学术研究动态

我国建立第一个地热资源数据库

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  • 1.中国科学院地质研究所100029       2.地质矿产部水文地质和工程地质研究所100081 3.北京大学地质系100871

               
             

收稿日期: 1991-05-17

  网络出版日期: 1992-05-01

基金资助

国家“七五”攻关项目

ESTABLISHMENT OF THE FIRST GEOTHERMAL RESOURCES DATA-BASE IN CHINA

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  • 1.Institute of Geology Academia Sinica,Beijing 100029;2.Institute of Hydrogeolog&Engineering Geology,Ministryy of Geology & Mineral Resources, Zhengding Heibei 050083;3.Department of Geology, Peking University, Beijing 100871

Received date: 1991-05-17

  Online published: 1992-05-01

摘要

示范性地热资源数据库由“地温、岩石热物理参数”、“热水水文地质试验参数和地下热水点”和“地热区热流水化学组分”三个子来统构成。数据库系统还配备有软件包,其中包括各种地温梯度、岩石放射性生热率、水文地质参数的计葬程序,热水水质类型的判别和多种地球化学温标的对比分析的程序,绘制钻孔岩石柱状图,钻孔温深曲线,岩石热导率和生热率频率直方图,水化学成分预率直方图,各种等值线图,以及水位和流量动态曲线的程序。
  

本文引用格式

熊亮萍 林锦漩 过帼颖 . 我国建立第一个地热资源数据库[J]. 地球科学进展, 1992 , 7(3) : 50 . DOI: 10.11867/j.issn.1001-8166.1992.03.0050

Abstract

 Demonstrative geothermal resources data-base consists of 3 subsystems ;  1) Geotemperature&rock thermo一physical property ; 2 ) Hydrogeological testing parameters of thermal water&thermal water sites;3)Chemical composition of thermal fluids in geothermal areas. Data-base system is accompanied with software set including various programs for calculation on geothermal gradient,  radioactive heat productivity and hydrogeological parameters,for identification of thermal water chemical type,for comparision of different geothermometers and for ploting lithological colum,geotherms , histograms ofthermal conductivity&. heat productivity, chemical composition of thermal waters, isotherms as well as curves of water table and flow rate.
     

参考文献


[1]史九林.数据库系统初步.北京:人民邮电出版社,1986年;

[2]康金玉,张承庆(译).数据库:设计、性能与管理结构方法.北京知识出版社,1987年,

[3]Marshall,J R.Assessment of Low-temperature geothermal resources of the United States-1982, Geological survey circular,1983; 892.

[4] Muffler, L J P.  and Cataldi, R.  Methods for regional, assessment of ge9thermal resources, Geothermics,  1978;  (7);  53-78

[5] Nathenson, M and Muffer, L F P.  Geothermal resources in hydrothermal convection systems and conduction-dominated areas.
    In; Assessment of geothermal resources of the United States-1975, 1975, 104-121

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