Study of Channel Erosion and Sediment Transportby Carl F. Nordin, Jr.,
Serial Information: Journal of the Hydraulics Division, 1964, Vol. 90, Issue 4, Pg. 173-192
Document Type: Journal Paper
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.
Subject Headings: Sediment transport | Erosion | Channel flow | Suspended sediment | Material properties | Developing countries | North America | United States | New Mexico
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