Abstract
Digital rock physics has seen significant advances owing to improvements in micro-computed tomography (MCT) imaging techniques and computing power. These advances allow for the visualization and accurate characterization of multiphase transport in porous media. Despite such advancements, image processing and particularly the task of denoising MCT images remains less explored. As such, selection of proper denoising method is a challenging optimization exercise of balancing the tradeoffs between minimizing noise and preserving original features. Despite its importance, there are no comparative studies in the geoscience domain that assess the performance of different denoising approaches, and their effect on image-based rock and fluid property estimates. Further, the application of machine learning and deep learning-based (DL) denoising models remains under-explored. In this research, we evaluate the performance of six commonly used denoising filters and compare them to five DL-based denoising protocols, namely, noise-to-clean (N2C), residual dense network (RDN), and cycle consistent generative adversarial network (CCGAN)—which require a clean reference (ground truth), as well as noise-to-noise (N2N) and noise-to-void (N2V)—which do not require a clean reference. We also propose hybrid or semi-supervised DL denoising models which only require a fraction of clean reference images. Using these models, we investigate the optimal number of high-exposure reference images that balances data acquisition cost and accurate petrophysical characterization. The performance of each denoising approach is evaluated using two sets of metrics: (1) standard denoising evaluation metrics, including peak signal-to-noise ratio (PSNR) and contrast-to-noise ratio (CNR), and (2) the resulting image-based petrophysical properties such as porosity, saturation, pore size distribution, phase connectivity, and specific surface area (SSA). Petrophysical estimates show that most traditional filters perform well when estimating bulk properties but show large errors for pore-scale properties like phase connectivity. Meanwhile, DL-based models give mixed outcomes, where supervised methods like N2C show the best performance, and an unsupervised model like N2V shows the worst performance. N2N75, which is a newly proposed semi-supervised variation of the N2N model, where 75% of the clean reference data is used for training, shows very promising outcomes for both traditional denoising performance metrics and petrophysical properties including both bulk and pore-scale measures. Lastly, N2C is found to be the most computationally efficient, while CCGAN is found to be the least, among the DL-based models considered in this study. Overall, this investigation shows that application of sophisticated supervised and semi-supervised DL-based denoising models can significantly reduce petrophysical characterization errors introduced during the denoising step. Furthermore, with the advancement of semi-supervised DL-based models, requirement of clean reference or ground truth images for training can be reduced and deployment of fast X-ray scanning can be made possible.
Highlights
AND INTRODUCTIONMicro-computed tomography (MCT) is a non-destructive technique used to visualize the internal structure of objects in a variety of disciplines including medicine, dentistry, tissue engineering, aerospace engineering, geology, and material and civil engineering (Orhan, 2020)
Pore-network modeling, which is used in a variety of digital rock studies to explain and predict macroscopic transport properties such as absolute permeability, relative permeability, and capillary pressure, uses simplified pore structures composed of a network of pores and throats, which can be directly extracted from the micro-computed tomography (MCT) images (Valvatne and Blunt, 2004; Jia et al, 2007; Dong et al, 2009; Mostaghimi et al, 2013; Berg et al, 2016; Zahaf et al, 2017; Raeini et al, 2019)
The red region shows that some small solid features can be inaccurately characterized as fluid, resulting in porosity estimation errors, while the green region demonstrates a blurry fluid-fluid interface in the low quality (LQ) image, which can lead to errors in estimating fluid saturation and petrophysical properties pertaining to fluid–fluid interfaces
Summary
AND INTRODUCTIONMicro-computed tomography (MCT) is a non-destructive technique used to visualize the internal structure of objects in a variety of disciplines including medicine, dentistry, tissue engineering, aerospace engineering, geology, and material and civil engineering (Orhan, 2020). The physical principle behind this technique is that X-rays attenuate differently as they penetrate through different materials depending on their density and atomic mass (Knoll, 2000; Attix, 2004; Ritman, 2004; Hsieh, 2015) This makes MCT an ideal tool for characterizing multiphase materials such as rocks with fluid phases of different densities. High-resolution MCT imaging was used to obtain quantitative pore-scale information about structure– function relationships (Jasti et al, 1993) They characterized the 3D pore structure in a glass bead pack and three Berea sandstone samples to determine whether topological properties such as pore connectivity and phase features of individual fluid phases such as saturation can be resolved. The accuracy of the model predictions depends on the accuracy of processing the images that feed into these models
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