Filtration in Composite Incompressible Media

2013

Closed access Metadata (CSL-JSON)
DOI 10.2991/978-94-6239-015-7_5
Data confidence 70 medium
How this score is calculated

It is built from checkable properties of the record itself: whether the article has a DOI, how many independent sources confirmed its data, whether the required fields are filled in, and how recent the latest confirmation is. Disagreement between sources and a missing identifier lower it. A value of 80 or above means the record was published without further checking; 60 to 79 means it is published at reduced confidence, with a manual check advisable. A record verified by an editor by hand is never pushed below 90 by a recalculation. This scores our data about the article, not the article itself.

Abstract

This chapter is devoted to filtration from reservoirs into porous media under gravity, and filtration in poroelastic media with variable pore space structure. The second problem consists of two different settings and based on the problem for two different poroelastic media with a common boundary. In the first setting we consider an arbitrary partition $$\varPi ^{(\delta )}=\{K^{(\delta )}_{1},...,K^{(\delta )}_{N_{\delta }}\}$$ of the domain $$\varOmega $$ , where the structure of $$K^{(\delta )}_{j}$$ is defined by the characteristic function $$\chi ^{(\varepsilon ,\delta )}$$ , and pass to the limit as $$\varepsilon \rightarrow 0$$ . After that we pass to the limit as $$\delta \rightarrow 0$$ . In the second setting we consider the same partition, but firstly pass to the limit as $$\delta \rightarrow 0$$ and after that pass to the limit as $$\varepsilon \rightarrow 0$$ . In both cases we obtain the same result. As basic models at the microscopic level we consider mathematical models $$\mathbb {M}_{24}$$ and $$\mathbb {M}_{15}$$ . Here we will keep the same notation as in previous chapters.