Web Release Date: February 14,
Arsenic and Manganese Contamination of Drinking Water Resources in Cambodia: Coincidence of Risk Areas with Low Relief Topography
and

Swiss Federal Institute of Aquatic Science and Technology, Eawag, CH-8600 Dübendorf, Switzerland, and Resource Development International-Cambodia, RDIC, P.O. Box 494, Phnom Penh, Cambodia
Received for review August 28, 2006
Revised manuscript received January 10, 2007
Accepted January 11, 2007
Abstract:
Arsenic contamination of groundwater has been identified
in Cambodia, where some 100,000 family-based wells
are used for drinking water needs. We conducted
a comprehensive groundwater survey in the Mekong
River floodplain, comprising an area of 3700 km2 (131
samples, 30 parameters). Seasonal fluctuations were also
studied. Arsenic ranged from 1 to 1340
g L-1 (average
163
g L-1), with 48% exceeding 10
g L-1. Elevated
manganese levels (57% >0.4 mg L-1) are posing an additional
health threat to the 1.2 million people living in this area.
With 350 people km-2 potentially exposed to chronic arsenic
poisoning, the magnitude is similar to that of Bangladesh
(200 km-2). Elevated arsenic levels are sharply restricted to
the Bassac and Mekong River banks and the alluvium
braided by these rivers (Kandal Province). Arsenic in this
province averaged 233
g L-1 (median 100
g L-1),
while concentrations to the west and east of the rivers
were <10
g L-1. Arsenic release from Holocene sediments
between the rivers is most likely caused by reductive
dissolution of metal oxides. Regions exhibiting low and
elevated arsenic levels are co-incident with the present
low relief topography featuring gently increasing elevation
to the west and east of a shallow valley-understood as
a relict of pre-Holocene topography. The full georeferenced
database of groundwater analysis is provided as Supporting
Information.
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