able values of specific storage, barometric increment in the aquifer, V a is the total volume efficiency, porosity, and matrix bulk modulus were of that increment, V m is the volume of the solid calculated, but the accuracy of these values is portion, and V w is the volume of the pore space. limited by the imprecise measurements of water level and barometric pressure and the possibility of leakage from imperfectly confined aquifers.
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