Seawater causes rapid trace metal mobilisation in coastal lowland acid sulfate soils: Implications of sea level rise for water quality

• Published in: Geoderma Vol. 160; no. 2; pp. 252 - 263
• Main Authors: Wong, Vanessa N.L., Johnston, Scott G., Burton, Edward D., Bush, Richard T., Sullivan, Leigh A., Slavich, Peter G.
• Format: Journal Article
• Language: English
• Published: Amsterdam Elsevier B.V 15.12.2010; Elsevier
• Subjects: Agronomy. Soil science and plant productions; Biological and medical sciences; Brackish; Cations; Coastal; Desorption; Earth sciences; Earth, ocean, space; Exact sciences and technology; Fundamental and applied biological sciences. Psychology; Geochemistry; Inundation; Marine; Metal mobilisation; Mineralogy; Sea level; Sea level rise; Sea water; Seawater inundation; Silicates; Soils; Surficial geology; Trace metals; Water geochemistry; Water quality; South Pacific; Southwest Pacific; New South Wales; Pacific Ocean; Tasman Sea; Australia; Sea level rise; Desorption; Seawater inundation; Metal mobilisation; trace metals; mobilization; cation exchange capacity; Australasia; metals; hydrochemistry; brackish water; solid solution; pH; soils; organic carbon; sea water; soil treatment; inundations; concentration; transport; floodplains; coastal plains; acidity; acid sulfate soils; water quality; desorption; sea level
• ISSN: 0016-7061; 1872-6259
• DOI: 10.1016/j.geoderma.2010.10.002

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 4 h. 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, Fe 2+, 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. ►Concentrations of soluble and exchangeable Al, Fe 2+, Ni, Mn and Zn in all soil extracts increased with increasing seawater concentration. ►Increasing trace metal concentrations with increasing seawater concentration are attributed to the combined effects of exchange processes and acidity. ►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. ►Saline inundation of acid sulfate soil environments, even by relatively brackish water may cause rapid, substantial, shorter-term water quality changes and a pulse release of acidity due to desorption of acidic metal cations.