Tens of thousands of people, located primarily on the Bengal Delta of southern and eastern Bangladesh, have been stricken with arsenical dermatitis, hyperkeratosis, and chronic and acute cases of arsenicosis, and other related diseases and maladies as a result of drinking arsenic-laden groundwater.
The groundwater extracted from over 10 million tube wells that have been installed in the shallow, unconfined aquifer system that exists throughout Bangladesh. The World Health Organization estimates that 40-60 million people are at risk from drinking arsenic-contaminated water in Bangladesh, and that this health risk also extends into West Bengal, India and into southern Nepal.
Most of the highly arsenic-contaminated wells in the delta are completed in the "shallow aquifer", which commonly lies at a depth of 50-150 feet below the surface. Due to the complex sedimentologic nature of the delta, it is difficult to predict whether or not the zone of high arsenic is hydrologically separate from the deeper aquifer system. The deeper aquifer systems within the delta have been shown to contain nearly arsenic-free water, and thus they are a largely untapped source of potential drinking water for people in Bangladesh. The deeper aquifer systems are probably the most valuable unused natural resource in the country, yet a detailed understanding of the groundwater quality and quantity in these systems does not yet exist. Before this valuable resource can be exploited, it is essential to understand whether or not the deeper aquifer systems will remain arsenic free if developed over time.
During January 2002, the Government of Bangladesh (GOB) sponsored an International Workshop, which resulted in recommendations for providing alternative sources of safe water. Possible sources of safe water include rainwater, surface water, and deep groundwater in addition to new or revamped water-treatment and water-distribution systems. The current project addresses the recommendations for using additional water wells, completed in both shallow and deep aquifers, as sources of safe water. The United States Geological Survey has been asked by USAID and US State Department, Dhaka to assist the government in Bangladesh in developing a strategy to better understand the ground-water arsenic situation and in particular to study possible alternative sources of clean water.
The USGS is currently conducting research on the deeper aquifer system in Bangladesh in areas associated with high levels of arsenic in the shallow groundwater. The work uses an integrated geologic, hydrologic, microbiologic, and geochemical approach to characterize the deep aquifer system and to develop mappable criteria that will identify sources of safe groundwater. This work is an integral step in the characterization of the hydrogeological framework needed to define the potential for developing safe and sustainable groundwater sources. The important questions to address are, "To what extent can the deep aquifer system of the delta be reliably used to provide an alternative drinking-water source for the Nation?"; "How much good-quality water can be produced from this resource?"; and, "How long will it last?".
The answers to these questions are scientifically challenging, yet these answers are needed to justify the costs of developing this resource and to ensure that this resource is not knowingly, or unknowingly, contaminated. There are three general components to the current project, namely: (1) evaluation of the hydrology, geochemistry, microbiology, and geology of the deep aquifer at selected sites; (2) coordination of ongoing and planned work among several GOB agencies; and (3) capacity building. The USGS is working with many GOB agencies, other Donor Nations, International agencies and other interested parties to help better define the problem of developing an integrated system of groundwater utilization and to develop methodologies to better understand the complexity of the natural hydrogeologic system.
Activities include:
- Test drilling, and aquifer testing in cooperation with the Bangladesh Water Development Board (BWDB)
- Core drilling and resistivity studies in cooperation with the Geological Survey of Bangladesh (GSB)
- Geophysical logging conducted in cooperation with Dhaka University Geology Department, and Columbia University
- Water sampling and analysis in cooperation with the Bangladesh Atomic Energy Commission (BAEC)
- XANES Analysis of sediments (micro-beam element/mineral analyses) with cooperation of Stanford University Synchrotron Radiation Laboratory (SSRL)
- Geochemical analysis of Borehole Sediments, including Optically Stimulated Luminescence Dating in cooperation with Dr. Steve Forman, University of Illinois at Chicago
Partners:
Geological Survey of Bangladesh
Bangladesh Water Development Board
Bangladesh Atomic Energy Commission
Dhaka University Geology Department
Bangladesh Arsenic Mitigation and Water Supply Program
U.S. Department of State
U.S. Agency for International Development
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Vulnerability of deep groundwater in the Bengal Aquifer System to contamination by arsenic
Shallow groundwater, the primary water source in the Bengal Basin, contains up to 100 times the World Health Organization (WHO) drinking-water guideline of 10g l 1 arsenic (As), threatening the health of 70 million people. Groundwater from a depth greater than 150m, which almost uniformly meets the WHO guideline, has become the preferred alternative source. The vulnerability of deep wells to contaAuthorsW.G. Burgess, M.A. Hoque, H.A. Michael, C.I. Voss, G. N. Breit, K.M. AhmedControls on groundwater flow in the Bengal Basin of India and Bangladesh: Regional modeling analysis
Groundwater for domestic and irrigation purposes is produced primarily from shallow parts of the Bengal Basin aquifer system (India and Bangladesh), which contains high concentrations of dissolved arsenic (exceeding worldwide drinking water standards), though deeper groundwater is generally low in arsenic. An essential first step for determining sustainable management of the deep groundwater resouAuthorsH.A. Michael, C.I. VossEstimation of regional-scale groundwater flow properties in the Bengal Basin of India and Bangladesh
Quantitative evaluation of management strategies for long-term supply of safe groundwater for drinking from the Bengal Basin aquifer (India and Bangladesh) requires estimation of the large-scale hydrogeologic properties that control flow. The Basin consists of a stratified, heterogeneous sequence of sediments with aquitards that may separate aquifers locally, but evidence does not support existencAuthorsH.A. Michael, C.I. VossEvaluation of the sustainability of deep groundwater as an arsenic-safe resource in the Bengal Basin
Tens of millions of people in the Bengal Basin region of Bangladesh and India drink groundwater containing unsafe concentrations of arsenic. This high-arsenic groundwater is produced from shallow (<100 m) depths by domestic and irrigation wells in the Bengal Basin aquifer system. The government of Bangladesh has begun to install wells to depths of >150 m where groundwater arsenic concentrations arAuthorsHolly A. Michaela, Clifford I. VossCompositional Data for Bengal Delta Sediment Collected from a Borehole at Rajoir, Bangladesh
Processes active within sediment of the Bengal basin have attracted world concern because of the locally high content of arsenic dissolved in ground water drawn from that sediment. Sediment samples were collected from a borehole in the town of Rajoir, Rajoir upazila, Madaripur district, Bangladesh, to investigate the processes contributing to arsenic contamination. The samples were mineralogicallyAuthorsGeorge N. Breit, James C. Yount, Md. Nehal Uddin, Ad. Atual Muneem, Heather Lowers, Cyrus J. Berry, John W. Whitney