Seawater causes rapid trace metal mobilisation in coastal lowland acid sulfate soils

Implications of sea level rise for water quality

Vanessa N L Wong, Scott G. Johnston, Edward D. Burton, Richard T. Bush, Leigh A. Sullivan, Peter G. Slavich

Research output: Contribution to journalArticle

15 Citations (Scopus)

Abstract

Coastal floodplains are highly vulnerable to inundation with saline water and the likelihood of inundation will increase with sea level rise. Sediment samples from floodplains containing coastal lowland acid sulfate soils (CLASS) in eastern Australia were subjected to increasing seawater concentration to examine the probable effects of sea level rise on acidity and metal desorption. Ten soils were mixed with synthetic seawater concentrations varying from 0% to 100% at a solid:solution ratio of 1:10 for 4h. There was a slight decrease in pH (≈0.5 units) with increasing seawater concentration following treatment, yet, calculated acidity increased significantly. In most soil treatments, Al was the dominant component of the calculated acidity pool. Al dominated the exchange complex in the CLASS and, correspondingly, was the major metal ion desorbed. In general, concentrations of soluble and exchangeable Al, Fe2+, Ni, Mn and Zn in all soil extracts increased with increasing salinity. Increasing trace metal concentrations with increasing seawater concentration is attributed to the combined effects of exchange processes and acidity. The increasing ionic strength of the seawater treatments displaces trace metals and protons adsorbed on sediments, causing an initial decrease in pH. Hydrolysis of desorbed acidic metal cations can further contribute to acidity and increase mobilisation of trace metals. These findings imply that saline inundation of CLASS environments, even by relatively brackish water may cause rapid, shorter-term water quality changes and a pulse release of acidity due to desorption of acidic metal cations.

Original languageEnglish
Pages (from-to)252-263
Number of pages12
JournalGeoderma
Volume160
Issue number2
DOIs
Publication statusPublished - 2010
Externally publishedYes

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acid sulfate soils
acid sulfate soil
sea level
trace metal
mobilization
acidity
trace elements
lowlands
water quality
seawater
metal
metals
desorption
floodplains
floodplain
cations
cation
sediments
soil
edaphic factors

Cite this

Wong, Vanessa N L ; Johnston, Scott G. ; Burton, Edward D. ; Bush, Richard T. ; Sullivan, Leigh A. ; Slavich, Peter G. / Seawater causes rapid trace metal mobilisation in coastal lowland acid sulfate soils : Implications of sea level rise for water quality. In: Geoderma. 2010 ; Vol. 160, No. 2. pp. 252-263.
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Seawater causes rapid trace metal mobilisation in coastal lowland acid sulfate soils : Implications of sea level rise for water quality. / Wong, Vanessa N L; Johnston, Scott G.; Burton, Edward D.; Bush, Richard T.; Sullivan, Leigh A.; Slavich, Peter G.

In: Geoderma, Vol. 160, No. 2, 2010, p. 252-263.

Research output: Contribution to journalArticle

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T1 - Seawater causes rapid trace metal mobilisation in coastal lowland acid sulfate soils

T2 - Implications of sea level rise for water quality

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AU - Slavich, Peter G.

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