| Literature DB >> 35474065 |
Jing Chai1,2, Yibo Ouyang3, Jinxuan Liu3,4, Dingding Zhang3,4, Wengang Du3, Jianfeng Yang3,4, Yongliang Liu3, Zhe Ma3.
Abstract
To overcome the limitation of the virtual extensometer method in measuring the crack opening displacement (COD) in the process of complex multi-crack propagation of rock, the measurement error of Digital Image Correlation (DIC) local deformation is theoretically analyzed. An improved virtual extensometer method for measuring the COD is proposed, which considers the temporal and spatial characteristics of crack development in the process of complex crack propagation. The accuracy of the proposed method is verified by the strain localization band numerical simulation test and indoor single crack simulation test. Furthermore, the method is applied to the two-dimensional similarity simulation test of simulating complex multi-fractures in rock stratum. The COD obtained by the traditional and improved methods is compared with the measured COD. The results show that in the case of multiple complex cracks, to obtain the COD accurately, the relative distance between the virtual extensometer measuring point and the crack should be greater than half of the sum of the width of the crack strain localization zone and the subset size. With the development of the crack, the relative distance between the virtual extensometer measuring point and the crack should increase with the increase of the width of the crack strain localization zone. The error of the COD measured by the traditional method increases with fracture development, and the maximum is 21.20%. The maximum relative error between the COD measured by the improved method and the measured crack opening is 3.61%. The research results improve the accuracy of the virtual extensometer in measuring the COD under complex multi-crack conditions.Entities:
Year: 2022 PMID: 35474065 PMCID: PMC9042950 DOI: 10.1038/s41598-022-08393-9
Source DB: PubMed Journal: Sci Rep ISSN: 2045-2322 Impact factor: 4.996
Figure 1Calculation principle of digital image correlation strain.
Figure 2Diagram of deformation around fracture measured by DIC.
Figure 3Implementation plan of improved method.
Figure 4Schematics of improved method.
Figure 5Numerical simulation of strain localization band.
Figure 6High precision displacement platform.
Figure 7DIC strain nephogram and measuring point layout.
Figure 8DIC measurement line test results.
Figure 9DIC measurement results.
Physical and mechanical properties of the strata.
| Layer number | Lithology | Thickness/m | Thickness of the model/cm | Ratio (sand: gypsum: CaCO3: coal) | Sand/kg | Gypsum/kg | CaCO3/kg |
|---|---|---|---|---|---|---|---|
| 1 | Loess | 42.00 | 28.0 | 1019 | 238.25 | 2.38 | 21.44 |
| 2 | Sandy mudstone | 14.76 | 9.8 | 919 | 82.89 | 0.92 | 8.29 |
| 3 | Siltstone | 21.55 | 14.4 | 837 | 119.53 | 4.48 | 10.46 |
| 4 | Medium sand | 28.75 | 19.2 | 837 | 159.47 | 5.98 | 13.95 |
| 5 | Siltstone | 6.70 | 4.5 | 937 | 37.63 | 1.25 | 2.93 |
| 6 | Medium sand | 9.96 | 6.6 | 828 | 55.24 | 1.38 | 5.52 |
| 7 | 1–2 Coal seam | 1.89 | 1.3 | 5.13 | 0.19 | 1.28 | |
| 8 | Fine sandstone | 2.85 | 1.9 | 937 | 16.01 | 0.53 | 1.24 |
| 9 | Fine sandstone | 6.55 | 4.4 | 837 | 36.33 | 1.36 | 3.18 |
| 10 | Siltstone | 3.80 | 2.5 | 828 | 21.08 | 0.53 | 2.11 |
| 11 | Fine sandstone | 5.90 | 3.9 | 837 | 32.73 | 1.23 | 2.86 |
| 12 | Siltstone | 1.00 | 0.7 | 937 | 5.62 | 0.19 | 0.44 |
| 13 | Fine sandstone | 11.00 | 7.3 | 828 | 61.01 | 1.53 | 6.10 |
| 14 | Fine sandstone | 2.16 | 1.4 | 937 | 12.13 | 0.27 | 1.08 |
| 15 | 2-2Coal seam | 4.60 | 3.1 | 12.48 | 0.47 | 3.12 | |
| 16 | Siltstone | 3.54 | 2.4 | 937 | 19.88 | 0.66 | 1.55 |
| 17 | Fine sandstone | 8.70 | 5.8 | 837 | 48.26 | 1.81 | 4.22 |
Figure 10Two-dimensional similar physical model and test.
Figure 11Development characteristics of complex multi-fracture.
Figure 12Layout of traditional method measuring points.
Figure 13Layout of improved method measuring points.