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About Gradually-Varied Flow (GVF) AUTUMN 2020 3.1 Normal Flow Vs Gradually-Varied Flow
This document discusses gradually-varied flow, which occurs when the downslope component of weight does not locally balance bed friction, such as due to hydraulic structures or changes in channel properties. It derives the gradually-varied flow equation, which relates the rate of change of water depth along the channel to the difference between the geometric slope and friction slope. The friction slope can be estimated using Manning's equation under the quasi-uniform flow assumption. Flow profiles are classified based on the actual depth relative to the critical depth and normal depth. Backwater curves occur when depth increases downstream, drawdown curves when it decreases, and normal flow when the slopes are equal.
Detailed Information
| Author: | ['a'] |
|---|---|
| Publication Year: | 2021 |
| Pages: | 15 |
| Language: | English |
| Format: | |
| Price: | FREE |
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