GIEC OpenIR
漳州地热田基岩裂隙水系统温度分布特征
曾玉超; 苏正; 吴能友; 王晓星; 胡剑
2012
Source Publication吉林大学学报地球科学版
ISSN1671-5888
Volume042Issue:003Pages:814
Abstract为研究漳州地热田基岩裂隙水系统温度分布特征,建立了新的三维基岩裂隙水系统概念模型,并利用Fluent软件求解模型。结果表明:基岩裂隙热水温度场受到断裂区的强烈控制,在北东—南西向断裂中,强烈对流形成的高温热柱刺穿了基岩顶部形成热田高温中心;基岩热流在断裂区中部高温区达到最大,在北东—南西方向上最大值为343.02mW/m2,在北西—南东方向最大值为368.72mW/m2,并向边缘逐渐降低;第四系孔隙水的存在和运动使得地表热流的最大值和局部值降低。未来漳州热田应加强深部温度的测量研究。
Language英语
Document Type期刊论文
Identifierhttp://ir.giec.ac.cn/handle/344007/20263
Collection中国科学院广州能源研究所
Affiliation中国科学院广州能源研究所
First Author AffilicationGuangZhou Institute of Energy Conversion,Chinese Academy of Sciences
Recommended Citation
GB/T 7714
曾玉超,苏正,吴能友,等. 漳州地热田基岩裂隙水系统温度分布特征[J]. 吉林大学学报地球科学版,2012,042(003):814.
APA 曾玉超,苏正,吴能友,王晓星,&胡剑.(2012).漳州地热田基岩裂隙水系统温度分布特征.吉林大学学报地球科学版,042(003),814.
MLA 曾玉超,et al."漳州地热田基岩裂隙水系统温度分布特征".吉林大学学报地球科学版 042.003(2012):814.
Files in This Item:
There are no files associated with this item.
Related Services
Recommend this item
Bookmark
Usage statistics
Export to Endnote
Google Scholar
Similar articles in Google Scholar
[曾玉超]'s Articles
[苏正]'s Articles
[吴能友]'s Articles
Baidu academic
Similar articles in Baidu academic
[曾玉超]'s Articles
[苏正]'s Articles
[吴能友]'s Articles
Bing Scholar
Similar articles in Bing Scholar
[曾玉超]'s Articles
[苏正]'s Articles
[吴能友]'s Articles
Terms of Use
No data!
Social Bookmark/Share
All comments (0)
No comment.
 

Items in the repository are protected by copyright, with all rights reserved, unless otherwise indicated.