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Permeability evolution in sandstone due to injection of CO2-saturated brine or supercritical CO2 at reservoir conditions

机译：在储层条件下注入饱和二氧化碳或超临界二氧化碳会导致砂岩渗透率的变化

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Iglauer S.; Sarmadivaleh M.; Al-Yaseri A.; Lebedev M.;
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年度 2014
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1. Permeability and relative permeability measurements for CO2-brine system at reservoir conditions in low permeable sandstones in Svalbard [J] . Farokhpoor Raheleh, Lindeberg Erik Gosta Bruno, Torsaeter Ole, Greenhouse Gases. Science and Technology . 2014,第1期

机译：斯瓦尔巴特群岛低渗透性砂岩储层条件下CO2-盐水系统的渗透率和相对渗透率测量
2. Steady-state supercritical CO2 and brine relative permeability in Berea sandstone at different temperature and pressure conditions [J] . Chen Xiongyu, Gao Shuang, Kianinejad Amir, Water resources research . 2017,第7期

机译：不同温度和压力条件下Berea砂岩的稳态超临界CO2和盐水相对渗透率
3. The Impact of Reservoir Conditions and Rock Heterogeneity on CO2-Brine Multiphase Flow In Permeable Sandstone [J] . Krevor Samuel, Reynolds Catriona, Al-Menhali Ali, Petrophysics: The SPWLA Journal of Formation Evaluation and Reservoir Description . 2016,第1期

机译：储层条件和岩石非均质性对渗透性砂岩中CO2盐水多相流的影响
4. Permeability evolution in sandstone due to injection of CO2-saturated brine or supercritical CO2 at reservoir conditions [C] . S. Iglauer, M. Sarmadivaleh, A. Al-Yaseri International Conference on Greenhouse Gas Control Technologies . 2015

机译：储层条件下的二氧化碳饱和盐水或超临界CO2引起的砂岩渗透性进化
5. An experimental study of relative permeability hysteresis, capillary trapping characteristics, and capillary pressure of CO2/brine systems at reservoir conditions. [D] . Akbarabadi, Morteza. 2013

机译：储层条件下CO2 /盐水系统相对渗透率滞后，毛细管捕集特征和毛细管压力的实验研究。
6. Artificial Weathering as a Function of CO2 Injection in Pahang Sandstone Malaysia: Investigation of Dissolution Rate in Surficial Condition [O] . Madjid Jalilavi, Mansoor Zoveidavianpoor, Farshid Attarhamed, -1

机译：马来西亚彭亨砂岩的人工风化与二氧化碳注入的关系：表面条件下溶解速率的研究
7. Impact of Reservoir Conditions on CO2-brine Relative Permeability in Sandstones [O] . Reynolds Catriona, Blunt Martin, Krevor Sam 2014

机译：储层条件对砂岩中CO2卤水相对渗透率的影响

Permeability evolution in sandstone due to injection of CO2-saturated brine or supercritical CO2 at reservoir conditions

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