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利用动态监测数据分析兰州市傍河水源地河水与地下水的补给关系
引用本文:张恒堂.利用动态监测数据分析兰州市傍河水源地河水与地下水的补给关系[J].甘肃地质学报,1995,4(1):73-76.
作者姓名:张恒堂
作者单位:甘肃省地矿局环境地质研究所
摘    要:根据地下水与河水动态监测数据,利用相关系数方法,推算出黄河水对地下水补给的滞后时间、补给速度以及黄河水位与地下水位之间的最大相关系数,从而得出河水位对地下水位的影响随距离的增大而减小的结论。

关 键 词:地下水动态  相关系数  滞后时间  补给速度  补给关系

RECHARGE RELATION BETWEEN STREAM AND GROUNDWATER SOURCE AREA OF WATER BESIDE A RIVER IN LANZHOU BY THE ANALYSIS OF THE DYNAMIC MONITORING DATA
Zhang Hengtang.RECHARGE RELATION BETWEEN STREAM AND GROUNDWATER SOURCE AREA OF WATER BESIDE A RIVER IN LANZHOU BY THE ANALYSIS OF THE DYNAMIC MONITORING DATA[J].Acta Geologica Gansu,1995,4(1):73-76.
Authors:Zhang Hengtang
Institution:Zhang Hengtang(Institute of Environmental Geology, Bureau of Geology and Mineral Resources of Gansu Province Lanzhou 730020)
Abstract:On the basis of the data of the dynamic monitor of stream and groundwater and bymeans of correlation coefficient, the feeding time of lag and velocity for the Yellow River togroundwater have been calculated as well as greatest correlation coefficient between the Yel-low River and groundwater water level.hus,we could get a conclusion that the effect of ri-ver stage to groundwater level decreases with increase of distance.
Keywords:Groundwater regime Correlation coefficient Time of lag Feeding velo- city Recharge relation
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