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Modeling impacts of climate change and human activities on groundwater resources using MODFLOW

机译:使用MODFLOW模拟气候变化和人类活动对地下水资源的影响

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This paper analyzes the impacts of climate change and human pressures on Yazd-Ardakan aquifer using the Hadley Centre Coupled Model, version 3 (HADCM(3)) circulation Model and A(2) emission scenario. Water levels in the study aquifer were simulated using three-dimensional finite-difference groundwater model (MODFLOW 2000) with GMS 8.3 as pre- and postprocessing software. Input for groundwater recharge time series under the climate change scenarios were derived using a regression equation based on the cumulative deviation from mean rainfall using MATLAB. Human pressures on the aquifer were modeled through climate change impacts on water requirements of cultivated areas. Three scenarios were simulated to represent the effects of climate change and human pressures on aquifer storage and hydraulic head. Climate change and human pressures (scenario 1) will reduce aquifer storage and result in decreasing hydraulic head by -0.56 m year(-1). Reduction in pumping water under scenario 2 (irrigation system modification) and scenario 3 (irrigation system modification and cropping patterns) will result in groundwater level fluctuation of about -0.32 and 0.08 m year(-1), respectively. Scenario 3 is capable of restoring and protecting the groundwater resources in Yazd-Ardakan aquifer. The results of this study are useful to obtain sustainable groundwater management in Yazd-Ardakan aquifer.
机译:本文使用Hadley中心耦合模型,版本3(HADCM(3))循环模型和A(2)排放情景分析了气候变化和人类压力对Yazd-Ardakan含水层的影响。使用三维有限差分地下水模型(MODFLOW 2000),以GMS 8.3作为预处理软件和后处理软件,对研究含水层中的水位进行了模拟。在气候变化情况下,地下水补给时间序列的输入是使用MATLAB基于基于平均降雨量的累积偏差的回归方程式得出的。通过气候变化对耕地需水量的影响来模拟含水层上的人为压力。模拟了三种情景,以表示气候变化和人为压力对含水层存储和水头的影响。气候变化和人为压力(方案1)将减少含水层的存储量,并导致水头下降-0.56 m year(-1)。在方案2(灌溉系统修改)和方案3(灌溉系统修改和耕作模式)下减少抽水量将分别导致地下水位波动约-0.32年和0.08 m year(-1)。方案3能够恢复和保护Yazd-Ardakan含水层中的地下水资源。这项研究的结果有助于获得亚兹德-阿达坎含水层的可持续地下水管理。

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