Example 4.7 A field pumping test was conducted from an aquifer of sandy soil of 4 m thickness confined between two impervious strata. When equilibrium was established, 90 liters of water was pumped Observation wells App Test well 129 net = 6m Impermeable stratum =3 m h, - 2.7 m h, =2.1 m H = 4 m Confined aquifer Impermeable Figure Ex. 4.7 MARCL DKER, INe. 270 Madison Avenue. New York. New York 10016 Copyright O Marcel Dekker, Inc. All rights reserved.

Principles of Geotechnical Engineering (MindTap Course List)
9th Edition
ISBN:9781305970939
Author:Braja M. Das, Khaled Sobhan
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Chapter7: Permeability
Section: Chapter Questions
Problem 7.22P: Refer to Figure 7.24. The following data were collected during the field permeability measurement of...
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Example 4.7
A field pumping test was conducted from an aquifer of sandy soil of 4 m thickness confined
between two impervious strata. When equilibrium was established, 90 liters of water was pumped
Observation wells
Test well
129
net
=6m
Impermeable stratum
= 3 m
hy = 2.7 m
h, = 2.1 m
H, = 4 m
Confined aquifer
Impermeable
Figure Ex. 4.7
MARCEL. DEKER, INC.
270 Madison Avenue. New York. New York 10016
Soil Permeability and Seepage
109
out per hour. The water elevation in an observation well 3.0 m away from the test well was 2.1 m
and another 6.0 m away was 2.7 m from the roof level of the impervious stratum of the aquifer. Find
the value of k of the soil in m/sec. (Fig. Ex. 4.7)
Copyright O Marcel Dekker, Inc. All rights reserved.
Transcribed Image Text:Example 4.7 A field pumping test was conducted from an aquifer of sandy soil of 4 m thickness confined between two impervious strata. When equilibrium was established, 90 liters of water was pumped Observation wells Test well 129 net =6m Impermeable stratum = 3 m hy = 2.7 m h, = 2.1 m H, = 4 m Confined aquifer Impermeable Figure Ex. 4.7 MARCEL. DEKER, INC. 270 Madison Avenue. New York. New York 10016 Soil Permeability and Seepage 109 out per hour. The water elevation in an observation well 3.0 m away from the test well was 2.1 m and another 6.0 m away was 2.7 m from the roof level of the impervious stratum of the aquifer. Find the value of k of the soil in m/sec. (Fig. Ex. 4.7) Copyright O Marcel Dekker, Inc. All rights reserved.
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