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(Proceedings of the 23rd Binghamton Symposium in geomorphology en Anglais - 1992)

Document title

The morphology of graded gravel rivers : a network perspective

published at : Special issue : Geomorphic systems

Authors(s) and Affiliation(s)

PIZZUTO J. E. ;

Abstract

Analytical hydraulic geometry equations are combined with a watershed model to quantify downstream trends in equilibrium fluvial morphology in gravel streams. The hydraulic geometry equations relate fluvial morphology to discharge, bedload transport rate and grain size; these independent variables are in turn determined by routing gravel supplied at zero-order basins through a channel network. The resulting model specifies the discharge, bedload transport rate, grain size, width, depth, slope and river bed elevation at every point in the drainage basin

Source

Congrès

Proceedings of the 23rd Binghamton Symposium in geomorphology , INCONNU (25/09/1992 - 27/09/1992)

published at : Geomorphology / ISSN 0169-555X

Editor : Elsevier, Amsterdam - PAYS-BAS (1987)

Millesime : 1992, vol. 5, no 3-5 [pp. 457-474]

Bibliographic references : 87 réf.

Language

Anglais

INIST-CNRS, Cote INIST : 21151

Tous droits réservés © Prodig - Bibliographie Géographique Internationale (BGI), 1993.
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