Receding and advancing (CO2 + brine + quartz) contact angles as a function of pressure, temperature, surface roughness, salt type and salinity
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- 作者：Ahmed Z. Al-Yaseria ; a.al-yaseri@postgrad.curtin.edu.au" class="auth_mail" title="E-mail the corresponding author ; Maxim Lebedevb ; m.lebedev@curtin.edu.au" class="auth_mail" title="E-mail the corresponding author ; Ahmed Barifcanic ; a.barifcani@curtin.edu.au" class="auth_mail" title="E-mail the corresponding author ; Stefan Iglauera ; stefan.iglauer@curtin.edu.au" class="auth_mail" title="E-mail the corresponding author
- 关键词：Carbon geo-sequestration ; Contact angle ; Quartz ; Surface roughness ; Brine salinities ; Carbon dioxide ; Residual trapping ; Structural trapping
- 刊名：Journal of Chemical Thermodynamics
- 出版年：2016
- 出版时间：February 2016
- 年：2016
- 卷：93
- 期：Complete
- 页码：416-423
- 全文大小：2335 K
文摘
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(Water + CO2) contact angle on quartz increases substantially with pressure and salinity.
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(Water + CO2) contact angle on quartz increases slightly with temperature.
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Surface roughness has only a minor influence on (water + CO2 + quartz) contact angles.