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作 者:张延军[1,2] 张通[1] 殷仁朝 郑杰 刘彤[1] 谢洋洋[1] Zhang Yanjun Zhang Tong Yin Renchao Zheng Jie Liu Tong Xie Yangyang(College of Construction Engineering of Jilin University, Changchun 130026, China Key Lab of Groundwater Resource and Environment Ministry of Education ,Jilin University, Changchun 130026, China Instituteof Karst Geology, ChineseAcademy of Geological Sciences, Guilin 541004, Guangxi, China Xiamen Institute of Geotechnical Engineering, Xiamen 361004, Fujian, China)
机构地区:[1]吉林大学建设工程学院,长春130026 [2]地下水资源与环境教育部重点实验室,长春130026 [3]中国地质科学院岩溶地质研究所,广西桂林541004 [4]厦门市地质工程勘察院,福建厦门361004
出 处:《吉林大学学报(地球科学版)》2017年第1期189-196,共8页Journal of Jilin University:Earth Science Edition
基 金:国家自然科学基金项目(41372239);高等学校博士学科点专项科研基金(20110061110055)~~
摘 要:地热异常区的探测对于地热能开发利用至关重要。利用2 m测温法和相关仪器对厦门东山某热泉地区进行实地探测,获取1~2m深度地层温度和导热系数数据,绘制研究区2m深度温度等值线图和浅层热流密度分布云图,圈定地热异常区。运用一维稳态热传导模型对研究区20 m深度地温进行反演,并与研究区20m深度实测温度进行对比分析。结果表明,2m测温法对地热异常区探测效果明显,一维稳态热传导模型对于20m深度地温的预测结果与实测结果较为一致。该方法可以作为地热探测初期的有效手段。Geothermal anomaly areas exploration is essential for the development and utilization of geothermal energy.2-meter temperature survey and associated apparatus are used to get temperature and thermal conductivity data of 1-2mdepth in a hot springs area of Dongshan,Xiamen.Then temperature contour map of 2mdepth and heat flow density distribution map of shallow layer are drawn,geothermalanomaly areas of research area are delineated.The one-dimensional steady-state heat conduction model is used for ground temperature inversion of 20 m depth.Then inversion results are compared with measured temperature of 20 mdepth.The results show that the effect of 2 meters temperature survey for geothermal anomaly areas is obvious and prediction result of one-dimensional steady-state heat conduction model is consistent with measured results.This method can be used as an effective mean for early stage geothermal exploration.
分 类 号:P642.22[天文地球—工程地质学]
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