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首页> 外文期刊>Journal of the Geological Society of India >Groundwater resources management through flow modeling in lower part of Bhagirathi - Jalangi interfluve, Nadia, West Bengal
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Groundwater resources management through flow modeling in lower part of Bhagirathi - Jalangi interfluve, Nadia, West Bengal

机译:通过Bhagirathi-Jalangi interfluve,纳迪亚,西孟加拉邦下部的流量模拟进行地下水资源管理

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摘要

Groundwater utilization in Nadia district, West Bengal has been subjected to rapid exploitation in the wake of increasing urbanization and production of agricultural commodities. It is, therefore, necessary to evaluate the existing trend and availability of groundwater in time and space and its movement for proper planning in future. In the present study, an attempt has been made develop a groundwater management model using Visual MODFLOW software. The groundwater flow model for the study area was formulated by using input hydrogeological data and appropriate boundary conditions. The groundwater flow pattern of the study area indicates the occurrence of base flow which feed both the Rivers Bhagirathi and Jalangi throughout the year. The computed hydraulic heads were calibrated by comparing with observed groundwater level data for years 2004 to 2006 and were verified with the data of 2007. The outcome of modeling shows that this model can be used for prediction purpose in the future by updating input boundary conditions and hydrologic stresses during the preceding year. The model optimized unit draft for deep tube well as 556.5 m ~3/day and the same for shallow tube well as 41 m ~3/day keeping the existing tube well structures in running condition and maintaining the present and recent past trends of groundwater level. The model can be further improved if more spatial and temporal input parameters are available and can be incorporated into the model for more realistic characterization of groundwater flow.
机译:随着城市化和农产品生产的增加,西孟加拉邦纳迪亚地区的地下水利用受到了迅速的开发。因此,有必要评估时间和空间上地下水的现有趋势和可用性以及地下水的运动,以便将来进行适当的规划。在本研究中,已尝试使用Visual MODFLOW软件开发地下水管理模型。利用输入的水文地质数据和适当的边界条件,建立了研究区的地下水流模型。研究区域的地下水流模式表明全年都有基础水流向Bhagirathi河和Jalangi河供水。通过与2004年至2006年的观测地下水位数据进行比较,对计算得出的水头进行了校准,并与2007年的数据进行了比较。建模结果表明,通过更新输入边界条件,该模型可用于将来的预测。前一年的水文压力。对于深管井,模型优化后的吃水量为556.5 m〜3 / day,对于浅管井,模型优化后的吃水量为41 m〜3 / day,保持现有管井结构处于运行状态,并保持当前和最近的地下水位趋势。如果有更多的空间和时间输入参数可用,则可以进一步改进该模型,并且可以将其合并到模型中以更现实地表征地下水流量。

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