在印度瓦拉达河流域,地下水模型模拟由于河流相互连接的地下水位

H. Ramesh, A. Mahesha
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引用次数: 0

摘要

使用二维Gelarkin有限元模型,本研究表征了印度卡纳塔克邦半湿润地区Varada盆地的地下水流动。该模型的特征包括通过进行描述含水层系统的泵试验来获取现场数据。在大量地质、水文和地形资料的基础上,对地质几何和含水层数量进行了分析。然后将含水层属性转换为模型代码用来求解流量控制方程的输入变量。现场试验结果表明,Varada盆地以承压含水层为主。为了标定地下水数值模型,模拟了稳态下的地下水流动。研究结果表明,观测到的地下水位与模拟的地下水位有较高的相关性。此外,还对地下水位及其暂态变化趋势进行了分析。利用验证后的地下水数值模型对流域内河流连通补给影响下的地下水位进行了预测。模型结果提供了一个很好的地下水水位的可视化表示,使资源管理者和决策者清楚地了解地下水水位与拟议的互联项目相互作用的本质。结果为进一步分析未来不同情景下的实施奠定了基础。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Groundwater modeling to simulate groundwater levels due to interlinking of rivers in Varada river basin, India
Using a two-dimensional Gelarkin finite element model, the present study characterizes groundwater flow in a Varada basin, a semi humid area of Karnataka, India. The model characterization involved taking field data by conducting pump tests describing an aquifer system. Geological geometry and the number of aquifers have been analyzed based on a large amount of geological, hydrogeological and topographical data. The aquifer properties are then transformed into input variables that the model code uses to solve governing equations of flow. The results of the field experiments showed that Varada basin is predominantly confined aquifer. For calibrating the numerical groundwater model, the groundwater flow was simulated in steady state. Results of study demonstrate a moderately high correlation between the observed and simulated groundwater level. In addition, the groundwater level and trend in the transient state has also been elucidated. The validated numerical groundwater model was used to predict the groundwater levels due to impact of recharge from the interlinking of rivers in the basin. The model result provides an excellent visual representation of groundwater levels, presenting resource managers and decision makers with a clear understanding of the nature of the interaction of groundwater levels with the proposed interlinking project. Results build a base for further analysis under different future scenarios for implementation.
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