Simple Vertical Drop Type, Sarda Type Falls, Straight Glacis Falls, Montague Type Falls, Inglis Falls, Baffle Falls


  • Simple Vertical Drop Type and Sarda Type Falls: A raised crest fall with a vertical impact was first of all introduced on Sarda Canal System in U.P., owing to its economy and simplicity. The necessity for economic falls arose because of the need of construction of a large number of smaller falls on the Sarda Canal System. In that area, a thin layer of sandy clay overlied a stratum of pure sand. If the canal bed was to be cut deep and up to the sand stratum, the seepage losses would have been tremendous. Hence, the depth of cutting had to be kept low, necessitating the construction of a large number of smaller falls.


  • In this type of a high crested fall, the nappe impinges into the water cushion below. There is no clear hydraulic jump and the energy dissipation is brought about by the turbulent diffusion, as the high velocity jet enters the deep pool of water downstream.

    Sarda type fall is a high crested fall, and if the discharge in the canal varies (say between 50 to 100%), the water will head up on the upstream side at low discharges. The reach upstream of the crest will silt up as the clearer water will pass downstream of the crest. Due to reduction in silt in the downstream discharge, there may be a tendency of scouring on d/s, so as to make the silt loss. Hence, this type of fall is not quite suitable for canals in which discharge varies within a wide range. A trapezoidal notch fall, although costlier than Sarda type or glacis type fall, is free from such troubles and, therefore, preferred for canals where the discharge is very small and also varies over a wide range.

    2.  Straight Glacis Falls: In this type of a modern fall, a 'straight glacis' (generally sloping 2 : 1) is provided after a 'raised crest'. The hydraulic jump is made to occur on the glacis, causing sufficient energy dissipation. This type of falls give very good performance if not flumed, although they may be flumed for economy. They are suitable up to 60 сumecs discharge and 1.5 m drop.


    3. Montague Type Falls: The energy dissipation on a straight glacis remain incomplete due to vertical component of velocity remaining unaffected. An improvement in energy dissipation may be brought about in this type of fall, by replacing the straight glacis by a parabolic glacis, commonly known as Montague Profile'.
    4.  Inglis Falls or Baffle Falls: A straight glacis type fall when added with a baffle platform and a baffle wall as shown in Fig. was developed by Inglis, and is called 'Inglis Fall' or Baffle Fall. They are quite suitable for all discharges and for drops of more than 1.5 m. They can be flumed easily as to affect economy. The baffle wall is provided at a calculated height and a calculated distance from the toe of the glacis, so as to ensure the formation of the jump on the baffle platform, as shown in Fig.












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