润湿
相对渗透率
含水层
溶解
磁导率
地温梯度
土壤科学
溶解度
石油工程
接触角
地质学
材料科学
岩土工程
热力学
化学
地下水
复合材料
物理
生物化学
物理化学
膜
地球物理学
有机化学
多孔性
作者
Mohsen Abbaszadeh,Seyed M. Shariatipour,Augustine O. Ifelebuegu
标识
DOI:10.1016/j.ijggc.2020.103101
摘要
The wettability of a formation is defined as the tendency of one fluid to spread on a surface in competition with other fluids which are also in contact with it. However, the impact of temperature on wettability in an aquifer and the modification of relative permeability curves based on the temperature variation in aquifers is not well covered in the literature. This study redresses this dearth of information by investigating the impact of temperature on wettability distribution in a reservoir and updating the relative permeability curves based on its temperature propagation. The impact of the latter is studied in relation to the solubility of CO2 injected into an aquifer using the numerical methods (i.e. ECLIPSE). If the CO2 injected has a temperature higher than the formation geothermal temperature, it can change the wettability of the formation further to a more CO2 wet condition. This increases the risk of leakage and also changes the relative permeability curves as the CO2 moves through the reservoir, a situation that needs to be considered in reservoir simulations. The results show that updating and modifying the relative permeability curves with temperature variation in an aquifer can increase the amount of CO2 dissolution there.
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