Environmental Isotope Hydrogeochemical Characteristics and Instructions of Geothermal Water in Xianyang Urban Area

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Abstract:

In order to find out the origin of geothermal water in Xianyang urban area and provide scientific basis for sustainable use, taking the geothermal water as study object, we systematically studied supply circulation mechanism of geothermal water in Xianyang urban area through environmental isotope hydrogeochemical methods, and come to the conclusion: geothermal water in Xianyang urban area is bounded by shore fracture of Wei River, which shows totally different hydrogeochemical features. The differences suggests that the geothermal water belongs to different tectonic geology units and sedimentary environment. The distribution characteristics of environmental isotope such as δD、δ18O and 14C confirmed that geothermal water exists contact between the study area and northwest of Wei River. The supply water source of geothermal water comes from the atmospheric precipitation of Holocene in northwest direction, its updating ability is poor except partial deep fault slightly being recharged from modern atmospheric water.

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Periodical:

Advanced Materials Research (Volumes 518-523)

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4161-4164

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May 2012

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© 2012 Trans Tech Publications Ltd. All Rights Reserved

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