Mechanism of anomalously increased oil displacement with aqueous viscoelastic polymer solutionsElectronic supplementary information (ESI) available: Details of core flooding experiments, details of polymer solution preparation, details of microfluidic networks, PIV images and experimental detail expanding on Fig. 3, videos from which images of Fig. 4 were derived and solution rheology for materials in Fig. 4. See DOI: 10.1039/c5sm00064e
Single-phase flows of viscoelastic polymer solutions in both microfluidic devices and rock cores exhibit apparent flow thickening. We demonstrate that this thickening occurs above a critical Deborah number corresponding to the onset of spatio-temporal fluctuations. These fluctuations are observed to...
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description | Single-phase flows of viscoelastic polymer solutions in both microfluidic devices and rock cores exhibit apparent flow thickening. We demonstrate that this thickening occurs above a critical Deborah number corresponding to the onset of spatio-temporal fluctuations. These fluctuations are observed to occur over a broad range of spatial and temporal scales consistent with elastic turbulence. The fluctuations provide a previously unreported mechanism for enhancing the displacement of a second, capillary trapped, immiscible phase.
Flows of viscoelastic polymer solutions in porous media exhibit elastic turbulence that destabilises and displaces trapped oil. |
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Flows of viscoelastic polymer solutions in porous media exhibit elastic turbulence that destabilises and displaces trapped oil.</abstract><doi>10.1039/c5sm00064e</doi><tpages>6</tpages></addata></record> |
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title | Mechanism of anomalously increased oil displacement with aqueous viscoelastic polymer solutionsElectronic supplementary information (ESI) available: Details of core flooding experiments, details of polymer solution preparation, details of microfluidic networks, PIV images and experimental detail expanding on Fig. 3, videos from which images of Fig. 4 were derived and solution rheology for materials in Fig. 4. See DOI: 10.1039/c5sm00064e |
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