Abstract
A numerical model of sediment sorting in meandering rivers is presented. In natural rivers, the spatial distribution of sediment mean size, along with that of the flow field and bed topography, is intimately tied to channel curvature. Coarser sediment, for example, tends to move along the inner bank upstream of the bend apex, and then crosses to the outer bank near the apex. This tendency for local spatial segregation of grain sizes of heterogeneous sediments is known as sediment sorting.
| Original language | English |
|---|---|
| Title of host publication | Proceedings, Congress of the International Association of Hydraulic Research, IAHR |
| Place of Publication | New York, NY, United States |
| Publisher | ASCE |
| Pages | 1439-1444 |
| Number of pages | 6 |
| Volume | B pt 2 |
| Publication status | Published - 1997 |
| Event | Proceedings of the 1997 27th Congress of the International Association of Hydraulic Research, IAHR. Part D - San Francisco, CA, USA Duration: 1997 Aug 10 → 1997 Aug 15 |
Other
| Other | Proceedings of the 1997 27th Congress of the International Association of Hydraulic Research, IAHR. Part D |
|---|---|
| City | San Francisco, CA, USA |
| Period | 97/8/10 → 97/8/15 |
Fingerprint
ASJC Scopus subject areas
- Engineering(all)
Cite this
Sediment sorting in meandering rivers. / Sekine, Masato.
Proceedings, Congress of the International Association of Hydraulic Research, IAHR. Vol. B pt 2 New York, NY, United States : ASCE, 1997. p. 1439-1444.Research output: Chapter in Book/Report/Conference proceeding › Conference contribution
}
TY - GEN
T1 - Sediment sorting in meandering rivers
AU - Sekine, Masato
PY - 1997
Y1 - 1997
N2 - A numerical model of sediment sorting in meandering rivers is presented. In natural rivers, the spatial distribution of sediment mean size, along with that of the flow field and bed topography, is intimately tied to channel curvature. Coarser sediment, for example, tends to move along the inner bank upstream of the bend apex, and then crosses to the outer bank near the apex. This tendency for local spatial segregation of grain sizes of heterogeneous sediments is known as sediment sorting.
AB - A numerical model of sediment sorting in meandering rivers is presented. In natural rivers, the spatial distribution of sediment mean size, along with that of the flow field and bed topography, is intimately tied to channel curvature. Coarser sediment, for example, tends to move along the inner bank upstream of the bend apex, and then crosses to the outer bank near the apex. This tendency for local spatial segregation of grain sizes of heterogeneous sediments is known as sediment sorting.
UR - http://www.scopus.com/inward/record.url?scp=0030716698&partnerID=8YFLogxK
UR - http://www.scopus.com/inward/citedby.url?scp=0030716698&partnerID=8YFLogxK
M3 - Conference contribution
AN - SCOPUS:0030716698
VL - B pt 2
SP - 1439
EP - 1444
BT - Proceedings, Congress of the International Association of Hydraulic Research, IAHR
PB - ASCE
CY - New York, NY, United States
ER -