Cited by 281Arsenic contamination and mitigationHeavy metals in environmentMine drainage and remediation techniques

Arsenic in shallow, reducing groundwaters in southern Asia: an environmental health disaster

Charlet, L., Polya, D. A.·2006·Elements

Abstract

Arsenic concentrations in shallow, reducing groundwaters in Bengal, Southeast Asia, and elsewhere constitute a major hazard to the health of people using these waters for drinking, cooking, or irrigation. A comparison of occurrences in the Ganges-Brahmaputra, Mekong, and Red River basins shows that common geological characteristics include (1) river drainage from the rapidly weathering Himalayas, (2) rapidly buried organic-bearing and relatively young (ca. Holocene) sediments, and (3) very low, basin-wide hydraulic gradients. Anaerobic microbial respiration, utilizing either sedimentary or surface-derived organic carbon, is one important process contributing to the mobilization of arsenic from host minerals, notably hydrous iron oxides. In spite of the paucity of data from before the extensive development of groundwater pumping in these areas, there is sufficient evidence to make a prima facie case that human activity might exacerbate arsenic release into these groundwaters. The difficulties in implementing comprehensive groundwater remediation suggest serious attention should be given to developing treatment technologies for alternative surface-water supplies.

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Crossref · 10.2113/gselements.2.2.91

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2 of 2 references verified0 citation errors · 0 not checkable

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  • Reductive dissolution of arsenic-bearing Fe(III) minerals is driven by metal reducing bacteria and fuelled by organic matter providing an electron donor.

    “a process which is driven by metal reducing bacteria and fuelled by organic matter providing an electron donor (Charlet and Polya, 2006;Islam et al., 2004;Postma et al., 2007;Bhattacharya et al., 1997;Rowland et al., 2009)”
  • In the Mekong Delta of Cambodia, anoxic sediment conditions created by extensive monsoonal flooding cause favourable anaerobic processes such as arsenate respiration to occur.

    “In the Mekong Delta of Cambodia, anoxic sediment conditions created by extensive monsoonal flooding cause favourable anaerobic processes such as arsenate respiration (a microbial process significantly contributing to arsenic mobilization via reductive dissolution of arsenic-bearing iron minerals) to occur (Charlet and Polya, 2006;Islam et al., 2004;Postma et al., 2007;Bhattacharya et al., 1997;Row”

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Authors
Charlet, L., & Polya, D. A.
Affiliations
  • Centre National de la Recherche Scientifique (FR)
  • University of Manchester (GB)
Venue
Elements
Published
2006-04-01
Volume
2
Issue
2
Pages
91-96
ISSN
  • 1811-5209 (ISSN-L)
  • 1811-5217
OpenAlex
W2132895747
Cited by
281
References
2
Citations by year
2026: 3 · 2025: 2 · 2024: 7 · 2023: 19 · 2022: 11 · 2021: 11 · 2020: 14 · 2019: 13 · 2018: 12 · 2017: 19 · 2016: 16 · 2015: 11 · 2014: 20 · 2013: 19 · 2012: 16
FWCI
15.27
Type
journal article
Language
en
Open access
closed
Locations
  • Elements (publishedVersion)
  • HAL (submittedVersion)
Funders
Engineering and Physical Sciences Research Council
Topics
  • Physical Sciences › Environmental Science › Environmental Chemistry › Arsenic contamination and mitigation
  • Physical Sciences › Environmental Science › Pollution › Heavy metals in environment
  • Physical Sciences › Environmental Science › Environmental Chemistry › Mine drainage and remediation techniques
Keywords
arsenic contamination, groundwater, reducing conditions, shallow aquifers, environmental health, public health crisis, South Asia

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