The variation of fluid pressure with height is described by the differential equation dP -pg dz Here, p is the specific density and g is the local acceleration of gravity. For an idea gas, MW(P) , where MW is the molar mass and R is the universal gas constant. Modeling RT the atmosphere as an isothermal column of ideal gas at 10 °C, estimate the ambient pressure, in atmosphere in Denver, where z = 1 mile relative to sea level. For air, take MW = 28.84 g/mole. %3D

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