coastal acid sulfate soils - marine and coasts...aass: actual acid sulfate soil or ‘sulfuric’...
TRANSCRIPT
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Coastal Acid Sulfate Soils
Vanessa Wong
MONASH
SCIENCE
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What are acid sulfate soils?
▪ Acid sulfate soils are soils and sediments containing oxidisable or
already oxidised metal sulfides (mainly pyrite – FeS2)
▪ PASS: potential acid sulfate soil, or ‘sulfidic’ soil when they remain in a
waterlogged state
▪ AASS: actual acid sulfate soil or ‘sulfuric’ soil when exposed to air and
oxidised
▪ These soils are normally found in marshy environments
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Formation of acid sulfate soils
▪ Coastal acid sulfate soils (CASS) formed about 10,000
years ago during periods of higher sea levels (sea levels
about 1.5 m higher than today)
▪ Pyrite forms in saline sediments where there is an
accumulation of:– Labile organic matter
– SO42-
– Fe3+
– An anaerobic
environment
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pyrite oxygen Colloidal Fe3+ Sulfuric acid
FeS2 + 15/4O2 + 7H2O → Fe(OH)3 + 4H+ + 4SO42-
• Pyrite is only stable under anaerobic conditions• Becomes problematic when exposed to oxygen• Oxidation can be caused by drainage, excavation, dredging, etc
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Impacts of acid sulfate soils
▪ Directly affects aquatic
ecosystems
– Discharges of acidity and rapid drop
in pH
– Discharges of trace metals resulting
in metal toxicity, especially Al
– Crystal clear water
– In extreme cases, fish kills occurs
▪ Colloidal iron oxides and iron flocs
coat benthos
▪ Concrete cancer
– Infrastructure instability
▪ Soil ripening
– Occurs as CASS dewater
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Where do they occur?
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Proposal: Presence of acid sulfate soils
▪ Quantify acidification
potential
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Proposal
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Formation of acid sulfate soils
▪ Pyrite forms in saline sediments where there is an
accumulation of:– Labile organic matter
– SO42-
– Fe3+
– An anaerobic
environment
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Proposal: pyrite and monosulfide formation
▪ Incubations
– Each treatment
can be mapped
▪ Vegetation
– Saltmarsh
– Mangrove
– Seaweed
▪ Surface water
– Seawater
– Brackish water
– Freshwater▪ Sediment compartments
– High Si
– High Fe
▪ Oxygen availability
– Complete inundation
– Wet/dry cycles
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Proposal: Inundation and resuspension
▪ Effects of inundation on
water quality
▪ Potential oxidation with
resuspension
– Effects on water quality
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Unknowns
▪ Most of our knowledge on acid
sulfate soils comes from the east
coast– Victorian embayments, estuaries and
estuarine floodplains are different to the
east coast
▪ Distribution of coastal and inland
acid sulfate soils and how they
interact
▪ Characterisation of acid sulfate
soils
▪ Formation of Victorian estuaries
– Formation of acid sulfate soils
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pH
3 4 5 6 7 8 9
Depth
(m
)
0.0
0.2
0.4
0.6
0.8
1.0
1.2
1.4
1.6
WE
SS
TAA (mol H+/t)
-40 0 40 80 120 160 200 240 280 320
Depth
(m
)
0.0
0.2
0.4
0.6
0.8
1.0
1.2
1.4
1.6
WE
SS
Net acidity (mol H+/t)
-1500 -1000 -500 0 500
Depth
(m
)
0.0
0.2
0.4
0.6
0.8
1.0
1.2
1.4
1.6
WE
SS
pH TAA (mol H+/t) Net Acidity (mol H+/t)
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pH
3 4 5 6 7 8 9
Depth
(m
)
0.0
0.2
0.4
0.6
0.8
1.0
1.2
1.4
1.6
WO
CTS
TAA (mol H+/t)
-40 0 40 80 120 160 200 240 280 320
De
pth
(m
)
0.0
0.2
0.4
0.6
0.8
1.0
1.2
1.4
1.6
WO
CTS
Net acidity (mol H+/t)
-1500 -1000 -500 0 500
De
pth
(m
)
0.0
0.2
0.4
0.6
0.8
1.0
1.2
1.4
1.6
WO
CTS
pH TAA (mol H+/t) Net Acidity (mol H+/t)