A bore is a hydraulic jump that propagates upstream into astill or slower-moving fluid, as in Fig.  on theSée-Sélune channel, near Mont Saint Michel in northwestFrance. The bore is moving at about 10 ft/s and is about onefoot high. Estimate (a) the depth of the water in this areaand (b) the velocity induced by the wave.

Q: A hydraulic jump is formed in a 2 m wide rectangular channel which is horizontal and frictionless.…

A: A wide rectangular channel- Width of the channel b=2 m, Post jump depth y2=0.8 m/s, Post jump…

Q: Q2) A progressive wave of period T-8 sec is travelling at a water depth of d=19 m. The equation of…

A: Progressive period T= 8 secwater depth d= 19 mSWL equation =need to find1- equation for wave profile…

Q: An abrupt rise of 1m was designed to control a hydraulic jump generated after a 5 m wide sluice gate…

A: Abrupt rise = 1 mWidth of sluice gate = 5 mOpening = 0.25 mFlow discharge = Flow depth = 1.25 mTo…

Q: A rectangular channel 3.7m wide conveys7.4m3/s of water at a depth of 300mm.If a hydraulic jump…

A:

Q: 5- An abrupt rise of 0.8 m was designed to control a hydraulic jump generated after a 4 m wide…

A: Abrupt rise = 0.8 mWidth of sluice gate = 4 mOpening = 0.2 mFlow discharge = Flow depth = 1.2 mTo…

Q: Route an overland flow hydrograph over a distance of 500 m using the analytical kinematic wave…

A: L = Distance = 500 m, b = Width = 75 m, So = Slope = 0.006, n = Mannings constant = 0.014 ,…

Q: 9. Normal depth occurs only for a uniform and steady flow. a) True b) False

A: Normal depth occurs only for a uniform and steady flow. a) True b) False

Q: 4.34 In the region just downstream of a sluice gate, the water may develop a reverse flow region as…

A:

Q: Determine the maximum horizontal and vertical velocity at a depth of 2.0m for a wave with the…

A: Wave period Wave height Water depth Depth of interest

Sediment transport

Sediment transport or Soil transport is the movement of solid particles, usually due to the combination of gravitational forces acting on the sediment, and the movement of the liquid at which the sediment enters. Soil erosion occurs in natural systems where the particles are sandstones (sand, rocks), mud, or clay; the liquid is air, water, or ice; and the gravitational force that works to move particles to the landing surface. Sediment transportation or soil migration due to the movement of liquids occurs in rivers, lakes, lakes, oceans, and other bodies of water as a result of currents and waves. Transportation is also caused by glaciers as they flow, and to places on earth under the influence of wind. Soil erosion due to gravity alone is possible in most sloping areas, including hills, scarves, cliffs, and the continental shelf — the continental boundary of the slope.