TWO PIEZOMETERS HAVE BEEN PLACED A LONG THE DIRECTION OF FLOW INA CONFINED AGUIFER THAT 13 30 m THICK. APART. THE DIFFERENCE IN PIEZOMETER HEAD IS 4.4 m ASSLMING THAT THE ACGDIFER IS ALMSIT MADE OF FINE SAND, CALCULATE THE FOLLOVING THE PIEZOMETERS ARE 280 m. a) THE TRAVEL TIME OF IVATE FLOW BETWEEN THE PIEZOMETERS? b) THE DIJCHARGE?. 4 c) THE DARCY VELOCITY

Q: The result of the liquid limit tests where N is the no of blows and w is the water content in % are…

A: Given  Trial no. of blow (N) water content (w)% 1 11 53.9 2 15 50.6 3 23 48.1 4 30 46 5…

Q: 7.16 A layered soil is shown in Figure 7.34. Given that = 10cm/sec 2.8 X 10 cm/sc. • H, = 2 m k, =…

A:

Q: In an oedometer test on a saturated specimen (G,- 2.70, the initial thickness Ho-2.0cm), when the…

A: According to given data In an oedometer test on a saturated specimen (G,- 2.70, the initial…

Q: when flowing through the same rock at 20°C? want weight = 8.44 kN/m³) 6.10 The maximum dry unit…

A: Given data - Relative compaction = 90% Max. dry unit weight in lab = 16 KN/m3 Gs = 2.7 k1 = 0.03…

Q: 1. (30 pts) The soil profile shown below consists of 10 meters of sandy silt overlying gravel. The…

A: Step 1:Step 2: Step 3: Step 4:

Q: A dry granite rock weighs 26 N. When it was submerged for 24 hours, its weight increased to 30 N.…

A: Given data- Initial weight of the rock w1=26NFinal weight of the rock w2=30NTo Find-Absorption of…

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.