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- W2388214318 abstract "Based on an analysis of chemical data of325 H 2SiO 3-rich groundwatersamples as well as their geochemical environments and geological settings, theauthors studied the relationship between the enrichment of H 2SiO 3 in groundwaterand the properties of the aquifer media and investigated geochemical characteristics of such groundwater. The results show that the formation of H 2SiO 3-enriched groundwater is closely related to such geochemical environmental factors as aquifer media and average SiO 2 abundance. The most favorable geological environment for the enrichment of H 2SiO 3 in groundwater is intermediate-acid intrusive rocks, followed by regional metamorphic rocks, eruptive rocks and clastic rocks. It is also revealed that the H 2SiO 3 concentration in the groundwater is related to water types and pH values. HCO 3-Ca type, HCO 3-Ca·Na type, alkaline typeand acid groundwaters are favorable to the enrichment of H 2SiO 3." @default.
- W2388214318 created "2016-06-24" @default.
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- W2388214318 date "2004-01-01" @default.
- W2388214318 modified "2023-09-23" @default.
- W2388214318 title "Geological-Geochemical Environment for the Enrichment of Trace Component H_2SiO_3 in Groundwater" @default.
- W2388214318 hasPublicationYear "2004" @default.
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