Arsenic Mobility and Groundwater Extraction in Bangladesh

Author:

Harvey Charles F.1,Swartz Christopher H.1,Badruzzaman A. B. M.2,Keon-Blute Nicole1,Yu Winston1,Ali M. Ashraf2,Jay Jenny1,Beckie Roger3,Niedan Volker1,Brabander Daniel1,Oates Peter M.1,Ashfaque Khandaker N.1,Islam Shafiqul4,Hemond Harold F.1,Ahmed M. Feroze2

Affiliation:

1. Ralph M. Parsons Laboratory, Department of Civil & Environmental Engineering, Massachusetts Institute of Technology, Cambridge, MA 01239, USA.

2. Bangladesh University of Engineering and Technology, Dhaka 1000, Bangladesh.

3. Department of Earth and Ocean Sciences, University of British Columbia, BC V6T 1Z1, Canada.

4. Department of Civil and Environmental Engineering, University of Cincinnati, Cincinnati, OH 45221, USA.

Abstract

High levels of arsenic in well water are causing widespread poisoning in Bangladesh. In a typical aquifer in southern Bangladesh, chemical data imply that arsenic mobilization is associated with recent inflow of carbon. High concentrations of radiocarbon-young methane indicate that young carbon has driven recent biogeochemical processes, and irrigation pumping is sufficient to have drawn water to the depth where dissolved arsenic is at a maximum. The results of field injection of molasses, nitrate, and low-arsenic water show that organic carbon or its degradation products may quickly mobilize arsenic, oxidants may lower arsenic concentrations, and sorption of arsenic is limited by saturation of aquifer materials.

Publisher

American Association for the Advancement of Science (AAAS)

Subject

Multidisciplinary

Reference21 articles.

1. D. G. Kinniburgh P. L. Smedley Eds. Arsenic Contamination of Groundwater in Bangladesh (British Geologic Survey Report WC/00/19 2001) (www.bgs.ac.uk/arsenic/Bangladesh).

2. Smith A. H., Lingas E. O., Rahman M., Bull. WHO 78, 1093 (2000).

3. Harvey C. F., Environ. Sci. 8, 491 (2001).

4. Arsenic poisoning of Bangladesh groundwater

5. A review of the source, behaviour and distribution of arsenic in natural waters

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