Effect of Soil and Water Conservation Measures on Ground Water Fluctuations and Recharge on Mutukula Watershed, Prakasam District

G. Rakesh
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Abstract

A watershed is commonly defined as an area, in which all water drains to a common point. From a hydrological perspective, a watershed is a useful unit of operation and analysis because; it facilitates a systems approach to land and water use, in interconnected upstream and downstream areas. Watershed projects aim to maximize the quantity of water available for crops, livestock and human consumption, through on-site soil and moisture conservation, infiltration into aquifers, and safe runoff into surface ponds. Hence, the present study conducted on experimental investigations on ground water fluctuations and recharge carried out using the water level indicator, empirical equations like proposed empirical relationship, Chaturvedi formula and Chaturvedi formula. The rainfall recharge was found to be less than 5 inches. On the other hand, average rainfall recharge computed from all three equations like proposed empirical relationship (1.43), Chaturvedi formula (0.92) and Modified Chaturvedi formula (1.94) inches. Where, it was found, in Modified Chaturvedi formula and empirical relationship being quite high. Therefore, Chaturvedi formula equation can conveniently be used for better and quick assessment of natural ground water recharge, in Mutukula watershed area.
Prakasam地区Mutukula流域水土保持措施对地下水波动和补给的影响
分水岭通常被定义为一个区域,所有的水都流向一个共同的点。从水文的角度来看,流域是一个有用的操作和分析单位,因为;它促进了在相互关联的上游和下游地区采用系统方法来利用土地和水。流域项目旨在通过现场土壤和水分保持、渗透到含水层以及安全径流进入地表池塘,最大限度地提高作物、牲畜和人类消费的水量。因此,本研究采用水位指标、提出的经验关系式、Chaturvedi公式、Chaturvedi公式等经验方程对地下水涨跌补给量进行了实验研究。雨量补给不足5英寸。另一方面,平均降雨量补给由三个方程计算,即建议的经验关系(1.43),Chaturvedi公式(0.92)和修正的Chaturvedi公式(1.94)英寸。其中,我们发现,在修正Chaturvedi公式中与经验关系相当高。因此,利用Chaturvedi公式方程可以方便地更好、快速地评价Mutukula流域地下水自然补给。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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