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Published on: February 25, 2015
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Reconstruction of three-dimensional porous media from a single two-dimensional image using three-step sampling
MingLiang Gao1, XiaoHai He2, QiZhi Teng2
1College of Electronics and Information Engineering, Sichuan University, Chengdu 610065, China and Northwest University for Nationalities, College of Electrical Engineering, Lanzhou 730030, China.
Physical Review. E, Statistical, Nonlinear, and Soft Matter Physics
|February 14, 2015
Summary
A novel three-step sampling method reconstructs 3D porous media from 2D images by controlling layer continuity and variability. This technique accurately replicates statistical characteristics of the original porous medium.
Area of Science:
- Geoscience
- Image Analysis
- Computational Modeling
Background:
- Reconstructing 3D porous media from 2D images is crucial for understanding material properties.
- Maintaining continuity and variability between reconstructed layers is essential for accurate representation.
- Existing methods struggle to precisely control these inter-layer characteristics.
Purpose of the Study:
- To develop an original sampling method for accurate 3D porous medium reconstruction.
- To ensure continuity and variability consistency with the training image (TI).
- To validate the method's efficacy using a Berea sandstone sample.
Main Methods:
- Proposed a "three-step sampling" method for 3D porous medium reconstruction.
- Sampling points extracted from template centers and edge areas using a two-point correlation function.
- Continuity and variability controlled across adjacent layers during sampling.
Main Results:
- The three-step sampling method successfully reconstructed 3D porous media.
- Reconstructed results closely matched the original sample's statistical characteristics.
- Key properties like porosity, pore/throat size, and relative permeability were accurately reproduced.
Conclusions:
- The proposed three-step sampling method effectively reconstructs 3D porous media from 2D images.
- This technique ensures high fidelity in replicating the statistical properties of the original medium.
- The method offers a reliable approach for digital rock physics and material science applications.

