Characterisation of dissolved organic matter in two contrasting arsenic-prone sites in Kandal Province, Cambodia

• Ultra-high resolution mass spectrometry study of As-prone aquifer dissolved organics. • Optical/molecular analyses indicate overall dominance of terrestrial-derived organics. • Likely microbial processing of organics since percolation into the aquifer. • Analyses support role dissolved organics play during microbial mediated As release. Aquifers throughout Asia are impacted by the release of geogenic arsenic (As) into groundwater by microbial reduction of As-bearing Fe(III) (oxy)hydroxide minerals, severely impacting water quality. Groundwater dissolved organic matter (DOM) is likely key to As release, mainly as electron donor or electron shuttles. This study used optical analyses and ultra-high resolution mass spectrometry to examine the sources and composition of groundwater DOM in the As-prone aquifers of Kandal Province, Cambodia, at boreholes with differing host lithology (clay- and sand-dominated). Groundwater and surface water DOM composition were related to As concentrations, to infer the potential role of DOM in promoting As release. Optical and molecular-level analyses indicated an overall dominance of terrestrial-derived DOM in the groundwater samples, with higher freshness index and relative abundance (RA) of aliphatic compounds in clay compared to sand-dominated lithology. Compared to surface water, groundwater DOM had relatively lower O/C ratios and nominal oxidation state of carbon (−0.19 to −0.13 compared to 0.04 for ground and surface water, respectively), with a lower %RA of aliphatic compounds and higher %RA of carboxyl-rich alicyclic molecules, suggesting microbial processing of DOM since percolation into the aquifer. Concentrations of As across both sites were negatively correlated with DOM tryptophan:fulvic-like fluorescence and the %RA of aliphatics, potentially indicating microbial degradation of biolabile DOM in connection with As release, which is consistent with its role as an electron donor source. Together these data support DOM composition as an important control on microbial mediated As release.

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Publication Details

Journal
Organic Geochemistry
Published
2024-10-20
DOI
https://doi.org/10.1016/j.orggeochem.2024.104886
Citations
4
Primary Topic
Arsenic contamination and mitigation
Type
article
Field-Weighted Citation Impact
1.00

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article

Characterisation of dissolved organic matter in two contrasting arsenic-prone sites in Kandal Province, Cambodia

Amy D. Holt, Amy M. McKenna, Laura A. Richards, Dan Lapworth et al.
4 citations
Organic Geochemistry
Arsenic contamination and mitigation
1.00
article

Characterisation of dissolved organic matter in two contrasting arsenic-prone sites in Kandal Province, Cambodia

Amy D. Holt, Amy M. McKenna, Laura A. Richards, Dan Lapworth, Bart E. van Dongen, Jonathan Richard Lloyd, Robert G. M. Spencer, David A. Polya, Oliver C. Moore
article en
4 citations

Abstract

• Ultra-high resolution mass spectrometry study of As-prone aquifer dissolved organics. • Optical/molecular analyses indicate overall dominance of terrestrial-derived organics. • Likely microbial processing of organics since percolation into the aquifer. • Analyses support role dissolved organics play during microbial mediated As release. Aquifers throughout Asia are impacted by the release of geogenic arsenic (As) into groundwater by microbial reduction of As-bearing Fe(III) (oxy)hydroxide minerals, severely impacting water quality. Groundwater dissolved organic matter (DOM) is likely key to As release, mainly as electron donor or electron shuttles. This study used optical analyses and ultra-high resolution mass spectrometry to examine the sources and composition of groundwater DOM in the As-prone aquifers of Kandal Province, Cambodia, at boreholes with differing host lithology (clay- and sand-dominated). Groundwater and surface water DOM composition were related to As concentrations, to infer the potential role of DOM in promoting As release. Optical and molecular-level analyses indicated an overall dominance of terrestrial-derived DOM in the groundwater samples, with higher freshness index and relative abundance (RA) of aliphatic compounds in clay compared to sand-dominated lithology. Compared to surface water, groundwater DOM had relatively lower O/C ratios and nominal oxidation state of carbon (−0.19 to −0.13 compared to 0.04 for ground and surface water, respectively), with a lower %RA of aliphatic compounds and higher %RA of carboxyl-rich alicyclic molecules, suggesting microbial processing of DOM since percolation into the aquifer. Concentrations of As across both sites were negatively correlated with DOM tryptophan:fulvic-like fluorescence and the %RA of aliphatics, potentially indicating microbial degradation of biolabile DOM in connection with As release, which is consistent with its role as an electron donor source. Together these data support DOM composition as an important control on microbial mediated As release.

Organic GeochemistryVol. 198
Florida State University (US), British Geological Survey (GB), University of Manchester (GB), National High Magnetic Field Laboratory (US), Colorado State University (US)
National Science Foundation, National High Magnetic Field Laboratory, Sight Research UK, British Geological Survey, Natural Environment Research Council, Division of Materials Research, Division of Chemistry, High Magnetic Field Laboratory, Chinese Academy of Sciences
Openalex Percentile: Top 26%
Arsenic contamination and mitigation
1.00
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