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Publikováno v:
Geomorphology. 395:108001
It has been observed that the relation between sediment storage and sediment transport rate in gravel-bed rivers exhibits counter-clockwise hysteresis, or aggradation-degradation cycles. Previous work has attributed these cycles to external changes t
Autor:
Dan Hogan, Marwan A. Hassan, André Zimmermann, Brett C. Eaton, Bonnie J. Smith, David S. Luzi
Bedforms in gravel-bed rivers range in size from 10 −2 to 10 3 m and have a wide range of affects on sediment transport and channel stability. To study the affect of these bedforms on sediment transport a classification scheme is proposed that brea
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::208e50379c59cd3ed5694be1bd80f298
https://doi.org/10.1016/s0928-2025(07)11137-8
https://doi.org/10.1016/s0928-2025(07)11137-8