17. Introduction to Open Channel Flow and Uniform Flow (Contnd.)
The chapter focuses on open channel flow and introduces the Manning's equation, emphasizing the relationship between flow velocity and hydraulic radius. It discusses the significance of Manning's resistance parameter and provides practical examples for calculating discharge, hydraulic radius, and other relevant parameters. Examples and exercises illustrate the application of the proposed equations in various scenarios.
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Sections
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What we have learnt
- Manning's equation represents the flow velocity in open channels in relation to hydraulic radius and slope.
- Various types of channels exhibit different Manning's resistance values, which are critical for calculations.
- Understanding how to calculate area, wetted perimeter, and other parameters is essential for determining flow rates in channels.
Key Concepts
- -- Manning's Equation
- An equation used to calculate the velocity of flow in open channels, expressed as V = (1/n) * R^(2/3) * S^(1/2), where V is the velocity, R is the hydraulic radius, S is the slope, and n is the Manning's coefficient.
- -- Hydraulic Radius
- The hydraulic radius (R) is the ratio of the cross-sectional area (A) of flow to the wetted perimeter (P), calculated as R = A/P.
- -- Manning's Resistance Parameter
- A coefficient that represents the roughness of the channel's surface affecting the flow rate; its value varies depending on the channel type.
- -- Reynolds Number
- A dimensionless number used to predict flow patterns in different fluid flow situations, expressed as Re = (R_h * V) / ν, where V is the flow velocity and ν is the kinematic viscosity of the fluid.
- -- Froude Number
- A dimensionless number that compares the flow inertial forces to gravitational forces, defined as Fr = V / √(g * y), where g is the acceleration due to gravity and y is the flow depth.
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