Investigating the changing pattern of groundwater levels and rainfall in the peninsular region of Bhagalpur and Khagaria, Bihar

Water Supply Pub Date : 2024-01-25 DOI:10.2166/ws.2024.010
Abhishek Kumar Choudhary, Vivekanand Singh
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Abstract

Groundwater is the primary source of water for domestic and irrigation purposes in the peninsular region of the Bhagalpur and Khagaria districts of Bihar. Though this region is bounded by perennial rivers on three sides, the groundwater level is decreasing day by day because of over exploitation and misuse. In this study, spatial and temporal analyses of rainfall and groundwater levels for pre- and post-monsoon seasons from 1996 to 2020 have been carried out using GIS tools, graphical plots, and statistical methods of pattern recognition. The spatial analysis of rainfall shows less rainfall in the western region of the study area, whereas it shows heavy rainfall in the region near the Vikramshila Bridge. The temporal analysis of rainfall shows decreasing trend in the whole study area and the rate of decrease was 25.05 mm/year during 1996–2020. The results of the pre-monsoon groundwater levels analysis show decreasing trend in the majority of wells, and the rate of decrease varies from 0.005 to 0.102 m/year. By contrast, the post-monsoon groundwater levels showed an increasing trend varying from 0.005 to 0.083 m/year at wells located near the river Ganga, except at Maheshkhunt. Thus, there is a need for proper groundwater management for a sustainable future.
调查比哈尔邦 Bhagalpur 和 Khagaria 半岛地区地下水位和降雨量的变化规律
地下水是比哈尔邦巴加尔布尔和卡加里亚地区半岛地区生活和灌溉用水的主要来源。虽然该地区三面环水,但由于过度开采和滥用,地下水位日益下降。本研究使用地理信息系统(GIS)工具、图表和模式识别统计方法,对 1996 年至 2020 年季风前后的降雨量和地下水位进行了时空分析。降雨量的空间分析表明,研究区西部地区降雨量较少,而维克拉姆希拉大桥附近地区降雨量较大。降雨量的时间分析表明,整个研究区域的降雨量呈下降趋势,1996-2020 年期间的降雨量降幅为 25.05 毫米/年。季风前地下水位分析结果显示,大部分水井的地下水位呈下降趋势,下降率在 0.005 至 0.102 米/年之间。相比之下,除 Maheshkhunt 外,位于甘加河附近的水井的季风后地下水位呈上升趋势,上升幅度在 0.005 至 0.083 米/年之间。因此,为了未来的可持续发展,有必要对地下水进行适当管理。
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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