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Variation of U, with T, and z/Hdr Proposed fill y 19.2 kN/m3 3,0 m 0 Compressibility of Soil teh 2.0 Y -18.5 kN/m3-; 1.5m-U F

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Answer #1

Initial excess hydrostatic pressure is equal to Increase in effective stress due to fill i.e

u_{i}=\Delta \sigma =19.2\times 3

= 57.6 kN/m2

We know that

T_{v}=\frac{c_{v}t}{d^{2}}

where Tv = time factor

cv = 0.0021 m2/day

t = 2000 days

d = drainage path = 10/2 = 5 m

Putting values

Tv = 0.0021x2000/52

= 0.168

Degree of Consolidation (U) for point B is calculated from graph

For point B

z = 3 , H = 5

z/H = 0.6 and Tv = 0.168

We get

U = 0.31

Also

U = 1 - uz/ui

where uz = excess pore pressure remaining

ui = initial excess pore pressure = 57.6 kN/m2

0.31 = 1 - uz/57.6

uz = 39.744 kN/m2

Also pore pressure at point B = u = 9.81x5 = 49.05 kN/m2

There total pore pressure at point B after 2000 days = u + uz

= 49.05 + 39.744 = 88.794 kN/m2

  

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Variation of U, with T, and z/Hdr Proposed fill y 19.2 kN/m3 3,0 m 0 Compressibility of Soil teh 2.0 Y -18.5 kN/m3-; 1.5m-U Fine to medium sand (SP) 2.0 m 2 1.5 0.7 0.8 3.0 m 0.9 4.0m Soft clay (CL)...
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