Environmental Assessment of Bottom Ash Pre-Treated with...

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LICENTIATE THESIS Environmental Assessment of Bottom Ash Pre-Treated with Zero Valent Iron Mirja Nilsson

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LICENTIATE T H E S I S

Department of Civil, Environmental and Natural Resources EngineeringDivision of Geosciences and Environmental Engineering

Environmental Assessment of Bottom Ash Pre-Treated with Zero Valent Iron

Mirja Nilsson

ISSN 1402-1757ISBN 978-91-7583-157-2 (print)ISBN 978-91-7583-158-9 (pdf)

Luleå University of Technology 2014

Mirja N

ilsson Environm

ental Assessm

ent of Bottom

Ash Pre-T

reated with Z

ero Valent Iron

ISSN: 1402-1757 ISBN 978-91-7583-XXX-X Se i listan och fyll i siffror där kryssen är

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Environmental Assessment of Bottom Ash

Pre-Treated with Zero Valent Iron

Mirja Nilsson

Luleå University of TechnologyDepartment of Civil, Environmental and Natural Resources Engineering

Division of Geosciences and Environmental Engineering

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Printed by Luleå University of Technology, Graphic Production 2014

ISSN 1402-1757 ISBN 978-91-7583-157-2 (print)ISBN 978-91-7583-158-9 (pdf)

Luleå 2014

www.ltu.se

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Environmental Assessment of Bottom Ash Pre-treated with Zero Valent Iron

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Summary

Bottom ash has similar properties as crushed rocks and gravel, and could replace some of the

40 million tonnes of virgin material used for road constructions each year. However, results

presented in the literature indicate that the leaching of e.g. Cr, Cu, Mo, Pb and Zn can cause a

threat to the surrounding environment if the material is used as it is. A common pre-treatment

method is carbonation, which will reduce the pH and thereby decrease the leaching of several

metals. This treatment is however not always enough, so alternative methods are needed. One

possibility could be to increase the number of sorption sites for the metals. The importance of

iron oxides as sorption sits for metals is known from both mineralogical studies of bottom ash

as well as from the remediation of contaminated soil, where iron is used as an amendment.

Zero valent iron (Fe0) was therefore added prior to accelerated aging in order to increase the

number of adsorption sites for metals and thereby improving the leaching quality.

The performed leaching tests showed that the addition of Fe0 prior to accelerated aging im-

proved the quality of the leachate compared with untreated bottom ash. There was also a sig-

nificant decrease of Cu, Cr, Mo and Zn from bottom ash treated with Fe0 prior to accelerated

aging compared with bottom ash submitted to only accelerated aging.

In order to make an environmental assessment of the bottom ash pre-treated with Fe0 prior to

accelerated aging geochemical modeling was performed using different pH and redox poten-

tials in order to simulate variations in the environment. The results indicated that the leaching

of Cr, Cr, Mo and Pb would not cause harm to the environment. Zn, however, was affected by

changes in pH and leached in harmful aounts at pH values velow 6 and above 10. There are

reasons to question the results from the geochemical modelling since the results from pH-stat

tests showed that several elements leached at potentially harmful levels at several of the tested

pH.

To fully evaluate the effect of addition of Fe0 should the mineralogy of the pre-treated bottom

ash be evaluated further, in order to see what forms iron oxides are present and if other metals

are associated with them. However, in order to improve the quality of bottom ash, focus

should be directed torwards what type of wastes that are incinerated and on the incineration

process.

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Environmental Assessment of Bottom Ash Pre-treated with Zero Valent Iron

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Acknowledgments

I am grateful to my supervisor, Professor Anders Lagerkvist, for the opportunity to work in

this research group, constructive feedback and support along the way.

I am grateful to my supervisor, Senior lecturer Lale Andreas for her feedback, encouragement

and support during this process.

I would like to thank Desiree Nordmark for patiently answering all my questions in the labor-

atory and Maria Gelfgren for the practical help, as well as Charles Belmonte, Irina Kacin-

skaja, Egle Kiaunyte and Hiroshi Nomura.

To all my present and former colleges at Waste Science and Technology, thank you for your

help and for providing an enjoyable working atmosphere.

To my family and friends, thank you.

Finally, I gratefully acknowledge the financial support provided by the partners of North

Waste Infrastructure; Bodens Kommun, Luleå Tekniska Universitet, RagnSells, Boden Ener-

gi, Norbottens Läns Landsting, Länsstyrelsen Norrbotten and the European Union.

Stockholm, November 2014

Mirja Nilsson

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Environmental Assessment of Bottom Ash Pre-treated with Zero Valent Iron

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Summary .................................................................................................................................................. I

Acknowledgments .................................................................................................................................. III

1 INTRODUCTION ................................................................................................................................ 1

1.1 Background ............................................................................................................................. 1

1.2 Objective ................................................................................................................................. 1

2 MATERIAL AND METHODS ...................................................................................................... 2

2.1 Material ................................................................................................................................... 2

2.1.1 Bottom ash ....................................................................................................................... 2

2.2 Methods ................................................................................................................................... 2

2.2.1 Pre-treatment of bottom ash ............................................................................................ 2

2.2.2 Leaching tests .................................................................................................................. 2

2.2.3 Buffering capacity ........................................................................................................... 3

2.2.4 Geochemical Modelling (Visual MINTEQ) .................................................................... 4

3 RESULTS AND DISCUSSION...................................................................................................... 4

3.1 Comparison of leaching methods – column, batch and pH-stat .............................................. 4

3.2 Comparing modeling and experimental results ....................................................................... 6

3.3 Environmental assessment – effects of pH and redox potential on leaching .......................... 7

3.4 Buffering capacity ................................................................................................................. 12

4 CONCLUSIONS ........................................................................................................................... 13

5 FUTURE RESEARCH .................................................................................................................. 13

6 REFERENCES .............................................................................................................................. 14

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1 INTRODUCTION

1.1 Background

Municipal solid wastes are in Sweden incinerated in waste-to-energy plants in order to pro-

duce energy and/or distance heating. After incineration are two different ashes produced; fly

ash that consist of volatile material that follow the flue gases and is trapped in the air pollution

control system, and bottom ash that are non-volatile material left at the bottom of the pan

(Chandler et al., 1997). Bottom ash has similar properties as gravel, sand and to some extent

crushed rocks, and can, therefore, replace some of the virgin materials now used in e.g. road

constructions. To improve the quality of bottom ash e.g. leaching of metals prior to use, is the

bottom ash metal separated and stored outdoors for a period (Statens geotekniska institut,

2006).

However storing the bottom ash outdoors in piles (3-5 meters) is not always sufficient to re-

duce leaching below the guideline values (Oja, 2012), and new pre-treatment methods are

therefore needed. Since iron oxides are known to bind metals (Saffarzadeh et al., 2011,

Cornelis et al., 2008 and Cornell and Schwertmann, 2003) can an increase of iron oxides be

one way to improve the leaching quality of the bottom in order to resuse it as a construction

material. Unpublished results of bottom ash pre-treated with accelerated aging and

accelerated aging with addition of elemental iron (Fe0), a byproduct from the company

MEROX, showed significant decreased leaching of e.g. Cu and Cr when Fe0 was added

(Paper III).

The Fe0-treatment can possibly be incorporated in waste-to-energy plants after the bottom ash

has been quenched and as it is transported away on the conveyor. In order to treat the 1 mil-

lion ton bottom ash produced each year in Sweden (Statistics Sweden, 2012) with 2% (w/w)

Fe0 would roughly 20 000 ton be required. MEROX produces about 4000 ton Fe

0 each year

(Personal communication Diana Orrling, MEROX). This pre-treatment can, therefore, only be

a local solution.

When assessing the leaching potential of a material like bottom ash, different approaches can

be used. In the laboratory can leaching test e.g. column, batch and pH-stat test be used. They

all use water as leachate but use different methods for the leaching procedure. Geochemical

modelling can be a tool in order to investigate how changing environmental factors affect the

leaching of metals from bottom ash (Dijkstra et al., 2002).

1.2 Objective

The overall aim of this study was to investigate how environmental factors affect the leaching

of metals from bottom ash pre-treated with accelerated aging and Fe0

using the geochemical

modelling program Visual MINTEQ. Another aspect was to evaluate how well the geochemi-

cal model describes the leaching from leaching tests. In order to do so were the following re-

search questions formulated.

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i. How comparable were results from column, batch and pH-stat tests?

ii. How well does the result from the geochemical model fit the results from the

leaching tests?

iii. How can changes in pH and redox potential affect leaching of Cr, Mo, Cu, Pb and

Zn?

2 MATERIAL AND METHODS

2.1 Material

2.1.1 Bottom ash

The bottom ash was produced at a local waste incinerator plant, and the major part of the ash

derived from MSW incineration during the winter 2011/2012 and spring, with some addition

from the incineration during the summer. The bottom ash was stored in piles outside prior to

metal and size separation. Samples of the 0-10 mm fraction were taken from the mobile metal

separation plant daily during five weeks in the summer of 2012, with the exception of five

days. In total 150 kg bottom ash was sampled.

2.2 Methods

2.2.1 Pre-treatment of bottom ash

Two pre-treatment methods; accelerated aging (A) and accelerated aging with addition of 2%

zero valent iron (AFe) were used. Untreated bottom ash (BA) was used as control. Aging,

without or with Fe0, was done with moistened bottom ash in large barrels that were connected

to a CO2-filled gasbag for two weeks at 30°C. For each treatment was 15 kg bottom ash used.

2.2.2 Leaching tests

Evaluating the leaching of bottom ash was done using different methods; column tests

(CEN/TS 14405) (SIS, 2004), batch (EN 12457-2) (SIS, 2003) and pH-stat (CEN/TS 14497)

(SIS, 2007). The tests all use water as leachate in a liquid to solid ratio (L/S) 10, but differ in

the duration, size and mass of material (Table 1).

Table 1 Differences between leaching tests – column, batch and pH-stat

Column Batch pH-stat

Duration About 30 days 24 h 48 h

L/S ratio 0.1, 0.2, 0.5, 1, 2, 5, 10 10 10

Particle size < 10 mm Crushed < 1 mm Sieved < 4 mm

Sample mass (DM) 2.7 kg 90 g 15 g

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In the up flow percolation column test, a constant flow of water passes by the bottom ash

whereas in batch tests were bottom ash shaken together with water. In pH-stat was bottom ash

shaken constant pH, adjusted by addition of acid (HNO3). In all leaching tests were the con-

centration (mg/l) of selected elements measured using ICP and expressed as mg/kg.

Leaching were compared against the guideline values in the handbook for Reuse of waste as

construction material for use above liner (SNV, 2010). If an element was not included in the

guideline values was the limit value for inert waste used instead (EC, 2003).

2.2.3 Buffering capacity

Acid neutralization capacity (ANC) (SS-EN ISO 9963-1:1994) (SIS, 1994) for the solid

bottom ash was determined using the standard for determining alkalinity in water. 1 g DM

milled bottom ash was added to 110 ml of deionized water and 0.1 M HCl was used as the

titrant in the automatic titration device (Titra Lab 90, software TimTalk 9 version 2.1) to

reach the equivalence points at pH 8.3 and pH 4.5. The ANC was then calculated according to

equation 1.

ANC = (c * V) / m (1)

Where,

c, concentration of the titrant

V, volume of the titrant

m, mass of the solid sample

An equation by Reardon and Moddle (1985) based on empirical data from measurements of

diffusion coefficients from mining wastes was used to calculate the effective diffusion coeffi-

cient (Deff) (equation 2).

Deff = 3.98 * 10-5

[(θ - θw - 0,05)/0,95]1,7

* T1,5

(2)

Where,

θ = porosity

θw = water filled porosity

T = temperature

The ANC (mol / kg DM) of the bottom ash pre-treated with accelerated aging and additon of

Fe0 at pH 9, 8 and 7 were used in order to estimate the time needed for carbon dioxide, at

normal pressure, to achieve the desired pH decrease (equation 3 and 4).

Fdiff = - Deff * dC/dx (3)

Time = Fdiff * 31536000 s (4)

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Where,

Fdiff = diffusion flow (mol/s*m2)

Deff = effective diffusion coefficient (m2s

-1)

dC = concentration gradient (mol/m3)

dx = depth of material (m)

2.2.4 Geochemical Modelling (Visual MINTEQ)

Geochemical modelling using the program Visual MINTEQ (Gustafsson, 2012) was done in

order to increase the understanding how leaching of Cr, Mo, Cu, Pb and Zn from pre-treated

bottom ash (AFe) would be affected by environmental changes e.g. variations in pH and

redox potential in a construction and also to see how well the modeling results were in

agreement with the leaching results.

The cumulative L/S 10 results from the column tests (CEN/TS 14405) were used in Visual

MINTEQ. They consisted of major cations (Ca2+

, Mg2+

, Na+, K

+) and anions (CO3

2-,Cl

-, SO4

2-

) and Si and trace elements Fe3+

, Mn2+

, Cu2+

, Zn2+

Al3+

, Pb2+

, Cr, As+5

, V+2

. Organic com-

plexation was included using the Stockholm Humic Model (SMH) (DOC 114.2 mg/l), since it

is important for leaching of elements like Cu. The assumption was made that 100% of the

DOM was fulvic acid (FA). Redox couples Cr(VI)/Cr(III), Mn(II)/Mn(III), HS

-/SO4

2- and

Fe(III)/Fe(II) were allowed in the model. Adsorption was modeled using HFO (Dzombak and

Morel, 1990), a wildly used model for adsorption to ferrihydrite. Aged ferrihydrite was

specified as possible solid phase. The temperature was set to 10 ˚C.

pH and redox potential were varied in the program in order to simulate environmental chang-

es. The pH and redox values used were; pH 4, 6, 8, 10, 12 and redox -600, -400, -200, 0, 200,

400, 600 and 800 (mV).

3 RESULTS AND DISCUSSION

3.1 Comparison of leaching methods – column, batch and pH-stat

The leaching from the BA at L/S 10 in the three used tests was compared after normalizing

the leached amounts of elements as percentage of the sum of elements analysed, see Figure 1.

The values were normalized in order to compare the leaching methods since the sum of ele-

ments analysed with ICP differed. The total sum analysed was 7100 mg/kg for the column test

9000 mg/kg for the batch test and 7300 mg/kg for the pH-stat test. As an example, Zink

leached 0.430, 2.96 and 0.0943 mg/kg in the three tests, respectively. This corresponds to

0.006, 0.04 and 0.001 % leached of the total amount leached in the respective test.

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Figure 1 Comparison of normalized leaching from column, batch and pH-stat, % of total analysed

for each element. Logarithmic scale. ■ column test, ▲ batch test and ♦ pH-stat test at pH 8.

Leaching of most elements was in similar proportion independent of the leaching test used,

indicated by values close together (Paper III). The least variation between the test methods

could be seen for major elements such as Ca, K and Na, which show availability controlled

leaching. It is, therefore, reasonable that they leached in similar portions independent of the

test used. The largest difference between the tests was observed for Al and Zn, which are pH

sensitive elements. Leaching of Zn was 30 times higher from column test compared with

batch and 5.7 times higher from pH-stat compared with batch whereas leaching of Al was 15

times higher for batch test and 5.7 times higher from pH-stat test compared with column test.

One possible explanation to the differences could be variations in pH of the leachate between

the tests. The leachate from the column had an average pH of about 7.9 compared with batch

test where pH was as high as 8.4 in one triplicate. Both Al and Zn have a pH dependent leach-

ing with a V-shaped curve where Al has its minimum leaching at pH 7 whereas Zn has the

minimum leaching around pH 9 (Figure 2).The higher leaching of Zn in the column test can

thus depend on lower pH in the leachate and the higher leaching of Al from batch test can

depend on the higher pH.

However, the difficulty of assigning an average pH value to leachate from the column test can

be a reason to question this argument. The pH was measured after each of the seven portions

that were accumulated to reach L/S 10. The samples were collected during six hours for the

first L/S-ratio up to 13 days for the last L/S-ratio and the pH for the seven samples varied be-

0.000001

0.00001

0.0001

0.001

0.01

0.1

1

10

100

Al As Ba Ca Cd Co Cr Cu Fe Si Hg K Mg Mn Mo Na Ni Pb V Zn

% o

f su

m o

f el

emen

ts a

nal

yzed

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tween 7.7 and 8.1. Another reason the leaching of elements like Al and Zn varies can depend

on the differences between the methods, like contact time or the size of the material.

Figure 2 Results from pH-stat for Al (■ dotted line) and Zn (▲solid line) as well as literature

values for Zn (▲) at pH 12.5 and 13 (Chandler et al. 1997).

3.2 Comparing modelling and experimental results

Geochemical modelling can be a tool in order to assess how the environment factors affect the

leaching from bottom ash (Dijkstra et al., 2002). There is also an increasing demand regarding

simulations using geochemical modelling for example to see how well stabilizations technics

work (Zhang et al., 2008). It is therefore of interest to analyse how well modelling results fits

leaching results. Results from the leaching tests; column, batch and pH-stat, as well as results

from the geochemical modeling, were normalized as % of the total sum of dissolved for each

element. Results from the leaching tests were compared with results from the geochemical

model (Figure 3).

Leaching test results were in general higher than calculated by the geochemical model, indi-

cated by values ˃ 1. The biggest difference was seen for As with ˃ 1000 times, as well as Al

and Pb with up to 100 times larger leaching from leaching tests. However, some results, espe-

cially from batch test, were 9 of 20 elements showed larger result from the geochemical mod-

el, indicated by a value ˂ 1. Leaching of major elements such as K and Na were most similar,

with a value close to zero (Figure 3).

0.01

0.1

1

10

100

1000

10000

0 2 4 6 8 10 12 14

mg/

kg D

M

pH

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Figure 3 Normalized results from column, batch and pH-stat (at pH 8) compared with normalized re-

sults from the geochemical modeling (pH 8, Eh 0.2 V and adsorption possible to aged ferrihydrite). ▪

column v.s. model, • batch v.s. model and x pH-stat v.s. model.

Figure 3 shows that the predicted results from the model in general were underestimated

compared with the experimental results, a value > 1, indicate that the geochemical model can-

not completely describe the results from leaching tests. Some of the variation can be ex-

plained by adsorption to aged ferrihydrite in the geochemical model. For example, As and Pb

were, according to the geochemical model, extensively adsorbed to aged ferrihydrite, 100 and

99%, respectively at pH 8 and Eh 0.2 V (for Pb see Figure 7). The adsorption to aged ferrihy-

drite decreases the amount dissolved As, Si and Pb in the model and the difference between

the geochemical model and leaching tests increases, indicating that adsorption is not im-

portant for these elements. The difference seen for Al can however not be explained by

adsorption, since nothing was adsorbed.

3.3 Environmental assessment – effects of pH and redox potential on leaching

The geochemical model Visual MINTEQ was used in order to increase the understanding how

leaching of Cr, Mo, Cu, Pb and Zn from bottom ash pre-treated with accelerated aging and

addition of Fe0 would be affected by environmental changes e.g. variations in pH and redox

potential. The redox potential in a road construction can become reducing in the centre below

the road but be oxidizing towards the edges (Bendz et al., 2006). According to modelling,

have pH and redox only small effects on the leached amounts whereas the part bound to ferri-

hydrite varies substantially, mainly depending on the pH (Figure 4-8).

0.01

0.1

1

10

100

1000

10000

100000

0 21

Al As Ba Ca Cd Co Cr Cu Fe Si Hg K Mg Mn Mo Na Ni Pb V Zn

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Leaching of Cr depends on the oxidative state, with Cr(VI) being a more mobile form than

Cr(III). Leaching results reported in the literature after aging both increase and decrease,

possibly due to different oxidative state being present (Paper I). In the model was the lowest

result of Cr predicted at pH 6 (Figure 4). The results for the two oxidative states showed that

at lower pH was adsorption of Cr(VI) higher and dissolved Cr was mainly present as Cr(III).

At higher pH was adsorption of Cr(III) higher and dissolved Cr was mainly present as Cr(VI)

(data not shown). This is in agreement with Dijkstra et al. (2002) that states that adsorption of

oxyanions to iron oxides increase at lower pH and adsorption of cations increase at higher pH.

However at very low pH can the protonation result in a lower affinity of anions and at very

high pH can the affinity of cations decrease. According to the model was pH 6 preferred in

order to keep the leaching of Cr to a minimum.

Cr

Red

ox

(V

)

0.8 0.0059

4

0.6 0.0059 0.0034 0.0061

4 44 26

0.4 0.0059 0.0034 0.0043 0.0083

4 44 31 0.0

0.2 0.0060 0.0035 0.0042 0.0059 0.0083

3 43 31 13 0.0

0 0.0059 0.0037 0.0043 0.0051 0.0062

5 39 30 17 0.0

─ 0.2 0.0021 0.0044 0.0051 0.0

66 28 17 0

─ 0.4 0.0030 0.0062

51 0.0

─ 0.6 0.0062

0.0

4 6 8 10 12

pH

Figure 4 Results predicted by the geochemical modeling program Visual MINTEQ Cr (mg/kg) (bold)

and % adsorbed to ferrihydrite. Green indicates leaching below the guideline value, 0.3 mg/kg.

Leaching of Cu reported in the literature decrease as a result of aging and can adsorb to both

iron oxides and Al-hydroxides (Paper I). Results from the model are in agreement with that

and showed that a higher amount of Cu was adsorbed to ferrihydrite at pH 6 and 8 resulting in

a lower amount of dissolved Cu (Figure 5).

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Cu

Red

ox

(V

)

0.8 0.14

0.6

0.6 0.14 0.10 0.10

0.6 28 23

0.4 0.14 0.10 0.10 0.14

0.5 28 23 0.1

0.2 0.14 0.10 0.10 0.14 0.14 0.3 25 23 0.1 0.0

0 0.14 0.11 0.11 0.14 0.14 0.6 18 20 0.1 0.0

─ 0.2 0.10 0.11 0.14 0.14

24 16 0.1 0.0

─ 0.4 0.14 0.14

0.0 0.0

─ 0.6 0.1

0.0

4 6 8 10 12

pH

Figure 5 Results predicted by the geochemical modeling program Visual MINTEQ Cu (mg/kg) (bold)

and % adsorbed to ferrihydrite. Green indicates leaching below the guideline value, 0.6 mg/kg.

Mo

Red

ox

(V

)

0.8 0.00037

100

0.6 0.00037 0.042 0.42

100 91 5

0.4 0.00037 0.042 0.42 0.44

100 91 5 0.0

0.2 0.00037 0.042 0.42 0.44 0.44

100 91 5 0.0 0.0

0 0.00024 0.042 0.42 0.44 0.44

100 91 5 0.0 0.0

─ 0.2

0.014 0.42 0.44 0.44

97 5 0.0 0.0

─ 0.4

0.44 0.44

0.0 0.0

─ 0.6

0.44

0.0

4 6 8 10 12

pH

Figure 6 Results predicted by the geochemical modeling program Visual MINTEQ Mo (mg/kg) (bold)

and % adsorbed to ferrihydrite. Green indicates leaching below leaching limit, 0.5 mg/kg.

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Results from the model showed that Mo (molybdate) was not affected by changes in redox

potential, and the lowest result was predicted at pH 4 with 100% adsorbed to ferrihydrite

(Figure 6). Iron oxides can bind Mo and the affinity for Mo increases with decreasing pH (Pa-

per I). Results from the pH-stat test showed the same pattern as modelling results with leach-

ing results close to the guideline value at pH > 6 and an extreme decrease in leaching at pH 4.

(Paper III).

The model predicted a much lower result for Pb at pH 6, 8 and 10 with the lowest at pH 10

(Figure 7). Leaching of Pb from aged bottom ash has been reported to be controlled by

sorption to e.g. Al-hydroxides, iron oxides (Paper I). Adsorption of cations increase with

increasing pH but can at extreme high pH decrease (Dijkstra et al., 2002).

Pb

Red

ox

(V

)

0.8 0.0019

19

0.6 0.0019 0.000033 0.000032

19 99 99

0.4 0.0019 0.000033 0.000032 0.000024

19 99 99 99

0.2 0.0019 0.000034 0.000032 0.000024 0.0018

19 99 99 99 23

0 0.0024 0.000037 0.000033 0.000024 0.0018

0.0 98 99 99 23

─ 0.2 0.0024 0.000035 0.000024 0.0018

0.0 99 99 23

─ 0.4 0.0024 0.0018

0.0 23

─ 0.6 0.0024

0.0

4 6 8 10 12

pH

Figure 7 Results predicted by the geochemical modeling program Visual MINTEQ Pb (mg/kg) (bold)

and % adsorbed to ferrihydrite. Green indicates leaching below the guideline value, 0.3 mg/kg.

Leaching of Zn in aged bottom ash is pH-dependent, and Zn has a high affinity for Al-

hydroxides and iron oxides (Paper I). The modelling results show that Zn was affected by

changes in pH and with the lowest predicted result at pH 8, where sorption to ferrihydrite was

the highest (Figure 8).

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Zn

Red

ox

(V

)

0.8 6.9

0.0

0.6 6.9 6.1 1.1

0.0 11 85

0.4 6.9 6.1 1.1 5.3

0.0 11 85 23

0.2 6.9 6.1 1.1 5.3 6.9 0.0 11 85 23 0.0

0 6.9 6.1 1.1 5.3 6.9 0.0 11 84 23 0.0

─ 0.2 6.9 1.1 5.3 6.9

0.0 84 23 0.0

─ 0.4 6.9 6.9

0.0 0.0

─ 0.6 6.9

0.0

4 6 8 10 12

pH

Figure 8 Results predicted by the geochemical modeling program Visual MINTEQ Zn (mg/kg) (bold)

and % adsorbed to ferrihydrite. Green indicates leaching below and red indicates leaching above the

guideline value, 3 mg/kg.

According to Visual MINTEQ was pre-treatment of bottom ash using Fe0 an effective method

in order to reduce the leaching of Cr, Cu, Mo and Pb since leaching was below the guideline

values for all modeling scenarios, even though variations in pH and redox had an effect on the

amout of metals dissolved in the model. The model suggested that pH of the material should

be ˂ 10 and ˃ 6 in order to maintain the leaching of Zn below the guideline value for use as a

construction material (SNV, 2010).

However, there are reasons to question the modelling results. First, results from pH-stat of the

pre-treated bottom ash showed a much higher leaching at certain pH than the geochemical

model. The leaching of Cr and Cu were at the level of the guideline values at pH 4 and 7,

respectively, while at pH 4 Cu leaching exceed the value about 40 times and Pb leaching with

a factor of 30. Mo leaching touched the limit value at pH ˃ 7 (Paper III). Second, modeling

using results from column test of untreated bottom ash gave similar results as pre-treated

bottom ash shown in Figure 4-8, which seems unlikely and agrees even less with the real pH

stat test results.

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3.4 Buffering capacity

Leaching of many elements is controlled by pH and it is therefore of interest to estimate the

time needed for carbonation to reduce pH in the bottom ash. Many cations forming metals

like Zn have their lowest leaching at pH 9 and reducing the pH lower than that increases the

leaching (Van der Sloot et al. 2004). The ANC of the solid samples of bottom ash pre-treated

with Fe0 were used in order to estimate the amount of H

+ needed to reduce the pH to 9, 8 and

7 (equation 1). The effective diffusion coefficient (Deff) was calculated using an empirical

equation by Reardon & Moddle (1985) (equation 2). Deff was then used to calculate the time

needed to reach pH 9, 8 and 7 in a pile with a height of 3 meters (equation 3 and 4). The re-

sults are presented in Table 2.

Table 2 Buffering capacity for bottom ash pre-treated with Fe0

pH 9 pH 8 pH 7

ANC (mol H+ / kg DM) 0.058 0.28 0.37

Years1 9 44 58

1Reardon & Moddle (1985)

44 years in order to reach pH 8 does not seem like a long time. However, the permeability in a

construction e.g. a road would probably be lower due to packing of the material and the cover

of the road and hence would the time needed for pH to decrease from just above pH 9 to pH 8

probably increase.

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4 CONCLUSIONS

Normalized results, % of the sum of total analysed for each element from column, batch and

pH-stat tests showed that major elements hade the least discrepancy between the tests.

Whereas Al and Zn showed the largest, possibly depending on pH difference between the

leaching tests. This indicates the importance of reporting pH-values when leaching results are

discussed.

The geochemical model described the leaching results within one order of magnitude for most

elements, except for Al, As, Si and Pb where the difference was as high as 5 orders of magni-

tude. The large variation can depend on a high adsorption of As, Si and Pb to aged ferrihy-

drite, resulting in a large variation in the amounts dissolved in the model and experimental

data. This implies that adsorption to aged ferrihydrite should be excluded in order to get a

better prediction regarding leaching of As, Si and Pb.

pH should be ˂ 10 and ˃ 6 according to the environmental assessment made using Visual

MINTEQ in order to maintain a low enough leaching of Zn. Cr, Cu, Mo and Pb were below

guideline values despite variations of pH and redox potential. The comparison of modelling

results against leaching results showed that Cu, Cr, Pb and Zn were underestimated in the

model. Results from pH-stat support this, since leaching of Cr, Cu, Mo and Pb from pH-stat

were well above the guideline values at specific pH values (Paper III). It is, therefore, possible

that the results in the environmental assessment were underestimated as well, giving a false

indication of the quality of the bottom ash. The used model therefore needs to be developed in

order to make beter predctions regarding quality of the bottom ash.

5 FUTURE RESEARCH

In order to increase the knowledge and improve the quality of bottom ash are the following

suggested.

- The mineralogy of bottom ash treated with Fe0 should be evaluated further in order to

detect specific iron compounds formed and weather metals like Cu, Cr and Zn are as-

sociated with them. Since non-crystalline iron oxides can be expected to form, a meth-

od capable of detecting them like scanning electron microscopy (SEM) shoild be ap-

plied.

- The evaluations of bottom ash commonly either focused on mineralogy or leaching.

These two should be combined in order to increase the understanding regarding leach-

ing of metals from bottom ash.

- However, the main focus for improving the quality of bottom ash should be made be-

fore the bottom ash is produced, by considering what is being incinerated and how it is

incinerated. There is a large potential for development in this area.

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