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Study on the calculation of geothermal fluids recoverable quantity and the distribution law of karst geothermal reservoirs in Hebei Plain |
ZHANG Dezhong, MA Yunqing, SU Yongqiang |
The 3rd Hydrogeology and Engineering Group of Hebei Bureau of Geology and Mineral Resources, Hengshui 053000, China |
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Abstract Using geothermal reservoirs method, analytical method, statistical analysis method and numerical simulation method, the authors evaluated and compared the geothermal fluids recoverable quantity of layered geothermal reservoirs in Hebei Plain. Geothermal reservoirs method and analytical method are suitable for geothermal fields with low exploration degree without geothermal wells or with only a small number of geothermal wells and productivity test data, so the calculation precision is relatively low. Statistical analysis method and numerical simulation method are suitable for geothermal fields with high exploration degree and multiple years of development and monitoring data, so the results are reliable. The karst geothermal reservoirs have the characteristics of high temperature, easy recharge and good sustainability, and they mainly occur in the Paleozoic and Middle-Upper Proterozoic strata and are covered by the Cenozoic strata, which is conducive to the thermal accumulation and insulation of the reservoirs. Karst fissures are widely distributed in the uplift zone of the bedrock’ forming deep hot water reservoirs. These reservoirs may develop into geothermal fields with great development and utilization value, and are the major reservoirs for further geothermal exploration and development.
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Received: 28 November 2017
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[1] 刘忠凯,吕文斌,冯来全,等.河北省地热资源调查评价与规划报告[R].衡水:河北省地矿局第三水文工程地质大队,2015. [2] 苏永强. 河北省地热能开发利用"十三五"规划报告[R].衡水:河北省地矿局第三水文工程地质大队,2016. [3] 张银妹,赵阳,刘江涛,等.河北省地热资源可开采量评价研究报告[R].衡水:河北省地矿局第三水文工程地质大队,2016. [4] 陈墨香. 华北地热[M].北京:科学出版社,1988. [5] 陈墨香,汪集旸,邓孝.中国地热资源——形成特点和潜力评估[M].北京:科学出版社,1994. [6] 阎敦实,于英太.京津冀油区地热资源评价与利用[M].武汉:中国地质大学出版社,2000. [7] 邓孝. 束鹿—宁晋地区地热资源评价研究报告[R].石家庄:中国地质科学院水文地质环境地质研究所,1990. [8] 张德忠,刘志刚,卢红柳,等.河北地热[M].北京:地质出版社,2013. [9] 赵静,王旭开,万力,等.深层地热资源评价中的回收率问题[J].地质科技情报,2008(6):89-92. [10] 张中祥,韩建江,徐健,等.沉积盆地型层状热储可采资源量计算方法探索[J].水文地质工程地质,2005,32(1):73-77. [11] 孙颖,许辉熙,刘久荣,等.中低温地热田的地热资源计算评价[J].安徽农业科学,2009,37(14):6535-6537. [12] 李郡,王全凯,王琰,等.河北省地热资源现状调查评价与区划报告[R].衡水:河北省地矿局第三水文工程地质大队,2015. [13] 王永波,丁文萍,田月,等.河北牛驼镇地热田高温地热水成因分析[J].城市地质,2016,11(3):59-64. [14] 李宜程. 山东省中深层地热资源开发潜力分区评价[D].济南:山东建筑大学,2016. [15] 吕东亮,林黎,林建旺,等.岩溶热储地热能可持续开发潜力的模糊综合评价[J].勘察科学技术,2008(4):20-23,52. [16] 刘福东,黄加力,李子果,等,河北省牛驼镇地热田地热尾水回灌试验[R].衡水市:河北省地矿局第三水文工程地质大队. 2012. [17] 周阳,邓念东,王凤,等.浅层地热能适宜性分区结构的分形原理[J].中国地质调查,2017,4(1):18-23. |
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