Q-7 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 (Mm³), the water table rose to 103.20 m. After this recharge, ground water pumping took place and the water table dropped down to 101.20 m. The volume of ground water pumped after the natural recharge, expressed (in Mm³ and round off to two).

Structural Analysis
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Q-7 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 (Mm³), the water table rose to 103.20 m. After
this recharge, ground water pumping took place and the
water table dropped down to 101.20 m. The volume of
ground water pumped after the natural recharge,
expressed (in Mm³ and round off to two).
Transcribed Image Text:Q-7 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 (Mm³), the water table rose to 103.20 m. After this recharge, ground water pumping took place and the water table dropped down to 101.20 m. The volume of ground water pumped after the natural recharge, expressed (in Mm³ and round off to two).
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