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纳米级狭缝孔隙中的水和二氧化碳毛细管桥:温度、压力和盐浓度对水接触角的影响

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

作者信息

Prado Camargo Arthur, Jusufi Arben, Lee Alex Gk, Koplik Joel, Morris Jeffrey F, Giovambattista Nicolas

机构信息

Instituto de Física, Universidade de São Paulo, 05508-090 Sao Paulo, SP, Brasil.

ExxonMobil Technology and Engineering Company, 1545 US Rt. 22 East, Annandale, New Jersey 08801, United States.

出版信息

Langmuir. 2024 Sep 3;40(35):18439-18450. doi: 10.1021/acs.langmuir.4c01185. Epub 2024 Aug 19.

DOI:10.1021/acs.langmuir.4c01185
PMID:39158401
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC11375785/
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 ( = 280-400 K and carbon dioxide pressures ≈ 0-80 MPa). The water-carbon dioxide system is confined by two parallel silica-based surfaces (hydroxylated β-cristobalite) separated by = 5 nm. The aim of this work is to study the WCB contact angle (θ) as a function of and . Our simulations indicate that θ varies weakly with temperature and pressure: Δθ ≈ 10-20° for increasing from ≈0 to 80 MPa ( = 320 K); Δθ ≈ -10° for 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. It is found that at the salt concentrations studied (mole fractions = = 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 being insensitive to the presence of NaCl.

摘要

我们对纳米级水毛细管桥(WCB)进行了分子动力学(MD)模拟,该水毛细管桥被二氧化碳包围,模拟的温度和压力范围很广(温度(T = 280 - 400K),二氧化碳压力(p_{CO_2}≈0 - 80MPa))。水 - 二氧化碳系统被两个平行的二氧化硅基表面(羟基化β - 方石英)所限制,这两个表面之间的距离(d = 5nm)。这项工作的目的是研究WCB接触角((\theta))随温度(T)和压力(p_{CO_2})的变化情况。我们的模拟表明,(\theta)随温度和压力的变化较弱:当(p_{CO_2})从约(0MPa)增加到(80MPa)((T = 320K))时,(\Delta\theta≈10 - 20°);当(T)从(320K)增加到(360K)(二氧化碳量固定)时,(\Delta\theta≈ - 10°)。有趣的是,在所有研究的条件下,在二氧化碳体积下方会形成一层薄水膜(1 - 2个水层厚)。我们的MD模拟表明,这是由于相对于二氧化碳,水与壁面形成氢键的能力增强。我们还研究了向WCB中添加盐(NaCl)及其对相应(\theta)的影响。发现在所研究的盐浓度下(摩尔分数(x_{NaCl}=x_{Na^ +}=x_{Cl^ -}=3.50),(9.81%)),NaCl在WCB内形成大晶粒,离子避开了水 - 二氧化碳界面和壁面表面。这导致(\theta)对NaCl的存在不敏感。

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本文引用的文献

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Langmuir. 2020 Jul 7;36(26):7246-7251. doi: 10.1021/acs.langmuir.0c00549. Epub 2020 Jun 17.
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Wettability of rock/CO/brine and rock/oil/CO-enriched-brine systems:Critical parametric analysis and future outlook.岩石/二氧化碳/盐水和岩石/油/富二氧化碳盐水体系的润湿性:关键参数分析与未来展望
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一氧化碳-水-二氧化硅体系中动态接触角的原子研究
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Measurement and estimation of CO-brine interfacial tension and rock wettability under CO sub- and super-critical conditions.在 CO 亚临界和超临界条件下测量和估计 CO-盐水界面张力和岩石润湿性。
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In Situ Local Contact Angle Measurement in a CO-Brine-Sand System Using Microfocused X-ray CT.使用微焦点 X 射线 CT 在 CO-盐水-砂系统中进行原位局部接触角测量。
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Molecular Dynamics Simulations of CO2/Water/Quartz Interfacial Properties: Impact of CO2 Dissolution in Water.二氧化碳/水/石英界面性质的分子动力学模拟:二氧化碳在水中溶解的影响
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