东古楼抽水试验对地下流体动态影响研究  

Study on the Influence of Donggulou Test of Water Pumping on Underground Fluid Regimen

作　　者：高立新[1] 车用太[2] 纪建国[1] 阎海滨[1] 刘成龙[2] 王翠萍 王海义 

机构地区：[1]内蒙古自治区地震局,呼和浩特010051 [2]中国地震局地质研究所,北京100029 [3]内蒙古自治区呼和浩特市地震局,呼和浩特010020

出　　处：《地震研究》2005年第2期172-177,共6页Journal of Seismological Research

基　　金：地震科学联合基金资助;项目编号.

摘　　要：为了研究抽水对水位、水温(地热)、气氡、气汞、水氡与水汞的影响,在内蒙古呼和浩特市东南的东古楼村进行了相关试验观测。结果表明,抽水对井水位的影响最大,影响距离可达680m;对水温影响也较为明显;对气氡与气汞动态的影响不明显;对水氡与水汞动态可能有一定影响,但影响幅度很小。In order to study the effect of water pumping on some subsurface fluid parameters such as well water level, water temperature (terrestrial heat), radon in air, mercury in air, radon in water and mercury in water, a test was done at the Donggulou village, southeast of Hohhot City, Inner Mongolia. The result shows that the influence of water pumping on well water level is biggest, far to a distance 680m, then the water temperature. It has not obvious influence on the radon and mercury in air, but maybe has some small influence on radon and mercury in water.

关 键 词：抽水影响 试验研究 地下流体 呼和浩特 

分 类 号：P315.72[天文地球—地震学]