1887

Abstract

The fluid system under considerations in this paper consists of three chemical components. The phase properties of this system depends on its composition and we assume that a maximum of two phases can be formed. The mathematical model governs the purely convective transport of this fluid system through a one dimensional homogeneous porous medium. The model is discussed through mathematical analysis and numerical experiments.

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/content/papers/10.3997/2214-4609.201411118
1990-09-11
2024-12-05
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