Fowler A. Mathematical Geoscience

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850 E Averaged Equations in Two Phase Flow

Using conservation of mass again, deduce from the above that the energy

equation can ﬁnally be written in the form

ρS



∂

∂t





∂

∂x





=−



∂S

ds−Su

∂

∂x

(p+ρχ)−

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