A ROLE OF SEDIMENT TRANSPORT IN ALLUVIAL CHANNELS.

Research output: Chapter in Book/Report/Conference proceedingChapter

2 Citations (Scopus)

Abstract

ONCE A CRITICAL AMOUNT OF SEDIMENT IS BEING MOVED IN AN ALLUVIAL CHANNEL, VELOCITY CAN BE EXPRESSED AS A FUNCTION OF SLOPE AND OF SIZE AND COMPOSITION OF THE MOVING SEDIMENT LOAD.DEPTH IS A REDUNDANT PARAMETER.AT SEDIMENT TRANSPORT RATES BELOW CRITICAL, DEPTH IS AN EFFECTIVE PARAMETER.METHODS OF DETERMINING THE SIZE AND COMPOSITION OF THE MOVING SEDIMENT LOAD ARE ANALYSED AS IS THE PROBLEM OF DETERMINING WHEN DEPTH BECOMES REDUNDANT.THE PHENOMENA OF FILL AND SCOUR AT ALLUVIAL CHANNEL SECTIONS IS ALSO CONSIDERED.(A)

Original languageEnglish (US)
Title of host publicationJ. HYDRAUL. DIV., ASCE
Volume99 , HY11
StatePublished - 1973
Externally publishedYes

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Sediment transport
Sediments
Scour
Chemical analysis

ASJC Scopus subject areas

  • Engineering(all)

Cite this

Maddock, T. (1973). A ROLE OF SEDIMENT TRANSPORT IN ALLUVIAL CHANNELS. In J. HYDRAUL. DIV., ASCE (Vol. 99 , HY11)

A ROLE OF SEDIMENT TRANSPORT IN ALLUVIAL CHANNELS. / Maddock, Thomas.

J. HYDRAUL. DIV., ASCE. Vol. 99 , HY11 1973.

Research output: Chapter in Book/Report/Conference proceedingChapter

Maddock, T 1973, A ROLE OF SEDIMENT TRANSPORT IN ALLUVIAL CHANNELS. in J. HYDRAUL. DIV., ASCE. vol. 99 , HY11.
Maddock T. A ROLE OF SEDIMENT TRANSPORT IN ALLUVIAL CHANNELS. In J. HYDRAUL. DIV., ASCE. Vol. 99 , HY11. 1973
Maddock, Thomas. / A ROLE OF SEDIMENT TRANSPORT IN ALLUVIAL CHANNELS. J. HYDRAUL. DIV., ASCE. Vol. 99 , HY11 1973.
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