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作 者:黄传霁 李春光[1,2] 景何仿[1,2] 乔桥 何金沙 HUANG Chuan-ji;LI Chun-guang;JING He-fang;QIAO Qiao;HE Jin-sha(School of Civil and Hydraulic Engineering,Ningxia University,Yinchuan 750021,China;Research Institute of Numerical Computation and Engineering Applications,North Minzu University,Yinchuan 750021,China)
机构地区:[1]宁夏大学土木与水利工程学院,宁夏银川750021 [2]北方民族大学数值计算与工程应用研究所,宁夏银川750021
出 处:《水电能源科学》2022年第1期14-17,111,共5页Water Resources and Power
基 金:国家自然科学基金项目(11761005,11861003);宁夏自治区科学技术研究重点研发计划项目(2019BEG03048)。
摘 要:为研究土地利用与降水变化对地下水位的影响,以黄河宁夏中宁段周边地区为研究区,建立地表水—地下水耦合的MIKE SHE分布式水文模型,并用观测井实测数据对模型参数进行率定和验证。结果表明,研究区地下水位随着降雨量的增加明显升高,并在9月份到达峰值1201.46 m;与基准组相比,对比组A年平均地下水位升高0.27 m,土地利用变化对水位升高影响作用占33.3%,降水则占66.7%;对比组B年平均地下水位升高0.51 m,土地利用变化对水位升高影响作用占35%,降水则占65%。In order to study the impacts of land use and precipitation changes on groundwater level,a surface water-groundwater coupling MIKE SHE distributed hydrological model was established for the surrounding area of the Zhongning Section of the Yellow River in Ningxia.The model parameters were calibrated and verified by the measured data of observation wells.The results show that the groundwater level in the study area increases obviously with the increase of rainfall,and reaches the peak value of 1201.46 m in September.Compare with the benchmark group,the annual average groundwater level of the comparison group A increases by 0.27 m,of which 33.3% is attributed to the change in land use and 66.7% to that in precipitation.The annual average groundwater level of the comparison group B increases by 0.51 m,of which 35%is attributed to the change in land use and 65% to that in precipitation.
关 键 词:MIKE SHE模型 土地利用变化 降水变化 地下水位
分 类 号:TV138[水利工程—水力学及河流动力学] P345[天文地球—水文科学]
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