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INVESTIGATION OF IMBIBITION SATURATION EXPONENT UNDER MIXED SALINITY ENVIRONMENT

机译:混合盐度环境下的吸收饱和度指数研究

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An important challenge in resistivity well logging is the interpretation of electrical data to derive the water/oil saturation of an oil reservoir during sea water injection for instance. The sea water resistivity is then commonly used to obtain the water saturation from Archie’s law,regardless of the potential mixing between formation brine and sea water;this is certainly valid close to the injection wellbore. However low frequency resistivity tools can have high enough depth of investigation to be affected by this mixed salinity environment. Cross-well electromagnetic(EM)resistivity method for instance,recently used to provide fluid distribution mapping at inter-well scale,can be significantly affected by the change in water resistivity during water flooding. A core analysis program was initiated to understand the change of resistivity in mixed salinity environment using the porous plate resistivity method in imbibition cycle. Despite the known existence of hysteresis between drainage and imbibition cycles,the cementation factor m and saturation exponent n,obtained from Archie’s law [1],are generally measured in the laboratory respectively before and during a primary drainage porous plate experiment with resistivity measurements. Imbibition tests are rarely performed,and when they are,no mixing effect is observed since the same formation brine is injected into the sample. In this paper,the brine mixing effect on rock electrical properties during a porous plate imbibition test is investigated and a simple salinity model is proposed to derive the equivalent resistivity of the brine mixture for appropriate water saturation calculation.
机译:电阻率井测井中的一个重要挑战是对电气数据的解释,以导出油藏在海水喷射过程中的水/油饱和度。然后,海水电阻率通常用于获得Archie律法的水饱和度,无论形成盐水和海水之间的潜在混合如何;这肯定是靠近喷射井孔的有效。然而,低频电阻率工具可以具有足够高的调查深度,以受到这种混合盐度环境的影响。例如,最近用于在井间规模提供流体分布映射的交叉孔电磁(EM)电阻率方法可以显着影响水淹没期间防水率的变化。开始使用多孔板电阻率法在吸收循环中了解核心分析计划以了解混合盐度环境中的电阻率的变化。尽管引流和吸收循环之间已知存在滞后,但从Archie的法律[1]中获得的胶结因子m和饱和指数n分别在初级排水多孔板实验之前和期间在实验室中测量电阻率测量。很少进行吸收测试,并且当它们是时,由于将相同的地层盐水注入样品中,因此不观察到混合效果。在本文中,研究了在多孔板内吸收试验期间对岩石电性能的盐水混合效果,提出了一种简单的盐度模型,从而导出了盐水混合物的等效电阻率,以进行适当的水饱和度计算。

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