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Accepted Papers - 3.pdf - UNESCO

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and weathering also control the water bearing<br />

capacity of laterites. Numerous voids and joints/<br />

fractures present in laterites provide free flow of<br />

ground water whereas lithomargic clay acts as<br />

effective aquiclude.<br />

Perspective of the area<br />

These areas are characterized by inherently<br />

heterogeneous and low yielding formations either<br />

exposed on surface or under moderately thin cover<br />

of soil. The soil is generally fragile and prone to<br />

severe erosion from hill slopes. The soil is deep<br />

black having low permeability that can hold only a<br />

fraction of water that falls on it. The ground water<br />

recharge is mainly through fissures and joints in<br />

exposed rocky strata. Although some of the areas<br />

coincide with high rainfall (2000-3000mm), yet the<br />

high topographic gradient and massive nature of<br />

underlying formations generate a high runoff and<br />

less of ground water recharge. Thus, development<br />

of water table is not very pronounced. Water occurs<br />

only as a small under ground pool in the form of<br />

perched water table along the elevated regions.<br />

However, in moderately sloping areas, the<br />

development of water table is common, but of steep<br />

gradient. The steep gradient leads to outflow of<br />

significant quantity of ground water from higher<br />

level to lower level as effluent base flow into rivers.<br />

Thus, depletion of water level is very quick in dug<br />

wells as well as in bore wells, which results into<br />

water scarcity soon after the monsoon season. These<br />

adverse topographic and hydrogeological conditions<br />

are inconducive for ground water development.<br />

Hence, construction of dug wells and bore wells is<br />

not techno- economically viable.<br />

Measures to Tackle Water Scarcity<br />

The techniques and methods used to<br />

overcome water scarcity vary from region to region<br />

depending upon their specific problems, nature of<br />

terrain, climate, hydrogeological conditions etc.<br />

Some of the appropriate techniques in such areas<br />

are enumerated below;<br />

Rain Water Harvesting<br />

Rainwater harvesting is old concept as far as<br />

India is concerned. Our ancestors had been doing it<br />

according to the means available then. Nevertheless,<br />

slowly with the advent of tap water supply the<br />

431<br />

rainwater harvesting has lost its importance. As in<br />

areas where water scarcity has become a common<br />

feature due to inadequate availability of source<br />

water, rainwater harvesting has become most viable<br />

option. It is necessary to resort to long-term<br />

measures in harvesting the rainwater to meet the<br />

daily demand. Though the objective of water<br />

harvesting in most cases is to store water for lean<br />

part of the year it also imparts indirect benefits such<br />

as recharging drinking water wells and hand pumps.<br />

In hilly areas, where water harvesting has been<br />

practiced together with afforestation and other<br />

methods of watershed development and land<br />

improvement, desaturated aquifers have also been<br />

recharged and water is available in abundance from<br />

ground water sources. For the hilltop villages,<br />

especially those included in the list of tanker<br />

villages, the water harvesting system could be the<br />

best solution for meeting the water demand during<br />

the dry months by impounding water in reservoirs.<br />

The other alternatives, such as drilling or digging<br />

wells, are not appropriate. Various methods of water<br />

harvesting are feasible in hilly terrain are as<br />

discussed below.<br />

Roof Top Rain Water Harvesting<br />

This system is useful mainly for drinking<br />

water purposes. The system consists of three<br />

components i.e. collection of rainwater, conveyance<br />

and storage. In this system, rainwater falling on<br />

roof of houses and other buildings is collected and<br />

conveyed through a system of pipes and semicircular<br />

channels of galvanized iron or PVC and is<br />

stored in tanks suitably located on the ground or<br />

underground. The practice is in vogue at the<br />

individual household level in remote hilly areas with<br />

high rainfall and also in some areas of moderate to<br />

low rainfall. This type of tank storage is common<br />

in areas where under ground storage in aquifer is<br />

not feasible. Roof catchments have the advantage<br />

that they can be constructed directly near the users,<br />

if the roof is suitable for this purpose. The amount<br />

of harvested water depends on roof area and its<br />

nature, and rainfall regime.<br />

Masnory Storage Tank<br />

In hilly areas where rainfall is high and<br />

number of rainy days widely spread over long<br />

period, Masonry storage tank structures of various

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