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Ephemeral streams - Hydraulic factors and their relation to the drainage net

Professional Paper 282-A

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  • Document: Document (pdf)
  • Related Works:
    • Related Work Professional Paper 212-B: River channel patterns: Braided, meandering, and straight
    • Related Work Professional Paper 212-C: River flood plains: Some observations on their formation
    • Related Work Professional Paper 212-D: Flow resistance in sinuous or irregular channels
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Abstract

The hydraulic factors of width, depth, velocity, and suspended sediment load of ephemeral streams near Santa Fe, N. Mex., were measured during flood flow. Later, channel slope was measured. These flood-flow data, in conjunction with an analysis of drainage-basin configuration by the methods proposed by Horton, are used to determine the generalized interrelation of stream order and hydraulic variables. The method developed for determining this interrelation allows an integration of the geographic and physiographic characteristics of a drainage basin with the channel characteristics; specifically, the interrelation of the length, number, and drainage area of streams of various sizes with their respective discharge, width, depth, velocity, slope, channel roughness, and suspended-sediment load.

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Additional publication details

Publication type:
Report
Publication Subtype:
USGS Numbered Series
Title:
Ephemeral streams - Hydraulic factors and their relation to the drainage net
Series title:
Professional Paper
Series number:
282
Chapter:
A
Year Published:
1956
Language:
English
Publisher:
U.S. Government Printing Office
Publisher location:
Washington D.C.
Description:
iv, 37 p.
Larger Work Type:
Report
Larger Work Subtype:
USGS Numbered Series
Larger Work Title:
Physiographic and hydraulic studies of rivers (Professional Paper 282)
Country:
United States
State:
New Mexico