To combat the present arsenic crisis, we badly need the following:
According to WHO, the possibility of getting skin lesions exists among those drinking 1.0 mg of arsenic per day for several years. And our analytical report on water (about 10000) jointly with Dhaka Community Hospital indicates that a large sum of population is consuming above 1.0 mg of arsenic per day. Our thousands of hair and nail analyses from the affected villages indicate that 70-80 % of population has higher arsenic body burden. Thus many may not be showing arsenical skin lesions but may be sub-clinically affected. Further, if it is true that arsenic toxicity appears after several years of exposure, then the picture may actually be for more grim than it appears at present, and children our future generations are at a greater risk.
The mistake that we made in the past and are persisting with it even today is the merciless exploitation of groundwater for irrigation without ever trying to adopt effective watershed management to harness our huge surface water resources and rain water. In Bangladesh, we have large area of wetlands, a huge area of flooded river basins, innumerable ox-bow lakes and big lagoons. Proper watershed management and the use of these water bodies for pisiculture, duck-breeding, and growing vegetables on their banks with people's participation could actually help the villagers become more prosperous. Instead of taking this course, we are digging more and more tubewells knowing fully well (from West Bengal experience) that in the long run these tube-wells run the risk of contamination.
Even for irrigation, we are digging deep tubewells when we are unable
to get water from the shallow tubewells during summer. Recently, a veteran
geologist has in an article captioned against such reckless use of groundwater
and has cited its disastrous consequences. It must be realised that water
held in deep aquifers takes decades, even centuries, to accumulate, and
recent rainfall does not replenish this resource. Recent isotope studies
carried out in Rajasthan, India have indicated that such water can be 6000
to 10,000 years old.