Remote semiautomatic instrumentation for intermittent streamflow measurement and suspended sediment sampling

1984 ◽  
Vol 11 (4) ◽  
pp. 993-996 ◽  
Author(s):  
John L. Honsaker ◽  
Ian A. Campbell ◽  
R. B. Bryan

Stream discharge and suspended sediment in ephemeral channels are measured by battery-powered instruments adapted for control by detection of rainfall. Solar cells recharge batteries between flow events. Key words: instruments, ephemeral channel, intermittent stream flow, suspended sediment, rain-activated, solar battery charging.

Author(s):  
K. Michael Nolan ◽  
John R. Gray ◽  
G. Douglas Glysson

1983 ◽  
Vol 29 (101) ◽  
pp. 185-190 ◽  
Author(s):  
Ian Beecroft

AbstractBetween 16 and 19 June 1981 a large water pocket of volume 183 000 m3 burst from glacier de Tsidjiore Nouve. From hourly stream discharge and suspended sediment concentration observations a suspended sediment output of 1 674 × 103 kg was calculated. The transport of bed-load was estimated at 3 840 × 103 kg, hence a total quantity of around 5 500 × 103 kg of sediment were removed from the catchment, including the pro-glacial field, in the four days of the outburst.


2013 ◽  
Vol 446-447 ◽  
pp. 1528-1533
Author(s):  
Sarunya Promkotra

Analytical results are considered the factors of suspended sediment concentration, fall velocity, dimensionless shear stress, transportation rate and stream discharge. As a result of suspended sediments of Loei, Huang and Mekong River, fine particles account for the applicability in sediment deposits. Floating suspended sediments explicit more clay minerals than suspended sediments. Suspended sediment concentration (SSC) in the estuarine of Loei River and Huang River are moderately less than Mekong River. Flow directions of the interconnected rivers to the mainstream-Mekong River lead to the quantity of SSC. Sediment concentrations attain to the dynamic response. Dimensionless shear stress relates to shear velocity, geometry and grain size of particles, and difference of flow velocity. This shear stress is directly comparative to flow velocity and clay mineral concentrations. The transport rate involves in the flow velocity, SSC and depth of the river. Moreover, stream discharge can be presumed by the geometry of the river and topography of sampling locations.


Solar Energy ◽  
1977 ◽  
Vol 19 (2) ◽  
pp. 171-177 ◽  
Author(s):  
S. Deb ◽  
M.K. Mukherjee ◽  
H. Saha

1974 ◽  
Vol 17 (1) ◽  
pp. M35-M44 ◽  
Author(s):  
Robert M. Beer ◽  
J.Paul Dauphin ◽  
Thomas S. Sholes

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