High resolution profile of inorganic aqueous geochemistry and key redox zones in an arsenic bearing aquifer in Cambodia

Richards, Laura A.; Magnone, Daniel; Sovann, Chansopheaktra; Kong, Chivuth; Uhlemann, Sebastian; Kuras, Oliver; van Dongen, Bart E.; Ballentine, Christopher J.; Polya, David A.. 2017 High resolution profile of inorganic aqueous geochemistry and key redox zones in an arsenic bearing aquifer in Cambodia. Science of The Total Environment, 590-591. 540-553. 10.1016/j.scitotenv.2017.02.217

Before downloading, please read NORA policies.

Preview

Text (Open Access Paper)
1-s2.0-S0048969717304825-main.pdf - Published Version
Available under License Creative Commons Attribution 4.0.
Download (2MB) | Preview

Official URL: https://doi.org/10.1016/j.scitotenv.2017.02.217

Abstract/Summary

Arsenic contamination of groundwaters in South and Southeast Asia is a major threat to public health. In order to better understand the geochemical controls on the mobility of arsenic in a heavily arsenic-affected aquifer in northern Kandal Province, Cambodia, key changes in inorganic aqueous geochemistry have been monitored at high vertical and lateral resolution along dominant groundwater flow paths along two distinct transects. The two transects are characterized by differing geochemical, hydrological and lithological conditions. Arsenic concentrations in groundwater are highly heterogenous, and are broadly positively associated with iron and negatively associated with sulfate and dissolved oxygen. The observed correlations are generally consistent with arsenic mobilization by reductive-dissolution of iron (hydr)oxides. Key redox zones, as identified using groupings of the PHREEQC model equilibrium electron activity of major redox couples (notably ammonium/nitrite; ammonium/nitrate; nitrite/nitrate; dissolved oxygen/water) have been identified and vary with depth, site and season. Mineral saturation is also characterized. Seasonal changes in groundwater chemistry were observed in areas which were (i) sandy and of high permeability; (ii) in close proximity to rivers; and/or (iii) in close proximity to ponds. Such changes are attributed to monsoonal-driven surface-groundwater interactions and are consistent with the separate provenance of recharge sources as identified using stable isotope mixing models.

Item Type:	Publication - Article
Digital Object Identifier (DOI):	10.1016/j.scitotenv.2017.02.217
ISSN:	00489697
Date made live:	03 Aug 2017 13:25 +0 (UTC)
URI:	https://nora.nerc.ac.uk/id/eprint/517474

Item Type:

Publication - Article

Digital Object Identifier (DOI):

10.1016/j.scitotenv.2017.02.217

ISSN:

00489697

Date made live:

03 Aug 2017 13:25 +0 (UTC)

URI:

https://nora.nerc.ac.uk/id/eprint/517474