In a homogeneous unconfined aquifer of area $3.00 \mathrm{~km}^{2},$ the water table was at an elevation of $102.00 \mathrm{~m}$. After a natural recharge of volume 0.90 million cubic meter $\left(\mathrm{Mm}^{3}\right),$ the water table rose to $103.20 \mathrm{~m}$. After this recharge, ground water pumping took place and the water table dropped down to $101.20 \mathrm{~m}$. The volume of ground water pumped after the natural recharge, expressed (in $\mathrm{Mm}^{3}$ and round off to two decimal places), is

Question ID - 157151 | SaraNextGen Top Answer

In a homogeneous unconfined aquifer of area $3.00 \mathrm{~km}^{2},$ the water table was at an elevation of $102.00 \mathrm{~m}$. After a natural recharge of volume 0.90 million cubic meter $\left(\mathrm{Mm}^{3}\right),$ the water table rose to $103.20 \mathrm{~m}$. After this recharge, ground water pumping took place and the water table dropped down to $101.20 \mathrm{~m}$. The volume of ground water pumped after the natural recharge, expressed (in $\mathrm{Mm}^{3}$ and round off to two decimal places), is