Estimating groundwater discharge to surface waters using heat as a tracer in low flux environments: the role of thermal conductivity
Author:
Affiliation:
1. University of Oslo; Department of Geosciences; PO Box 1047 Blindern 0316 Oslo Norway
2. University of Copenhagen; Department of Geosciences and Natural Resources Management; Øster Voldgade 10 1350 K Copenhagen Denmark
Publisher
Wiley
Subject
Water Science and Technology
Link
http://onlinelibrary.wiley.com/wol1/doi/10.1002/hyp.10568/fullpdf
Reference61 articles.
1. Heat as a ground water tracer;Anderson;Ground Water,2005
2. Transient or steady-state? Using vertical temperature profiles to quantify groundwater-surface water exchange;Anibas;Hydrological Processes,2009
3. Using solver to determine vertical groundwater velocities by temperature variations, Purdue University, Indiana, USA;Arriaga;Hydrogeology Journal,2004
4. Baird A Wilby RL 1999 Eco-hydrology: plants and water in terrestrial and aquatic environments
5. Rates of vertical groundwater movement estimated from the Earth's thermal profile;Bredehoeft;Water Resources Research,1965
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