8.11 It takes a certain length of time for the liquid level in a tank of diameter D to drop from position h, to position h, as the tank is being drained through an orifice

Q: m-Ø orifice is on the vertical side of a closed tank. The tank rests on a flat ground and the…

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Q: 4-61. Oil flows into the mixing tank through pipe A at 0.05 m/s, and glycerin flows into the tank…

A: To find the average density-

Q: graphs four particles in s shown in Fig. P4.10. The Ar 0.002 s. The location the photos, are shown…

A: Given:-∆t=0.002secTo find:-fluid velocity

Q: diameter = 60 cm height = 60 cm The open cylindrical tank is two-thirds full of water.…

A: H=0.4m R=60/2 R=30cm

Q: 1. A cylindrical tank, 1.5m inside diameter has an orifice at its side 0.25m above the bottom. If…

A: Reference : Water resources, Orifices.Given :Diameter of orifice, height of water.To determine :1.…

Q: A tank initially contains 100 gallons of brine in which there is dissolved 20 lb of salt. Starting…

A:

Q: 2.74 A tank of cross-sectional area A is filled with a liquid of specific weight y₁ as shown in Fig.…

A:

Q: An oil of density 892 kg/m³ is flowing in a pipe having an internal diameter 5cm. This pipe is…

A:

Q: t’s required to determine the height (H) when the flow is 120 L/s ؟

A: Flow rate Q = 120 L/s Area A = π4*0.252 = 0.049 m2  V = 1200.049 = 2.45 m/s Calculation of 'Re'  Re…

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.