In the lowlands of Nepal, as well as in several other
South Asian
countries, the level of arsenic in groundwater extracted from Quaternary
alluvial sediments frequently exceeds the World Health Organization
(WHO) drinking water guideline of 10 μg/L. The widely accepted
explanation refers to the reductive dissolution of Fe-bearing minerals
releasing As-oxyanions from the soil minerals. However, this hypothesis
is only to some extent applicable. Given that arsenic and iron in
the groundwater are weakly correlated or decoupled and iron(III) (hydr)oxides
are scarcely present, a substantial portion of As and Fe has to be
retained in clay minerals. The low concentration of iron in groundwater
can be explained by the origin of As and Fe in the rocks (leucogranites);
in the High Himalayas, they are low in Fe but considerably enriched
in Li, B, As, Se, Br, Sr, Mo, Cd, P, and U. This unique geochemical
setting has a major impact on the performance of the Kanchan Arsenic
Filters (KAFs) used to eliminate As from groundwater in Nepal. Lack
of sufficient Fe in groundwater, combined with limited release of
iron by corrosion of iron nails, call for an adapted version of these
filters. The first results from 20 modified filters show a clear increase
in As removal efficiency, achieved mainly by the replacement of old
nails, an added upper sand layer over the nails, and elongation of
the outlet tube to avoid wet–dry cycles and to keep the nail
bed immersed. Proper instructions to the users on the operation and
maintenance of filters, by replacing the reactive materials (iron
nails) and the lower sand bed regularly, are imperative.