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A 300 mm diameter test well penetrates 27 m below the static water table. After 24 hours of pumping at 69 liters/sec, the water level in an observation well at a distance of 95 m from the test well is lowered 0.5 m and the other observation well at a distance of 35 m from the test well, the drawdown is 1.1 m. Compute the transmissibility of the aquifer in m2/day. 1631.48 1745.90 O 1579.04 1507.52

A 300 mm diameter test well penetrates 27 m below the static water table. After 24 hours of pumping at 69 liters/sec, the water level in an observation well at a distance of 95 m from the test well is lowered 0.5 m and the other observation well at a distance of 35 m from the test well, the drawdown is 1.1 m. Compute the transmissibility of the aquifer in m2/day. 1631.48 1745.90 O 1579.04 1507.52

Structural Analysis
Structural Analysis
6th Edition
ISBN:9781337630931
Author:KASSIMALI, Aslam.
Publisher:KASSIMALI, Aslam.
Chapter2: Loads On Structures
Section: Chapter Questions
Problem 1P
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A 300 mm diameter test well penetrates 27 m below the static water table. After 24 hours of pumping at 69 liters/sec, the water level in an observation well at a distance of 95 m from the test well is lowered 0.5 m and the other observation well at a distance of 35 m from the test well, the drawdown is 1.1 m. Compute the transmissibility of the aquifer in m2/day. 1631.48 1745.90 1579.04 1507.52
Transcribed Image Text:A 300 mm diameter test well penetrates 27 m below the static water table. After 24 hours of pumping at 69 liters/sec, the water level in an observation well at a distance of 95 m from the test well is lowered 0.5 m and the other observation well at a distance of 35 m from the test well, the drawdown is 1.1 m. Compute the transmissibility of the aquifer in m2/day. 1631.48 1745.90 1579.04 1507.52
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