Transient or steady-state? Using vertical temperature profiles to quantify groundwater-surface water exchange

Heat is recognized as a natural tracer to identify the exchange of water between the groundwater and surface water compartment. One-dimensional (1D) heat transport models have the ability to obtain quantitative estimates of vertical fluxes through the sediment matrix. Input to these models can come...

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Bibliographic Details
Published in:	Hydrological processes Vol. 23; no. 15; pp. 2165 - 2177
Main Authors:	Anibas, Christian, Fleckenstein, Jan H, Volze, Nina, Buis, Kerst, Verhoeven, Ronny, Meire, Patrick, Batelaan, Okke
Format:	Journal Article Conference Proceeding
Language:	English
Published:	Chichester, UK John Wiley & Sons, Ltd 15-07-2009 Wiley
Subjects:	Earth sciences Earth, ocean, space Exact sciences and technology FEMME groundwater-surface water interaction heat transport modelling Hydrogeology Hydrology. Hydrogeology hyporheic zone temperature VS2DH Belgium Central Europe Europe Germany Western Europe time series analysis groundwater-surface water interaction heat balance springs simulation ground water aquifers temperature flux lakes boundary conditions heat transport modelling energy rivers models interfaces tracers seepage transport hyporheic zone surface water depth acid mine dewatering VS2DH FEMME seasonal variations
Online Access:	Get full text
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