作者:ZHANG Suxin,SHENG Yanrui,DING Zhihua,ZHANG Ziguang
摘要:Based on the well water level data in Majiagou Mine in Tangshan City since 2000,it is suggested that the water level rise from 2008-2014 is possibly associated with reduced infiltration caused by less precipitation,together with the effect of less groundwater exploitation. However,the water level rise from 1992-1998 cannot be interpreted properly if we extend the data source back to 1991. After comparing the data with long-term water level data of five wells with different hydro-geological units in Tangshan and Qinhuangdao, the study indicates that the long-term water level variation cannot be only attributed to the effect of less precipitation and the control of groundwater exploitation,but also with the influence of regional stress field change.With the support of regional geological and tectonic information,combined with the comprehensive analysis of CBM data obtained from the coal field,new understandings of the dynamic characteristics of annual variation are obtained.
發文機構:Hebei Earthquake Agency
關鍵詞:MajiagouWellWaterlevelVariationcharacteristicsStressfield
分類號: TD163[礦業工程—礦山地質測量]P641.4[天文地球—地質礦產勘探]