scholarly journals SEDIMENT YIELD AND SUSPENDED SEDIMENT TRANSPORT IN THE CHIKUGOGAWA RIVER BASIN

2008 ◽  
Vol 52 ◽  
pp. 553-558 ◽  
Author(s):  
Katsuhide YOKOYAMA ◽  
Shintaro FUJIZUKA ◽  
Tetsuhiro NAKAZAWA ◽  
Soutaro TAKASHIMA
Keyword(s):  
Sediment Transport ◽  
Suspended Sediment ◽  
River Basin ◽  
Sediment Yield ◽  
Suspended Sediment Transport

scholarly journals Suspended sediment transport in a river basin estimated by chemical composition analysis

2010 ◽  
Vol 4 ◽  
pp. 55-59 ◽  
Author(s):  
Tetsuya Ishida ◽  
Keisuke Nakayama ◽  
Tomonari Okada ◽  
Yasuyuki Maruya ◽  
Kiyofumi Onishi ◽  
...  
Keyword(s):  
Chemical Composition ◽  
Sediment Transport ◽  
Suspended Sediment ◽  
River Basin ◽  
Suspended Sediment Transport ◽  
Composition Analysis ◽  
Chemical Composition Analysis

scholarly journals Spatial distribution of soil erosion and suspended sediment transport rate for Chou-Shui river basin

2014 ◽  
Vol 123 (7) ◽  
pp. 1517-1539 ◽  
Author(s):  
Chin-Ping Lin ◽  
Ching-Nuo Chen ◽  
Yu-Min Wang ◽  
Chih-Heng Tsai ◽  
Chang-Tai Tsai
Keyword(s):  
Spatial Distribution ◽  
Sediment Transport ◽  
Soil Erosion ◽  
Suspended Sediment ◽  
River Basin ◽  
Transport Rate ◽  
Suspended Sediment Transport ◽  
Sediment Transport Rate

scholarly journals Long-term suspended sediment transport in the Goodwater Creek Experimental Watershed and Salt River Basin, Missouri, USA

2013 ◽  
Vol 49 (11) ◽  
pp. 7827-7830 ◽  
Author(s):  
Claire Baffaut ◽  
Fessehaie Ghidey ◽  
Kenneth A. Sudduth ◽  
Robert N. Lerch ◽  
E. John Sadler
Keyword(s):  
Sediment Transport ◽  
Suspended Sediment ◽  
River Basin ◽  
Suspended Sediment Transport ◽  
Salt River

Spatial and temporal patterns of suspended-sediment yield in the Saskatchewan River basin

1988 ◽  
Vol 25 (9) ◽  
pp. 1450-1463 ◽  
Author(s):  
P. E. Ashmore ◽  
T. J. Day
Keyword(s):  
Suspended Sediment ◽  
River Basin ◽  
Sediment Yield ◽  
Sediment Concentration ◽  
Suspended Sediment Transport ◽  
Spatial And Temporal Patterns ◽  
Prairie Streams ◽  
The North ◽  
Discharge Regime ◽  
Pattern Of Variation

Long-term suspended-sediment concentration and load records are available for 23 Water Survey of Canada sediment-monitoring stations in the Saskatchewan River basin, where the drainage areas range from 10 to over 300 000 km2. Mean annual sediment yield is greatest in the western Alberta Plains along the Oldman and Red Deer rivers (over 100 t km−2 year−1) and tends to increase downstream along the North and South Saskatchewan rivers until major reservoirs in Saskatchewan intervene. Average sediment concentration shows a pattern of variation similar to that of yield. Temporal aspects of suspended-sediment transport vary along the drainage network. The range and skewness of the yield–duration and concentration–duration curves are greater in the intermediate-size basins close to the Rocky Mountains and in two small basins with Prairie sources than they are in the large Prairie streams with mountain sources and the glacier-fed upper North Saskatchewan River. Similarly, infrequent flows transport a larger proportion of the annual load in the smaller Foothills and western Plains basins than in the large Prairie streams because of differences in drainage area and discharge regime.

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