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Experiments on gravitational phase separation of binary immiscible fluids

Published online by Cambridge University Press:  30 October 2007

MISUZU SATO  and
IKURO SUMITA
MISUZU SATO
Affiliation:
Division of Earth & Environmental Sciences, Graduate School of Natural Sciences and Technology, Kanazawa University, Kanazawa 920-1192, Japan
IKURO SUMITA
Affiliation:
Division of Earth & Environmental Sciences, Graduate School of Natural Sciences and Technology, Kanazawa University, Kanazawa 920-1192, Japan
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Abstract

We conduct experiments on gravitational phase separation of binary immiscible fluids using an oil–water mixture and study how the volumetric and viscosity ratios of the two phases control the separation process. First, we change the volumetric fraction of the two phases. We find that the initial phase separation rate depends strongly on the volumetric ratio of the two phases, and can be modelled by a buoyancy-driven permeable flow using the Blake–Kozeny–Carman permeability formula. Next, we change the viscosity ratios of the two fluids, and we find that there are two distinct regimes with different styles of phase separation. Small viscosity ratio (<100) cases are characterized by a sharp lower boundary and a vertically homogeneous mixture layer. On the other hand, high viscosity ratio (>100) cases are characterized by a diffuse lower boundary and a large vertical gradient of porosity. A polyhedral foam structure develops at the top of the mixture layer which is slow to rupture and to transform into a uniform oil layer. These differences can be interpreted to arise from a faster coalescence rate relative to the separation rate at high viscosity ratios. We simultaneously measured electrical resistivity in order to monitor the temporal change of the mean porosity in the mixture layer. The measurements were found to be consistent with the visual observation.

Type
Papers
Information
Journal of Fluid Mechanics , Volume 591 , 25 November 2007 , pp. 289 - 319
Copyright
Copyright © Cambridge University Press 2007

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