冀中平原深部地下热水资源可更新特征与依据——以辛集馆陶组地下热水系统为例  

Renewal Characteristics and Basis of the Geothermal Water Resources in Middle Hebei Plain: A Case Study of the Guantao Formation Underground Geothermal Water System

作　　者：张光辉[1] 李卓[2] 严明疆[1] 王茜[1] 王威[1] ZHANG Guang-hui LI Zhuo YAN Ming-jiang WANG Qian WANG Wei(Institute of Hydrogeology and Environmental Geology, Chinese Academy of Geological Sciences, Shijiazhuang, Hebei 050061 Institute of Hebei Geological Engineering ＆ Prospecting, Shijiazhuang, Hebei 050051)

机构地区：[1]中国地质科学院水文地质环境地质研究所,河北石家庄050061 [2]河北省地矿局水文工程地质勘查院,河北石家庄050051

出　　处：《地球学报》2016年第5期637-644,共8页Acta Geoscientica Sinica

基　　金：中国地质调查局地质调查项目(编号:12120115049701);国家自然科学基金项目(编号:41172214)联合资助~~

摘　　要：针对冀中平原深部地下热水资源可更新性问题,以辛集馆陶组地下热水系统为例,采用相同开采强度下地下热水位降幅异常变化的识别方法,通过2000年以来该地下热水位年际及月际降幅与开采量和上游山区年降水量之间响应变化特征研究,结果表明:(1)冀中平原辛集地区馆陶组地下热水资源具有一定的可更新能力,与上游山区年降水量变化相关,还与地下水位埋深、当年开采引起的水位降幅大小和开采疏干层位砾粗砂岩及细砂岩占比状况有关;(2)辛集地区馆陶组地下热水大规模开采,是该地下水系统获得上游区侧向流入补给的必要条件,属于开采激发型补给,更新补给的资源数量有限;(3)从2000年以来该区地下热水水位动态变化趋势来看,目前该区地下热水资源已处于超采状态,需要压采或人工回灌增大补给,否则难以可持续开发利用。To tackle the problem of the geothermal water resources updatable characteristics in the GuantaoFormation of the middle Hebei plain, the authors adopted the identification method of abnormal variation of thegeothermal water level under the same pumping intensity to study the characteristics of annual and monthlydecline of the geothermal water level in response to the pumping and annual precipitation in the upper reaches ofthe geothermal water system since 2000. Some conclusions have been reached： （1） The geothermal waterresources of Guantao Formation has a certain renewable capability, which is related to such factors as thevariation of annual precipitation in the upper area of the geothermal water system, the buried depth, the declinerange of the geothermal water level, and the ratio between the coarse sandstone and the fine sandstone in thedecline range; （2） Large-scale exploitation of the geothermal water in the Guantao Formation is a necessarycondition of being recharged from lateral inflow recharge in the upper reaches of the geothermal water system; itbelongs to the pumping induced recharge, and the number of the recharge resources is not large; （3） The trend ofthe geothermal water level since 2000 shows that the geothermal water system has been in overdraft state, andhence it is necessary to increase the supply of pressure or artificial recharge; otherwise, the sustainabledevelopment and utilization seem to be very difficult or even impossible.

关 键 词：冀中平原 地下热水 可更新性 降水量 上游区补给 

分 类 号：P314.1[天文地球—固体地球物理学] P641.8[天文地球—地球物理学]