摘要
通过对西安地区承压井和地热井水位及开采量和分层沉降量等资料分析后得出 :西安市区地面沉降和地裂缝活动是由于过量开采承压水所引起的。目前西安市深层地热水开采还没有加剧西安市区地面沉降和地裂缝活动。控制并减少承压水的开采量 。
Based on the data analyses of the water level and the quantity of pressure water well and hot water well, and the subsidence deformation in different stratum, we get that the ground subsidence and the activity of ground fissure in Xi'an area are caused by the overexploited pressure water. It shows that the geothermal exploitations doesn't intensify the surface subsidence and the activity of ground fissure. It is the best way for decreasing the ground subsidence and the activity of the ground fissure that we must control and decrease the exploitation of pressure water in Xi'an city.
出处
《水文地质工程地质》
CAS
CSCD
2002年第1期72-74,共3页
Hydrogeology & Engineering Geology
关键词
地热水
承压水
地面沉降
地裂缝
西安市
开采量
geothermal exploitation
ground subsidence
ground fissure
relationship