Polymer Flow Through Porous Media: Numerical Prediction of the Contribution of Slip to the Apparent Viscosity

被引:0
|
作者
F. Zami-Pierre
R. de Loubens
M. Quintard
Y. Davit
机构
[1] Université de Toulouse,Institut de Mécanique des Fluides de Toulouse (IMFT)
[2] CNRS,undefined
[3] INPT,undefined
[4] UPS,undefined
[5] Total,undefined
[6] CSTJF,undefined
来源
Transport in Porous Media | 2017年 / 119卷
关键词
Porous media; Polymer; Apparent slip; Apparent viscosity;
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中图分类号
学科分类号
摘要
The flow of polymer solutions in porous media is often described using Darcy’s law with an apparent viscosity capturing the observed thinning or thickening effects. While the macroscale form is well accepted, the fundamentals of the pore-scale mechanisms, their link with the apparent viscosity, and their relative influence are still a matter of debate. Besides the complex effects associated with the rheology of the bulk fluid, the flow is also deeply influenced by the mechanisms occurring close to the solid/liquid interface, where polymer molecules can arrange and interact in a complex manner. In this paper, we focus on a repulsive mechanism, where polymer molecules are pushed away from the interface, yielding a so-called depletion layer in the vicinity of the wall. This depletion layer acts as a lubricating film that may be represented by an effective slip boundary condition. Here, our goal is to provide a simple mean to evaluate the contribution of this slip effect to the apparent viscosity. To do so, we solve the pore-scale flow numerically in idealized porous media with a slip length evaluated analytically in a tube. Besides its simplicity, the advantage of our approach is also that it captures relatively well the apparent viscosity obtained from core-flood experiments, using only a limited number of inputs. Therefore, it may be useful in many applications to rapidly estimate the influence of the depletion layer effect over the macroscale flow and its relative contribution compared to other phenomena, such as non-Newtonian effects.
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页码:521 / 538
页数:17
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