|本期目录/Table of Contents|

[1]胡 扬,马致远,余 娟,等.关中盆地地下热水接受补给时温度及热储层温度的估算[J].地球科学与环境学报,2009,31(02):173-176.
 HU Yang,MA Zhi-yuan,YU Juan,et al.Estimation of the Making-up Temperature of Geothermy Water and the Thermal Reservoir Temperature in the Guanzhong Basin[J].Journal of Earth Sciences and Environment,2009,31(02):173-176.
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关中盆地地下热水接受补给时温度及热储层温度的估算(PDF)
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《地球科学与环境学报》[ISSN:1672-6561/CN:61-1423/P]

卷:
第31卷
期数:
2009年第02期
页码:
173-176
栏目:
水资源与地质工程
出版日期:
2009-06-15

文章信息/Info

Title:
Estimation of the Making-up Temperature of Geothermy Water and the Thermal Reservoir Temperature in the Guanzhong Basin
文章编号:
1672-6561(2009)02-0173-04
作者:
胡 扬1马致远1余 娟1李 青2张跟全3贾旭兵1
(1.长安大学 环境科学与工程学院,陕西 西安 710054; 2.西安地质矿产研究所, 陕西 西安 710054; 3.咸阳市地热资源开发管理办公室, 陕西 咸阳 712000)
Author(s):
HU Yang1 MA Zhi-yuan1 YU Juan1 LI Qing2 ZHANG Gen-quan3 JIA Xu-bing1
(1.School of Environmental Sciences and Engineering, Chang'an University, Xi'an 710054, Shaanxi, China; 2.Xi'an Institute of Geology and Mineral Resources, Xi'an 710054, Shaanxi, China; 3.Xianyang Developmentof Geothermal Resources Management Office, Xianyang 712000, Shaanxi, China)
关键词:
地下热水同位素温度热储层
Keywords:
geothermy water isotope temperature thermal reservoir
分类号:
P314.1
DOI:
-
文献标志码:
A
摘要:
通过对关中盆地地热井中地下热水的同位素和水化学成分分析,结合研究区的地热地质和水文地质条件,进行了地下热水补给时的温度研究,结果表明,关中盆地地下热水接受补给时的温度以西安地区最低,咸阳次之。同时应用Na-K-Mg三角图和水化学平衡温度理论的方法,估算在平衡条件下关中盆地最大热储温度为118℃。热储温度计算结果表明,关中盆地腹部应为中低温热储层。
Abstract:
By analyzing the isotope and the data of hydrochemistry composition of geothermal water from the geothermal wells in Guanzhong basin, and the conditions of geothermal geology and hydrogeology in the area, the making-up temperature of geothermal water is researched. The results show that the lowest making-up temperature of the geothermal water in Guanzhong basin is in Xi'an, and Xianyang has a lower making-up temperature than Xi'an. With the method of Na-K-Mg triangular diagram and hydrochemistry balance temperature theory, it is estimated that the maximum thermal reservoir temperature in Guanzhong basin is 118 ℃ in equilibrium condition. From the calculation results of temperature, the center of Guanzhong basin should be mesothermal and microtherm reservoir.

参考文献/References:

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备注/Memo

备注/Memo:
收稿日期:2008-07-20
基金项目: 陕西省自然科学基金项目(SJ08-ZT08); 中国地质调查局项目(1212010535416)
作者简介: 胡 扬(1979-),男,浙江无锡人,工学硕士研究生,从事水文地质、环境同位素水文地质研究。E-mail:hysep4@yahoo.com.cn

更新日期/Last Update: 2009-06-20