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Let ${\chi }_1(\mathbf{x},t)$ equal one in phase one and zero in phase two; its interface value is immaterial for area integrals. In the absence of phase change or interfacial mass transfer, the distributional phase mass conservation is ${\partial }_t({\chi }_1\rho )+\nabla \cdot ({\chi }_1\rho \mathbf{u})=0$. For a cross-section $S$ of area $A$, defineHere the symbol $u_x$ in the integral denotes the axial velocity component, not a derivative. Integrating through an arbitrary axial slice and using zero normal flux at the rigid pipe wall givesThe velocity is mass weighted, so the averaged mass flux factors exactly; an unweighted phase mean would not in general have this property. This is the cross-section averaged phase mass balance.

For phase two use ${\chi }_2=1-{\chi }_1$, volume fraction $1-\alpha$, andThen $\boxed{{\partial }_t[{\rho }_2(1-\alpha )]+{\partial }_x[{\rho }_2(1-\alpha )u_2]=0}$. Mean quantities in a phase that is absent are unnecessary; the products giving conserved masses and fluxes remain the meaningful variables.