ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
北京小汤山地区第四系高氟地下水与地热水关系研究
  
关键词:urban geology  high-fluoride groundwater  geothermal water  geothermal reservoir
基金项目:北京市自然科学基金项目(编号: 8181002)
作者单位E-mail
刘宗明 北京市地质矿产勘查院
自然资源部浅层地热能重点实验室 
472584949@qq.com 
孙少游 北京市市政工程设计研究总院有限公司 418171619@qq.com 
马静晨 自然资源部浅层地热能重点实验室
北京市工程地质研究所 
 
郭帅 北京市工程地质研究所  
李翔 北京市地质矿产勘查院
自然资源部浅层地热能重点实验室 
 
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摘要:
Study on the Relationship between Quaternary High-fluorine Groundwater and Geothermal Water in Xiaotangshan Area, Beijing
      The fluorine content of deep groundwater generally exceeds the standard in Xiaotangshan area of Beijing, which seriously restricts the regional water supply. Based on the collection of basic geological, hydrogeological, and geothermal geological data, the relationship between quaternary high-fluorine groundwater and geothermal water was studied. The study showed that Xiaotangshan area is in the nuclear part of the anticline. In this area, the geothermal reservoir is in contact with the quaternary strata. Under the influence of tectonic stress, a large number of tensile fractures have developed in the geothermal reservoir. Moreover, as quaternary strata are loose and thin, this area has become a geothermal enrichment zone. Under high temperature and pressure, the fluoride content of geothermal water is generally high. Because of the mixing of geothermal water and quaternary deep groundwater, the fluoride content of quaternary deep groundwater increases and high-fluoride groundwater is formed.
LIU Zongming,SUN Shaoyou,MA Jingchen,GUO Shuai,LI Xiang.2024.Study on the Relationship between Quaternary High-fluorine Groundwater and Geothermal Water in Xiaotangshan Area, Beijing[J].Acta Geoscientica Sinica,45(1):63-72.
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