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Gabriel C. Rau

Researcher at Karlsruhe Institute of Technology

Publications -  67
Citations -  1586

Gabriel C. Rau is an academic researcher from Karlsruhe Institute of Technology. The author has contributed to research in topics: Groundwater & Hydrogeology. The author has an hindex of 20, co-authored 53 publications receiving 1194 citations. Previous affiliations of Gabriel C. Rau include Flinders University & University of New South Wales.

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Heat as a tracer to quantify water flow in near-surface sediments

TL;DR: A recent review as mentioned in this paper summarizes the existing body of research investigating natural and induced heat transport, and analyzes the progression in fundamental and natural process understanding through the qualitative and quantitative use of heat as a tracer.
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Experimental investigation of the thermal dispersivity term and its significance in the heat transport equation for flow in sediments

TL;DR: In this article, the authors proposed an empirical formulation for thermal dispersion with Darcy flow in natural porous media and clarified the disagreement regarding its significance, and demonstrated that heat transport with natural groundwater flow velocities can reach a transition zone between conduction and convection.
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Analytical methods that use natural heat as a tracer to quantify surface water–groundwater exchange, evaluated using field temperature records

TL;DR: In this article, the applicability of analytical solutions derived from the heat transport equation to the streambed environments was analyzed using the recorded temperature time series, which was found to lose water to the aquifer, supported by simultaneously recorded hydraulic gradients.
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A 1‐D analytical method for estimating surface water–groundwater interactions and effective thermal diffusivity using temperature time series

TL;DR: In this article, the amplitude ratio and phase shift of pairs of temperature time series at the SW-GW interface were used to estimate the Darcy velocity, which can indicate periods where assumptions to the analytical solution are violated.