利用变分自动编码器增强了井下光谱测井的矿物定量和不确定度分析

P. Craddock, Prakhar Srivastava, H. Datir, D. Rose, T. Zhou, L. Mosse, Lalitha Venkataramanan
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引用次数: 0

摘要

本文描述了一种基于变分自编码器框架的创新机器学习应用程序,该应用程序使用地球化学光谱测井中原子元素浓度的测量作为输入,量化沉积地层中常见矿物的浓度和相关不确定性。该算法包括输入、编码器、解码器、输出和一个新的成本函数,用于在训练过程中优化模型系数。该算法的输入是一组原子元素的干重浓度及其相关的不确定度。第一个输出是一组14种矿物的干重分数,第二个输出是一组原始元素的重建干重浓度。两组产出都包括对其预测的不确定性的估计。编码器和解码器是多层前馈人工神经网络(ANN),其系数(权值)在标定(训练)过程中优化。成本函数同时最小化矿物和重建元素输出的误差(精度度量)和方差(精度或鲁棒性度量)。权重的训练是使用一组数千个独立的、高保真的元素和矿物(石英、钾长石、斜长石、伊利石、蒙脱石、高岭石、绿泥石、云母、方解石、白云石、铁云石、菱铁矿、黄铁矿和硬石膏)数据的岩心样本完成的。与现有的依赖简单线性、经验或最近邻函数估计地层岩性或矿物学的方法相比,该算法具有显著的优势。人工神经网络在数值上捕捉了元素和矿物之间的多维和非线性地球化学关系(映射),这是以前的方法无法充分描述的。训练是通过反向传播和对每个元素输入的高斯分布样本进行迭代的,而不是每次迭代(epoch)的每个样本的单个值。选择这些高斯分布是为了具体表示测井测量中干重元素的独特统计不确定性。在训练过程中从高斯分布中采样减少了过拟合的可能性,为对数解释提供了鲁棒性,并进一步实现了对矿物和重建元素输出的不确定性的校准估计,所有这些都是以前的方法所缺乏的。该算法的框架是有目的的推广,它可以适应各种地球化学光谱工具。该算法合理地近似于“全球平均”模型,既不需要不同的校准,也不需要专家参数化或干预来解释常见的油田沉积地层,尽管该框架也是有目的地一般化的,因此可以针对需要的局部环境进行优化。本文介绍了利用测井资料估算油田地层矿物类型和丰度的方法在现场的应用。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
ENHANCED MINERAL QUANTIFICATION AND UNCERTAINTY ANALYSIS FROM DOWNHOLE SPECTROSCOPY LOGS USING VARIATIONAL AUTOENCODERS
This paper describes an innovative machine learning application, based on variational autoencoder frameworks, to quantify the concentrations and associated uncertainties of common minerals in sedimentary formations using the measurement of atomic element concentrations from geochemical spectroscopy logs as inputs. The algorithm comprises an input(s), encoder, decoder, output(s), and a novel cost function to optimize the model coefficients during training. The input to the algorithm is a set of dry-weight concentrations of atomic elements with their associated uncertainty. The first output is a set of dry-weight fractions of fourteen minerals, and the second output is a set of reconstructed dry-weight concentrations of the original elements. Both sets of outputs include estimates of uncertainty on their predictions. The encoder and decoder are multilayer feed-forward artificial neural networks (ANN), with their coefficients (weights) optimized during calibration (training). The cost function simultaneously minimizes error (the accuracy metric) and variance (the precision or robustness metric) on the mineral and reconstructed elemental outputs. Training of the weights is done using a set of several-thousand core samples with independent, high-fidelity elemental and mineral (quartz, potassium-feldspar, plagioclase-feldspar, illite, smectite, kaolinite, chlorite, mica, calcite, dolomite, ankerite, siderite, pyrite, and anhydrite) data. The algorithm provides notable advantages over existing methods to estimate formation lithology or mineralogy relying on simple linear, empirical, or nearest-neighbor functions. The ANN numerically capture the multi-dimensional and nonlinear geochemical relationship (mapping) between elements and minerals that is insufficiently described by prior methods. Training is iterative via backpropagation and samples from Gaussian distributions on each of the elemental inputs, rather than single values, for every sample at each iteration (epoch). These Gaussian distributions are chosen to specifically represent the unique statistical uncertainty of the dry-weight elements in the logging measurements. Sampling from Gaussian distributions during training reduces the potential for overfitting, provides robustness for log interpretations, and further enables a calibrated estimate of uncertainty on the mineral and reconstructed elemental outputs, all of which are lacking in prior methods. The framework of the algorithm is purposefully generalizable that it can be adapted across geochemical spectroscopy tools. The algorithm reasonably approximates a ‘global-average’ model that requires neither different calibrations nor expert parameterization or intervention for interpreting common oilfield sedimentary formations, although the framework is again purposefully generalizable so it can be optimized for local environments where desirable. The paper showcases field application of the method for estimating mineral type and abundance in oilfield formations from wellbore logging measurements.
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