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- W2363706953 abstract "Fuzhou geothermal field is a low-medium temperature geothermal system of convective type and its geothermal reservoir is the intrusive rocks of Late Yanshanian stage.The sample analysis of different types of groundwater in Fuzhou Basin indicates that it contains different amount of trace elements.It is shown that the trace elements content is related to the lithology of aquifer,and also to the temperature of groundwater.The content of trace elements in Quaternary pore water is higher than that in bedrock fracture water except for some trace elements,while some elements,such as Ga,Rb,Sb,Se,Sr and Tl,are increasing with the temperature in groundwater.In Quaternary geothermal water,formed by the mixing of bedrock geothermal water and Quaternary pore water,the contents of As,Cd,Cu,Mo,Pb,Sb,Se and Sr are increased remarkably.This implies that these elements have been dissolved during mixing process.Clustering analysis,among the contents of trace elements in geothermal water and in intrusive rocks formed different period around the Fuzhou Basin,shows that the geochemistry environment of geothermal water is main related to Fuzhou intrusive rock,Kuiqi intrusive rock and Wenbishan intrusive rock,and the trace elements in geothermal water are originated from the interactions between the geothermal water and the intrusive rocks." @default.
- W2363706953 created "2016-06-24" @default.
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- W2363706953 date "2008-01-01" @default.
- W2363706953 modified "2023-09-25" @default.
- W2363706953 title "Characteristics of Trace Elements of Geothermal Water in Fuzhou Basin" @default.
- W2363706953 hasPublicationYear "2008" @default.
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