3 m L M Z 3.3 m W1 d 10 m W2 F P K Y 4 m

Q: A gravity dam made of concrete is shown in Figure 2. Consider hydrostatic uplift and water at normal…

A:

Q: A couple M of moment 8 kN·m acting in a vertical plane is applied to a W200 * 19.3 rolled-steel beam…

A: Given section - W200 x 19.3 rolled steel  beam M = 8kN.m

Q: A beam-spring system is shown L = 5m EI-2.5 × 10³ kN-m² figure below. heee 000 k = 40 kN m-10 kN k=…

A: For given spring-beam system,Initial displacement of 5 mmInitial velocity: 135 mm/sto find the…

Q: THE CONCRETE DAM SHOWN WEIGHS 23.6 Kn/m' AND REST ON A SOLID FOUNDATION. DETERM THE MAXIMUM…

A:

Q: Find effective stress at A and determine the stability of cut under given condition. (ii) What…

A: Calculation of soil mechanics problemPart i) effective stress at A and…

Q: An embankment load on a silty clay soil layer as shown below. Determine the stress increase under…

A:

Q: The beam shown has a rectangular cross section with a depth h = 240 mm. Determine the width b of the…

A: It is required to find the width of the beam.

Q: PROBLEM 1: The homogeneous structure shown weighs 21.45 kN per square meter of cross-section. The…

A: Weight of cross section (y) = 21.45 KN/m2Determinea. The equivalent force of uniform load P1.b.…

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.