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A laboratory scale approach to wettability restoration in chalk core samples

机译:实验室规模的粉笔芯样品润湿性恢复方法

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摘要

Wettability in chalk has been studied comprehensively to understand fluid flow mechanisms impacting coreflooding experiments. Wettability becomes paramount in understanding the parameters influencing chalk-fluid interactions. The main objective of this work is to evaluate as to which degree the wettability in chalk core samples can be controlled in the laboratory. Kansas chalk samples saturated with brine (1.1 M/64284 ppm NaCl) and an oil mixture (60% - 40% by volume of Heidrun oil and heptane) were aged at a constant temperature of 90oC with aging time as the laboratory control variable. A multimodal method incorporating contact angle measurements, wettability index via USBM test, and SEM-MLA analysis was applied in evaluating wettability. A systematic approach was applied with the three different methods to quantify the degree of uncertainty linked to a) wettability estimation and b) the aging procedure to control wettability alteration of Kansas chalk. With a comprehensive suite of samples, we were successfully able to alter the wettability of chalk cores.
机译:已对白垩的润湿性进行了全面研究,以了解影响岩心驱替实验的流体流动机理。在了解影响白垩-流体相互作用的参数时,润湿性变得至关重要。这项工作的主要目的是评估在实验室中粉笔芯样品的润湿性可以控制到什么程度。在盐水(1.1 M / 64284 ppm NaCl)和油混合物(Heidrun油和庚烷的体积百分比为60%-40%)中饱和的堪萨斯州白垩样品在90oC的恒定温度下老化,老化时间为实验室控制变量。结合接触角测量,通过USBM测试的润湿性指数和SEM-MLA分析的多峰方法用于评估润湿性。系统的方法与三种不同的方法一起应用,以量化与a)润湿性估计和b)老化程序相关的不确定性程度,以控制堪萨斯粉笔的润湿性变化。借助一整套样品,我们成功地改变了粉笔芯的润湿性。

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