Groundwater Flow in the Ganges Delta

Author:

Harvey Charles F.1234

Affiliation:

1. Ralph M. Parsons Laboratory

2. CEE, MIT, 48–321

3. Cambridge, MA 02139, USA

4. E-mail:

Publisher

American Association for the Advancement of Science (AAAS)

Subject

Multidisciplinary

Reference21 articles.

1. Large Groundwater Strontium Flux to the Oceans from the Bengal Basin and the Marine Strontium Isotope Record

2. Arsenic poisoning of Bangladesh groundwater

3. “National water plan project final report: Volume 2 Resources; chapter 10 water resources” (Ministry of Irrigation Government of Bangladesh Dhaka 1986) pp. 2 and 82.

4. British Geologic Survey Department of Public Health Engineering Government of Bangladesh Mott MacDonald Ltd. Groundwater Studies for Arsenic Contamination in Bangladesh. Phase I: Rapid Investigation Phase main report and five supplementary volumes (1999; www.bgs.ac.uk/arsenic/bphase1/b_intro.htm).

5. Darcy's law for fresh groundwater outflow Q at the coast is Q = WBKi where W is the coast length (500 km) B is an upper limit on the aquifer thickness (200 m) K is an upper limit for hydraulic conductivity (10 −3 m/s) and i is the gradient.

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