Table 1 Fractal dimensions of waviness and unevenness of rock joint sample S1 at varying sample sizes.
From: Unveiling the mystery of scale dependence of surface roughness of natural rock joints
Resolution (mm) | Fractal estimation | Sample size (\(\mathrm mm \times mm\)) | |||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|
\(100 \times 100\) | \(200 \times 200\) | \(300 \times 300\) | \(400 \times 400\) | \(500 \times 500\) | \(600 \times 600\) | \(700 \times 700\) | \(800 \times 800\) | \(900 \times 900\) | \(1000 \times 1000\) | ||
0.5 | \(D_w\) | 2.1520 | 2.1617 | 2.1865 | 2.1585 | 2.2316 | 2.2106 | 2.2273 | 2.2316 | 2.2623 | 2.2505 |
\(A_w\) | − 3.373 | − 3.237 | − 3.074 | − 3.093 | − 2.909 | − 3.028 | − 3.006 | − 3.020 | − 2.938 | − 2.973 | |
\(R^2_w\) | 0.9985 | 0.9992 | 0.9979 | 0.9989 | 0.9949 | 0.9977 | 0.9972 | 0.9982 | 0.9946 | 0.9937 | |
\(D_u\) | 2.6782 | 2.7546 | 2.7019 | 2.7190 | 2.7312 | 2.8284 | 2.7409 | 2.8942 | 2.8792 | 2.8776 | |
\(A_u\) | − 2.169 | − 1.875 | − 1.948 | − 1.822 | − 1.836 | − 1.409 | − 1.796 | − 1.210 | − 1.287 | − 1.149 | |
\(R^2_u\) | 0.9955 | 0.9421 | 0.9582 | 0.9323 | 0.9455 | 0.9338 | 0.9265 | 0.9251 | 0.9285 | 0.9674 | |
1.0 | \(D_w\) | 2.2594 | 2.2145 | 2.2341 | 2.1845 | 2.2678 | 2.2544 | 2.2641 | 2.2713 | 2.3010 | 2.3042 |
\(A_w\) | − 2.410 | − 2.445 | − 2.389 | − 2.391 | − 2.207 | − 2.304 | − 2.309 | − 2.316 | − 2.251 | − 2.216 | |
\(R^2_w\) | 1.0000 | 0.9997 | 0.9987 | 0.9987 | 0.9985 | 0.9979 | 0.9986 | 0.9996 | 0.9967 | 0.9945 | |
\(D_u\) | 2.6913 | 2.7627 | 2.8697 | 2.8753 | 2.6819 | 2.8871 | 2.8554 | 2.9061 | 2.8976 | 2.9208 | |
\(A_u\) | − 2.002 | − 1.743 | − 1.303 | − 1.163 | − 1.161 | − 1.171 | − 1.277 | − 1.132 | − 1.191 | − 0.962 | |
\(R^2_w\) | 0.9954 | 0.9493 | 0.9368 | 0.9181 | 0.9258 | 0.9325 | 0.9848 | 0.9238 | 0.9171 | 0.9273 | |
2.0 | \(D_w\) | 2.4097 | 2.1913 | 2.2624 | 2.1844 | 2.3209 | 2.2796 | 2.2936 | 2.2872 | 2.3509 | 2.3505 |
\(A_w\) | − 1.573 | − 1.954 | − 1.710 | − 1.818 | − 1.535 | − 1.687 | − 1.696 | − 1.749 | − 1.590 | − 1.564 | |
\(R^2_w\) | 1.0000 | 0.9975 | 0.9920 | 0.9963 | 0.9960 | 0.9953 | 0.9972 | 0.9990 | 0.9956 | 0.9903 | |
\(D_u\) | 2.7348 | 2.8312 | 2.8836 | 2.8415 | 2.8879 | 2.9206 | 2.9379 | 2.9366 | 2.9460 | 2.935 | |
\(A_u\) | − 1.630 | − 1.541 | − 1.295 | − 1.298 | − 1.215 | − 1.128 | − 1.099 | − 1.118 | − 1.101 | − 0.941 | |
\(R^2_u\) | 1.0000 | 1.0000 | 0.9113 | 0.9124 | 0.9118 | 0.9783 | 0.9756 | 0.9918 | 0.9531 | 0.9326 | |