15. What would be the probable depth of flow of a river 100 m wide carrying 280 m³/s with a slope of 0.00028 and n = 0,040?

Q: wide rectangular channel dug from clean earth (n=0.024) is to conduct a flow of 15 m3/s per meter of…

A: n = 0.024 Q = 15m3/sec   It has been asked in the question to determine the depth of flow for normal…

Q: 27. A rectangular canal 2.24 m wide and 1.12 m deep has a full capacity of 8 m3/s. Assuming n =…

A:

Q: A concrete-lined drainage canal (ε = 0.08 in) is to be constructed to carry water at a maximum rate…

A: Given: Concrete-lined drainage canal Flow rate, Q = 105 GPM Cross-section of the channel =…

Q: A rectangular channel 22 feet wide carries a flow of 25,000 cfs on a slope of 0.01. Manning's n for…

A:

Q: A rectangular canal 2.24 m wide and 1.12 m deep has a full capacity of 8 m3/s. Assuming n = 0.0152…

A: A rectangular canal 2.24 m wide and 1.12 m deep has a full capacity of 8 m3/s. Assuming n = 0.0152…

Q: 1. Figure 2 shows a cross section of an improved river channel for flood protection. At what flow…

A: The Manning's n for the main channel =0.04 The Manning's n for the overbank = 0.06 The slope of the…

Q: A rectangular with a width of 3.54 and n= 0.0154 is to carry water at a flow rate of 13.54 m3/s…

A: The values given in the question are as follows:Width of the rectangular channel(B)=3.54 mmanning's…

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.