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Wenhui Li

Researcher at University of Alberta

Publications -  18
Citations -  358

Wenhui Li is an academic researcher from University of Alberta. The author has contributed to research in topics: Chemistry & Medicine. The author has an hindex of 7, co-authored 13 publications receiving 167 citations.

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Smart mobility control agent for enhanced oil recovery during CO2 flooding in ultra-low permeability reservoirs

TL;DR: In this paper, a CO2-responsive smart mobility control system to generate bulk gel by wormlike micelles (WLMs) to mitigate gas channeling has great potentials for enhanced oil recovery in ultra-low permeability reservoirs.
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Slip length of methane flow under shale reservoir conditions: Effect of pore size and pressure

TL;DR: In this article, a molecular simulation study of methane flow in organic nanopores under shale reservoir conditions (temperature: 300-450 K, pressure: 10-60 MPa), with pore sizes ranging from 2 to 20nm, was performed.
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Molecular dynamics simulations of natural gas-water interfacial tensions over wide range of pressures

Wenhui Li, +1 more
- 15 Jan 2019 - 
TL;DR: In this article, the authors used molecular dynamics simulations to study hydrocarbon-water interfacial tension up to 5000 bar at various temperature conditions, and they found that IFTs decrease with increasing temperature at low pressure conditions, while the differences become insignificant at high pressures.
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CO2 solubility in brine in silica nanopores in relation to geological CO2 sequestration in tight formations: Effect of salinity and pH

TL;DR: In this article, the effects of salinity and pH on CO2 solubility in brine in silica nanopores under typical geological conditions (353 k and 175 k) were studied.
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Hydrophilicity/hydrophobicity driven CO2 solubility in kaolinite nanopores in relation to carbon sequestration

TL;DR: In this paper, the effects of surface characteristics on CO2 solubility under nano-confinement by deploying kaolinite nanopores as a model under typical geological conditions (373 k and up to 400 k).