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The document discusses supercritical and subcritical flow, which are flow regimes in geomorphology and fluid dynamics that affect water behavior in rivers and channels. Supercritical flow is fast and turbulent, leading to erosion and narrow channels, while subcritical flow is slower and more tranquil, promoting sediment deposition and wider channels. Additionally, it covers steady and uniform flow, as well as turbulent and laminar flow, highlighting their characteristics and implications for sediment transp

Author
mayangsushil758
Language
EN

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