Wetting transition and fluid trapping in a microfluidic fracture
Y Qiu, K Xu, AA Pahlavan… - Proceedings of the …, 2023 - National Acad Sciences
Immiscible fluid–fluid displacement in confined geometries is a fundamental process
occurring in many natural phenomena and technological applications, from geological CO2
sequestration to microfluidics. Due to the interactions between the fluids and the solid walls,
fluid invasion undergoes a wetting transition from complete displacement at low
displacement rates to leaving a film of the defending fluid on the confining surfaces at high
displacement rates. While most real surfaces are rough, fundamental questions remain …
occurring in many natural phenomena and technological applications, from geological CO2
sequestration to microfluidics. Due to the interactions between the fluids and the solid walls,
fluid invasion undergoes a wetting transition from complete displacement at low
displacement rates to leaving a film of the defending fluid on the confining surfaces at high
displacement rates. While most real surfaces are rough, fundamental questions remain …
Wetting transition and fluid trapping in a microfluidic fracture
Immiscible fluid–fluid displacement in confined geometries is a fundamental process
occurring in many natural phenomena and technological applications, from geological CO2
sequestration to microfluidics. Due to the interactions between the fluids and the solid walls,
fluid invasion undergoes a wetting transition from complete displacement at low
displacement rates to leaving a film of the defending fluid on the confining surfaces at high
displacement rates. While most real surfaces are rough, fundamental questions remain …
occurring in many natural phenomena and technological applications, from geological CO2
sequestration to microfluidics. Due to the interactions between the fluids and the solid walls,
fluid invasion undergoes a wetting transition from complete displacement at low
displacement rates to leaving a film of the defending fluid on the confining surfaces at high
displacement rates. While most real surfaces are rough, fundamental questions remain …
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