抽水对地下水位、汞、氡的影响——以古城试验为例  

Effect of Pumping Water on Observation of Water Level,Hg and Rn According to Gucheng Test

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

机构地区：[1]内蒙古自治区地震局,内蒙古呼和浩特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,内蒙古呼和浩特010020 [4]内蒙古自治区赤峰市地震局,内蒙古赤峰024000

出　　处：《西北地震学报》2006年第2期144-148,共5页Northwestern Seismological Journal

基　　金：地震科学联合基金资助

摘　　要：介绍了在内蒙古古城进行的同层抽水对水位、水温(地热)、气氡、气汞、水氡与水汞影响的观测试验及其结果。结果表明,抽水对井水位影响最大,影响距离可达近1 km;对水温影响较为明显;对气氡、气汞的影响不明显;水氡与水汞的动态可能有一定影响,但影响幅度不大。The test for the influence of the same layer pumping water to observation of water level , water temperature, escaping radon, escaping Hg, water radon, and water Hg in Gucheng village, Inner Mongolia Autonomous Region, is introduced. The test result shows that the main influence is on the underground water level, the influ evidence. The influence on Hg are not important. ence distance is about 1 km. The influence on water temperature is relatively escaping radon and Hg are not evidence. The influence on water radon and

关 键 词：抽水 地下流体 试验 古城 

分 类 号：P332[天文地球—水文科学] P641.3[水利工程—水文学及水资源]