Table 2 Fractal dimensions of waviness and unevenness of rock joint sample S2 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 | \(D_w\) | 2.1663 | 2.2253 | 2.2264 | 2.2501 | 2.2412 | 2.2200 | 2.2330 | 2.2508 | 2.447 | 2.2242 |
\(A_w\) | − 3.248 | − 3.114 | − 3.091 | − 3.004 | − 2.988 | − 3.070 | − 3.029 | − 2.978 | − 2.972 | − 3.059 | |
\(R^2_w\) | 0.9978 | 0.9959 | 0.9952 | 0.9944 | 0.9960 | 0.9985 | 0.9974 | 0.9968 | 0.9962 | 0.9976 | |
\(D_u\) | 2.6690 | 2.7391 | 2.6969 | 2.7573 | 2.6501 | 2.7402 | 2.7288 | 2.7443 | 2.7335 | 2.7737 | |
\(A_u\) | − 2.142 | − 1.900 | − 1.972 | − 1.763 | − 2.171 | − 1.857 | − 1.881 | − 1.852 | − 1.855 | − 1.579 | |
\(R^2_u\) | 0.9898 | 0.9393 | 0.9000 | 0.9745 | 0.9928 | 0.9175 | 0.9305 | 0.9193 | 0.9119 | 0.9395 | |
1.0 | \(D_w\) | 2.2448 | 2.3214 | 2.2892 | 2.3257 | 2.2884 | 2.2586 | 2.2754 | 2.2944 | 2.2852 | 2.2664 |
\(A_w\) | − 2.471 | − 2.252 | − 2.317 | − 2.212 | − 2.259 | − 2.364 | − 2.314 | − 2.269 | − 2.271 | − 2.335 | |
\(R^2_w\) | 1.0000 | 0.9978 | 0.9950 | 0.9941 | 0.9993 | 0.9993 | 0.9989 | 0.9991 | 0.9973 | 0.9988 | |
\(D_u\) | 2.6250 | 2.6325 | 2.8642 | 2.9069 | 2.6473 | 2.9132 | 2.8751 | 2.9210 | 2.9117 | 2.9195 | |
\(A_u\) | − 2.062 | − 2.057 | − 1.315 | − 1.199 | − 1.989 | − 1.180 | − 1.281 | − 1.148 | − 1.153 | − 0.976 | |
\(R^2_w\) | 1.0000 | 0.9977 | 0.9363 | 0.9761 | 0.9962 | 0.9496 | 0.9585 | 0.9941 | 0.9230 | 0.9277 | |
2.0 | \(D_w\) | 2.2194 | 2.3634 | 2.3395 | 2.3433 | 2.3378 | 2.2842 | 2.2892 | 2.3141 | 2.3313 | 2.2840 |
\(A_w\) | − 2.037 | − 1.627 | − 1.666 | − 1.646 | − 1.645 | − 1.759 | − 1.764 | − 1.701 | − 1.617 | − 1.762 | |
\(R^2_w\) | 1.0000 | 0.9911 | 0.9906 | 0.9930 | 0.9969 | 0.9992 | 0.9978 | 0.9982 | 0.9958 | 0.9975 | |
\(D_u\) | 2.7017 | 2.8733 | 2.8909 | 2.9162 | 2.9193 | 2.9588 | 2.9654 | 2.9606 | 2.9593 | 2.9542 | |
\(A_u\) | − 1.750 | − 1.384 | − 1.297 | − 1.267 | − 1.263 | − 1.118 | − 1.092 | − 1.113 | − 1.095 | − 0.936 | |
\(R^2_u\) | 1.0000 | 1.0000 | 0.9550 | 0.9194 | 0.9226 | 0.9224 | 0.9181 | 0.9912 | 0.9358 | 0.9598 | |