首页> 外文会议>SPWLA Annual Logging Symposium;Society of Petrophysicists and Well Log Analysts, inc >ESTIMATING THE PERMEABILITY OF CARBONATE ROCKS BY PRINCIPAL COMPONENT REGRESSIONS OF NMR AND MICP DATA
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ESTIMATING THE PERMEABILITY OF CARBONATE ROCKS BY PRINCIPAL COMPONENT REGRESSIONS OF NMR AND MICP DATA

机译:通过NMR和MICP数据的主成分回归估计碳酸盐岩的渗透率。

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The estimation of continuous downhole permeability is widely performed by nuclear magnetic resonance (NMR) using the classical approaches of Seevers-Kenyon and Timur-Coates. The first approach uses an average of the relaxation times, whereas the latter approach is based on the fractional fluid content computed from a relaxation time distribution cutoff. However, several case studies in the literature reported that these estimators might fail when applied to carbonate rocks in which permeability is often less correlated to porosity, irreducible water content and relaxation times. Furthermore, carbonate rocks may have more complex pore body and throat size distributions (e.g., bimodal distributions) that may be poorly described by a single parameter of the NMR distribution (i.e., the average or the cutoff).This study develops an estimator that uses multiple NMR distribution bins, representing a general case of the classical estimators. This multivariate approach evaluates the size information encoded in each relaxation time bin to estimate permeability. The multivariate estimators are calibrated with absolute permeability using principal component regression (PCR), whereas classical estimators uses standard multiple linear regression. PCR reliably describes relaxation time distributions in a simple and linear-independent manner according to data variance and is a potentially suitable tool for this multivariate calibration task. The performance of the classical and multivariate estimators are compared after undergoing full cross-validationAn important feature of the novel multivariate approach is the possibility of simultaneously using longitudinal (T_1) and transverse (T_2) relaxation times or simply using a specific segment of the T_(1,2) distribution. Both situations could be highly useful for well logging because NMR activations can either simultaneously acquire complete T_1 and T_2 data or can emphasize certain components (e.g., the irreducible fluid signal). Moreover, the multivariate estimators can also be applied to size-scaled T_(1,2) distributions for cases in which relaxation times are less sensitive to permeability, which may occur in many carbonates. By employing mercury injection capillary pressure (MICP) data for NMR size scaling, permeability estimates are improved considerably compared to the non-scaled estimates. The superior results achieved with the novel multivariate estimators over the classical estimators indicate that NMR well logging data should be further explored to improve the accuracy of permeability estimates.
机译:连续井下渗透率的估计是使用Seevers-Kenyon和Timur-Coates的经典方法通过核磁共振(NMR)进行的。第一种方法使用弛豫时间的平均值,而后一种方法基于从弛豫时间分布截止值计算出的分数流体含量。但是,文献中的一些案例研究表明,将这些估算器应用于渗透率通常与孔隙率,不可约水含量和弛豫时间相关性较小的碳酸盐岩时,可能会失败。此外,碳酸盐岩可能具有更复杂的孔隙体和喉道尺寸分布(例如,双峰分布),而这些分布可能无法通过NMR分布的单个参数(即平均值或临界值)来描述。 这项研究开发了一种使用多个NMR分布箱的估算器,代表了经典估算器的一般情况。这种多变量方法评估在每个弛豫时间仓中编码的大小信息,以估计渗透率。使用主成分回归(PCR)使用绝对渗透率对多元估计量进行校准,而经典估计量则使用标准的多元线性回归进行校正。 PCR根据数据方差以简单且与线性无关的方式可靠地描述了弛豫时间分布,并且是该多元校准任务的潜在合适工具。经过全面的交叉验证后,比较了经典估计量和多元估计量的性能 新颖的多变量方法的一个重要特征是可以同时使用纵向(T_1)和横向(T_2)弛豫时间,或仅使用T_(1,2)分布的特定段的可能性。两种情况都可能对测井非常有用,因为NMR激活既可以同时获取完整的T_1和T_2数据,也可以强调某些分量(例如,不可还原的流体信号)。此外,对于弛豫时间对渗透率较不敏感的情况(在许多碳酸盐中可能会发生变化的情况),也可以将多元估计量应用于规模缩放的T_(1,2)分布。通过使用汞注入毛细管压力(MICP)数据进行NMR尺寸缩放,与未缩放的估计相比,渗透率估计得到了显着改善。与传统的估算器相比,新型多元估算器获得的优异结果表明,应进一步探索NMR测井数据,以提高渗透率估算的准确性。

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