首页> 外文会议>International Symposium of the Society of Core Analysts >WETTABILITY AND RELATIVE PERMEABILITY OF LOWER CRETACEOUS CARBONATE ROCK RESERVOIR,SAUDI ARABIA
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WETTABILITY AND RELATIVE PERMEABILITY OF LOWER CRETACEOUS CARBONATE ROCK RESERVOIR,SAUDI ARABIA

机译:沙特阿拉伯下白垩纪碳酸盐岩层的润湿性和相对渗透性

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摘要

Results and discussions in this paper relate to a Lower Cretaceous carbonate reservoir located in southeastern Saudi Arabia.It is a heterogeneous carbonate formation with various facies due to diagenetic alteration of the original rock fabric.The reservoir is large and prolific with mixed-wet characteristics.Because of the economic importance and variety of oil-recovery mechanisms operative or possible in the reservoir,the multiphase recovery behavior has been extensively studied.Also,various wettability tests were carried out using Amott and USBM methods.This paper describes the variation in wettability and relative permeability of Lower Cretaceous carbonate reservoir and the multi-phase simulations of the experimental results.It shows that measurements are consistent with recent theories of the relationship between water saturation,relative permeability,and wettability as described by Jadhunadan and Morrow,1991.However,the results indicate that the wettability of the reservoir changes from water-wet low on structure near the oil/water contact to mixed or neutral wet behavior higher on structure.Oil-wetting character increases towards the top of oil column and is correlated to decreasing water saturation.The results revealed that changes in wettability are accompanied by changes in waterflood efficiency and facies of deposition.
机译:本文的结果与讨论涉及位于沙特阿拉伯东南部的下白垩纪碳酸盐储层。是由于原始岩石织物的成岩改变,具有各种相的异质碳酸盐形成。储层具有较大且杂于混合湿湿特性。由于储层中的经济重要性和各种油恢复机制,多相回收行为已经过广泛研究.SCO,使用AMOTT和USBM方法进行各种润湿性测试。本文描述了润湿性的变化和下白垩统碳酸盐贮存器的相对渗透性和实验结果的多相模拟。图表表明,测量与最近的水饱和度,相对渗透性和润湿性之间的关系的理论一致,如Jadhunadan和Morrow,1991.如何,结果表明,水库变化的润湿性来自油/水接触附近的水湿较低的结构,与结构更高的混合或中性湿行为。润湿性朝向油柱顶部增加,与降低水饱和度相关。结果显示润湿性的变化伴随着水料效率的变化和沉积的相位。

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