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Some Issues Related To Water Harvesting Ponds For Conservation Ground Water Recharge

机译:与集水池塘养护和地下水补给有关的一些问题

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The water harvesting ponds collect not only the surface runoff, but also have an effect over the replenishment to the deep aquifer. And when direct shafts are pierced from these ponds into the aquifers below, the aquifers too get polluted and an aquifer once polluted can never be cleaned. As a measure to combat water shortages, harvesting of rain water and runoff is practiced . This practice has certainly been successful in raising the shallow water table at many places and farmers have been able to give primary and secondary irrigation to rabi crops. Although it has been widely claimed that the ground water table has been rising due to watershed programmes at many places in India, in reality and in spite of all these programmes, the deep ground water has been declining very fast. A major factor is a drag force which is created near the pond on the ground water contained in the soil profile above the semi permeable membrane, of the deep aquifer. Specially when such pond is constructed near a natural drainage system. All the micro pores which were closed over the years get opened and the drainage of the ground water stored in the upstream profile into the pond starts. This in turn lowers the water head which forces the water to penetrate and replenish the deep aquifer. In vertisols , the lateral or horizontal hydraulic conductivity is far greater(.3cm/day) than vertical hydraulic conductivity (.05cm/day) and thus the ground water flows towards the pond at a much greater rate than earlier as the evaporation from the pond surface pulls the water from the earth profile adjacent to it.
机译:集水池不仅收集地表径流,而且还对深层含水层的补给产生影响。当直接竖井从这些池塘刺入下面的含水层时,含水层也将受到污染,一旦被污染,含水层将永远无法被清洁。作为解决缺水的一种措施,人们采取了雨水收集和径流的方式。这种做法无疑在许多地方提高了地下水位,而且农民已经能够对狂犬病作物进行一次和二次灌溉。尽管人们普遍认为,由于印度许多地方的分水岭方案,地下水位一直在上升,但实际上,尽管有所有这些方案,但深层地下水却一直在迅速下降。一个主要的因素是在深水层的半透膜上方的土壤剖面中的地下水附近的池塘附近产生的阻力。特别是当这种池塘建在自然排水系统附近时。多年来封闭的所有微孔都被打开,并且开始将上游剖面中存储的地下水排入池塘。反过来,这会降低水位,迫使水渗透并补充深层含水层。在杂散区中,横向或水平的水力传导率(.3cm /天)远大于垂直的水力传导率(.05cm /天),因此地下水流向池塘的速率比从池塘中蒸发时要早得多表面将水从与其相邻的地球剖面中拉出。

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