利用电阻率测井确定常规和非常规油藏的流层指标

J. W. González, Alejandro Jose Linares, Diego Armando Rodriguez, Alexander Castro Chacon, J. Vásquez
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引用次数: 0

摘要

流动区指标(FZI)取决于渗透率和孔隙度。储层的渗透率是最难确定的属性之一,因为计算渗透率的模型使用了多种测井数据(伽马射线、密度-中子、声波等)。渗透率建模使用了复杂的方法,如匹配学习、模糊逻辑、聚类、多元线性回归等,最后,每个储层的渗透率模型都是唯一的。这项工作的目的是通过常规和非常规储层的深电阻率(Rt)和浅电阻率(Rs)测井来确定流动带指示器(FZI)。基本上,该方法包括研究钻井过程中泥浆过滤侵入的现象,以及电阻率测井的行为。侵入会影响井附近的多孔性和渗透性地层的一些性质。一般来说,在渗透性很强的储层中,侵入程度较小,而在渗透性较差的储层、致密、溶洞型碳酸盐岩或裂缝性地层中则相反。在此基础上,提出了确定FZI的数学模型,即适用于水基和油基泥浆的对数函数。如果电阻率相等,则没有泥浆过滤侵入,渗透率为零。如果电阻率差值不为零,则污泥滤液侵入,因此渗透率大于零,表明储层有流动区。还有其他与侵入无关的井眼、地层和工具条件可能会产生RT和RS之间的差异。这些将在下面简要说明。FZI模型识别了储层中的流动带。岩心FZI和核磁共振(NMRI)测井数据与模型计算的FZI相关。地层测试器的流度数据与计算的FZI基本一致。频谱噪声和PLT测井入流层与FZI具有良好的相关性。这种方法可以应用于任何类型的储层。在探井中,该方法可以定义并提出设置地层测试器的最佳区域,从而优化作业时间。在进行岩石物理评估之前,FZI结果可以根据岩石质量识别储层的远景区。此外,还可以利用所获得的结果监测井的生产和注入行为。最后,FZI作为一个自变量降低了渗透率模型的不确定性,因为FZI与岩石的结构和相密切相关。最简单的表示就是电阻率随孔隙度的变化。因此,如果孔隙度与相有关,地层因子F也与相有关,那么电阻率测井就成为一种很好的相鉴别方法。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Determining a Flow Zone Indicator in Conventional and Unconventional Reservoirs Using Resistivity Logs
The Flow Zone Indicator (FZI) depends on permeability and porosity. The permeability of a reservoir is one of the most difficult properties to determine, since the models to calculate permeability use input from several logs (gamma ray, density-neutron, sonic, etc.). Permeability modeling is done using complex methodologies such as: matching learning, fuzzy logic, cluster, multiple linear regression, etc., and at the end, permeability models end up being unique for each reservoir. The objective of this work is to determine a flow zone indicator (FZI) from the deep (Rt) and shallow resistivity (Rs) logs in conventional and unconventional reservoirs. Basically, the methodology consisted of studying the phenomenon of the invasion of mud filtration during the drilling of the wells, and the behavior of resistivity logs. Invasion affects some properties of porous and permeable formations in the vicinity of a well. In general, the invasion is small in very porous and permeable reservoirs, the opposite is in poorly permeable reservoirs, tight, vuggy carbonates or fractured formations. Based on the above, a mathematical model was proposed to determine the FZI, as a logarithmic function which is applicable in both water and oil-based muds. If the resistivities are equal, then there is no mud filtration invasion, and the permeability is zero. If the difference in resistivity is different from zero, there is invasion of the sludge filtrate and therefore the permeability is greater than zero, indicating flow zones in the reservoir. There are other borehole, formation and tool conditions that may generate difference between RT and RS which are not related to invasion. These will be explained briefly below. The FZI model identified the flow zones in the reservoir. FZI from core and Nuclear Magnetic Resonance (NMRI) log data correlated with the FZI calculated with the model. The mobility data of formation testers agreed with the calculated FZI. Also, spectral noise and PLT logs inflow zones showed excellent correlation with the FZI. This methodology can be applied in any type of reservoir. In exploration wells the methodology allows to define and propose the best zones to set the formation testers, thus optimizing operational time. Before performing a petrophysical assessment, FZI results can identify prospective zones of the reservoir based on rock quality. Also, the production and injection behavior of the wells can be monitored with the obtained results. And finally, the FZI as an independent variable decreases the uncertainty of a permeability model, because the FZI is intimately related to the texture of the rock and the facies. The simplest expression of this is the resistivity variation with changes of porosity. Therefore, if porosity is related to facies, so is the formation factor (F), and then the resistivity log becomes an excellent facies discriminator.
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