scholarly journals Classification and quantification of pore shapes in sandstone reservoir rocks with 3-D X-ray micro-computed tomography

2015 ◽  
Vol 7 (4) ◽  
pp. 3441-3479 ◽  
Author(s):  
M. Schmitt ◽  
M. Halisch ◽  
C. Müller ◽  
C. P. Fernandes

Abstract. Recent years have seen a growing interest in the characterization of the pore morphologies of reservoir rocks and how the spatial organization of pore traits affects the macro behaviour of rock-fluid systems. With the availability of 3-D high-resolution imaging (e.g. μ-CT), the detailed quantification of particle shapes has been facilitated by progress in computer science. Here, we show how the shapes of irregular rock particles (pores) can be classified and quantified based on binary 3-D images. The methodology requires the measurement of basic 3-D particle descriptors and a shape classification that involves the similarity of artificial objects, which is based on main pore network detachments and 3-D sample sizes. The results were validated for three sandstones (S1, S2 and S3) from distinct reservoirs, and most of the pore shapes were found to be plate- and cube-like. Furthermore, this study generalizes a practical way to correlate specific particle shapes, such as rods, blades, cuboids, plates and cubes, to characterize asymmetric particles of any material type with 3-D image analysis.

Solid Earth ◽  
2016 ◽  
Vol 7 (1) ◽  
pp. 285-300 ◽  
Author(s):  
Mayka Schmitt ◽  
Matthias Halisch ◽  
Cornelia Müller ◽  
Celso Peres Fernandes

Abstract. Recent years have seen a growing interest in the characterization of the pore morphologies of reservoir rocks and how the spatial organization of pore traits affects the macro behavior of rock–fluid systems. With the availability of 3-D high-resolution imaging, such as x-ray micro-computed tomography (µ-CT), the detailed quantification of particle shapes has been facilitated by progress in computer science. Here, we show how the shapes of irregular rock particles (pores) can be classified and quantified based on binary 3-D images. The methodology requires the measurement of basic 3-D particle descriptors (length, width, and thickness) and a shape classification that involves the similarity of artificial objects, which is based on main pore network detachments and 3-D sample sizes. Two main pore components were identified from the analyzed volumes: pore networks and residual pore ganglia. A watershed algorithm was applied to preserve the pore morphology after separating the main pore networks, which is essential for the pore shape characterization. The results were validated for three sandstones (S1, S2, and S3) from distinct reservoirs, and most of the pore shapes were found to be plate- and cube-like, ranging from 39.49 to 50.94 % and from 58.80 to 45.18 % when the Feret caliper descriptor was investigated in a 10003 voxel volume. Furthermore, this study generalizes a practical way to correlate specific particle shapes, such as rods, blades, cuboids, plates, and cubes to characterize asymmetric particles of any material type with 3-D image analysis.


2020 ◽  
Vol 10 (1) ◽  
Author(s):  
Diana Ceballos-Francisco ◽  
Nuria García-Carrillo ◽  
Alberto Cuesta ◽  
María Ángeles Esteban

Geophysics ◽  
2002 ◽  
Vol 67 (1) ◽  
pp. 230-240 ◽  
Author(s):  
Patrick N. J. Rasolofosaon ◽  
Bernard E. Zinszner

We developed new experimental and theoretical tools for the measurement and the characterization of arbitrary elasticity tensors and permeability tensors in rocks. They include an experimental technique for the 3‐D visualization of hydraulic invasion fronts in rock samples by monitoring the injection of salt solutions by X‐ray tomography, and a technique for inverting the complete set of the six coefficients of the permeability tensor from invasion front images. In addition, a technique for measuring the complete set of the 21 elastic coefficients, a technique allowing the identification and the orientation in the 3‐D space of the symmetry elements (planes, axes), and a technique for approximating the considered elastic tensor by a tensor of simpler symmetry with the quantification of the error induced by such an approximation have been developed. We apply these tools to various types of reservoir rocks and observed quite contrasted behaviors. In some rocks, the elastic anisotropy and the hydraulic anisotropy are closely correlated, for instance in terms of the symmetry directions. This is the case when elastic anisotropy and hydraulic anisotropy share the same cause (e.g., layering, fractures). In contrast, in some other rocks, hydraulic properties and elastic properties are clearly uncorrelated. These results highlight the challenge we have to face in order to estimate the rock permeability and to monitor the fluid flow from seismic measurements in the field.


2017 ◽  
Vol 35 (8) ◽  
pp. 933-938 ◽  
Author(s):  
Roberto Pisano ◽  
Antonello A. Barresi ◽  
Luigi C. Capozzi ◽  
Giorgia Novajra ◽  
Irene Oddone ◽  
...  

2019 ◽  
Vol 9 (2) ◽  
Author(s):  
Chih‐Wei Hsu ◽  
Sowmya Kalaga ◽  
Uchechukwu Akoma ◽  
Tara L. Rasmussen ◽  
Audrey E. Christiansen ◽  
...  

2020 ◽  
Vol 279 ◽  
pp. 105895
Author(s):  
B. Yu ◽  
W. Fan ◽  
J.H. Fan ◽  
T.A. Dijkstra ◽  
Y.N. Wei ◽  
...  

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