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The hydraulics of flow in the irrigation and drainage channels is indeed complex for many reasons in natural conditions. Such channels are required to carry a certain specified discharge of water which is charged with sediment load of suspended and bed material. The boundaries of the channel are thus in a state of constant flux. Bed and banks, although initially flat surfaces, may soon be covered with ripples and dunes. These are in effect large elements of surface roughness having a strong influence on the overall channel friction. Stability of these channels is defined as a state of equilibrium such that the particles on the surface of such channels are in a critical condition of movement. A channel shape which ensures that the particles everywhere on the channel surface are subjected to a resultant boundary stress which equals the critical shear stress is a stable profile. When the capacity for transporting sediment of a channel is equal to the time rate of sediment supply at its he
Title: IRRIGATION AND DRAINAGE MANAGEMENT
Publisher: STUDIUM PRESS (INDIA) PVT.LTD.
Publication Date: 2012
Condition: New
Seller: Majestic Books, Hounslow, United Kingdom
Condition: New. pp. 402. Seller Inventory # 96295649
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Condition: New. pp. 402. Seller Inventory # 1897183028
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Paperback. Condition: Like New. Like New. book. Seller Inventory # ERICA77519336992806
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