NTL Record

Title Stream Channel Stability Assessment
Record ID 64232
Personal Name
Creator
Brice, J. C.
Corporate Creator Geological Survey (U.S.)
Corporate
Contributor
United States. Department of Transportation. Federal Highway Administration. Office of Research
Publisher United States. Federal Highway Administration
Publication Date 19820101
Language English
Abstract Channel instability is manifested as lateral bank erosion, progressive degradation of the streambed, or natural scour and fill of the streambed. Lateral stability is related to stream type, and four major stream types having different stability characteristics are distinguished: equiwidth, wide-bend point bar, braided point-bar and braided. Measurements of bank erosion on a study group of 36 streams indicate that equiwidth streams have the lowest lateral erosion rates and braided point-bar streams the highest. Also, erosion rates Increase with stream size. Significant degradation of the streambed can usually be detected from indirect field evidence. The sites of greatest potential scour along a channel can be identified from channel configuration.
Rosap ID dot:34974
Rosap URL https://rosap.ntl.bts.gov/view/dot/34974
TRT Terms Aerial photography; Alluvium; Altitude; Stream banks; Channel stabilization; Erosion; Film; Flow; Maps; Measurement; Photographic equipment; Scour; Shape; Size; Sizing apparatus; Mechanical stability; Mechanical strain; Streambeds; Surveys
General Subjects Degradation; Elevation; Flow rate
Geographical
Coverage
United States
TRIS Online
Accession No
369798
Contract Number P.O. No. DTFH61-81-P-30085
Report Number FHWA/RD-82/021
Resource type Tech Report
URL https://ntlrepository.blob.core.windows.net/lib/64000/64200/64232/FHWA-RD-82-21.pdf
Format PDF
Database NTL Digital Repository