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An equation for estimating water saturation in clean formations utilizing resistivity and sonic logs: theory and application

机译:利用电阻率和声波测井估算洁净地层中水饱和度的方程式:理论与应用

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An equation estimating water saturation values from resistivity and sonic logs, which are the common available logs in most of the wells and formations, was investigated for different lithologies. It is essential based on the combination of Archie's and Raiga's relationships, with their respective coefficients a, m, n, and x. Application of this equation to real field data in the USA and Egypt show particularly good agreement in a variety of cases, in particular, if the formation true resistivity (R_t) is greater than 5 OMEGA m. In the case where R_t is less than 5 OMEGA m, multiplication of this equation by a certain correction factor is recommended. This factor, which can be empirically estimated, was found to be ranging numerically from 1 to 1.8 depending on the shale transit time (DELTA_(tsh)) and cementation exponent (m). With the exception of core measurements, and where no porosity tools other than sonic logs are available, this equation can be considered as a good predictor for estimating water saturation in clean formations (non-shaly). In case of clay content, the application of the equation should include the same correaction procedures of the sonic log reading those applied in usual interpretation. Worthy of remarks is that this equation gives reasonable and reliable values for rocks having transit time ranging between 40 and 150 mus/ft; above this range, the usefulness of this equation must remain in doubt. Knowledge of porosity is not necessary in such evaluation, which reflect the general usefulness of this equation. More data are needed to test the the existing relation in numerous conditions.
机译:针对不同的岩性,研究了根据电阻率和声波测井估计水饱和度值的方程式,而声波测井是大多数井和地层中常见的测井曲线。这是基于Archie和Raiga关系以及它们各自的系数a,m,n和x的组合所必需的。在许多情况下,尤其是在地层真实电阻率(R_t)大于5 OMEGA m的情况下,将该方程应用于美国和埃及的实地数据显示出特别好的一致性。在R_t小于5 OMEGA m的情况下,建议将该方程乘以某个校正因子。可以凭经验估算的该因素在数值上取决于页岩通过时间(DELTA_(tsh))和胶结指数(m),范围从1到1.8。除岩心测量外,除声波测井外没有其他孔隙度测量工具可用时,该方程式可作为估算洁净地层(非页岩)中水饱和度的良好预测器。在粘土含量的情况下,方程的应用应包括与声波测井相同的校正程序,该程序与通常解释中所应用的程序相同。值得一提的是,该方程为过渡时间在40至150 mus / ft之间的岩石提供了合理而可靠的值。超过这个范围,这个方程式的实用性必须保持怀疑。在这种评估中不需要了解孔隙度,这反映了该方程式的一般用途。需要更多数据才能在多种条件下测试现有关系。

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