Caputo Alessia, Calcagni Maria Teresa, Salerno Giovanni, Mammoliti Elisa, Castellini Paolo
Department of Industrial Engineering and Mathematical Sciences, Polytechnic University of Marche, 60131 Ancona, Italy.
Department of Science and Engineering of Matter, Environment and Urban Planning, Polytechnic University of Marche, 60131 Ancona, Italy.
Sensors (Basel). 2025 Jul 15;25(14):4409. doi: 10.3390/s25144409.
This study presents a comprehensive methodology for the detection and characterization of fractures in geological samples using X-ray computed tomography (CT). By combining convolution-based image processing techniques with advanced neural network-based segmentation, the proposed approach achieves high precision in identifying complex fracture networks. The method was applied to a marly limestone sample from the Maiolica Formation, part of the Umbria-Marche stratigraphic succession (Northern Apennines, Italy), a geological context where fractures often vary in size and contrast and are frequently filled with minerals such as calcite or clays, making their detection challenging. A critical part of the work involved addressing multiple sources of uncertainty that can impact fracture identification and measurement. These included the inherent spatial resolution limit of the CT system (voxel size of 70.69 μm), low contrast between fractures and the surrounding matrix, artifacts introduced by the tomographic reconstruction process (specifically the Radon transform), and noise from both the imaging system and environmental factors. To mitigate these challenges, we employed a series of preprocessing steps such as Gaussian and median filtering to enhance image quality and reduce noise, scanning from multiple angles to improve data redundancy, and intensity normalization to compensate for shading artifacts. The neural network segmentation demonstrated superior capability in distinguishing fractures filled with various materials from the host rock, overcoming the limitations observed in traditional convolution-based methods. Overall, this integrated workflow significantly improves the reliability and accuracy of fracture quantification in CT data, providing a robust and reproducible framework for the analysis of discontinuities in heterogeneous and complex geological materials.
本研究提出了一种利用X射线计算机断层扫描(CT)检测和表征地质样品中裂缝的综合方法。通过将基于卷积的图像处理技术与先进的基于神经网络的分割方法相结合,该方法在识别复杂裂缝网络方面达到了高精度。该方法应用于来自麦奥里卡组的泥灰质石灰岩样品,该组是翁布里亚-马尔凯地层序列(意大利亚平宁山脉北部)的一部分,在这个地质环境中,裂缝的大小和对比度往往各不相同,并且经常填充有方解石或粘土等矿物质,这使得裂缝的检测具有挑战性。这项工作的一个关键部分是解决可能影响裂缝识别和测量的多种不确定性来源。这些包括CT系统固有的空间分辨率限制(体素大小为70.69μm)、裂缝与周围基质之间的低对比度、断层重建过程(特别是拉东变换)引入的伪影以及成像系统和环境因素产生的噪声。为了应对这些挑战,我们采用了一系列预处理步骤,如高斯滤波和中值滤波以提高图像质量并减少噪声、从多个角度扫描以提高数据冗余度以及强度归一化以补偿阴影伪影。神经网络分割在区分填充有各种材料的裂缝与母岩方面表现出卓越的能力,克服了传统基于卷积的方法中观察到的局限性。总体而言,这种集成工作流程显著提高了CT数据中裂缝量化的可靠性和准确性,为分析非均质和复杂地质材料中的不连续性提供了一个稳健且可重复的框架。