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Effect of Temperature, Wettability and Relative Permeability on Oil Recovery from Oil-wet Chalk

机译:温度,润湿性和相对渗透率对从油湿粉笔中采油的影响

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It is customary, for convenience, to use relative permeability data produced at room temperature. This paper shows that this practice underestimates oil recovery rates and ultimate recovery from chalk rocks for high temperature reservoirs. Above a certain temperature (80°C in this work) a reduction of oil recovery was observed. The reduction in oil recovery is reflected by the shift of relative permeability data towards more oil-wet at high temperature (tested here 130°C). However, both IFT and contact angle measurements indicate an increase in water wetness as temperature increases, which contradict the results obtained by relative permeability experiments. This phenomenon may be explained based on the total interaction potential, which basically consists of van der Waals attractive and short-range Born repulsive and double layer electrostatic forces. The fluid/rock interactions is shown to be dominated by the repulsive forces above 80°C, hence increase fine detachment enhancing oil trapping. In other words the indicated oil wetness by relative permeability is misleading.
机译:为了方便起见,通常使用在室温下产生的相对磁导率数据。本文表明,这种做法低估了高温储层白垩岩的采油率和最终采收率。在一定温度以上(本工作中为80°C),发现采油量减少。相对采油率数据在高温下(此处在130°C下进行测试)向更多的油湿方向移动,反映出采油量的减少。但是,IFT和接触角测量均表明水的湿度随着温度的升高而增加,这与通过相对渗透率实验获得的结果相矛盾。可以基于总的交互作用电位来解释这种现象,该交互作用电位主要由范德华力和短程Born排斥力以及双层静电力组成。流体/岩石相互作用被显示为高于80°C的排斥力所支配,因此增加了精细分离,增强了油的捕集。换句话说,通过相对渗透率指示的油湿度是误导的。

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