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作 者:朱鹏涛[1] 沈宁[2] 李自芮[1] 马禾青[1] ZHU Pengtao;SHEN Ning;LI Zirui;MA Heqing(Earthquake Agency of Ningxia Hui Autonomous Region,Yinchuan 750001,China;Yinchuan Reference Station,Earthquake Agency of Ningxia Hui Autonomous Region,Yinchuan 75000,China)
机构地区:[1]宁夏回族自治区地震局,银川750001 [2]宁夏回族自治区地震局银川基准台,银川750001
出 处:《华南地震》2020年第3期55-62,共8页South China Journal of Seismology
基 金:中国地震局地震科技星火计划(XH19048);宁夏自然科学基金(2020AAC03438);宁夏地震科学基金(NX201802)联合资助。
摘 要:结合西吉王民井区域水文地质条件,从气压、降雨、李马河水库等对水位的影响进行频谱分析、回归分析、降雨量对比分析。结果表明:王民井水位变化主要受气压和降雨的影响;李马河水库建成时间与水位下降趋势变缓时间一致,对王民井水位动态变化可能产生影响,且水库的建成可能使区域地下水达到一种新的动态平衡。Based on the hydrogeological conditions of the Wangmin well area in Xiji and from air pressure,rainfall,Limahe Reservoir and other factors that affect the water level,this paper conducts spectrum analysis,regression analysis and rainfall comparison analysis.The results show that the water level changes of Wangmin well are mainly affected by air pressure and rainfall;the completion time of the Limahe Reservoir,which was built in the upper stream of the observation point in the second half of 2016,is consistent with the time when the water level decreased,which may affect the dynamic changes of water level of Wangmin well,and the completion of the reservoir may rebalance the regional groundwater dynamic.
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