Determining thermal diffusivity using near‐surface periodic temperature variations and its implications for tracing groundwater movement at the eastern margin of the Tibetan Plateau-Reference-Cited by-同舟云学术

Determining thermal diffusivity using near‐surface periodic temperature variations and its implications for tracing groundwater movement at the eastern margin of the Tibetan Plateau

Published:2019-02-15 Issue:8 Volume:33 Page:1276-1286
ISSN:0885-6087
Container-title:Hydrological Processes
language:en
Short-container-title:Hydrological Processes

Author:

Liu Qiongying¹^ORCID,Chen Shunyun²,Jiang Liangwen³,Wang Dong³,Yang Zhuzhuan¹,Chen Lichun¹

Affiliation:

1. Division of Medium to Long Term Earthquake PredictionInstitute of Geology, China Earthquake Administration Beijing 100029 China

2. State Key Laboratory of Earthquake DynamicsInstitute of Geology, China Earthquake Administration Beijing China

3. China Railway Eryuan Engineering Group Co., Ltd. Chengdu 610031 China

Funder

National Natural Science Foundation of China

Publisher

Wiley

Subject

Water Science and Technology

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1002/hyp.13399

Reference38 articles.

1. Heat as a Ground Water Tracer

2. Determining the thermal diffusivity of the ground based on subsoil temperatures. Preliminary results of an experimental geothermal borehole study Q-THERMIE-UNIOVI

3. On the use of surface and ground temperature data to recover soil water content information

4. Determination of upward/downward groundwater fluxes using transient variations of soil profile temperature: test of the method with Voyons (Aube, France) experimental data

5. Interpreting Repeated Temperature-Depth Profiles for Groundwater Flow

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