田辉, 郭晓东, 都基众, 张梅桂. 大庆市地下水降落漏斗现状分析[J]. 地质与资源, 2011, 20(5): 339-342. DOI: 10.13686/j.cnki.dzyzy.2011.05.015
    引用本文: 田辉, 郭晓东, 都基众, 张梅桂. 大庆市地下水降落漏斗现状分析[J]. 地质与资源, 2011, 20(5): 339-342. DOI: 10.13686/j.cnki.dzyzy.2011.05.015
    TIAN Hui, GUO Xiao-dong, DU Ji-zhong, ZHANG Mei-gui. ANALYSIS ON THE DEPRESSION CONE OF GROUNDWATER IN DAQING CITY, HEILONGJIANG PROVINCE[J]. Geology and Resources, 2011, 20(5): 339-342. DOI: 10.13686/j.cnki.dzyzy.2011.05.015
    Citation: TIAN Hui, GUO Xiao-dong, DU Ji-zhong, ZHANG Mei-gui. ANALYSIS ON THE DEPRESSION CONE OF GROUNDWATER IN DAQING CITY, HEILONGJIANG PROVINCE[J]. Geology and Resources, 2011, 20(5): 339-342. DOI: 10.13686/j.cnki.dzyzy.2011.05.015

    大庆市地下水降落漏斗现状分析

    ANALYSIS ON THE DEPRESSION CONE OF GROUNDWATER IN DAQING CITY, HEILONGJIANG PROVINCE

    • 摘要: 大庆市主城区长期过量开采承压水,致使地下水水位持续下降,形成地下水降落漏斗.依据多年地下水开采量及地下水动态监测资料,分析了中心城区地下水降落漏斗的形成与发展趋势.研究表明,地下水降落漏斗的规模直接受开采量大小的控制,水位的变化与开采量的变化呈正相关.

       

      Abstract: Because of the excessive mining of confined water in a long period, the groundwater level in Daqing City has continuously declined to form the cone of depression. Based on the multi-year data of mining amount of groundwater resources and dynamic monitoring for groundwater, the formation and developing trend of the depression cone are analyzed. The result shows that the size of the depression cone is directly controlled by the mining amount of groundwater. The variation of water level is positively correlated to that of the mining amount.

       

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