Subsurface flow mixing in coarse, braided river deposits

Coarse, braided river deposits show a large hydraulic heterogeneity on the metre scale. One of the main depositional elements found in such deposits is a trough structure filled with layers of bimodal gravel and open-framework gravel, the latter being highly permeable. However, the impact of such tr...

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Bibliographic Details
Main Authors: E. Huber, P. Huggenberger
Format: Article
Language:English
Published: Copernicus Publications 2016-05-01
Series:Hydrology and Earth System Sciences
Online Access:http://www.hydrol-earth-syst-sci.net/20/2035/2016/hess-20-2035-2016.pdf