Ven Te Chow Hydrosystems Laboratory, Department of Civil and
Environmental Engineering, University of Illinois at Urbana–Champaign,
Urbana, IL 61801, USA
Ven Te Chow Hydrosystems Laboratory, Department of Civil and
Environmental Engineering, University of Illinois at Urbana–Champaign,
Urbana, IL 61801, USA
Department of Geology, University of Illinois at Urbana–Champaign,
Urbana, IL 61801, USA
Colin P. Stark
Lamont Doherty Earth Observatory, Columbia University, Palisades, NY 10964, USA
Viewed
Total article views: 3,161 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
Supplement
BibTeX
EndNote
2,181
893
87
3,161
238
77
80
HTML: 2,181
PDF: 893
XML: 87
Total: 3,161
Supplement: 238
BibTeX: 77
EndNote: 80
Views and downloads (calculated since 27 Feb 2019)
Cumulative views and downloads
(calculated since 27 Feb 2019)
Total article views: 2,215 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
Supplement
BibTeX
EndNote
1,634
500
81
2,215
130
68
71
HTML: 1,634
PDF: 500
XML: 81
Total: 2,215
Supplement: 130
BibTeX: 68
EndNote: 71
Views and downloads (calculated since 09 Oct 2019)
Cumulative views and downloads
(calculated since 09 Oct 2019)
Total article views: 946 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
Supplement
BibTeX
EndNote
547
393
6
946
108
9
9
HTML: 547
PDF: 393
XML: 6
Total: 946
Supplement: 108
BibTeX: 9
EndNote: 9
Views and downloads (calculated since 27 Feb 2019)
Cumulative views and downloads
(calculated since 27 Feb 2019)
Viewed (geographical distribution)
Total article views: 3,161 (including HTML, PDF, and XML)
Thereof 2,904 with geography defined
and 257 with unknown origin.
Total article views: 2,215 (including HTML, PDF, and XML)
Thereof 2,055 with geography defined
and 160 with unknown origin.
Total article views: 946 (including HTML, PDF, and XML)
Thereof 849 with geography defined
and 97 with unknown origin.
This paper describes the case of a meandering bedrock river with loose sediment on the bed. In such rivers, the sediment hits and erodes the bed as it moves with the flow. We did experiments in a laboratory flume to identify the areas where the sediment moves and those where it deposits. We discovered that the size and location of those areas change with the amount of sediment in the channel and its curvature. The fluctuations of sediment cover over the bed drive the erosion potential.
This paper describes the case of a meandering bedrock river with loose sediment on the bed. In...