Experimental study of the immiscible displacement of shear-thinning fluids in pore networks
The pore scale mechanisms and network scale transient pattern of the immiscible displacement of a shear-thinning nonwetting oil phase (NWP) by a Newtonian wetting aqueous phase (WP) are investigated. Visualization imbibition experiments are performed on transparent glass-etched pore networks at a co...
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Veröffentlicht in: | Journal of colloid and interface science 2003-11, Vol.267 (1), p.217-232 |
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Format: | Artikel |
Sprache: | eng |
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Zusammenfassung: | The pore scale mechanisms and network scale transient pattern of the immiscible displacement of a shear-thinning nonwetting oil phase (NWP) by a Newtonian wetting aqueous phase (WP) are investigated. Visualization imbibition experiments are performed on transparent glass-etched pore networks at a constant unfavorable viscosity ratio and varying values of the capillary number (
Ca), and equilibrium contact angle (
θ
e
). Dispersions of ozokerite in paraffin oil are used as the shear-thinning NWP, and aqueous solutions of PEG colored with methylene blue are used as the Newtonian WP. At high
Ca values, the tip splitting and lateral spreading of WP viscous fingers are suppressed; at intermediate
Ca values, the primary viscous fingers expand laterally with the growth of smaller capillary fingers; at low
Ca values, network spanning clusters of capillary fingers separated by hydraulically conductive noninvaded zones of NWP arise. The spatial distribution of the mobility of shear-thinning NWP over the pore network is very broad. Pore network regions of low NWP mobility are invaded through a precursor advancement/swelling mechanism even at relatively high
Ca and
θ
e
values; this mechanism leads to irregular interfacial configurations and retention of a substantial amount of NWP along pore walls; it becomes the dominant mechanism in displacements performed at low
Ca and
θ
e
values. The residual NWP saturation increases and the end WP relative permeability decreases as
Ca increases and both become more sensitive to this parameter as the shear-thinning behavior strengthens. The shear-thinning NWP is primarily entrapped in individual pores of the network rather than in clusters of pores bypassed by the WP. At relatively high flow rates, the amplitude of the variations of pressure drop, caused by fluid redistribution in the pore network, increase with shear-thinning strengthening, whereas at low flow rates, the motion of stable and unstable menisci in pores is reflected in strong pressure drop fluctuations. |
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ISSN: | 0021-9797 1095-7103 |
DOI: | 10.1016/S0021-9797(03)00635-0 |