Advances in Understanding Wettability of Tight Oil Formations: A Montney Case Study

渗吸 润湿 石英 石油工程 卤水 地质学 毛细管压力 接触角 致密油 白云石 油页岩 相对渗透率 方解石 油藏 非常规油 矿物学 材料科学 岩土工程 复合材料 化学 多孔介质 多孔性 古生物学 有机化学 发芽 生物 植物
作者
Ali Habibi,Hassan Dehghanpour,Mojtaba Binazadeh,Donald Bryan,Gordon Uswak
出处
期刊:SPE reservoir evaluation & engineering [Society of Petroleum Engineers]
卷期号:19 (04): 583-603 被引量:48
标识
DOI:10.2118/175157-pa
摘要

Summary This paper presents comprehensive rock/fluid experiments, by use of reservoir rock and fluids, to investigate wetting affinity of the Montney (MT) tight oil play in the Western Canadian Sedimentary Basin. Wettability characterization is essential for selecting optimum fracturing and treatment fluids by completion engineers and for selecting appropriate relative permeability and capillary pressure curves by reservoir engineers. Application of the conventional techniques for wettability evaluation of tight rocks is challenging primarily because of their extremely low permeability and complex pore structure. The objective of this paper is to develop an alternative laboratory protocol for evaluating the wettability of tight oil rocks reliably. First, we conducted systematic spontaneous-imbibition tests on fresh core samples from two different wells drilled in the MT formation. We measured the air/brine, air/oil, and brine/oil contact angles for all samples. We used the end pieces of the samples to conduct scanning electron microscopy (SEM) and analysis of the elemental mapping, or energy-dispersive X-ray spectroscopy (EDS). Finally, we investigated the spontaneous imbibition of brine (or oil) into the samples partly saturated with oil (or brine). Both oil and brine spontaneously imbibe into the fresh samples, composed of quartz, carbonates (dolomite/calcite), clay minerals, feldspars, and organic matter. The results indicate that the effective pore network exhibits a mixed-wet behavior. Moreover, brine spontaneously imbibes into and forces the oil out of the oil-saturated samples, whereas oil cannot imbibe into the brine-saturated samples. This indicates that in the presence of both oil and brine, the rock affinity to brine is higher than that to oil.

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