I.1 Geogenic and anthropogenic sources of arsenic: Significance and characterisation Arsenic mobilization during seawater inundation of acid sulfate soils—hydrogeochemical coupling at the tidal fringe

doi:10.1201/b12522-13

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I.1 Geogenic and anthropogenic sources of arsenic: Significance and characterisation Arsenic mobilization during seawater inundation of acid sulfate soils—hydrogeochemical coupling at the tidal fringe

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I.1 Geogenic and anthropogenic sources of arsenic: Significance and characterisation Arsenic mobilization during seawater inundation of acid sulfate soils—hydrogeochemical coupling at the tidal fringe

DOI link for I.1 Geogenic and anthropogenic sources of arsenic: Significance and characterisation Arsenic mobilization during seawater inundation of acid sulfate soils—hydrogeochemical coupling at the tidal fringe

I.1 Geogenic and anthropogenic sources of arsenic: Significance and characterisation Arsenic mobilization during seawater inundation of acid sulfate soils—hydrogeochemical coupling at the tidal fringe book

I.1 Geogenic and anthropogenic sources of arsenic: Significance and characterisation Arsenic mobilization during seawater inundation of acid sulfate soils—hydrogeochemical coupling at the tidal fringe

DOI link for I.1 Geogenic and anthropogenic sources of arsenic: Significance and characterisation Arsenic mobilization during seawater inundation of acid sulfate soils—hydrogeochemical coupling at the tidal fringe

I.1 Geogenic and anthropogenic sources of arsenic: Significance and characterisation Arsenic mobilization during seawater inundation of acid sulfate soils—hydrogeochemical coupling at the tidal fringe book

ByS.G. Johnston, E.D. Burton, A.F. Keene, R.T. Bush & L.A. Sullivan

BookUnderstanding the Geological and Medical Interface of Arsenic - As 2012

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Edition 1st Edition

First Published 2012

Imprint CRC Press

Pages 2

eBook ISBN 9780429216831

ABSTRACT

The study site is a ∼200 ha Holocene sedimentary coastal plain adjacent to Cairns in tropical northern Australia. A tide excluding wall was constructed around the site in the 1970’s. Tide exclusion and intensive drainage caused the oxidation of iron-sulfides and formation of severe acid sulfate soils across the site. A remediation program commenced at the site in 2001-2002. This has involved incrementally increasing tidal inundation of acid sulfate soils.

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