Publication Date:
2015-03-11
Description:
Article The onset of sediment transport is commonly believed to be an abrupt process, which influences our understanding of river erosion and landscape dynamics. Houssais et al. show instead a continuous transition from a creeping to a granular-flow regime by monitoring internal motion in a sediment bed. Nature Communications doi: 10.1038/ncomms7527 Authors: Morgane Houssais, Carlos P. Ortiz, Douglas J. Durian, Douglas J. Jerolmack
Electronic ISSN:
2041-1723
Topics:
Biology
,
Chemistry and Pharmacology
,
Natural Sciences in General
,
Physics
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