Hydrogeological framework and water balance studies in parts of Krishni-Yamuna interstream area, Western Uttar Pradesh, India

被引:23
作者
Ahmed, Izrar [1 ]
Umar, Rashid [1 ]
机构
[1] Aligarh Muslim Univ, Dept Geol, Aligarh 202002, Uttar Pradesh, India
来源
ENVIRONMENTAL GEOLOGY | 2008年 / 53卷 / 08期
关键词
hydrogeology; groundwater balance; irrigation return flows; Muzaffarnagar; India;
D O I
10.1007/s00254-007-0778-7
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
The Krishni-Yamuna interstream area is a micro-watershed in the Central Ganga Plain and a highly fertile track of Western Uttar Pradesh. The Sugarcane and wheat are the major crops of the area. Aquifers of Quaternary age form the major source of Irrigation and municipal water supplies. A detailed hydrogeological investigation was carried out in the study area with an objective to assess aquifer framework, groundwater quality and its resource potential. The hydrogeological cross section reveals occurrence of alternate layers of clay and sand. Aquifer broadly behaves as a single bodied aquifer down to the depth of 100 m bgl (metre below ground level) as the clay layers laterally pinch out. The depth to water in the area varies between 5 and 16.5 m bgl. The general groundwater flow direction is from NE to SW with few local variations. An attempt has been made to evaluate groundwater resources of the area. The water budget method focuses on the various components contributing to groundwater flow and groundwater storage changes. Changes in ground water storage can be attributed to rainfall recharge, irrigation return flow and ground water inflow to the basin minus baseflow (ground water discharge to streams or springs), evapotranspiration from ground water, pumping and ground water outflow from the basin. The recharge is obtained in the study area using Water table fluctuation and Tritium methods. The results of water balance study show that the total recharge in to the interstream region is of the order of 185.25 million m(3) and discharge from the study area is of the order of 203.24 million m(3), leaving a deficit balance of -17.99 million m(3). Therefore, the present status of groundwater development in the present study area has acquired the declining trend. Thus, the hydrogeological analysis and water balance studies shows that the groundwater development has attained a critical state in the region.
引用
收藏
页码:1723 / 1730
页数:8
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