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南阳城区地下热水同位素特征及其水文地质意义
引用本文:王朝平,龚巍峥,许卫国. 南阳城区地下热水同位素特征及其水文地质意义[J]. 地下水, 2012, 0(2): 1-2,30
作者姓名:王朝平  龚巍峥  许卫国
作者单位:河南省地质矿产勘查开发局第一地质勘查院
基金项目:河南省地矿厅1998年“河南省南阳市(城区)地热资源综合研究”科研项目
摘    要:南阳城区地下热水的氢氧稳定同位素研究表明,本区地热水起源于降水补给。氚同位素揭示了地热水的形成年龄,采用同位素方法对本区地下热水与浅层冷水的混合作用对地下热水温度的影响进行了讨论,探讨了南阳城区地下热水的了解补给运移条件。

关 键 词:南阳城区  地下热水  同位素  水文地质意义

The Isotope Characteristics of the Geothermal Water in Nanyang Area and Its Hydro-geology Function
WANG Zhao-ping,XU Wei-guo. The Isotope Characteristics of the Geothermal Water in Nanyang Area and Its Hydro-geology Function[J]. Groundwater, 2012, 0(2): 1-2,30
Authors:WANG Zhao-ping  XU Wei-guo
Affiliation:,GONG Wei-zheng(The 1st Geological Exploration Institute,Henan Bureau of Geology and Mineral Exploration and Development,Nanyang 473056,Henan)
Abstract:To study on the hydrogen and oxygen stable isotope of the geothermal water in Nanyang City,it shows that the origin of geothermal water in the area is precipitation recharged.Geothermal water tritium revealed the formation of the age,we use isotope method of the underground water of the shallow cold water mixing with underground water temperature is discussed to explore the understanding of Nanyang City recharge underground water movement conditions.
Keywords:Nanyang City  underground hot water  isotope  hydro-geological significance
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