Time-series temperature analyses indicate conduction and diffusion are dominant heat-transfer processes in fine sediment, low-flow streams-Reference-Cited by-同舟云学术

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

Published:2021-05 Issue: Volume:768 Page:144367
ISSN:0048-9697
Container-title:Science of The Total Environment
language:en
Short-container-title:Science of The Total Environment

Author:

Scotch Chester G.,Murgulet Dorina,Constantz James

Funder

Texas A&M University-Corpus Christi

Coastal Bend Bays Estuaries Program

Publisher

Elsevier BV

Subject

Pollution,Waste Management and Disposal,Environmental Chemistry,Environmental Engineering

Reference73 articles.

1. Stream-aquifer interactions in the Maules creek catchment, Namoi valley, New South Wales, Australia;Andersen;Hydrogeology Journal,2009

2. Heat as a ground water tracer;Anderson;Groundwater,2005

3. Quaternary Evolution of the East Texas Coast and Continental Shelf;Anderson,1992

4. Transient or steady-state? Using vertical temperature profiles to quantify groundwater–surface water exchange;Anibas;Hydrological Processes,2009

5. Mechanisms of osmotic flow and volume change in clay soils;Barbour;Canadian Geotechnical Journal,1989

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