中国地质环境监测院主办
高级检索

基于示踪试验及动态数据的北京小汤山地区地热资源量评价

,  ,  ,  ,  ,  ,  , 

文章导航 > 水文地质工程地质 > 2020 > 47(5): 196-200

上一篇

下一篇

杨亚军, 丁桂伶, 徐巍, 李海京, 鲁鹤, 王雨石, 张俊华, 王翊虹. 2020. 基于示踪试验及动态数据的北京小汤山地区地热资源量评价. 水文地质工程地质, 47(5): 196-200. doi: 10.16030/j.cnki.issn.1000-3665.201808029
引用本文: 杨亚军, 丁桂伶, 徐巍, 李海京, 鲁鹤, 王雨石, 张俊华, 王翊虹. 2020. 基于示踪试验及动态数据的北京小汤山地区地热资源量评价. 水文地质工程地质, 47(5): 196-200. doi: 10.16030/j.cnki.issn.1000-3665.201808029
shu
YANG Yajun, DING Guiling, XU Wei, LI Haijing, LU He, WANG Yushi, ZHANG Junhua, WANG Yihong. 2020. Tracer test and geothermal resource quantity evaluation based on dynamic data in the Xiaotangshan area of Beijing. Hydrogeology & Engineering Geology, 47(5): 196-200. doi: 10.16030/j.cnki.issn.1000-3665.201808029
Citation: YANG Yajun, DING Guiling, XU Wei, LI Haijing, LU He, WANG Yushi, ZHANG Junhua, WANG Yihong. 2020. Tracer test and geothermal resource quantity evaluation based on dynamic data in the Xiaotangshan area of Beijing. Hydrogeology & Engineering Geology, 47(5): 196-200. doi: 10.16030/j.cnki.issn.1000-3665.201808029
shu

基于示踪试验及动态数据的北京小汤山地区地热资源量评价

  • 北京市地质工程勘察院, 北京 100048

详细信息
    作者简介: 杨亚军(1968-),男,硕士,高工,主要从事地热资源勘察、资源量评价、监测预警及开发利用等工作。E-mail:460349858@qq.com
    通讯作者: 丁桂伶(1982-),女,博士,高工,主要从事地热资源及泥石流灾害调查评价、动态监测及预警研究等工作。E-mail:06115242@bjtu.edu.cn

  • 中图分类号: P314

Tracer test and geothermal resource quantity evaluation based on dynamic data in the Xiaotangshan area of Beijing

  • Beijing Geological Engineering Survey Institute, Beijing 100048, China

More Information

    摘要
  • 北京市地热资源丰富，开发历史悠久，用户众多。为科学合理评价地热资源潜力，更好地可持续开发利用地热资源。结合实际开采利用情况，充分考虑了回灌的影响，并以小汤山热田详细勘察资料和长序列的监测数据为基础，采用示踪试验和数值计算方法，给出了典型地热井要保持100 a温度不下降可持续开发利用的地热流体资源量为340 m3/h；结合地热流体温度监测数据，发现年均净开采量与年均水位下降成对数相关性，且在保持地热流体温度不发生显著变化的前提下，年均水位下降2.0 m，可以保障的最少年均可开采量为365.1×104m3。结合小汤山热田多年的开发利用资料和经验，提出合理科学可持续的开发利用地热资源，必须坚持“以热定采，以灌定采”模式。
    Geothermal resources are very rich in Beijing with a long development history and many user companies. In order to scientifically and rationally evaluate geothermal resources, the actual exploitation and utilization and the influence of recharge are fully considered. Based on the detailed survey data and the long series of monitoring data of the Xiaotangshan geothermal field, tracer tests are used to calculate the resources of a typical geothermal heating project in the Xiaotangshan area, and the available resources are estimated as 340 m3/h under the current temperature kept for 100 years. At the same time, the long-term dynamic monitoring data are used to analyze the whole thermal field in the Xiaotangshan area. The results show that the average annual net production is correlated with the average annual groundwater level decrease, and the geothermal resources are 365.1×104 m3 while the annual groundwater level decline is controlled at 2.0 m. Combined with the development and utilization data and experience of the Xiaotangshan geothermal field for many years, it is considered that the reasonable and scientific development and utilization of geothermal resources must adhere to the mode of “fixed mining by heat and irrigated mining”.
    • HTML全文
  • 加载中
    • 参考文献(11)
  • [1]

    北京市国土资源局. 北京市地热资源2006~2020年可持续利用规划[R]. 北京:北京市国土资源局, 2006.[Beijing Municipal Bureau of Land and Resources. Sustainable utilization planning of geothermal resources in Beijing during 2006-2020[R]. Beijing:Beijing Municipal Bureau of Land and Resources, 2006.(in Chinese)]

    [2]

    中华人民共和国国家质量监督检验检疫总局, 中国国家标准化管理委员会.地热资源地质勘查规范:GB/T 11615-2010[S].北京:中国标准出版社, 2010.[General Administration of Quality Supervision, Inspection and Quarantine of the People's Republic of China, Standardization Administration of the People's Republic of China. Geologic exploration standard of geothermal resources:GB/T 11615-2010[S]. Beijing:Standards Press of China, 2010.(in Chinese)]

    [3]

    吴基文,王广涛,翟晓荣,等.淮南矿区地热地质特征与地热资源评价[J].煤炭学报,2019,44(8):2566-2578.[WU J W, WANG G T, ZHAI X R, et al. Geothermal geological characteristics and geothermal resources evaluation of Huainan mining area[J].Journal of China Coal Society,2019,44(8):2566-2578.(in Chinese)]

    [4]

    AXELSSON G, FLOVENZ O G, HAUKSDOTTIR S, et al. Analysis of tracer test data, and injection-induced cooling, in the Laugaland geothermal field, N-Iceland[J]. Geothermics, 2001,30(6):697-725.

    [5]

    王树芳,刘久荣,林沛,等. 岩溶热储回灌实验与示踪试验研究[J]. 水文地质工程地质,2013,40(6):129-133.[WANG S F, LIU J R, LIN P, et al. A study of reinjection experiment and tracer test in a karst geothermal reservoir[J]. Hydrogeology & Engineering Geology, 2013,40(6):129-133.(in Chinese)]

    [6]

    杨义栋,李芳芳, 张瀚予.焦作-商丘断裂永城段地热资源评价[J].能源与环保,2020,42(1):127-131.[YANG Y D, LI F F, ZHANG H Y. Evaluation of geothermal resources in Yongcheng section of Jiaozuo-Shangqiu Fault[J]. China Energy and Environmental Protection, 2020,42(1):127-131.(in Chinese)]

    [7]

    任光远.基于热储法的银川盆地地热资源评价[J]. 环境与发展, 2019, 31(10):30-31.[REN G Y. Geothermal resource evaluation of Yinchuan Basin based on thermal storage method[J]. Environment and Development, 2019, 31(10):30-31.(in Chinese)]

    [8]

    赵志宏,刘桂宏,谭现锋,等.基于等效渗流通道模型的地热尾水回灌理论模型[J].水文地质工程地质,2017,44(3):158-164.[ZHAO Z H, LIU G H, TAN X F, et al. Theoretical model of geothermal tail water reinjection based on the equivalent flow channel model[J]. Hydrogeology & Engineering Geology, 2017, 44(3):158-164.(in Chinese)]

    [9]

    杨杨,赵良杰,苏春田,等.基于CFP的岩溶管道流溶质运移数值模拟研究[J].水文地质工程地质,2019, 46(4):51-57.[YANG Y,ZHAO L J,SU C T,et al. A study of the solute transport model for karst conduits based on CFP[J]. Hydrogeology & Engineering Geology, 2019, 46(4):51-57.(in Chinese)]

    [10]

    李元杰. 地热回灌示踪技术及热储模拟实验研究[D]. 北京:中国地质科学院,2010.[LI Y J. Study on geothermal reinjection of tracer technology and simulation of thermal energy storage[D]. Beijing:Chinese Academy of Geological Sciences, 2010.(in Chinese)]

    [11]

    刘凯, 叶超, 刘玉忠, 等. 北京地区地热资源潜力区划[J]. 工程地质学报, 2018,26(2):551-560.[LIU K, YE C, LIU Y Z,et al. Regionalization of geothermal resource potential in BeiJing[J].Journal of Engineering Geology,2018,26(2):551-560.(in Chinese)]

    • 相关文章
  • 施引文献
  • 资源附件(0)
  • 加载中
计量
  • 文章访问数:  842
  • PDF下载数:  94
  • 施引文献:  0
出版历程
收稿日期:  2019-09-13
修回日期:  2019-12-24

目录

    版权所有：中国地质调查局发展研究中心 copyright @2020
    返回