ZHANG Hui-mei, WANG Yun-fei. Multi-scale analysis of damage evolution of freezing-thawing red sandstones[J]. 2022, 43(8): 2103-2114.
DOI:
ZHANG Hui-mei, WANG Yun-fei. Multi-scale analysis of damage evolution of freezing-thawing red sandstones[J]. 2022, 43(8): 2103-2114.DOI: 10.16285/j.rsm.2021.1726.
Multi-scale analysis of damage evolution of freezing-thawing red sandstones
Wetake red sandstone as the research object and apply the freeze-thawcycles
CT scans and mechanical properties experiments. We use image processingtechnology combined with genetic algorithm optimization model to achieve the denoise
enhancement
segmentation and three-dimensional reconstruction of CT scanimages after 0
5
10
20
and 40 freeze-thaw cycles. With the damageidentification and comparative study of the same object across scales
weestablished a prediction formula of elastic modulus deterioration based onmesoscopic damage. Therefore
the macroscopic mechanical behavior offreeze-thaw red sandstones can be interpreted from the physical nature of the materialmeso-structure. The results show that genetic algorithm based on imagemaximum entropy can quickly and accurately select the threshold for imagesegmentation
and achieve the recognition of matrix and defects in rock meso-structure.With the increase of freezing and thawing cycles
the porosity of rockincreases
and the fractal dimension of pore decreases. On the meso-scale
theevolution shows that the pores expand and the number increases
but thestructural complexity decreases. The macroscopic and mesoscopic damagevariables defined by the traditional methods are based on the effective bearingarea and elastic modulus
and they fail to fully consider the damage physicalmechanism and the internal structure information of the material. The damageevolution curves are different. Based on the two physical mechanisms
we definethe meso-damage variable and the macro-damage variable that considers the naturalrock damage
which achieves the combination of macroscopic and mesoscopic damages.Finally
according to the relationship between meso-structure evolution andmacroscopic mechanical response in the process of freeze-thaw cycles
wepropose a prediction formula of elastic modulus degradation
and analyze thedifferent dominant roles of pore size and pore structure morphology through thedamage process. We interpret the mechanical mechanism of macroscopic sandstonefreeze-thaw damage based on the meso-structure physical mechanisms.