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汤水寨温泉带状热储特征及其热储量评价
引用本文:廖海吉,蓝俊康,洪淑娜,闫志为,黄希明.汤水寨温泉带状热储特征及其热储量评价[J].桂林工学院学报,2013(3):449-453.
作者姓名:廖海吉  蓝俊康  洪淑娜  闫志为  黄希明
作者单位:[1]桂林理工大学广西矿冶与环境科学实验中心,广西桂林541004 [2]桂林理工大学环境科学与工程学院,广西桂林541004 [3]广西地质环境监测总站,广西桂林541001
基金项目:广西空间信息与测绘重点实验室开放基金项目(桂科能1103108-28);广西矿冶与环境科学实验中心资助项目(KH2012ZD004)
摘    要:汤水寨地热田出露处为大面积分布的花岗岩,且其深部的岩体完整,岩体渗透性差,故判断其为带状热储.据泉水及其附近雨水的氚含量检测,该泉水是由大气降雨所补给,泉水在地下的循环时间至少在10年以上.鉴于该带状热储层的体积较小,储水量及其热储量均十分有限,建议对其只进行小规模开发利用,仅利用其自流量作保健饮用或保健洗浴用水.

关 键 词:温泉  热储量  评价  汤水寨  贺州  广西

Geothermal Reserves Evaluation and Characteristics of Zoned Reservoir in Tangshuizhai Spring Area
Affiliation:LIAO Hai-ji, LAN Jun-kang1, HONG Shu-naI, YAN Zhi-weiI, HUANG Xi.ming2 ( 1. a. Guangxi Scientific Experiment Center of Mining, Metallurgy and Environment; ix College of Environmen- tal Science and Engineering, Guilin University of Technology, Guilin 541004, China; 2. Geological Environ- ment Monitoring Station of Guangxi Chuang Autonomous Region, Guilin 541004, China)
Abstract:Granite is widely distributed around Tangshuizhai geothermal area. As the rock is integrity and poor in penetration in the depth, the geothermal field is classified as zoned reservoir. The data of Tritium concentra- tions in precipitation and in Tangshuizhai hot springs indicates that the spring water are of meteoric origin and the circulation time is at least ten years. As small volume, limited water storage and less geothermal reserves, the exploitation of the geothermal field should be in small scale. The hot springs can only be used for health drinking or bathing.
Keywords:hot spring  geothermal reserves  evaluation  Tangshuizhai  Hezhou  GUangxi
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