Hydrochemical Characteristics and Indication to Geothermal Genesis of Low-Medium-Temperature Convection Geothermal Field in Yanshan Orogenic Basin, China

doi:10.3390/w16030433

IOCAS-IR

	Hydrochemical Characteristics and Indication to Geothermal Genesis of Low-Medium-Temperature Convection Geothermal Field in Yanshan Orogenic Basin, China
	Yuan, Wenzhen 1,2; Xing, Yifei 1,2; Wei, Meihua 3,4; Guo, Xinran 5; Liu, Jin 6; Gao, Jun 1; Zhang, Changsheng 3,4; Zhai, Yuanzheng 7
	2024-02-01
发表期刊	WATER
卷号	16 期号:3 页码:17
通讯作者	Xing, Yifei(xingyifei@cags.ac.cn)
摘要	The central part of the Zhangjiakou area is occupied by the Yanshan orogenic basin. A large number of piedmont faults developed over time, controlling the exposure of geothermal anomalies. The fluid chemistry characteristics and their influence on the heat generation mechanism of the medium- and low-temperature convective geothermal field in the area are not fully understood. In this study, the geothermal fluid was sampled and tested, and the hydrogeological background conditions were analyzed. The results show that the sulfate in geothermal fluid originates from the dissolution of gypsum or H2S oxidation in deep magma. The geothermal fluid in the faulted basin flows upward after deep circulation and interacts with shallow groundwater. The main source of geothermal fluid is atmospheric precipitation. The temperature of the hot reservoir is between 82 degrees C and 121 degrees C, and the depth of geothermal water circulation is more than 3200 m. It can be seen that the geothermal resources in this area are formed by the long-term contact of residual magma, geothermal heating and mechanical heating of neotectonic movement after atmospheric precipitation recharge.
关键词	geothermal fluid hydrogeochemical genesis mechanism convection Yanshan orogenic basin
DOI	10.3390/w16030433
收录类别	SCI
语种	英语
资助项目	National Natural Science Foundation of China
WOS研究方向	Environmental Sciences & Ecology ; Water Resources
WOS类目	Environmental Sciences ; Water Resources
WOS记录号	WOS:001160180700001
出版者	MDPI
WOS关键词	GROUNDWATERS ; CO2 ; HYDROGEOCHEMISTRY ; GEOCHEMISTRY ; XIONGAN ; WATERS ; SYSTEM ; AREA
引用统计
文献类型	期刊论文
条目标识符	http://ir.qdio.ac.cn/handle/337002/184457
专题	中国科学院海洋研究所
通讯作者	Xing, Yifei
作者单位	1.Chinese Acad Geol Sci, Beijing 100037, Peoples R China 2.Minist Nat Resources Peoples Republ China, Key Lab Shallow Geothermal Energy, Beijing 100195, Peoples R China 3.Shanxi Geol Engn Explorat Inst Co Ltd, Taiyuan 030024, Peoples R China 4.Shanxi Key Lab Explorat & Exploitat Geothermal Res, Taiyuan 030024, Peoples R China 5.Chongqing Univ Sci & Technol, Coll Oil & Gas Engn, Chongqing 401331, Peoples R China 6.Chinese Acad Sci, Inst Oceanol, Qingdao 266071, Peoples R China 7.Beijing Normal Univ, Coll Water Sci, Beijing 100875, Peoples R China
推荐引用方式 GB/T 7714	Yuan, Wenzhen,Xing, Yifei,Wei, Meihua,et al. Hydrochemical Characteristics and Indication to Geothermal Genesis of Low-Medium-Temperature Convection Geothermal Field in Yanshan Orogenic Basin, China[J]. WATER,2024,16(3):17.
APA	Yuan, Wenzhen.,Xing, Yifei.,Wei, Meihua.,Guo, Xinran.,Liu, Jin.,...&Zhai, Yuanzheng.(2024).Hydrochemical Characteristics and Indication to Geothermal Genesis of Low-Medium-Temperature Convection Geothermal Field in Yanshan Orogenic Basin, China.WATER,16(3),17.
MLA	Yuan, Wenzhen,et al."Hydrochemical Characteristics and Indication to Geothermal Genesis of Low-Medium-Temperature Convection Geothermal Field in Yanshan Orogenic Basin, China".WATER 16.3(2024):17.