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Study of Channel Erosion and Sediment Transport
Observations of channel erosion, flow, and sediment transport for the Rio Puerco, in New Mexico, indicate that the characteristics of the channel and of the channel material change rapidly because of deposition and erosion, and that the ephemeral flows carry extremely high concentrations of suspended sediment that influence flow and transport characteristics.
Study of Channel Erosion and Sediment Transport
Observations of channel erosion, flow, and sediment transport for the Rio Puerco, in New Mexico, indicate that the characteristics of the channel and of the channel material change rapidly because of deposition and erosion, and that the ephemeral flows carry extremely high concentrations of suspended sediment that influence flow and transport characteristics.
Study of Channel Erosion and Sediment Transport
Nordin, Carl F. (author)
Journal of the Hydraulics Division ; 90 ; 173-192
2021-01-01
201964-01-01 pages
Article (Journal)
Electronic Resource
Unknown
Study of channel erosion and sediment transport
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