Poisoned waters
A highly disturbing state of affairs is revealed in a commentary in
Science for 21 June from D. Kirk Nordstrom of the Water Resources
Division of the US Geological Survey in Colorado. He points out that,
with a world population exceeding six million, a fundamental resource
for human survival, water, is shrinking. An estimate from the World Health
Organization indicates that 43 per cent of the population lack adequate
sanitation, while 22 per cent have no clean drinking water.
The failure of surface water supplies has led to increased dependence
upon ground water in many parts of the world. In India and Bangladesh
this move has resulted in 36 million people having to consume water dangerously
contaminated with arsenic. In many other places, too, notably Taiwan,
the threat is known to exist.
Arsenic is not abundant throughout the earth's continental crust. It
is usually concentrated in sulphide-bearing mineral deposits, especially
pyrite, and in deposits of hydrated iron oxides. The degree to which arsenic
is solubilised so as to enter ground waters depends on pH, redox conditions
and temperature. High arsenic concentrations occur in many geothermal
waters, and concentrations exceeding the now accepted drinking water standard
of not more than 10mcg per litre are not uncommon.
Significant contributors to arsenic in water supplies are organic-rich
or black shales, alluvial sediments of Holocene date with slow flushing
rates, mineralised and mined areas (particularly gold deposits), volcanic
strata and thermal springs. The distribution is not simple. Waters with
high levels of arsenic include the thermal sources of Kamchatka, New Zealand,
Japan, Alaska, California and Wyoming, where black shales abound, whereas
the waters of Hawaii and Iceland are low in the element. Arsenic concentrations
may change over periods of a few years, which makes dealing with them
difficult.
In another article in the same journal, public health scientists from
the University of California discuss the possible effects of drinking
water of high arsenic content. Arsenic was one of the first chemicals
associated with cancer — high rates of lung cancer in miners in Saxony
being noted in 1879. Then skin cancers were encountered in patients treated
with arsenical medicines. It was much later, in the 1930s, that skin cancers
were linked to drinking water containing arsenic in Argentina and other
places. More evidence from Argentina in the 1960s associated drinking
water with internal cancers, particularly of the lung and urinary tract.
Failure to deal with the situation promptly may have been due to the
fact that most drinking water standards were set on the basis of animal
studies, and that other factors such as smoking complicated the picture.
Moreover, progress may have been impeded by discussion over the existence
of a threshold for arsenic exposure, below which it would not have any
toxic effect. "Prudent public health decisions should not wait until there
is proof of serious cancer risks at low exposure" remark the commentators.
Back to Top
|