The figure shows the layers of soll in a tube that is 100mm by 150mm in cross-section. Water is supplied to maintain a constant head difference of 450mm across the sample. The hydraulic conductivity of the soils in the direction of flow through them are tabulated as shown. Compute the flow rate in cm:/hr. k = 2 x 10 cm/s K = 1.75 x 10 cm/s k = 3.7 x 10 cm/s K= 2.1 x 10" cm/s Water upply outfiow S0 mm A D 50 mm 200 200 200

Fundamentals of Geotechnical Engineering (MindTap Course List)
5th Edition
ISBN:9781305635180
Author:Braja M. Das, Nagaratnam Sivakugan
Publisher:Braja M. Das, Nagaratnam Sivakugan
Chapter6: Hydraulic Conductivity
Section: Chapter Questions
Problem 6.10P
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The figure shows the layers of soll in a tube that is 100mm by 150mm in
cross-section. Water is supplied to maintain a constant head difference of 450mm across the
sample. The hydraulic conductivity of the soils in the direction of flow through them are
tabulated as shown. Compute the flow rate in cm:/hr.
k = 2 x 10* cm/s
Kç = 1.75 x 10- cm/s
k = 3.7 x 10 cm/s
K= 2.1 x 10 cm/s
Water
upply
outfiow
50 mm
A
D.
50 mm
200
200
200
mm
Transcribed Image Text:The figure shows the layers of soll in a tube that is 100mm by 150mm in cross-section. Water is supplied to maintain a constant head difference of 450mm across the sample. The hydraulic conductivity of the soils in the direction of flow through them are tabulated as shown. Compute the flow rate in cm:/hr. k = 2 x 10* cm/s Kç = 1.75 x 10- cm/s k = 3.7 x 10 cm/s K= 2.1 x 10 cm/s Water upply outfiow 50 mm A D. 50 mm 200 200 200 mm
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