摘要
为了深入研究导水断层对地温场的影响及温度场和地下水流场的耦合机理,以淮北矿区徐广楼井田F38断层为研究对象,利用COMSOL Multiphysics软件模拟分析了其断层带附近地温异常的原因,清晰地反演了导水断层对地温场影响的整个过程。
To research the influence of water-conductive fault on geothermal field and the coupling mechanism between temperature field and groundwater flow field in depth,set F38 fault of Xuguanglou coal mine in Huaibei Coalfield as a research object, and simulated and analyzed the reason why the temperature was abnormal beside the fault zone by COMSOL Multiphysics, and inverted the whole process of the influence of water-conductive fault on geothermal field clearly.
出处
《煤炭技术》
CAS
北大核心
2014年第6期61-63,共3页
Coal Technology
基金
安徽省国土资源科技项目(2011-K-13)
国家自然科学基金项目(41272278)
高等学校博士学科点专项科研基金(20123415110002)
关键词
导水断层
地温场
影响
数值模拟
water-conductive fault
geothermal field
influence
numerical simulation
