shear stress batch test

Na+ NH4+ K+ Ca2+ Mg2+ PO4

3-

Effluent (mg/L) 92 493 1927 1927 44 237

Figure 10 – Schematic overview of the BMP set-up

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Table 4 - Overview of the set-up of the shear stress batch test

Shaking (+) Shaking (-)

Sludge (+) 9 flasks 9 flasks Sludge (-) 9 flasks 9 flasks

Figure 11 - Sludge containing alginate beads (left) and water containing alginate beads (right)

5.2 POTASSIUM AND PHOSPHATE BATCH TEST The second batch test was used to evaluate if the 1.3% alginate matrix was affected by different

concentrations of PO43- and K+. Eight different treatments were conducted, with 3 replicates of each

treatment. This provides a total of 24 serum flasks. Each serum flask was filled with 40 mL of synthetic

medium (section 2.2.3, without D-glucose) and a certain amount of K+ (in the form of KCl) and/or a

certain amount of PO43- (in the form of Na2HPO4). Table 5 gives an overview of the different

concentrations of K+ and PO43- of the different treatments, as well as the concentrations of Cl- and Na+.

The 24 serum flasks were placed on a shaker (120 rpm) to imitate reactor shear conditions, for 24 days.

On day 0, 2, 7, 10, 14 and 24 the content of each of the serum flasks were placed individually on a mm

grid with a total surface 1 cm2 to see whether the beads decreased in size or not. After taking a

photograph, the flasks were again filled with the same beads as they contained before.

Table 5 - Overview of the different potassium and phosphate treatments

K+ (g/L) Cl- (g/L) Na+ (mg/L) PO43- (mg/L)

Treatment 110 n.a.* 37.9 49 n.a.* Treatment 2 0.875 0.80 0 0 Treatment 3 1.75 1.60 0 0 Treatment 4 3.5 3.20 0 0 Treatment 5 0 0 98 202.5 Treatment 6 0 0 196 405 Treatment 7 0 0 392 810 Treatment 8 1.75 1.60 196 405

*n.a. = not available

10 Values for tap water derived from The open University

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RESULTS

1 CHARACTERIZATION OF INOCULUM The TSS and VSS concentrations of the fresh granular sludge were measured in quadruplicate (Table

6). The TSS represent both the inorganic and organic fraction of the sludge, while the VSS only include

the organic material of the sludge. Both anion and cation measurements were also conducted on the

granular sludge in triplicate (Table 6).

Table 6 - Mean TSS and VSS values of the granular sludge inoculum in g/kg and their associated

standard deviations and mean cation and anion concentrations in mg/L of the granular sludge and

their associated standard deviations.

TSS

Sludge (g/kg) 51.6 ± 1.7

VSS

Sludge (g/kg) 44.7 ± 1.5

Cations

Na+ NH4+ K+ Ca2+ Mg2+

Sludge (mg/L) 103.6 ± 25.8 106.5 ± 26.4 1702.7 ± 85.6 19.9 ± 34.6 105.6 ± 4.1

Anions

Cl- PO43- SO4

2- NO3-

Sludge (mg/L) 145.2 ± 3.6 93.7 ± 9.1 254.4 ± 15.1 57.9 ± 0.5

2 CHARACTERIZATION OF MOLASSE The total organic ammonia nitrogen content was calculated by determining the TKN and the TAN in

triplicate. Measurements of the TS and VS of the molasse were analyzed in quadruplicate, while COD

measurements were done in duplicate. Anion, as well as cation triplicate measurements were also

conducted on the molasse (Table 7).

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Table 7 - TAN, TKN, total organic nitrogen of molasse in g N/L, TS, VS and COD values of molasse and

their associated standard deviations in g/kg and the mean cation and anion measurements of the

molasse and their associated standard deviations in mg/L.

Molasse

TKN (g N/L) 179.2 ± 73.1

TAN (g N/L) 6.0 ± 2.7

Total organic nitrogen (g N/L) 173.2 ± 73.2

TS (g/kg) 549.7 ± 1.9

VS (g/kg) 340.4 ± 7.7

COD (g COD/kg) 453.5 ± 16.4

Cations

Na+ NH4+ K+ Ca2+ Mg2+

Molasse (mg/L) 2749 ± 55 1743 ± 39.99 762 ± 436 122 ± 6 4529 ± 228

Anions

Cl- PO43- SO4

2- NO3-

Molasse (mg/L) 8800 ± 650 10 750 ± 245 7770 ± 170 2247 ± 23

3 START-UP Due to technical problems with the gas counters and the COD measurements, no reliable results of

biogas production could be obtained. After the inoculation of the reactor, the alginate matrix in reactor

A was completely disintegrated after 30 days (Figure 12).

The initial pH in reactor A was 6.39 and in the

control reactor 6.83, which showed a difference of

0.44 between the initial pH of both reactors. After

24 days, both reactors reached constant pH values

(7.28 ± 0.09 in reactor A and 7.26 ± 0.09 in the

control reactor), with only a limited difference of

0.02 between both reactors (Figure 13).

The total VFA concentration refers to the sum of

the carbon concentrations of acetate, propionate,

butyrate, iso-butyrate, valerate, iso-valerate,

caproate and iso-caproate 11 . Throughout the

entire start-up, VFA concentrations in both

reactors remained very low, with total VFA

concentrations not exceeding 30 mg C/L. These

low VFA values are likely not causing any changes

in pH.

11 Due to the low pH created when extracting the samples, VFA are converted into the free acid form.

Therefore, sum of all VFA concentrations can only be made if all the values are converted to mg C/L.

A Day 0 A Day 30 Control Day 0

Figure 12 - Evolution of the disintegration of

the alginate matrix during the start-up

(alginate 1.3%) in reactor A (left) and the

granular sludge on day 1 in the control reactor

(right)

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Figure 13 - Graphs of the start-up of the reactors (1.3% alginate, molasse, reactor A: encapsulated

granules, control reactor natural granules): course of the pH of reactor A and the control reactor (top),

course of total VFA concentration of reactor A and of the control reactor (bottom)

0

250

500

750

1000

1250

1500

1750

2000

2250

2500

0 5 10 15 20 25 30 35 40 45 50

Cat

ion

co

nce

ntr

atio

n(m

g/L)

Time (Days)

Figure 14 - Graph of the cation concentrations during the start-up: Na+ encapsulated granules (---), Na+

natural granules (···), NH4+ encapsulated granules (---), NH4

+ natural granules (···), K+ encapsulated

granules (---), K+ natural granules (···), Ca2+ encapsulated granules (---), Ca2+ natural granules (···), Mg2+

encapsulated granules (---), Mg2+ natural granules (···)

6,20

6,40

6,60

6,80

7,00

7,20

7,40

7,60

7,80

0 5 10 15 20 25 30 35 40 45 50

pH

Time (Days)

0

5

10

15

20

25

30

0 5 10 15 20 25 30 35 40 45 50

Tota

l VFA

co

nce

ntr

atio

n(m

g C

/L)

Time (Days)

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The Na+, NH4+ and the Mg2+ concentrations in both reactors remained lower than 500 mg/L. On the

contrary, the K+ concentrations of both reactors were much higher, with concentrations above 1000

mg/L, but they were following a similar course in both reactors. The Ca2+ concentrations in the control

reactor remained constant during the entire start-up with an average value of 130 ± 26 mg/L. In

contrast, the initial Ca2+ concentration in reactor A was 12 times higher than the initial Ca2+

concentration in the control reactor. After 10 days, the Ca2+ concentration in reactor A started to

decrease until after 30 days, a constant average Ca2+ concentration of 94 ± 26 mg/L was reached (Figure

14).

4 REACTOR EXPERIMENTS

4.1 DISINTEGRATION OF THE ALGINATE MATRIX The decrease in the level of sludge in reactor A can be explained by the disintegration of the alginate

matrix. In other words, the more the sludge level decreased, the more the alginate matrix was

disintegrated (Figure 15). For each experiment, a gradually disintegration of the matrix was observed.

In experiment 1 (1), the entire matrix was broken down after 10 days, in experiment 2 (2) after 13 days,

in the third part of experiment 3 (3c) after 7 days and in the last part of experiment 3 (3d) after 15

days. In experiment 2 and in the last part of experiment 3, the encapsulated granules were floating.

After 3 to 4 days, the beads sunk again.

Experiment 1, 1.3% alginate

A Day 0 A Day 7 A Day 10 Control Day 0

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Experiment 2, 1.3% alginate

A Day 0 A Day 3 A Day 6 A Day 10 A Day 13 Control Day 0

Experiment 3c, 1.8% alginate

A Day 0 A Day 4 A Day 7 Control Day 0

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Experiment 3d, 0.5% alginate + CMC

A day 0 A Day 2 A Day 6 A Day 8 A Day 9 A Day 13 A Day 14 A Day 15 Control Day 0

Figure 15 – Evolution of the disintegration of the alginate matrix in reactor A (left) and the granular

sludge of the control reactor on day 0 (right) of experiment 1, experiment 2, experiment 3 part 3 and

4

4.1 PH The two red lines in Figure 16 represent the optimal pH range for AD. The initial pH values of the

reactors of experiment 1 (1) were both 7.36. Between day 1 and day 7, the pH in reactor A tended to

be on average 0.29 ± 0.1 lower than in the control reactor. From day 7, pH values of both reactor A

and the control reactor were constant with values of 7.19 ± 0.05 and 7.31 ± 0.08, respectively. In

experiment 2 (2), the pH of the control reactor was little above the optimal upper limit for AD with a

constant value of 7.58 ± 0.02. The pH values of reactor A were lower with values of approximately 6.82

± 0.07. During the first, the second and the third part of experiment 3 the pH values of both reactors

stayed under the optimal lower limit for AD. In the first part of experiment 3 (3a), the pH in reactor A

was on average 0.19 ± 0.1 lower than the pH in the control reactor. At the start of the second part of

experiment 3 (3b) a severe drop in pH in reactor A from 6.64 to 6.02 was observed, after which the pH

increased again to value of 6.63. The pH in the control reactor stayed constant with a value of 6.72 ±

0.13. During the third part of experiment 3 (3c), the pH of the control reactor stayed constant with pH

values of 6.63 ± 0.03. The pH in reactor A remained at 6.58 ± 0.07, except after 5 days, where the pH

value decreased to a value of 6.42, after which it increased again. In the last part of experiment 3 (3d),

the pH values of both reactors started low (6.43 in reactor A and 6.56 in the control reactor), but

increased over time. After 8 days, reactor A reached a value of 6.96 and the control reactor a value of

7.13. After 8 days the pH values decreased again to values of 6.59 in reactor A and 6.56 in the control

reactor at the end of the last experiment (Figure 16).

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4.2 VOLATILE FATTY ACIDS The graph of Figure 17 plotted the total VFA concentration in mg C/L as a function of time. The total

VFA concentration refers to the sum of the carbon concentrations of acetate, propionate, butyrate,

iso-butyrate, valerate, iso-valerate, caproate and iso-caproate. The most abundant VFA throughout

the experiments were acetate, propionate and butyrate. In the first experiment (1), the total VFA

concentration in reactor A started at 24 mg C/L, and increased to a value of 332 mg C/L on day 3, which

explains the drop in pH on day 3. The VFA concentrations of the control reactor remained below the

detection limit during the entire experiment, except at the start of the experiment and on day 7.

However, on day 3 a drop in pH in the control reactor could be observed, but the accumulation of VFA

was not the cause. During entire experiment 2 (2), total VFA concentrations of the control reactor were

approaching zero (6 ± 1 mg C/L), which is consistent with the constant pH course of the control reactor.

The total VFA concentration of reactor A started at 37 mg C/L, after which the concentration decreased

to a value of approximately 10 mg C/L after 9 days. It should be noted that the only VFA concentration

above the detection limit was caproate. The VFA concentrations of the control reactor in the first part

of experiment 3 (3a) were below detection limit, except on day 2 of experiment 3a, where the total

VFA concentration reached a value of 15 mg C/L. Such low VFA concentrations aren’t likely to cause

pH variations. However, the pH value of the control reactor decreased after 2 days with a value of

more than one pH unit. On the other hand, after 2 days, a high total VFA concentration (264 mg C/L)

was reached in reactor A. This is in line with the pH drop after day 2 of experiment 3a in reactor A.

After day 2, the amount of VFA in reactor A gradually decreased again, while the pH gradually increased

again. In the second part of experiment 3 (3b), after 3 days, a very high total VFA concentration (535

mg C/L) was reached in reactor A. This corresponds with the large pH drop in reactor A (6.02) after 3

days. After 3 days, the total VFA concentration in reactor A reached approximately zero again (6 ± 1

mg C/L). During the entire part 2 of experiment 3, VFA concentrations in the control reactor remained

close to zero, which is in line with the constant pH values in the reactor. During the entire third part of

Figure 16 - The pH of reactor A (containing granules encapsulated in alginate) and in the control

reactor (containing natural granules) during the different experiments

6,00

6,20

6,40

6,60

6,80

7,00

7,20

7,40

7,60

7,80

8,00

0 5 10 15 20 25 30 35 40 45 50 55 60 65 70

pH

Time (Days)

1 2 3a 3b 3c 3d

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40

experiment 3 (3c), the total VFA concentrations in the control reactor were below the detection limit.

From day 3 to day 5 of experiment 3c, the total VFA concentration in reactor A was on average 148 ±

7 mg C/L. After 5 days, the total VFA concentration started to decrease to reach values below the

detection limit towards the end of the experiment. This is in line with the pH increase in reactor A,

after 5 days. During the entire last part of experiment 3 (3d), the total VFA concentrations in both

reactor A and B, reached approximately zero with values of 5 ± 4 mg C/L and 4 ± 3 mg C/L, respectively,

except after 2 days of the experiment, were the total VFA concentration in reactor A reached a value

of 61 mg C/L (Figure 17).

4.3 VOLUMETRIC METHANE PRODUCTION The volumetric methane production of both reactors started to increase after the start of the

experiment 1 (1). After day 2, the control reactor produced on average 427 ± 18 mL CH4/L/d more than

reactor A. Reactor A produced on average 1033 ± 218 mL CH4/L/d during experiment 1. At a certain

moment, on day 10, the tube of the influent pump of the control reactor came outside of the feed,

which, thus, couldn’t pump feed into the reactor anymore. The control reactor, therefore, didn’t get

any feed for several hours. This explains the sudden decrease in methane production in the control

reactor from 1578 mL CH4/L/d on day 10 to 864 mL CH4/L/d on day 14. The average volumetric

methane production of the control reactor, when excluding the data from day 14, was 1264 ± 373 mL

CH4/L/d. At the start of experiment 2 (2) the control reactor produced very little methane (10 ± 3 mL

CH4/L/d). After 6 days, the control reactor didn’t produce methane anymore. On the other hand,

reactor A produced methane during 8 days, with the highest volumetric methane production after 5

days (76 mL CH4/L/d). After 7 days, the volumetric methane production in reactor A also reached a

value of zero and no methane was produced anymore. Throughout entire experiment 3, a lower

volumetric methane production in both reactors can be observed, compared to the volumetric

methane production in experiment 1. In the first part of experiment 3 (3a) the volumetric methane

1 2 3 3 3c 3d

0

50

100

150

200

250

300

350

400

450

500

550

600

0 5 10 15 20 25 30 35 40 45 50 55 60 65 70

Tota

l VFA

co

nce

ntr

atio

n(m

g C

/L)

Time (Days)

Figure 17 – Total VFA concentration in reactor A (containing granules encapsulated in alginate) and

in the control reactor (containing natural granules) during the different experiments

1 2 3a 3b 3c 3d

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41

production of both reactors remained constant. The average volumetric methane production in

reactor A was 624 ± 35 mL CH4/L/d and in the control reactor 729 ± 118 mL CH4/L/d. In the beginning

of the second part of experiment 3 (3b), reactor A only produced 267 mL CH4/L/d, while the control

reactor produced 511 mL CH4/L/d. The low amount of methane in reactor A can be associated with the

drop in pH after 4 days. Towards the end, both reactors produced a similar amount of methane (383

mL CH4/L/d in reactor A and 299 mL CH4/L/d in the control reactor). During the third part of experiment

3 (3c), the volumetric methane production in the control reactor fluctuated between 450 and 600 mL

CH4/L/d, while the volumetric methane production in reactor A gradually decreased over time. At the

start, 652 mL CH4/L/d was produced, while after 10 days, only 273 mL CH4/L/d was produced in reactor

A. The volumetric biogas production values in the last part of experiment 3 (3d) were similar in both

reactors. Almost no difference can be seen between both reactors, while during most of the time of

the other experiments the methane production in reactor A lagged behind the methane production in

the control reactor. After 8 days, a drop in methane production can be observed in both reactors (636

to 196 mL CH4/L/d in reactor A, 634 to 311 mL CH4/L/d in the control reactor). The OLR of the influent

vessels of that day of reactor A and of the control reactor were 2.2 and 3 g COD/L, respectively. The

deviation between both values was probably due to an error in the weighing of glucose. The OLR should

have had a value of 5 g COD/L. Probably a too low amount of glucose was added to the influent, which

can explain the drop in both reactors (Figure 18).

0

200

400

600

800

1000

1200

1400

1600

1800

0 5 10 15 20 25 30 35 40 45 50 55 60 65 70

Vo

lum

etri

c m

eth

ane

pro

du

ctio

n

(mL

CH

4/L

/d)

Time (Days)

1 2 3a 3b 3c 3d

Figure 18 - Total volumetric methane production in reactor A (containing granules encapsulated in

alginate) and in the control reactor (containing natural granules) during the different experiments

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4.4 METHANE YIELD When excluding the datapoint on day 14 of the control reactor in experiment 1 (1), the natural granules

allowed from day 4, an average methane yield of 20.6 ± 2.8% more than the encapsulated granules.

When calculating the methane yields of experiment 2 (2) one need to divide by the added COD, which

is zero and division by zero is undefined. Therefore no graphs could be made of the methane yield in

reactor A and in the control reactor of experiment 2. Instead the alginate degradation rate was

calculated for reactor A (Appendix 2). The total amount of consumed COD in reactor A, in the form of

alginate, was 0.80 g, which corresponds to 0.92 g alginate12. This means that only 6.96% of the initial

amount of alginate was converted to biogas. The total amount of produced CH4 in reactor A during the

entire experiment was 277 mL. After 7 days, the methane production stopped, and, thus, alginate was

not consumed any longer. Therefore, the alginate degradation rate is calculated within a timeframe of

168h and equals 5.48 mg/h or 2.74 mg/L/h. In the first part of experiment 3 (3a), during 7 days, the

natural granules achieved a 19.8 ± 11.7% higher methane yield than the encapsulated granules. After

7 days, the yields of both reactors were similar with a value of 75.8 ± 5.1% in reactor A and 80.1 ± 8.8%

in the control reactor. In the second part of experiment 3 (3b), after 4 days, the control reactor allowed

a methane yield that was 24.0% higher than in reactor A. On the other hand, after 7 days reactor A had

a 18.1% higher methane yield than the control reactor. During the entire third part of experiment 3

(3c), the methane yield in the control reactor remained constant with a value of 71.4 ± 3.1%. The

methane yield in reactor A (72.7 ± 2.5%) was during the first 7 days similar to the control reactor. After

7 days, the methane yield in reactor A decreased to 51.8%. In the last part of experiment 3 (3d), both

methane yields are following a similar course. In the beginning of 3d, the yield of both reactors was

rather low (18.59% in reactor A and 43.41% in the control reactor), but increased fast to even 97.9%

in reactor A and 97.8% in the control reactor after 10 days. However, after this peak, the methane yield

in both reactors decreased again to a yield of 52.8% in reactor A and 52.2% in the control reactor

towards the end of experiment 3d (Figure 19).

12 15 g of sodium alginate (C6H7NaO6) was added, which corresponds to a total amount of 13.25 g alginate (C6H7O6

-). The calculations for the COD of alginate can be found in appendix 2.

0

10

20

30

40

50

60

70

80

90

100

0 5 10 15 20 25 30 35 40 45 50 55 60 65 70

Met

han

e yi

eld

(%

)

Time (Days)

1 2 3a 3b 3c 3d

Figure 19 – Methane yield in reactor A (containing granules encapsulated in alginate) and in the

control reactor (containing natural granules) during the different experiments

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43

4.5 CATIONS Because the sludge was encapsulated by dropping a mix of sodium alginate and sludge into a CaCl2

solution, a graph of Ca2+ concentrations was constructed. No big differences in other cation

concentrations were observed among both reactors. In Appendix 3 (Table 13), an overview of the

cation concentrations in reactor A and the control reactor during the different experiments can be

found. During entire experiment 1 (1) and 2 (2), Ca2+ concentrations in the control reactor were on

average 39 ± 13 mg/L. At the start of experiment 3 (3a), an increase of 83 mg/L was observed, after

which the Ca2+ concentration in the control reactor became constant again (107 ± 9 mg/L). No

datapoints of reactor A were available for the second part of experiment 3 (3b) and only the last

datapoint of the third part of experiment 3 (3c) of reactor A was available. In experiment 1, as well as

in experiment 2 and the first and last part of experiment 3, the Ca2+ concentrations first increased in

reactor A, after which they decreased again The maximum Ca2+ concentration of experiment 1 (1) was

140 mg/L, of experiment 2 (2) 383 mg/L, of the first part of experiment 3 (3a) 439 mg/L and of the last

part of experiment 3 (3d) 274 mg/L. No interesting trend can be seen in the Ca2+ concentrations

throughout the different experiments. However, during the disintegration of the alginate matrix, Ca2+

concentrations in reactor A first increased and after the alginate matrix had been disintegrated, Ca2+

concentrations decreased again to normal values (Figure 20).

Figure 20 – Calcium concentrations in reactor A (containing granules encapsulated in alginate) and

in the control reactor (containing natural granules) during the different experiments

0

50

100

150

200

250

300

350

400

450

500

0 5 10 15 20 25 30 35 40 45 50 55 60 65 70

Cal

ciu

m c

on

cen

trat

ion

(mg

/L)

Time (Days)

1 2 3a 3b 3c 3d

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5 BIOCHEMICAL METHANE POTENTIAL (BMP) TEST The natural granules didn’t need a lot of time to adapt, and reached already after 3 days their maximal

amount of produced methane. On the contrary, the encapsulated granules needed more time (7days)

before reaching their maximal amount of produced methane (Figure 21). The natural granules

produced on average 29 ± 34 mL CH4/ g VS more than the encapsulated ones. In addition, the natural

granules reached on average a yield of 16.6 ± 19.6% more than the encapsulated granules (Table

8).Table 8 – Final methane production per g VS, final methane yield

Table 8 – Final methane production per g VS, final methane yield and final pH

Natural granules Encapsulated granules

Methane yield (mL CH4/g VS) 124 ± 34 95 ± 5 Methane yield (%) 70.7 ± 19.4 54.0 ± 2.9 pH 7.62 ± 0.03 7.04 ± 0.06

0

20

40

60

80

100

120

140

160

180

0 2 4 6 8 10 12 14 16 18 20

Met

han

e yi

eld

(mL

CH

4/g

VS)

Time (Days)

B1 Natural granulesB2 Natural granulesB3 Natural granulesA1 Encapsulated granulesA2 Encapsulated granulesA3 Encapsulated granules

0

10

20

30

40

50

60

70

80

90

100

0 2 4 6 8 10 12 14 16 18 20

Met

han

e yi

eld

(%

)

Time (Days)

B1 Natural granulesB2 Natural granulesB3 Natural granulesA1 Encapsulated granulesA2 Encapsulated granulesA3 Encapsulated granules

Figure 21 – Amount of produced methane (top) and methane yield (bottom) of granules

encapsulated in alginate and of control (natural granules)

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6 BATCH TEST

6.1 SHEAR STRESS BATCH TEST An overview of the pictures of 1 of the 9 replicates of each situation A, B, C or D can be found in Table

9. Pictures of all the 32 serums flask, and, thus, pictures of each replicate, can be found in Appendix 4.

When comparing the evolution of C and D, the alginate matrix disintegrated faster in C than in D, which

indicates a contribution of the shear stress to the disintegration of the alginate. When comparing the

evolution of A and B, the same can be perceived. However, in these flasks, the contribution of the

degradation of the alginate matrix by the biomass also played an important role. Putting B and D,

where shear stress didn’t play a role, next to each other, it can be seen that in B, the matrix is already

completely disintegrated after 14 days, while after 14 days in D, there is still some alginate matrix left.

Table 9 - Evolution of granules over a period of 14 days

Timepoint Day 0 Day 3 Day 7 Day 11 Day 14

A (encapsulated granules with shaking)

B (encapsulated granules without shaking)

C (encapsulated water with shaking)

D (encapsulated water without shaking)

6.2 POTASSIUM AND PHOSPHATE BATCH TEST Each treatment was conducted in triplicate. The evolution of each treatment for only one replicate can

be found in Table 10, the other replicates can be found in Appendix 5. The beads of the treatments

with only K+, behaved in the same way as the beads in the control. Therefore, it can be concluded that

K+ had no effect on the stability of the alginate beads. However, the PO43- treatments did show an

effect on the stability of the beads. In addition, the higher the concentration of PO43-, the stronger the

effect. It should also be noted that the beads swelled in the 405 mg PO43-/L treatment as well as in the

810 mg PO43-/L. The last treatment is a combination of potassium and phosphate. After day 10 the

beads are completely disintegrated. Also here, a swelling can be observed (Table 10).

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Table 10 - Evolution of the disintegration of beads over a period of 25 days

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DISCUSSION

1 DISINTEGRATION OF THE ALGINATE MATRIX During the different experiments, the disintegration of the alginate matrix was observed. The

disintegration of these beads can take place in three possible different ways. The first is that the

microbial biomass uses alginate as a C-source. The second way is that high concentrations of Na+ in the

effluent can cause swelling and consequently disintegration of the matrix, and the last reason is that

the shear stress present in the reactor accelerates the disintegration of the beads as a result of

degradation by the microbial biomass. For a better understanding of these findings, the structure of

alginate should be considered more in-depth.

Alginate is a polysaccharide extracted from brown

algae. It is a linear copolymer containing blocks of

(1-4)-linked β-D-mannuronate (M) and α-L-

guluronate (G). The blocks are composed of

consecutive G residues, consecutive M residues

and alternating M and G residues. Figure 22 gives

the structure of alginate. Alginate is industrially

available in the form of sodium alginate. The Na+-

ions react with the negatively charged carboxyl-

groups of the guluronate and the mannuronate blocks. When divalent cations, such as Ca2+, are added

to sodium alginate, the Na+-ions are driven out by the Ca2+ - ions and cross-linking between the M and

G blocks occurs, resulting in a gel structure. The binding of the Ca2+-ions with the guluronate units,

form the so-called tight egg-box structure and, in contrast to mannuronate, serve mainly as the stable

structure within the gel. Figure 23 gives a schematic overview of sodium alginate (left) and calcium

alginate (middle), as well as a SEM-EDS of the tight egg-box structure of calcium alginate (right). On

the SEM-EDS of calcium alginate, the cross-linking is clearly visible (Ayarza et al., 2016; Ji-Sheng et al.,

2011; Yong & Mooney, 2012).

Figure 22- Structure of alginate

Figure 23 – Sodium alginate (left), Calcium alginate (middle), SEM-EDS of Calcium alginate (right)

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1.1 DISINTEGRATION DUE TO DEGRADATION BY THE MICROBIAL BIOMASS The degradation of the alginate by the granular sludge is proven by experiment 2. No C-source was

present, but reactor A, containing the alginate encapsulated sludge, still did produce methane, which

indicates the use of alginate as C-source to produce methane. This is not surprising, many research is

already done on the use of macro- and microalgae as renewable substrates for AD. Brown algae, which

contain approximately 40% of alginate, have been highlighted as the most promising feedstock as a

renewable resource (Bohutskyi & Bouwer, 2012). Alginate is depolymerized through an alginate

degradation pathway mediated by alginate lyase. First, the alginate polymer is hydrolyzed into

oligomers by an endolytic lyase, which is called endotype lyase. Next, the oligomers are degraded into

unsaturated monomers through the action of an exolytic enzyme, known as exotype alginate lyase.

These monomers are eventually converted to pyruvate and glyceraldehyde-3-phosphate, which are

key intermediates of the glycolytic pathway (Kita et al., 2016).

The total added COD to reactor A in experiment 2 (2) was 11.52 g of which only 0.80 g was consumed.

After 7 days (168u), the whole matrix was disintegrated. From 11.52 g COD, 4.032 L CH4 can be

produced with an alginate degradation rate of 68 mg/h or 34 mg/L/h. However, only 277 mL CH4 was

produced with an alginate degradation rate of only 5.48 mg/h or 2.74 mg/L/h. The obtained volumetric

methane production and alginate degradation rate are lower than the theoretical obtained values.

Literature also reports higher values. Moen et al. studied in 1997 the alginate degradation during AD

of Laminaria hyperborean stipes. L. hyperborean is a specie of large brown algae, and contains

approximately 35% of alginate (Hanssen et al., 1987). Moen et al. reported a anaerobic sodium alginate

degradation rate of 230 mg/L/h, which corresponds to an alginate degradation rate of 203 mg/L/h.

This alginate degradation rate is approximately 70 times higher than 2.74 mg/L/h and 6 times higher

than the theoretical alginate degradation rate (34 mg/L/h). The difference in rate may be related to

the difference between sodium alginate and calcium alginate. Reactor A contained levels of calcium

alginate, while Moen et al. reported degradation rates of sodium alginate. The complexation with

calcium (Figure 23) limits the acces of alginate lyase to alginate, which is therefore degraded more

slowly than sodium alginate. However, because of the malfunctioning of the gas counters, which

created an underestimation of the total amount of biogas produced, this explanation is not conclusive

yet. Moen et al. also concluded that after 75h, minor amounts of alginate were degraded. In

experiment 2, no methane was produced after 168h, and, thus, no alginate was degraded anymore

after 168h. Moen & Østgaard also did research in 1997 on the aerobic degradation of calcium alginate

and sodium alginate. They reported an aerobic calcium alginate degradation rate of 160 – 200 mg /L/h,

which corresponds to an alginate degradation rate of 130-163 mg/L/h and an aerobic sodium alginate

degradation rate of 240 mg/L/h, which corresponds to an alginate degradation rate of 212 mg/L/h.

From these values, the difference between the lower degradation rate of Ca-alginate and the higher

degradation rate of Na-alginate is clearly visible.

1.2 HIGH CONCENTRATIONS OF NA+ CAUSE SWELLING AND

CONSEQUENTLY DISINTEGRATION

The effect of PO43- on the alginate matrix can be derived by comparing the treatments of the phosphate

potassium batch test with the different PO43- concentrations of Table 10 with the control treatment.

Phosphate concentrations lower than 202.5 mg PO43-/L do not have any effect on the disintegration of

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the alginate matrix. However, PO43- concentrations above 405 mg PO4

3-/L, do play a role in the

disintegration of the alginate beads. From Table 10, it can also be seen that the alginate matrix first

swells, and subsequently disintegrates due to the presence of PO43-. The swelling is a result of the

uptake of water by the matrix. Bajpai & Sharma investigated in 2004 the swelling and degradation

behavior in a PO43- buffer (PBS) of alginate beads crosslinked with Ca2+. When preparing the alginate

beads, they dropped a solution of 4% sodium alginate into 2, 3 and 4% CaCl2 solutions. Next, the

alginate beads were placed in a 0.1 M PBS buffer. After analyzing the % of weight change, they

concluded that it wasn’t the PO43-, but the Na+, present in the PBS buffer, that induced the swelling.

They proposed the following theory: the Na+ ions from the PO43- buffer first undergo ion exchange with

the Ca2+ ions mainly bound to the M blocks, which destabilizes the structure and causes the beads to

swell due to the uptake of water. The released Ca2+ ions react with the dissolved PO43- to form

Ca3(PO4)2, which is insoluble in water and consequently precipitates. In a later stage, ion exchange also

occurs between the Na+ ions and the Ca2+ ions bound to the G blocks losing the stable egg-box

structure. Finally, the alginate beads disintegrate and eventually dissolve. The used PO43- buffer in the

potassium phosphate batch test was Na2HPO3, therefore the theory of Bajpai & Sharma may, thus, also

be applied to the PO43- treatments of Table 10. It should be noted that, when opening the serum flasks,

a small layer of precipitation could be observed, which was probably the precipitated Ca3(PO4)2.

However, the alginate beads treated with 202.5 mg PO43-/L almost didn’t swell or disintegrate. This is

probably because an insufficient amount of Na+ ions (98 mg Na+/L) was present to disintegrate the

beads. In conclusion, the alginate beads swell and disintegrate due to high concentrations of Na+ (>100

mg Na+/L, see Table 5) instead of PO43-.

From Table 10, it can be derived that K+ concentrations don’t affect the stability of the beads, which is

not in line with the theory of Bajpai & Sharma. If the same theory is followed, the K+ ions undergo ion

exchange with the Ca2+ ions and the released Ca2+ ions react with the Cl- ions. However, this is not the

case, because no swelling and no disintegration was observed. This is probably because of the relative

stronger affinity of Na+ over K+ to the carboxyl-groups (Vrbka et al., 2006).

1.3 SHEAR STRESS ACCELERATES THE DISINTEGRATION AS A RESULT OF

MICROBIAL DEGRADATION At the start of the shear stress batch test, the encapsulated water beads were placed in serum flasks

containing effluent of reactor A and the control reactor of experiment 1 (molasse as influent). The

cation concentrations of this effluent can be found in Table 3. When comparing the disintegration of C

(encapsulated water with shaking) and D (encapsulated water without shaking) of Table 9, it can be

clearly seen that the beads within the serum flasks placed on the shaker, disintegrated more rapidly

than the beads within those flasks not placed on the shaker. On the contrary, the water beads of the

control of the potassium phosphate batch test were added to serum flasks containing only tap water.

These serum flasks were also placed on a shaker. Nevertheless, the beads of this control almost didn’t

disintegrate. In this case, shear stress alone almost had no effect on the stability of the alginate matrix.

However, the strength and rigidity of alginate beads depend on the relative amount of G and M blocks

in the alginate polymer, on the Ca2+ concentration and on the sodium alginate concentration. Mancini

et al. did research on the mechanical properties of alginate gels. They concluded that the rigidity of

alginate depends on the amount of G and M-blocks. In other words, high guluronic ‘G’ alginates are

more rigid than high mannuronic ‘M’ alginates, because binding between Ca2+ and G blocks results in

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a stable tight egg-box structure of alginate. Bajpai & Sharma found in 2004 that the lower the

percentage of CaCl2, the higher the water uptake, the bigger the swelling and, thus, the faster the

disintegration. Higher Ca2+ concentrations may thus result in a slower disintegration of the alginate

matrix. They also hypothesized that with an increase in alginate concentration, the number of

crosslinking points should increase, thus, resulting in delayed degradation. In addition, the increased

alginate density may also result in decreased mesh size within the gel beads, thus, making the ion-

exchange process slower (Bajpai & Sharma, 2004; Mancini et al., 1999). However, decreased mesh size

will also result in slower migration and consequently a slower uptake of COD and other nutrients by

the microbial biomass encapsulated in the alginate matrix. Summarized, depending on the type of

alginate and on how the beads are made, shear stress may or may not have an influence on the

disintegration of the alginate matrix.

Nevertheless, one can conclude from Table 9 that the shear stress, present in the reactor, did

accelerate the disintegration of the beads. The reason why the encapsulated water beads of the shear

stress batch test (both shaking and not shaking) did disintegrate and the encapsulated water beads of

the control of the potassium phosphate test didn’t disintegrate, can be explained by comparing three

different situations. The first situation refers to the control of the potassium phosphate batch test. The

second situation refers to the treatment of the potassium phosphate batch test with 405 mg PO43-/L.

And the last situation refers to the shear stress batch test with the encapsulated water beads (with

shaking). The properties of these three different situations can be found in Table 14 in Appendix 6 and

the swelling and the disintegration of these three situations in Table 15 in Appendix 6. It should be

noted that the beads of the shear stress batch test didn’t swell at all, while swelling was expected,

because the beads did disintegrate. However, Table 14 shows that the Na+ concentration in the tap

water and the effluent was much lower than in the PO43- treatment. Due to the low Na+ concentration

in situation 1, no swelling occurred. Therefore, no swelling occurred in situation 3 neither. A possible

explanation for the disintegration in situation 3, is that the effluent derived from the reactors still did

contain some small amounts of biomass. This biomass was probably responsible for the disintegration

of the alginate matrix, which was accelerated by the shear stress induced by the shaker. In conclusion,

the shear stress in the reactor accelerates the disintegration of the alginate matrix as a result of

microbial degradation, because the organic matter can come in close contact with the microbial

biomass, but doesn’t have an effect on the stability of the alginate matrix alone.

2 CHARACTERISTICS OF THE ENCAPSULATED SLUDGE

2.1 PH OF THE ENCAPSULATED SLUDGE During the entire three experiments, the pH in the reactor containing the encapsulated granules was

always lower than the pH in the reactor containing the natural granules. At the start of each

experiment, a pH drop was observed in reactor A, accompanied by an increase in VFA concentration.

Because the pH in the control reactor was during each experiment more or less constant, the observed

pH drop and VFA increase in reactor A may be a result of the encapsulation of the granular sludge. The

following hypothesis is proposed: when the sludge is encapsulated in an alginate matrix, the microbial

biomass need to adapt to the new growth conditions, this is the so-called lag phase. The hydrolytic,

acidogenic and acetogenic bacteria probably have a shorter lag phase than the methanogenic archaea.

Therefore, VFA are already produced, while the methanogens still need to adapt. This results in VFA

accumulation and a consequent decrease in pH. From the moment the methanogens are adapted, they

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start to convert the VFA into biogas accompanied by a drop in VFA concentration and an increase in

pH. Akuzawa et al. showed that the accumulation of VFA in most situations reflects an imbalance

between acid producers (mostly bacteria) and consumers, and is usually associated with a drop in pH,

reinforcing the previous assumption.

When comparing the first part of experiment 3 (1.3% alginate, 3a) with the second part of experiment

3 (1.3% alginate + glucose, 3b) in reactor A, it can be seen that VFA in 3a accumulated after 2 days,

while the VFA in 3b accumulated after 4 days. In addition, the accumulated VFA concentrations in 3b

were twice as high as the concentrations of the accumulated VFA in 3a (Figure 16,Figure 17). Two

factors may play a role in the VFA accumulation in 3b. The first factor is the accumulation of VFA, due

to a longer lag phase of the methanogens. The second factor is the presence of the extra glucose in

the alginate encapsulated beads. During experiment 2 (2), no C- source was added, while during

experiment 3 (3) an OLR of 2.5 g COD/L/d was applied instead of 5 g COD/L/d as in experiment 1 (1).

This means, that in the beginning of 3b, the OLR existed of 2.5 g COD/L/d plus the present glucose in

the beads (5 g COD/L). This can result in an organic overload and a consequent accumulation of VFA.

In other words, the conversion of glucose to biogas by methanogens lagged behind the rapid

conversion of glucose to VFA by the acidogens and acetogens with VFA accumulation and a

consequently decrease in methane production as result. Experimental studies showed that higher

influent COD concentrations can lead to the formation of higher VFA concentrations (Buyukkamaci &

Filibeli, 2004). In addition, organic overloading initially results in the accumulation of acetate and H2,

which is in line with the relative high amount of acetate (577 mg/L) present in reactor A, after 4 days

in 3b (De Vrieze, 2014). Hickey & Switzenbaum reported that monitoring CO2 can provide information

on the level of stress being exerted on the CO2-reducing methanogenic population. The percentage of

CO2 after 4 days in reactor A in 3b was 45%, while in the control reactor a percentage of 30% CO2 was

observed, which also points to a possible organic overloading in reactor A (Hickey & Switzenbaum,

1988).

During experiment 1 (1), the pH of both reactors stayed between the optimal upper and lower limit.

From experiment 3 (3) onwards, the pH in both reactors fell below the optimal upper limit. This drop

in pH may be a result of the change from molasse to a synthetic medium with a lower buffering capacity

than molasse, due to lower PO43- concentrations. In a less well buffered system, the breakdown of the

buffering capacity, for example due to the production of VFA, happens faster than in a better buffered

system (Akuzawa et al., 2011). In experiment 2 (2), the pH in the control reactor didn’t fall below the

optimal lower limit, because no C-source was added, and, thus, no production of VFA occurred,

resulting in a stable and high pH.

2.2 METHANE PRODUCTION OF THE ENCAPSULATED SLUDGE Experiment 1 (1) can confirm the hypothesis made in 2.1, concerning the adaptation to the

encapsulation matrix. In experiment 1, the methane production in the reactor containing the

encapsulated beads is delayed, compared to the methane production in the other reactor. Reactor A

reached a methane production of 1305 mL CH4/L/d after 14 days, while the control reactor already

reached a volumetric methane production of 1361 after 4 days. This can be explained by the hypothesis

made in 2.1. The microbial biomass in reactor A, and especially the methanogens, first experience a

lag phase, as a consequence of the encapsulation, while the microbial biomass in the control reactor

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immediately starts to produce biogas. Only when the methanogens are fully adapted to their

environment, a maximal amount of biogas can be produced.

When experiment 3 (3) started, a drop in volumetric methane production can be observed. Both

reactors in experiment (3) still produced biogas, but in much lower amount compared to experiment

1 (1), which can be attributed to the change from molasse to a synthetic medium. First of all, the buffer

capacity of the synthetic medium is lower, resulting in an overall lower pH (< 6.8, optimal lower limit).

When the HRT of the reactor is long enough for growth of methanogens, weakly acidic conditions do

not thoroughly inhibit methanogenic activity. However, the hydrogenotrophic methanogens are more

tolerant to acidic conditions than the acetoclastic methanogens which activity was inhibited (I. S. Kim

et al., 2004; Ye et al., 2013). Second, by changing the influent from molasse to the synthetic medium,

the OLR was also changed from 5 g COD/L/d to 2.5 g COD/L/d. Borja & Colmenarejo showed that an

increase in OLR, produced an increase in methane gas production per volume of the reactor. However,

an increase in OLR determined a progressive decrease in the removal efficiency. They found that the

best removal efficiencies were obtained at OLR values in the range of 1.0 – 4.1 g COD/L/d. At 8.1 g

COD/L/d, the removal efficiency dropped suddenly (Borja & Colmenarejo, 2005). From this, it can be

concluded that the decrease from 5 g COD/L/d to 2.5 g COD/L/d is co-responsible for the decrease in

methane production in experiment 3 (3).

2.3 ELEVATED CA2+ LEVELS IN THE REACTOR CONTAINING THE

ENCAPSULATED SLUDGE Important differences in Ca2+ concentrations among both reactors can be observed. The small increase

of 83 mg Ca2+/L in the control reactor between experiment 1 (1) and experiment 3 (3) was caused by

the change of molasse to synthetic medium, which contained a higher Ca2+ concentration than molasse

(3 mg Ca2+/L in molasse, 46 mg Ca2+/L in synthetic medium). However, Ca2+ concentrations in

experiment 3 were 108 ± 9 mg/L (> 46 mg/L), while Ca2+ concentrations in experiment 2 were only 35

± 4 mg/L (≈ 46 mg/L), although the same synthetic medium was used (Table 11). This may be attributed

to the inactivity of the microbial biomass in the control reactor during experiment 2 (2), compared to

the active biomass in experiment 3 (3). Because no C-source was added in 2, the microbial biomass in

the control reactor was not allowed to grow. In addition, it can be seen that no NH4+ was consumed,

indicating that they probably almost didn’t synthesize amino acids, DNA or RNA, and therefore didn’t

grow. It is also known that the growth of bacteria on media containing a marginal supply of glucose

results in abrupt cessation of growth when the substrate supply is exhausted (M. Lawrence &

Raymond, 1973). The higher levels of Ca2+ in 3 in the control reactor may thus be a consequence of

microbial growth. Bacteria and archaea get their energy from coupled transport. Dimroth reported in

1991 that H+ is the most common coupling ion for bioenergetic functions. Therefore, Cai & Lytton

proposed that it is likely that the bacterial and archaea exchangers utilize the H+ gradient, instead of

Na+, to extrude cytosolic Ca2+, which may, thus, elevate the Ca2+ levels in the effluent of the control

reactor (Cai & Lytton, 2004; Dimroth, 1991). This also may explain why the Na+ and K+ concentrations

in the control reactor didn’t differ among 2 and 3. However, it is not sure in which extent Ca2+/H+

exchangers may bring about changes in the Ca2+ concentrations in the effluent of the control reactor.

However, microorganisms also use Na+ or K+/H+ exchangers, but no differences in Na+ and K+

concentrations in the control reactor among 2 and 3 are observed (Booth, 1985).

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Table 11 – Mean cation concentrations of effluent of experiment 2 and 3 and theoretical cation

concentrations of synthetic medium 1 and 2 in the control reactor

Control reactor Na+ NH4+ K+ Ca2+ Mg2+

Synthetic medium 1, 2 (mg/L) 230 169 450 46 12 Effluent Experiment 2 (mg/L) 254 ± 11 175 ± 11 454 ± 4 35 ± 4 40 ± 8 Effluent Experiment 3 (mg/L) 236 ± 17 74 ± 20 394 ± 44 108 ± 9 17 ± 2

At the start of each experiment, an increase in Ca2+ concentration in reactor A can be observed. After

about 6 days, the Ca2+ concentration start to decrease again. This increase and decrease in Ca2+

concentration can be explained by Figure 15 and by the hypothesis made in 1.2. In each experiment,

after about 6 days, the whole alginate matrix is degraded. This means that also the Ca2+ ions are

exempted from the alginate matrix and replaced by Na+, which increases the Ca2+ concentration in

reactor A. After about 10 days, the excess Ca2+ concentrations are removed with the effluent and

‘normal’ Ca2+ concentrations can be observed again. However, no change in Na+ concentrations are

observed in reactor A. This can be explained by the conclusion made in 1.1. The microbial degradation

of the alginate matrix occurs simultaneously with the substitution of Ca2+ by Na+. When the alginate

matrix is completely degraded by the microorganisms, no Na+ ions are trapped in the matrix anymore

(Figure 20).

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CONCLUSION AND FUTURE PERSPECTIVES First, the encapsulation of granular sludge with an alginate matrix didn’t stop the AD process from

working. The amount of biogas produced by the encapsulated granular sludge was similar to the

natural granular sludge. However, the initial pH and VFA concentrations in the reactor containing the

encapsulated granular sludge were lower and higher, respectively, than in the control reactor, due to

a longer lag-phase of the methanogens, which also resulted in a maximal biogas production that was

reached less quickly than in the control reactor.

Second, the alginate matrix was used as carbon-source, and, consequently, degraded by the microbial

biomass. It was also observed that shear stress, occurring in the reactor, accelerates the degradation

of the alginate matrix by the microbial biomass. Therefore, addition of compounds slowing down the

degradation of the alginate matrix, such as formaldehyde, may be considered. Formaldehyde is widely

used in quite high concentrations to slow down microbial decomposition of brown seaweeds (Moen

et al., 1997b). However, this organic compound, which is very toxic to humans and a threat to the

environment, needs to be added in sufficiently low concentrations to avoid inhibition of the

methanogens. Literature also reports that the microbial biomass of the AD process is also capable of

degrading formaldehyde (Moen & Østgaard, 1997; Vidal et al., 1999). Therefore, research can be done

on different concentrations of formaldehyde, whether or not integrated in the alginate matrix, to find

the optimal concentration at which AD isn’t inhibited, and degradation of alginate by the microbial

biomass is slowed down. Other encapsulation matrices, such as chitosan, may also be tested. El-

Mamouni et al. reported in 1998 that chitosan enhanced the granulation process acting similarly to

the extracellular polymers (ECP). Turtakovsky et al. did research on the dechlorination of wastewaters

by chitosan encapsulated anaerobic species. No sign of bead disintegration was observed over the five-

week period of reactor operation. Therefore, chitosan may be a suitable candidate for the

encapsulation of the granular sludge (El-Mamouni et al., 1998; Turtakovsky et al., 1997).

Last, it was found that high concentrations of Na+ (> 100 mg/L) interfere with the cross-linked Ca2+,

resulting in swelling and consequently disintegrating of the matrix. Bajpai & Sharma found that the

lower the percentage of CaCl2, the higher the water uptake, the bigger the swelling and, thus, the

slower the disintegration. Therefore, higher percentages of CaCl2 may be tested to stabilize the

alginate matrix. Another way to increase the stability of the matrix is the use of Ba2+, instead of Ca2+

for the cross-linking of the matrix. Barium has a larger radius than Ca2+, and is supposed to fill a large

space between the alginate molecules with smaller voids. The exchange of the large Ba2+ ions with Na+

ions may be hindered resulting in a lower water uptake and higher stability, which was confirmed by a

study conducted by Bajpai & Sharma in 2004 (Bajpai & Sharma, 2004).

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APPENDIX 1: ANION AND CATION COMPOSITION

OF SYNTHETIC MEDIUM 1 AND 2 The anion and cation composition of the synthetic media are calculated theoretically and can be found

in Table 12.

Table 12 - Theoretically calculated anion and cation concentrations of synthetic medium 1 and 2

Cations

Na+ NH4+ K+ Ca2+ Mg2+

Synthetic medium (mg/L) 230 169 450 46 12

Anions

Cl- PO43- SO4

2- CO3-

Synthetic medium (mg/L) 487 144 413 1200

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APPENDIX 2: CALCULATIONS OF COD OF ALGINATE In experiment 2, 15 g of sodium alginate (C6H7NaO6) was mixed with 448 g sludge and 552 g H2O. This

solution was dropped gradually in a CaCl2 solution, after which the beads were added to a reactor with

a volume of 2 L. This means that a total amount of 13.25 g alginate (C6H7O6-) was added to a reactor

volume of 2 L.

𝑀𝑤 (𝐶6𝐻7𝑂6_)

𝑀𝑤 (𝐶6𝐻7𝑁𝑎𝑂6)∗ 15 𝑔 𝐶6𝐻7𝑁𝑎𝑂6 =

175.12

198.11∗ 15 = 13.25 𝑔 𝐶6𝐻7𝑂6

_

The final alginate concentration in the reactor is thus 6.63 g/L. To calculate the COD of 6.63 g alginate/L,

following reaction is required:

𝐶6𝐻7𝑂6_ + 4.75 𝑂2

→ 6𝐶𝑂2 + 3.5𝐻2𝑂

The total number of moles of C6H7O6- is 0.038 mol/L, so the total number of moles of O2 is 4.75 * 0.038

= 0.18 mol/L. This amount of mol corresponds to a mass of oxygen of 0.18 mol * 32 g/mol = 5.76 g/L.

This is the total amount of oxygen that can be consumed by the reaction, which equals the COD. The

COD concentration in the reactor is thus 5.76 g/L and the total amount of COD added to the reactor is

2 L * 5.67 g/L = 11.52 g.

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APPENDIX 3: CATION CONCENTRATIONS OF THE

THREE EXPERIMENTS

Different cation concentrations were observed in experiment 1, in which molasse was used as

feedstock compared to experiment 2 and 3, in which a synthetic medium was used as feedstock. The

reactors in experiment 1 contained much higher concentrations of NH4+, K+ and Mg2+ and lower

concentrations of Na+ and Ca2+.

Table 13 – Cation concentrations in reactor A (containing granules encapsulated in alginate) and in

the control reactor (containing natural granules) during the different experiments

Reactor A (mg/L) Control reactor (mg/L) Days Na+ NH4

+ K+ Ca2+ Mg2+ Na+ NH4+ K+ Ca2+ Mg2+

Experiment 1

0 160 483 1971 31 43 95 465 1896 62 38 7 94 458 1791 139 86 80 489 1623 29 40

14 84 389 1856 37 47 100 524 2260 33 52

Experiment 2

5 260 142 433 383 27 247 183 439 33 45 13 262 155 426 159 17 262 168 432 38 34

Experiment 3a

7 252 56 378 439 20 235 71 380 96 21

Experiment 3b

4 273 60 362 / 19 226 75 354 103 16

Experiment 3c

3 305 20 347 / 16 205 38 325 122 13 10 252 77 421 221 15 255 78 436 106 17

Experiment 3d

6 214 55 347 274 16 235 72 410 117 18 9 238 97 398 187 17 248 107 416 110 19

13 254 79 446 133 17 252 78 443 99 17

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APPENDIX 4: REPLICATES SHEAR STRESS BATCH

TEST

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APPENDIX 5: REPLICATES POTASSIUM AND

PHOSPHATE BATCH TEST

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APPENDIX 6: COMPARISON BETWEEN SHEAR

STRESS BATCH TEST AND POTASSIUM PHOSPHATE

BATCH TEST The properties of three different situations can be found in Table 14 and the swelling and disintegration

of these three situations can be found in Table 15. Situation 1 refers to the control of the potassium

phosphate batch test. Situation 2 refers to the shear stress batch test with the encapsulated water

beads (with shaking) and the last situation refers to the shear stress batch test with the encapsulated

water beads (with shaking).

Table 14 – Properties of serum flasks filled with encapsulated water beads and tap water (situation

1), a solution of 405 mg PO43-/L (situation 2) or effluent (situation 3)

Situation Solution Na+ NH4+ K+ Ca2+ Mg2+ PO4

3- Disintegration Swelling

1 Tap water13 (mg/L) 49 n.a. n.a. 102 9 n.a. No No

2 405 mg PO4

3-

(mg/L) 196 / / / / 405 Yes Yes

3 Effluent (mg/L) 92 493 1927 42 44 237 Yes No

* n.a. = not available

13 (The open University, n.d.)

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Table 15 - Comparison between the swelling and disintegrations of the control of potassium

phosphate batch test (situation 1), the treatment with 405 mg PO43- mg/L of the potassium

phosphate batch test (situation 2) and the shaken encapsulated water beads of the shear stress

batch test (situation 3)

Day 0 Day 2 Day 7 Day 10 Day 14

1 Tap

water

2 405 mg PO4

3- /L

Day 0 Day 3 Day 7 Day 11 Day 14

3 Effluent