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Time-series temperature analyses indicate conduction and diffusion are dominant heat-transfer processes in fine sediment, low-flow streams

Chester G. Scotch, , James Constantz
Published: 10 May 2021
Science of The Total Environment , Volume 768; doi:10.1016/j.scitotenv.2020.144367

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Keywords: Oso Creek Texas / Time-series temperature / Stream-groundwater exchange / Fine-sediment streambed

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