1887
2nd Australasian Exploration Geoscience Conference: Data to Discovery
  • ISSN: 2202-0586
  • E-ISSN:

Abstract

Summary

Analysing rock micro-structure from micro-computed tomographic images of porous media is vital to understand fluid-flow and estimating petrophysical properties like permeability. The two main approaches of analysing rock micro-structure are (1) through experiments, a timeconsuming process and (2) using numerical simulations which are a part of the standard digital rock physics (DRP) workflow. The standard DRP workflow requires the micro-computed tomographic (micro-CT) images to be segmented into distinct phases (pores and minerals). Segmentation is a user-biased and manual process. It relies heavily on the user to choose a threshold(s) that distinguishes unique phases present in the rock microstructure. Thus, introducing uncertainty in these petrophysical properties. Our approach to resolving this subjectivity and uncertainty in analysing rock microstructure is to directly apply techniques on the micro-CT images or the greyscale images, rather than using segmented images. For this purpose, we use a pattern recognition technique namely the Grey-Level Cooccurrence Matrix (GLCM). The GLCM technique is used to calculate spatial maps that describe features present in the rock micro-structure. Calculating these spatial maps at varying length-scales by using different displacement vectors aid in analysing the grain-sizes, grain-pore interface and pore-sizes. Unlike the histograms which only preserve the frequency of intensity values that represent different features in micro-CT images, GLCM is a secondorder pattern recognition technique that additionally preserves the spatial variation and occurrence of grey-level intensity values. This method of studying the rock microstructure using greyscale images and pattern-recognition techniques provides an advantage over the conventional segmentation techniques because full-information regarding the rock micro-structure captured during microcomputed tomography is preserved and a threshold-less workflow leads to lesser user subjectivity. Lastly, the GLCM based analysis also provides a pathway for automated investigation of rock-microstructure.

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/content/journals/10.1080/22020586.2019.12073166
2019-12-01
2026-01-14
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References

  1. Blunt, M. J., Bijeljic, B., Dong, H., Gharbi, O., Iglauer, S., Mostaghimi, P., Paluzny, A. & Pentland, C. (2013) ‘Pore-scale imaging and modelling’, Advances in Water Resources. Elsevier Ltd, 51, pp. 197–216. doi: 10.1016/j.advwatres.2012.03.003.
  2. Haralick, R. M. and Shanmugam, K. (1973) ‘Computer classification of reservoir sandstones’, IEEE Transactions on Geoscience Electronics, 11(4), pp. 171–177. doi: 10.1109/TGE.1973.294312.
  3. Haralick, R. M., Shanmugam, K. and Dinstein, I. (1973) ‘Textural Features for Image Classification’, IEEE Transactions on Systems, Man and Cybernetics, SMC-3(6), pp. 610–621. doi: 10.1109/TSMC.1973.4309314.
  4. Iassonov, P., Gebrenegus, T. and Tuller, M. (2009) ‘Segmentation of X-ray computed tomography images of porous materials: A crucial step for characterization and quantitative analysis of pore structures’, Water Resources Research, 45(9), pp. 1–12. doi: 10.1029/2009WR008087.
  5. Singh, A., Armstrong, R. T., Regenauer‐Lieb, K., & Mostaghimi, P. (2019). Rock characterization using gray‐level co‐occurrence matrix: An objective perspective of digital rock statistics. Water Resources Research, 55. https://doi.org/10.1029/2018WR023342
/content/journals/10.1080/22020586.2019.12073166
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  • Article Type: Research Article
Keyword(s): GLCM; micro-CT; Pattern recognition; petrophysical properties; porous media
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