用微尺度方法表征碳酸盐岩润湿性

Mahmoud Aboushanab, Khaloud Al Naimi, M. Al Kobaisi, Md. Motiur Rahman, M. Arif, Mohamed Mahmoud
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引用次数: 0

摘要

润湿性是影响相对渗透率和毛管压力的重要因素,而相对渗透率和毛管压力又影响油气采收率。碳酸盐表面的润湿性由于其不同的润湿行为而具有挑战性。传统上使用宏观接触角观测来量化润湿性。然而,宏观接触角在三相接触线的精确识别方面受到影响。在本研究中,提出了一种新的微尺度方法来确定岩石表面润湿性。在这里,我们使用了五种不同的中东碳酸盐样品,它们具有不同的矿物学。微观尺度的接触角采用环境扫描电子显微镜(ESEM)冷凝蒸发法测定,宏观尺度的接触角采用经典的固滴法测定。结果表明,宏观接触角和微观接触角之间存在显著差异,表明在不同的测量尺度下润湿性会发生变化。根据微接触角的不同,观察到所有样品的混合湿态,因为一些样品在大多数测量位置经历水湿行为,而它们在少数位置表现为中间湿行为。然而,基于宏观接触角,只能识别一种润湿行为。因此,全面的润湿性表征需要在微观尺度上的洞察力来捕捉润湿行为的变化。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Wettability Characterization of Carbonate Rocks Using a Micro-Scale Approach
Wettability is an important factor that influences relative permeabilities and capillary pressure, which in turn impacts the hydrocarbon recovery. Wettability of carbonate surfaces is typically challenging due to their diverse wetting behavior. Wettability has been conventionally quantified using the macro-scale contact angle observations. However, macro contact angle suffers in terms of precise identification of the three-phase contact line. In this study, a new micro-scale approach is presented to determine rock surface wettability. Here we used five different Middle Eastern carbonate samples with different mineralogy. The micro-scale contact angles are evaluated via Environmental Scanning Electron Microscopy (ESEM) using condensation-evaporation approach while the classical sessile drop method is used to determine the macro-contact angles. The results show a notable difference between macro and micro contact angles which suggests wettability variation at different scale of measurement. Depending on micro contact angles, mixed-wet state for all samples is observed, as some samples experienced water-wet behaviour at most of the measured locations, while they showed intermediate-wet behaviour at a few locations. However, based on macro contact angles, only one wetting behaviour is recognized. Therefore, a thorough wettability characterization would require insights at the micro-scale to capture variations in wetting behavior.
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