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首页> 外文期刊>Hydrogeology journal >Groundwater conceptualization and modeling using distributed SWAT-based recharge for the semi-arid agricultural Neishaboor plain, Iran
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Groundwater conceptualization and modeling using distributed SWAT-based recharge for the semi-arid agricultural Neishaboor plain, Iran

机译:伊朗内沙博尔半干旱农业地区利用基于SWAT的分布式补给进行地下水概念化和建模

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Increased irrigation in the Neishaboor watershed, Iran, during the last few decades has caused serious groundwater depletion, making the development of comprehensive mitigation strategies and tools increasingly important. In this study, SWAT and MODFLOW were employed to integratively simulate surface-water and groundwater flows. SWAT and MODFLOW were iteratively executed to compute spatial and temporal distributions of hydrologic components. The combined SWAT-MODFLOW model was calibrated (2000-2010) and validated (2010-2012) based on streamflow, wheat yield, groundwater extraction, and groundwater-level data. This multi-criteria calibration procedure provided greater confidence for the partitioning of water between soil storage, actual evapotranspiration, and aquifer recharge. The SWAT model provided satisfactory predictions of the hydrologic budget for the watershed outlet. It also provided good predictions of irrigated wheat yield and groundwater extraction. The 10-year mean annual recharge rate estimated using the combined model varied greatly, ranging from 0 to 960 mm, with an average of 176 mm. This result showed good agreement with the independently estimated annual recharge rate from an earlier study. The combined model provides a robust tool for the sustainable planning and management of water resources for areas with stressed aquifers where interaction between groundwater and surface water cannot be easily assessed.
机译:在过去的几十年中,伊朗内沙博尔流域的灌溉增加导致严重的地下水枯竭,因此制定综合的缓解策略和工具变得越来越重要。在这项研究中,SWAT和MODFLOW被用来综合模拟地表水和地下水流。迭代执行SWAT和MODFLOW以计算水文分量的时空分布。基于流量,小麦产量,地下水提取量和地下水位数据,对组合的SWAT-MODFLOW模型进行了校准(2000-2010年)和验证(2010-2012年)。这种多标准的校准程序为土壤存储,实际蒸散和含水层补给之间的水分配提供了更大的信心。 SWAT模型为流域出口的水文预算提供了令人满意的预测。它还为灌溉小麦的产量和地下水提取提供了良好的预测。使用组合模型估算的10年平均年充电率变化很大,范围从0到960 mm,平均为176 mm。该结果表明与早期研究的独立估算的年度补给率非常吻合。组合模型为含水层压力大的地区提供了一个可靠的工具,可用于水资源的可持续规划和管理,而地下水和地表水之间的相互作用不易评估。

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