院报 ›› 2018, Vol. 35 ›› Issue (12): 39-45.DOI: 10.11988/ckyyb.20170696

• 水资源与环境 • 上一篇    下一篇

地温示踪技术在地下水科学中的应用研究进展

董林垚1, 陈建耀2, JunShimada3, 尹政兴4   

  1. 1. 水土保持研究所,武汉 430010;
    2.中山大学 地理科学与规划学院,广州 510000;
    3.熊本大学 自然科学研究院,日本 熊本 8608555;
    4.长江勘测规划设计研究院 市政与交通院,武汉 430010
  • 收稿日期:2017-06-16 出版日期:2018-12-01 发布日期:2018-12-18
  • 作者简介:董林垚(1987-),男,湖北襄阳人,高级工程师,博士,主要从事水文水资源方面的研究。E-mail:linyaodonghydro@foxmail.com
  • 基金资助:
    国家自然科学基金项目(41501037)

Research Progress of Heat as a Tracer to Interpret Scientific Problems in Hydrogeology

DONG Lin-yao1, CHEN Jian-yao2, Jun Shimada3, YIN Zheng-xing4   

  1. 1. Soil and Water Conservation Department, Yangtze River Scientific Research Institute, Wuhan 430010, China;
    2.School of Geography Science and Planning, Sun Yat-sen University, Guangzhou 510000, China;
    3.Graduate School of Science and Technology, Kumamoto University, Kumamoto 8608555, Japan;
    4.Department of Urban Construction and Transportation,Changjiang Institute of Survey,Planning,Design and Research, Wuhan 430010, China
  • Received:2017-06-16 Online:2018-12-01 Published:2018-12-18

摘要: 对含水层流场与温度场耦合作用原理及地温示踪技术在地下水科学中的应用进行评述,总结了地温示踪技术在前沿地下水科学中的应用进展:①探究地表暖化-地下水流动对地温的影响;②计算含水层水文地质参数;③解析滨海含水层地下水循环过程。温度示踪法具有低成本、无污染、易于连续观测等优点,在地下水科学研究中具有广阔的前景,但利用温度示踪技术解析地下水科学问题目前仅适用于各向同性含水层,关于地下水气相和固相的交互过程中温度变化的研究亟待加强。

关键词: 地下水, 流场, 温度场, 示踪技术, 含水层, 水文地质参数

Abstract: The theory and application of heat as a tracer to interpret groundwater flowing was reviewed in this paper. The application of heat tracer in the frontier groundwater science was summarized as following: (1) interpretation of the impact of surface warming and groundwater flowing to subsurface temperature; (2) calculation of hydrogeological parameters; (3) investigation on groundwater circulation in coastal aquifer. As a tracer with low expense, no pollution and easy to be observed, heat can be applied widely in the field of subsurface hydrology and engineering. However, the technique of heat as a tracer can only be applied into the interpretation of groundwater problems in homogeneous aquifers. Research on the interaction between solid and atmosphere in subsurface environment should be enhanced.

Key words: groundwater, flow line, thermal regime, heat tracer technique, aquifer, hydrogeological parameters

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