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USE OF CEC-DEPENDENT CEMENTATION AND SATURATION EXPONENTS IN SHALY SAND RESISTIVITY MODELS

机译:在泥质砂岩电阻率模型中使用CEC依赖的固结和饱和指数

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Researchers at Louisiana State University (LSU) have introduced several petrophysical models expressing the electric properties of shaly sands. These models, to be used for hydrocarbon detection, are based on the Waxman and Smits (W-S) concept of supplementing the water conductivity with clay counter-ions conductivity. The models also utilize the Dual Water (D-W) concept, which incorporates a free and a bound water each occupying a specific volume of the total pore space. However, unlike W-S and D-W models, the LSU models treat the counter-ion conductivity as that of a hypothetical sodium chloride solution. The latest version of the LSU models considers that the electric current follows two distinct paths, one through the free electrolyte and the other through the bound water. Hence, two different formation factors, expressed using two different cementation exponents, were used to express the free water and the bound water term. The two cementation exponents are estimated in the adjacent clean sand and pure shale. The results of extensive laboratory experiments, described in this paper, show that the use of two cementation exponents to characterize electrical behavior in shaly sand is substantially better than the conventional use of one cementation exponent value. In addition, the experimental results show that a correlation between saturation exponent value, n and CEC exists. Also, brine saturation of 15,000 ppm was found to be the upper limit of “low” salinity range in which extra care is needed for shaly sand evaluation.
机译:路易斯安那州立大学(LSU)的研究人员介绍了几种岩石物理模型,这些模型表达了泥质砂岩的电学性质。这些用于碳氢化合物检测的模型基于Waxman和Smits(W-S)概念,即用粘土抗衡离子电导率补充水电导率。这些模型还利用了双重水(D-W)概念,该概念结合了自由水和结合水,每个水都占据了总孔隙空间的特定体积。但是,与W-S和D-W模型不同,LSU模型将抗衡离子电导率视为假设的氯化钠溶液的抗衡离子电导率。 LSU模型的最新版本认为电流遵循两个不同的路径,一个路径通过自由电解质,另一路径通过结合水。因此,使用两个不同的胶结指数表示的两个不同的形成因子被用来表示游离水和结合水项。在相邻的干净砂岩和纯页岩中估计了这两种胶结指数。本文所述的大量实验室实验结果表明,使用两种胶结指数来表征泥质砂岩中的电行为比常规使用一种胶结指数值要好得多。另外,实验结果表明,饱和指数n和CEC之间存在相关性。同样,发现盐水饱和度为15,000 ppm是“低”盐度范围的上限,在该范围内需要格外小心进行页岩砂评估。

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