Nature 454, 505-508 (24 July 2008) | doi:10.1038/nature07093; Received 22 May 2007; Accepted 15 May 2008

Near-surface wetland sediments as a source of arsenic release to ground water in Asia

Matthew L. Polizzotto1, Benjamin D. Kocar1, Shawn G. Benner2, Michael Sampson3 & Scott Fendorf1

  1. School of Earth Sciences, Stanford University, Stanford, California 94305, USA
  2. Department of Geosciences, Boise State University, Boise, Idaho 83705, USA
  3. Resource Development International – Cambodia, PO Box 494, Phnom Penh, Cambodia

Correspondence to: Scott Fendorf1 Correspondence and requests for materials should be addressed to S.F. (Email: fendorf@stanford.edu).

Tens of millions of people in south and southeast Asia routinely consume ground water that has unsafe arsenic levels1, 2. Arsenic is naturally derived from eroded Himalayan sediments, and is believed to enter solution following reductive release from solid phases under anaerobic conditions. However, the processes governing aqueous concentrations and locations of arsenic release to pore water remain unresolved, limiting our ability to predict arsenic concentrations spatially (between wells) and temporally (future concentrations) and to assess the impact of human activities on the arsenic problem3, 4, 5, 6, 7, 8, 9. This uncertainty is partly attributed to a poor understanding of groundwater flow paths altered by extensive irrigation pumping in the Ganges-Brahmaputra delta10, where most research has focused. Here, using hydrologic and (bio)geochemical measurements, we show that on the minimally disturbed Mekong delta of Cambodia, arsenic is released from near-surface, river-derived sediments and transported, on a centennial timescale, through the underlying aquifer back to the river. Owing to similarities in geologic deposition, aquifer source rock and regional hydrologic gradients11, 12, 13, 14, 15, our results represent a model for understanding pre-disturbance conditions for other major deltas in Asia. Furthermore, the observation of strong hydrologic influence on arsenic behaviour indicates that release and transport of arsenic are sensitive to continuing and impending anthropogenic disturbances. In particular, groundwater pumping for irrigation, changes in agricultural practices, sediment excavation, levee construction and upstream dam installations will alter the hydraulic regime and/or arsenic source material and, by extension, influence groundwater arsenic concentrations and the future of this health problem.


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