CAJ | 학술논문

根据山西省水资源短缺、地下水超采严重的现状，分析了影响地下水变化的因素，采用2006-2010年5个盆地222个测井地下水埋深（水位）资料，复核2004年山西省第二次地下水资源调查评价之后的地下水变化，重点分析了地下水埋深变化、发生水位下降的区域及对局部地下水流向的改变。结果表明：2006-2010年山西省盆地内地下水位总体呈下降趋势，埋深增大，超采区局部有所缓解；各盆地地下水埋深季节性差异明显，不具有一致性；大同、临汾、长治盆地分别有85％、71％、90％的测井地下水埋深增加，太原盆地地下水埋深存在剧烈变化的测点；盆地地下水流向没有发生根本性改变。
근거산서성수자원단결、지하수초채엄중적현상，분석료영향지하수변화적인소，채용2006-2010년5개분지222개측정지하수매심（수위）자료，복핵2004년산서성제이차지하수자원조사평개지후적지하수변화，중점분석료지하수매심변화、발생수위하강적구역급대국부지하수류향적개변。결과표명：2006-2010년산서성분지내지하수위총체정하강추세，매심증대，초채구국부유소완해；각분지지하수매심계절성차이명현，불구유일치성；대동、림분、장치분지분별유85％、71％、90％적측정지하수매심증가，태원분지지하수매심존재극렬변화적측점；분지지하수류향몰유발생근본성개변。
Based on the current status of water shortafe and the serious over exploitation of froundwater in Shanxi Province,this paper analyzed the factors that influencinf froundwater chanfes. Adoptinf the data of froundwater depth/level of 222 observed wells which distributed in 5 basins from 2006 to 2010,this paper checked the froundwater variation after the second evaluation of froundwater resources of Shanxi Province,especially the chanfes of froundwater depth,the location of froundwater level decrease and the chanfes of flow direction. The results show that the froundwater level is declined and the buried depth is increased overall from 2006 to 2010 in the basins,while a few of overdraft areas are improved;the seasonal froundwater depths are freat different and are not consistent in different basins;there are 85%,71% and 90% of monitorinf wells where froundw-ater buried depth increases in Datonf,Linfen and Chanfzhi basins respectively,while there exists drastic chanfes of froundwater buried depth in Taiyuan basin;the froundwater flow has not been chanfed thoroufhly in the basins.