n= 2 (b)

Q: (Flowrate) Water flows through the rectangular channel shown in the figure below with a uniform…

A: a)b)

Q: 8- Water flows through a horizontal reducing bend shown in Figure 3 below at an unknown bend angle,…

A:

Q: m Water is flowing through a horizontal pipe of diameter 150mm at a velocity of 2-. A circular solid…

A: Given:Pipe diameter, D = 150 mm = 0.15 mVelocity of flow, V = 2 m/sDiameter of solid plate, d = 120…

Q: Use the Cauchy-Reiman Eq. and Darcy’s Law in terms of the discharge potential to prove that the Φ…

A:

Q: The velocity field for steady, incompressible, two-dimensional flow through a converging duct is:…

A: Given, Velocity, V = (U0 + bx)i - by  where, U0 and b are constants to determine streamline equation…

Q: The flow through a rectangular channel (width in x and height in z) is nonuniform with a velocit…

A: We have to determine the expression for flow rate and average velocity using contants and we have to…

Q: A sluice gate, as shown in figure 01, is used to control the upstream water level in a 3 m wide…

A:

Q: The flow through a rectangular channel (width in x and height in z) is nonuniform with a velocity…

A:

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.