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Understanding bioaccumulation and
biotransformation processes of high
priority contaminants in fiber banks
sediments in the northern Baltic Seasediments in the northern Baltic Sea
Darya Kupryianchyk1,*, Channa Yath1, Terry Bidleman1, Henrik
Larsson2, Per Liljelind1, Agneta Andersson3, Owen Rowe3, Johan
Wikner2,3, Peter Haglund1, Mats Tysklind1
1Department of Chemistry, Umeå University, Sweden
2Umeå Marine Research Center, Hörnefors, Sweden
3Department of Ecology and Environmental Science, Umeå University, Sweden
*E-mail: darya.kupryianchyk@umu.se
Pulp and paper industry in Sweden
1. http://www.isover-technical-insulation.co.za/About-ISOVER/Reference-
project/Industry-insulation-for-south-africa/Smurfit-Kappa-Kraftliner-Mill-Piteaa
2. http://www.vinnova.se/upload/EPiStorePDF/va_14_08.pdf 2
• requires the availability of water
• concentrated along the coast of northern Sweden
(Norrland)
Fiber banks areas
• Rich in fiber, cellulose/lignin
• Contaminated with PCBs,
PAH, and other POPs
• Effect of sediment properties
on sorption?
• What are biodegradation and
”primary source”
• What are biodegradation and
biotransformation processes
in fiber banks sediments?
3
Secondary source
Objectives
• sediment-to-water exchange of POPs in fiber
banks sediment,
• how differences in properties of contaminated• how differences in properties of contaminated
sediments affect bioaccumulation and
biodegradation of POPs,
• Effect of species-specific traits on
bioaccumulation
4
Sampling locations
Norrbyn
(reference)
Örnsköldsvik
5
Kramfors
Bioaccumulation experiment
Kramfors
No biota
Macoma
balthica
Marenzelleria
spp
T=28 days
Climate controlled room
6
Örnsköldsvik
Norrbyn (ref)
Chemical analysis
Extraction
• Sediment and biota –with toluene by
accelerated solvent extractor
• Pore water – with polyoxymethyene (76um)
– extraction with heptane/acetone 80/20– extraction with heptane/acetone 80/20
Instrumental analysis: GC - high resolution
MS with columns specific to the task:
• DB5ms for quantitative work and
• the cyclodextrin stationary phase CP-Chiral-
Dex-CB for enantiospecific analysis.
7
Chemical analysis
20
40
60
80
Csed,ng/g
SedimentCB180
CB153
CB138
CB118
CB101
CB52
CB28
5
10
15
20
Cpw,pg/L
Pore waterCB180
CB153
CB138
CB118
CB101
CB52
CB28
CB180
• Sediment – Kramfors and Ö-vik are class V according to the
Swedish classification of contaminated sediments;
• pore water - high abundance of low molecular congeners, e.g. CB28,
52 and 101;
0
NOR KRA ORN
0
NOR KRA ORN
0
200
400
600
800
1000
1200
NOR KRA ORN NOR KRA ORN
Mar Mac
Cbiota,ng/glipids
Biota
CB180
CB153
CB138
CB118
CB101
CB52
CB28
• good agreement between PCB profiles in sediment and
invertebrates -> sediment is a primary source of PCBs;
4
6
8
10
LogKd,L/kg
Log Kd vs Log Kow
Örnsköldsvik
Sorption
1
2
3
4
5
6
7
talorganicandinorganic
carbon,%d.w.
Total organic and inorganic
Örnsöldsvik
Kramfors
Norrbyn
2
4
5,0 5,5 6,0 6,5 7,0 7,5 8,0
LogKow
Kramfors
Norrbyn
92
4
6
8
10
12
5,0 5,5 6,0 6,5 7,0 7,5 8,0
LogKoc,L/kg
LogKow
Log Koc vsLog Kow
Örnsköldsvik
Kramfors
Norrbyn
0
1
TOC TIC
Tota
Lignin and cellulose
0
5
10
15
20
Relativeabundance,%
Lignin
20
40
60
80
100
Relativeabundance,%
Cellulose
10
0
2
4
6
8
Önrsköldsvik Kramfors Norrbyn
Cellulose/lignin
Cellulose/lignin
Önrsköldsvik Kramfors Norrbyn 0
Önrsköldsvik Kramfors Norrbyn
y = 0,7603x + 2,7033
R² = 0,408
y = 1,2456x + 0,6421
R² = 0,7337
4
5
6
7
8
9
10
LogBAF,LogKoc
Örnsköldsvik
LogBAF
LogKoc
Sorption to sediment OC and biota lipids
y = 1,7028x - 3,648
R² = 0,7134
y = 1,1707x + 0,202
R² = 0,583
4
5
6
7
8
9
10
LogBAF,LogKoc
Kramfors
LogBAF
LogKoc
4
5,0 5,5 6,0 6,5 7,0 7,5 8,0
Log Kow
11
LogKoc exceeded LogBAF
by 1-1.5 orders of
magnitude in Örnsköldsvik,
however LogKoc were
comparable to LogBAF in
Kramfors and Norrbyn
sediments.
y = 1,809x - 4,2942
R² = 0,7633
y = 1,6897x - 3,8155
R² = 0,8151
4
5
6
7
8
9
10
5,0 5,5 6,0 6,5 7,0 7,5 8,0
LogBAF,LogKoc
Log Kow
Norrbyn
LogBAF
LogKoc
4
5,0 5,5 6,0 6,5 7,0 7,5 8,0
Log Kow
Sorption to sediment OC and biota lipids
y = 1,0485x + 0,2138
R² = 0,5556
y = 1,3948x - 0,393
R² = 0,8358
4
5
6
7
8
9
10
LogBAF,LogKoc
Örnsköldsvik
LogBAF
LogKoc
y = 1,1042x + 0,3527
R² = 0,572
y = 1,2151x - 0,1794
R² = 0,7177
4
5
6
7
8
9
10
LogBAF,LogKoc
Kramfors
LogBAF
LogKoc
12
4
5,0 5,5 6,0 6,5 7,0 7,5 8,0
Log Kow
4
5,0 5,5 6,0 6,5 7,0 7,5 8,0
Log Kow
y = 1,0577x + 0,3857
R² = 0,6529
y = 1,6949x - 3,9442
R² = 0,9659
4
5
6
7
8
9
10
5,0 5,5 6,0 6,5 7,0 7,5 8,0
LogBAF,LogKoc
Log Kow
Norrbyn
LogBAF
LogKoc
Similar results for
Marenzelleria spp but no
difference between the
species
0
1
2
3
LogBSAF
BSAF vsLog Kow. Macoma balthica
Örnsköldsvik
Kramfors
Norrbyn
Biota to sediment accumulation factor
-1
5,0 5,5 6,0 6,5 7,0 7,5 8,0
LogKow
13-2
-1
0
1
2
3
4
5,0 5,5 6,0 6,5 7,0 7,5 8,0
LogBSAF
LogKow
BSAF vsLog Kow. Marenzelleria spp
Örnsköldsvik
Kramfors
Norrbyn
Chiral PCBs as tracers of transport
and accumulation processes
Primary
emisions
(racemic
chemicals)
Mix
Sediment,
water
chemicals)
Secondary
emisions
(nonracemic
chemicals
Non-racemic enantiomer proportions -> biological
degradation, metabolism in soil water, organisms
0,3
0,4
0,5
0,6
0,7
EF
Kramfors
0,3
0,4
0,5
0,6
0,7
EF
Örnsköldsvik
Chiral PCBs as tracers of transport
and accumulation processes
0,3
CB95 CB91 CB136 CB149 CB176
sediment pore water
Macoma balthica Marenzelleria spp
0,3
CB95 CB91 CB136 CB149 CB176
sediment pore water
Macoma balthica Marenzelleria spp
15
0,3
0,4
0,5
0,6
0,7
CB95 CB91 CB136 CB149 CB176
EF
Norrbyn
sediment pore water
Macoma balthica Marenzelleria spp
Chiral PCBs as tracers of transport
and accumulation processes
• Most chiral PCBs in sediments were racemic -> recent
pollution or lack of enantioselective microbial
degradation
• nonracemic EFs of PCB 136 in Örnsköldsvik and 91 in
Kramfors indicate metabolism for these PCBs, so other PCBs
may also be degrading, but not enantioselectivelymay also be degrading, but not enantioselectively
• EFs in pore water should be the same as in sediment due to
dynamic contaminant exchange among them
• Nonrecemic EF of PCB 95 and 136 in Macoma balthica
samples -> enantioselective metabolism
16
Acknowledgments
The research was supported by the Swedish Research
Council for Environment, Agricultural Sciences and Spatial
Planning (Formas)

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Kupryianchyk: Understanding bioaccumulation and biotransformation processes of high priority contaminants

  • 1. Understanding bioaccumulation and biotransformation processes of high priority contaminants in fiber banks sediments in the northern Baltic Seasediments in the northern Baltic Sea Darya Kupryianchyk1,*, Channa Yath1, Terry Bidleman1, Henrik Larsson2, Per Liljelind1, Agneta Andersson3, Owen Rowe3, Johan Wikner2,3, Peter Haglund1, Mats Tysklind1 1Department of Chemistry, Umeå University, Sweden 2Umeå Marine Research Center, Hörnefors, Sweden 3Department of Ecology and Environmental Science, Umeå University, Sweden *E-mail: darya.kupryianchyk@umu.se
  • 2. Pulp and paper industry in Sweden 1. http://www.isover-technical-insulation.co.za/About-ISOVER/Reference- project/Industry-insulation-for-south-africa/Smurfit-Kappa-Kraftliner-Mill-Piteaa 2. http://www.vinnova.se/upload/EPiStorePDF/va_14_08.pdf 2 • requires the availability of water • concentrated along the coast of northern Sweden (Norrland)
  • 3. Fiber banks areas • Rich in fiber, cellulose/lignin • Contaminated with PCBs, PAH, and other POPs • Effect of sediment properties on sorption? • What are biodegradation and ”primary source” • What are biodegradation and biotransformation processes in fiber banks sediments? 3 Secondary source
  • 4. Objectives • sediment-to-water exchange of POPs in fiber banks sediment, • how differences in properties of contaminated• how differences in properties of contaminated sediments affect bioaccumulation and biodegradation of POPs, • Effect of species-specific traits on bioaccumulation 4
  • 6. Bioaccumulation experiment Kramfors No biota Macoma balthica Marenzelleria spp T=28 days Climate controlled room 6 Örnsköldsvik Norrbyn (ref)
  • 7. Chemical analysis Extraction • Sediment and biota –with toluene by accelerated solvent extractor • Pore water – with polyoxymethyene (76um) – extraction with heptane/acetone 80/20– extraction with heptane/acetone 80/20 Instrumental analysis: GC - high resolution MS with columns specific to the task: • DB5ms for quantitative work and • the cyclodextrin stationary phase CP-Chiral- Dex-CB for enantiospecific analysis. 7
  • 8. Chemical analysis 20 40 60 80 Csed,ng/g SedimentCB180 CB153 CB138 CB118 CB101 CB52 CB28 5 10 15 20 Cpw,pg/L Pore waterCB180 CB153 CB138 CB118 CB101 CB52 CB28 CB180 • Sediment – Kramfors and Ö-vik are class V according to the Swedish classification of contaminated sediments; • pore water - high abundance of low molecular congeners, e.g. CB28, 52 and 101; 0 NOR KRA ORN 0 NOR KRA ORN 0 200 400 600 800 1000 1200 NOR KRA ORN NOR KRA ORN Mar Mac Cbiota,ng/glipids Biota CB180 CB153 CB138 CB118 CB101 CB52 CB28 • good agreement between PCB profiles in sediment and invertebrates -> sediment is a primary source of PCBs;
  • 9. 4 6 8 10 LogKd,L/kg Log Kd vs Log Kow Örnsköldsvik Sorption 1 2 3 4 5 6 7 talorganicandinorganic carbon,%d.w. Total organic and inorganic Örnsöldsvik Kramfors Norrbyn 2 4 5,0 5,5 6,0 6,5 7,0 7,5 8,0 LogKow Kramfors Norrbyn 92 4 6 8 10 12 5,0 5,5 6,0 6,5 7,0 7,5 8,0 LogKoc,L/kg LogKow Log Koc vsLog Kow Örnsköldsvik Kramfors Norrbyn 0 1 TOC TIC Tota
  • 10. Lignin and cellulose 0 5 10 15 20 Relativeabundance,% Lignin 20 40 60 80 100 Relativeabundance,% Cellulose 10 0 2 4 6 8 Önrsköldsvik Kramfors Norrbyn Cellulose/lignin Cellulose/lignin Önrsköldsvik Kramfors Norrbyn 0 Önrsköldsvik Kramfors Norrbyn
  • 11. y = 0,7603x + 2,7033 R² = 0,408 y = 1,2456x + 0,6421 R² = 0,7337 4 5 6 7 8 9 10 LogBAF,LogKoc Örnsköldsvik LogBAF LogKoc Sorption to sediment OC and biota lipids y = 1,7028x - 3,648 R² = 0,7134 y = 1,1707x + 0,202 R² = 0,583 4 5 6 7 8 9 10 LogBAF,LogKoc Kramfors LogBAF LogKoc 4 5,0 5,5 6,0 6,5 7,0 7,5 8,0 Log Kow 11 LogKoc exceeded LogBAF by 1-1.5 orders of magnitude in Örnsköldsvik, however LogKoc were comparable to LogBAF in Kramfors and Norrbyn sediments. y = 1,809x - 4,2942 R² = 0,7633 y = 1,6897x - 3,8155 R² = 0,8151 4 5 6 7 8 9 10 5,0 5,5 6,0 6,5 7,0 7,5 8,0 LogBAF,LogKoc Log Kow Norrbyn LogBAF LogKoc 4 5,0 5,5 6,0 6,5 7,0 7,5 8,0 Log Kow
  • 12. Sorption to sediment OC and biota lipids y = 1,0485x + 0,2138 R² = 0,5556 y = 1,3948x - 0,393 R² = 0,8358 4 5 6 7 8 9 10 LogBAF,LogKoc Örnsköldsvik LogBAF LogKoc y = 1,1042x + 0,3527 R² = 0,572 y = 1,2151x - 0,1794 R² = 0,7177 4 5 6 7 8 9 10 LogBAF,LogKoc Kramfors LogBAF LogKoc 12 4 5,0 5,5 6,0 6,5 7,0 7,5 8,0 Log Kow 4 5,0 5,5 6,0 6,5 7,0 7,5 8,0 Log Kow y = 1,0577x + 0,3857 R² = 0,6529 y = 1,6949x - 3,9442 R² = 0,9659 4 5 6 7 8 9 10 5,0 5,5 6,0 6,5 7,0 7,5 8,0 LogBAF,LogKoc Log Kow Norrbyn LogBAF LogKoc Similar results for Marenzelleria spp but no difference between the species
  • 13. 0 1 2 3 LogBSAF BSAF vsLog Kow. Macoma balthica Örnsköldsvik Kramfors Norrbyn Biota to sediment accumulation factor -1 5,0 5,5 6,0 6,5 7,0 7,5 8,0 LogKow 13-2 -1 0 1 2 3 4 5,0 5,5 6,0 6,5 7,0 7,5 8,0 LogBSAF LogKow BSAF vsLog Kow. Marenzelleria spp Örnsköldsvik Kramfors Norrbyn
  • 14. Chiral PCBs as tracers of transport and accumulation processes Primary emisions (racemic chemicals) Mix Sediment, water chemicals) Secondary emisions (nonracemic chemicals Non-racemic enantiomer proportions -> biological degradation, metabolism in soil water, organisms
  • 15. 0,3 0,4 0,5 0,6 0,7 EF Kramfors 0,3 0,4 0,5 0,6 0,7 EF Örnsköldsvik Chiral PCBs as tracers of transport and accumulation processes 0,3 CB95 CB91 CB136 CB149 CB176 sediment pore water Macoma balthica Marenzelleria spp 0,3 CB95 CB91 CB136 CB149 CB176 sediment pore water Macoma balthica Marenzelleria spp 15 0,3 0,4 0,5 0,6 0,7 CB95 CB91 CB136 CB149 CB176 EF Norrbyn sediment pore water Macoma balthica Marenzelleria spp
  • 16. Chiral PCBs as tracers of transport and accumulation processes • Most chiral PCBs in sediments were racemic -> recent pollution or lack of enantioselective microbial degradation • nonracemic EFs of PCB 136 in Örnsköldsvik and 91 in Kramfors indicate metabolism for these PCBs, so other PCBs may also be degrading, but not enantioselectivelymay also be degrading, but not enantioselectively • EFs in pore water should be the same as in sediment due to dynamic contaminant exchange among them • Nonrecemic EF of PCB 95 and 136 in Macoma balthica samples -> enantioselective metabolism 16
  • 17. Acknowledgments The research was supported by the Swedish Research Council for Environment, Agricultural Sciences and Spatial Planning (Formas)