IAHR, founded in 1935, is a worldwide independent member-based organisation of engineers and water specialists working in fields related to the hydro-environmental sciences and their practical application. Activities range from river and maritime hydraulics to water resources development and eco-hydraulics, through to ice engineering, hydroinformatics, and hydraulic machinery.
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You are here : eLibrary : IAHR World Congress Proceedings : 35th IAHR Congress - Chengdu (2013) : THEME 1 - KEYNOTE AND INVITED LECTURES : River Self-Formation and Regime Channel Geometry in the Light of Thermodynamic Principles
River Self-Formation and Regime Channel Geometry in the Light of Thermodynamic Principles
Author : Ana Maria Ferreira da Silva
The process of self-formation of alluvial streams is considered in the light of the first and second laws of thermodynamics, and the Gibb?s equation. The stream is treated as an isolated and irreversible system. The related energy-analysis of a self-forming alluvium stream suggests that river self-formation is derived from the need of a stream to progressively decrease its average flow velocity to accommodate the increase in the entropy of the system with the passage of time. The regime development thus appears as the process in which the river alters its configuration (cross-sectional geometry, slope and effective roughness) so that the smallest possible value of average flow velocity (or, equivalently, of the Froude number) is reached. A method for the computation of regime flow width, depth and slope, based on the channel formation criterion resulting from this work, is presented. The regime channels computed from this method are compared with field and laboratory data from various sources.
File Size : 447,169 bytes
File Type : Adobe Acrobat Document
Chapter : IAHR World Congress Proceedings
Category : 35th IAHR Congress - Chengdu (2013)
Article : THEME 1 - KEYNOTE AND INVITED LECTURES
Date Published : 18/07/2016
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