In a deposit of normally consolidated dry sand, a cone penetration test was conducted. Following are the results: Depth (m) Point resistance of cone, q. (MN/m²) 1.5 2.06 3.0 4.23 4.5 6.01 6.0 8.18 7.5 9.97 9.0 12.42 Assuming the dry unit weight of sand to be 16 kN/m², estimate the average peak friction angle, ø', of the sand. Use Eq. (3.53). 1 Pa D, = 0.5 305Q.OCR!8 Pa

Q: I. For the beams below, determine the location of the maximum deflection using double integration…

A:

Q: Q.12. The velocity distribution in the boundary layer is given by: 3 1 η n² F V 2 2 y In which n=…

A:

Q: Solve it By slope deflection method

A:

Q: By Double Integration, find the magnitude of the midspan deflection. Assume El is constant. 6W…

A: Given  W= 84

Q: For the beams below, determine the location of the maximum deflection using double integration…

A:

Q: A laminar boundary layer velocity profile is approximated by u/U= 2(y/6) -2(y/6) + (y/6) for y ≤ 6,…

A: In the velocity boundary layer, the flow velocity is distributed among different fluid layers…

Q: 200 KN wot E = 200 G Pa A = 20 cm² 10 m C

A: Displacement ∆=∑PkLAEwhere P=load in member due to applied loadk=force in member due to unit load…

Q: 2. Derive an equation that describes the vertical deflection of the beam, y(x), and also calculate…

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.