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In a homogeneous unconfined aquifer of area 3.00 km², the water table was at an elevation of 102.00 m. A natural recharge of volume 0.90 million cubic meter (Mm²), the water table rose to 103.20 m. After this rech ground water pumping took place and the water table dropped down to 101.020 m. The volume of ground pumped after the natural recharge, expressed (in Mm² and round off to two decimal places), is

In a homogeneous unconfined aquifer of area 3.00 km², the water table was at an elevation of 102.00 m. A natural recharge of volume 0.90 million cubic meter (Mm²), the water table rose to 103.20 m. After this rech ground water pumping took place and the water table dropped down to 101.020 m. The volume of ground pumped after the natural recharge, expressed (in Mm² and round off to two decimal places), is

Structural Analysis
Structural Analysis
6th Edition
ISBN:9781337630931
Author:KASSIMALI, Aslam.
Publisher:KASSIMALI, Aslam.
Chapter2: Loads On Structures
Section: Chapter Questions
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In a homogeneous unconfined aquifer of area 3.00 km², the water table was at an elevation of 102.00 m. After a natural recharge of volume 0.90 million cubic meter (Mm²), the water table rose to 103.20 m. After this recharge, ground water pumping took place and the water table dropped down to 101.020 m. The volume of ground water pumped after the natural recharge, expressed (in Mm² and round off to two decimal places), is
Transcribed Image Text:In a homogeneous unconfined aquifer of area 3.00 km², the water table was at an elevation of 102.00 m. After a natural recharge of volume 0.90 million cubic meter (Mm²), the water table rose to 103.20 m. After this recharge, ground water pumping took place and the water table dropped down to 101.020 m. The volume of ground water pumped after the natural recharge, expressed (in Mm² and round off to two decimal places), is
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