Water and Carbon Dioxide Capillary Bridges in Nanoscale Slit Pores: Effects of Temperature, Pressure, and Salt Concentration on the Water Contact Angle

We perform molecular dynamics (MD) simulations of a nanoscale water capillary bridge (WCB) surrounded by carbon dioxide over a wide range of temperatures and pressures (<i>T</i> = 280-400 K and carbon dioxide pressures <mml:math xmlns:mml="http://www.w3.org/1998/Math/MathML"><mml:msub><mml:mrow><mml:mi>P</mml:mi></mml:mrow><mml:mrow><mml:msub><mml:mrow><mml:mi>CO</mml:mi></mml:mrow><mml:mrow><mml:mn>2</mml:mn></mml:mrow></mml:msub></mml:mrow></mml:msub></mml:math> ≈ 0-80 MPa). The water-carbon dioxide system is confined by two parallel silica-based surfaces (hydroxylated β-cristobalite) separated by <i>h</i> = 5 nm. The aim of this work is to study the WCB contact angle (θ<sub>c</sub>) as a function of <i>T</i> and <mml:math xmlns:mml="http://www.w3.org/1998/Math/MathML"><mml:msub><mml:mrow><mml:mi>P</mml:mi></mml:mrow><mml:mrow><mml:msub><mml:mrow><mml:mi>CO</mml:mi></mml:mrow><mml:mrow><mml:mn>2</mml:mn></mml:mrow></mml:msub></mml:mrow></mml:msub></mml:math>. Our simulations indicate that θ<sub>c</sub> varies weakly with temperature and pressure: Δθ<sub>c</sub> ≈ 10-20° for <mml:math xmlns:mml="http://www.w3.org/1998/Math/MathML"><mml:msub><mml:mrow><mml:mi>P</mml:mi></mml:mrow><mml:mrow><mml:msub><mml:mrow><mml:mi>CO</mml:mi></mml:mrow><mml:mrow><mml:mn>2</mml:mn></mml:mrow></mml:msub></mml:mrow></mml:msub></mml:math> increasing from ≈0 to 80 MPa (<i>T</i> = 320 K); Δθ<sub>c</sub> ≈ -10° for <i>T</i> increasing from 320 to 360 K (with a fixed amount of carbon dioxide). Interestingly, at all conditions studied, a thin film of water (1-2 water layers-thick) forms under the carbon dioxide volume. Our MD simulations suggest that this is due to the enhanced ability of water, relative to carbon dioxide, to form hydrogen-bonds with the walls. We also study the effects of adding salt (NaCl) to the WCB and corresponding θ<sub>c</sub>. It is found that at the salt concentrations studied (mole fractions <i>x</i><sub>Na</sub> = <i>x</i><sub>Cl</sub> = 3.50, 9.81%), the NaCl forms a large crystallite within the WCB with the ions avoiding the water-carbon dioxide interface and the walls surface. This results in θ<sub>c</sub> being insensitive to the presence of NaCl.

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Journal
Langmuir
Published
2024-08-19
DOI
https://doi.org/10.1021/acs.langmuir.4c01185
Citations
6
Primary Topic
CO2 Sequestration and Geologic Interactions
Type
article
Field-Weighted Citation Impact
1.23

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article

Water and Carbon Dioxide Capillary Bridges in Nanoscale Slit Pores: Effects of Temperature, Pressure, and Salt Concentration on the Water Contact Angle

Jeffrey F. Morris, Arben Jusufi, Nicolás Giovambattista, Joel Koplik et al.
6 citations
Langmuir
CO2 Sequestration and Geologic Interactions
1.23
article

Water and Carbon Dioxide Capillary Bridges in Nanoscale Slit Pores: Effects of Temperature, Pressure, and Salt Concentration on the Water Contact Angle

Jeffrey F. Morris, Arben Jusufi, Nicolás Giovambattista, Joel Koplik, A. Camargo, Alex Gk Lee
article en
6 citations

Abstract

We perform molecular dynamics (MD) simulations of a nanoscale water capillary bridge (WCB) surrounded by carbon dioxide over a wide range of temperatures and pressures (<i>T</i> = 280-400 K and carbon dioxide pressures <mml:math xmlns:mml="http://www.w3.org/1998/Math/MathML"><mml:msub><mml:mrow><mml:mi>P</mml:mi></mml:mrow><mml:mrow><mml:msub><mml:mrow><mml:mi>CO</mml:mi></mml:mrow><mml:mrow><mml:mn>2</mml:mn></mml:mrow></mml:msub></mml:mrow></mml:msub></mml:math> ≈ 0-80 MPa). The water-carbon dioxide system is confined by two parallel silica-based surfaces (hydroxylated β-cristobalite) separated by <i>h</i> = 5 nm. The aim of this work is to study the WCB contact angle (θ<sub>c</sub>) as a function of <i>T</i> and <mml:math xmlns:mml="http://www.w3.org/1998/Math/MathML"><mml:msub><mml:mrow><mml:mi>P</mml:mi></mml:mrow><mml:mrow><mml:msub><mml:mrow><mml:mi>CO</mml:mi></mml:mrow><mml:mrow><mml:mn>2</mml:mn></mml:mrow></mml:msub></mml:mrow></mml:msub></mml:math>. Our simulations indicate that θ<sub>c</sub> varies weakly with temperature and pressure: Δθ<sub>c</sub> ≈ 10-20° for <mml:math xmlns:mml="http://www.w3.org/1998/Math/MathML"><mml:msub><mml:mrow><mml:mi>P</mml:mi></mml:mrow><mml:mrow><mml:msub><mml:mrow><mml:mi>CO</mml:mi></mml:mrow><mml:mrow><mml:mn>2</mml:mn></mml:mrow></mml:msub></mml:mrow></mml:msub></mml:math> increasing from ≈0 to 80 MPa (<i>T</i> = 320 K); Δθ<sub>c</sub> ≈ -10° for <i>T</i> increasing from 320 to 360 K (with a fixed amount of carbon dioxide). Interestingly, at all conditions studied, a thin film of water (1-2 water layers-thick) forms under the carbon dioxide volume. Our MD simulations suggest that this is due to the enhanced ability of water, relative to carbon dioxide, to form hydrogen-bonds with the walls. We also study the effects of adding salt (NaCl) to the WCB and corresponding θ<sub>c</sub>. It is found that at the salt concentrations studied (mole fractions <i>x</i><sub>Na</sub> = <i>x</i><sub>Cl</sub> = 3.50, 9.81%), the NaCl forms a large crystallite within the WCB with the ions avoiding the water-carbon dioxide interface and the walls surface. This results in θ<sub>c</sub> being insensitive to the presence of NaCl.

LangmuirVol. 40(35)
The Graduate Center, CUNY (US), City College of New York (US), City University of New York (US), Universidade de São Paulo (BR), Brooklyn College (US), ExxonMobil (United States) (US)
ExxonMobil Research and Engineering Company, Division of Chemistry, Division of Human Resource Development
Clean water and sanitation
Openalex Percentile: Top 23%
CO2 Sequestration and Geologic Interactions
1.23
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