Thank u Q.22A field pumping test was conducted from an aquifer of sandy soil of 4 m thickness confinedbetween two impervious strata. When equilibrium was established, 90 liters of water was pumpedObservation wellsApTest wellme.7= 6mImpermeable stratum= 3 mh = 2.7 mh, = 2.1 mConfined aquiferH, = 4 mImpermeableout per hour. The water elevation in an observation well 3.0 m away from the test well was 2.1 mand another 6.0 m away was 2.7 m from the roof level of the impervious stratum of the aquifer. Findthe value of k of the soil in m/sec. (

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Q.22 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 Ap Test well Ime ち=6m Impermeable stratum = 3 m hz = 2.7 m h, = 2.1 m Confined aquifer H, = 4 m Impermeable 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. (

Q.22 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 Ap Test well Ime ち=6m Impermeable stratum = 3 m hz = 2.7 m h, = 2.1 m Confined aquifer H, = 4 m Impermeable 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. (

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 6.15P

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