印度Kachchh盆地非均质生物扰动砂岩润湿性研究及毛管压力估算

Adityam Dutta
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摘要

建模和流动模拟的油藏特征是假设岩石的均质性。异质性被忽视,以防止发生储备管理的复杂性。生物扰动砂岩储层是一种非均质性储层,在许多产油盆地中都有明显的发现。研究这些非均相体系的流体特性至关重要,因为变化的特性将影响所得的润湿性行为。因此,在生物扰动的非均质储层中,对润湿性的估计将有助于估计此类地层的流动行为和油气采收率的可能结果。在此背景下,设计了一种集体方法来了解Kachchh盆地生物扰动砂岩的储层行为。样品来自露头,分析包括建立的岩心/岩石分析的标准实验程序,以估计润湿性。本文探讨了各种生物扰动样品测量收缩角的实验分析。考虑时间和梯度因素,测量了油湿岩心和水湿岩心的接触角。结合获得的接触角值、孔径(半径)和界面张力数据,计算了不同等级生物扰动砂岩的毛细压力。研究结果表明,利用岩石的毛细压力行为和吸排流的滞后趋势,可以设计和提出生物扰动非均质砂岩的最终模型。
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Wettability Studies and Estimation of Capillary Pressure on Heterogeneous Bioturbated Sandstones from Kachchh Basin, India
Reservoir characterisation for modelling and flow simulation is done assuming the homogenous nature of the rock. Heterogeneity is overlooked to prevent occurrences of reserve management complexities. Bioturbated sandstone reservoirs are heterogeneous and prominently found in many petroleum producing basins. Studying the fluid characteristics of these heterogeneous systems is essential, as with changing characters will affect the resulting wettability behaviour. Thus, in a bioturbated heterogeneous reservoir, estimation of the wettability will help in estimating the flow behaviour and possible outcomes of hydrocarbon oil and gas recovery from such formations. With this background, a collective approach has been designed to understand the reservoir behaviour of bioturbated sandstones from Kachchh Basin. The samples are from outcrop, and the analysis includes established standard experimental procedures of core/rock analysis for estimating wettability. The paper explores the experimental analysis of the measuring contract angle in various bioturbated samples. Contact angles of both oil-wet and water-wet cores were measured considering time and gradient factors. Capillary pressure of the various grades of bioturbated sandstones was calculated combining obtained data on contact angle values along with the pore size (radius) and interfacial tension data. The results suggest that the final model can be designed and proposed for the characterisation of bioturbated heterogeneous sandstones using the Capillary pressure behaviour of rocks along with hysteresis trend of imbibition and drainage flows.
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