地温示踪技术在地下水科学中的应用研究进展

董林垚; 陈建耀; JunShimada; 尹政兴

doi:10.11988/ckyyb.20170696

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

水资源与环境

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

作者信息 +

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

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

Author information +

文章历史 +

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。

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.

导出引用

董林垚, 陈建耀, JunShimada, 尹政兴. 地温示踪技术在地下水科学中的应用研究进展[J]. 长江科学院院报. 2018, 35(12): 39-45 https://doi.org/10.11988/ckyyb.20170696

DONG Lin-yao, CHEN Jian-yao, Jun Shimada, YIN Zheng-xing. Research Progress of Heat as a Tracer to Interpret Scientific Problems in Hydrogeology[J]. Journal of Changjiang River Scientific Research Institute. 2018, 35(12): 39-45 https://doi.org/10.11988/ckyyb.20170696

中图分类号： P641

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