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Simulation of effects of agricultural activities on groundwater level by combining FEFLOW and GIS

机译:结合FEFLOW和GIS模拟农业活动对地下水位的影响。

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Abstract Effects of agricultural activities are obvious in arid‐inland regions. A numerical model for two‐dimensional phreatic groundwater flow was developed based on the water budget in the Minqin oasis, a typical arid‐inland region. The spatial data of source/sink terms were processed by combining global information system (GIS) and the finite element subsurface flow (FEFLOW) model. The verified results showed errors for the model of 0.37 and 0.48 m respectively in the Quanba and Huqu areas. The groundwater level changes were simulated with the developed model. The results indicate that groundwater level maintained a decreasing trend of 1.8 and 1.1m year‐1 respectively in the Quanba and Huqu areas under current water resource utilisation. Therefore, further study is needed to determine the rational exploitation volume of groundwater and distribution schemes for surface water.
机译:摘要农业活动的影响在干旱内陆地区很明显。基于典型的干旱内陆地区民勤绿洲的水量预算,建立了二维潜水地下水流的数值模型。通过结合全球信息系统(GIS)和有限元地下流(FEFLOW)模型来处理源/汇项的空间数据。验证结果表明,该模型在泉坝和壶曲地区的误差分别为0.37和0.48 m。用开发的模型模拟了地下水位的变化。结果表明,在当前水资源利用下,广坝和壶曲地区地下水位在1年中分别保持了1.8和110万的下降趋势。因此,需要进一步研究确定地下水的合理开采量和地表水分配方案。

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