Table 1 The representative correlations between UCS (MPa) and Brazilian tensile strength (MPa).
Equations | R2 | Rock-types | No. of samples | References |
---|---|---|---|---|
\(\:\text{UCS=(4-10)BTS}\) | – | – | – | Hosking20 |
\(\:\text{UCS=(17-28)BTS}\) | – | Coal | – | Pomeroy and Foote21 |
\(\:\text{UCS=3.27BTS}-\text{0.97}\) | – | Limestone, sandstone, mudstone and siltstone | – | Hobbs23 |
\(\:\text{UCS=2.84BTS}-\text{3.39}\) | – | Limestone, sandstone, mudstone and siltstone | – | Hobbs24 |
\(\:\text{UCS=3.6}\text{BTS}\text{+15.2}\) | – | Coal measure rocks | 229 | Szlavin22 |
\(\:\text{UCS=(8-14)BTS}\) | – | Igneous rocks (Hong Kong, China) | – | Lumb25 |
\(\:\text{UCS=(7.9-9.72)BTS}\) | – | Granite, basalt, quartzite (India) | 13 | Gupta and Rao26 |
\(\:\text{UCS=12.2BTS}\) | – | Limestone (Nigeria) | – | Teme28 |
\(\:\text{UCS=(10-20)BTS}\) | – | Mudstone, limestone, granite, sandstone | – | Brook29 |
\(\:\text{UCS=(5-50)BTS}\) | – | Various rock types | – | Lade30 |
\(\:\text{UCS=6.71}\text{BTS}\text{+36.0}\) | 0.61 | Sandstone (South Africa) | 27 | Bell and Lindsay31 |
\(\:\text{UCS=(6.74-10.26)BTS}\) | – | Granite and limestone | – | Din and Rafiq32 |
\(\:\text{UCS=6.67}\text{BTS}\text{+0.73}\) | 0.92 | Granite, granodiorite (Turkey) | 10 | Tuğrul and Zarif33 |
\(\:\text{UCS=8BTS}\) | – | Brittle rocks | - | Brady and Brown34 |
\(\:\text{UCS=6.8}\text{BTS}\text{+13.5}\) | 0.65 | Greywackes (Turkey) | 82 | Gokceoglu and Zorlu35 |
\(\:\text{UCS=4.9BTS}\) | – | Calcarenite | 5 | Coviello et al.36 |
\(\:\text{UCS=6.2BTS}\) | – | Gasbeton | ||
\(\:\text{UCS=2.38}{\text{BTS}}^{\text{1.0725}}\) | 0.79 | Limestone, granite, marble (Turkey) | – | Altindag and Guney27 |
\(\:\text{UCS=2.86}{\text{e}}^{\text{0.015}}\text{BTS}\) | - | Coal | – | Arioglu and Tokgoz37 |
\(\:\text{UCS=10.61BTS}\) | 0.54 | Limestone, marble, Serpentinite (Turkey) | 46 | Kahraman et al.38 |
\(\:\text{UCS=5.86}\text{BTS}\text{+17.5}\) | – | Limestone (Iran) | 32 | Rajabzadeh et al.39 |
\(\:\text{UCS=8.60BTS}-\text{27.57}\) | – | Diagenetic dolomitic limestone (Iran) | ||
\(\:\text{UCS=12.4BTS}-\text{9.0}\) | – | – | – | Sivakugan et al.40 |
\(\:\text{UCS=7.22}\text{BTS}\text{+40.077}\) | 0.61 | Granite, granodiorite (Turkey) | 6 | Yesiloglu-Gultekin et al.41 |
\(\:\text{UCS=4.874}\text{BTS}\text{+24.301}\) | 0.90 | Metabasalt, dacite, basalt (Turkey) | 37 | Karaman et al.42 |
\(\:\text{UCS=15.36BTS}-\text{10.303}\) | Shale, old alluvium (Nusajaya, Malaysia) | 40 | Mohamad et al.43 | |
\(\:\text{UCS=10.03}\text{BTS}\text{+55.19}\) | 0.92 | Hornfels schist (Iran) | 8 | Fereidooni44 |
\(\:\text{UCS=10.4}\text{BTS}\text{+18.2}\) | 0.63 | Flint (Europe) | 7 | Aliyu et al.13 |
\(\:\text{UCS=3.469}\text{BTS}\text{+15.73}\) | Travertine (Iran) | 32 | Ebdali et al.45 | |
\(\:\text{UCS=7.73}{\text{BTS}}^{\text{1.197}}\) | 0.90 | Andesite, limestone, marble (Turkey) | 93 | Teymen and Mengüç46 |
\(\:\text{UCS=4.2327}\text{BTS}\text{+13.638}\) | 0.53 | Gypsum (United Arab Emirates) | 48 | Arman47 |
\(\:\text{UCS=7.26}\text{BTS}\) | 0.95 | Carbonate rocks (Iran) | 107 | Sadeghi et al.48 |
\(\:\text{UCS=8.1442}\text{BTS}\) | 0.83 | Various | 443 | Kong et al.49 |