Core porosity from weights: Pore volume comes from {(saturated weight in air - dry weight in air)}/$\rho_f$. Bulk volume comes from {(saturated weight in air - immersed weight)}/$\rho_f$. Then $\phi = V_p/V_b$.
A piece of granite floats at the interface of mercury and water. If the densities of granite, water and mercury are \( \rho, \rho_1, \rho_2 \) respectively, the ratio of volume of granite in water to that in mercury is 
