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Utilizing the strength conversion factor in the estimation of uniaxial compressive strength from the point load index

机译:利用强度转换因子从点载荷指数估算单轴抗压强度

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The strength conversion factor (k) is the ratio between the uniaxial compressive strength (UCS) and the point load index (PLI). It has been used to estimate the UCS from the PLI since the 1960s. Many researchers have investigated the relationship between UCS and PLI for various rock types of different geological origins, such as igneous, sedimentary, and metamorphic rocks. In this study, the k values for subclasses of igneous (pyroclastic, volcanic, and plutonic), sedimentary (chemical and clastic), and metamorphic (foliated and nonfoliated) rocks were evaluated. For this purpose, UCS and PLI data for a total of 410 rock samples extracted from literature published around the world as well as UCS and PLI data obtained in this work for 80 rock samples taken from the Eastern Black Sea Region in Turkey were evaluated together to determine the k values of different rock classes. Strength conversion factors were obtained using zero-intercept regression analysis, formulation, and a graphical approach. This study confirmed that there is no single k value that is applicable to all rock classes. According to statistical analyses, k varied between 12.98 and 18.55 for the rocks studied. These findings demonstrate that the k values derived in this work can be reliably used to estimate the strengths of rock samples with specific lithologies.
机译:强度转换系数(k)是单轴抗压强度(UCS)与点载荷指数(PLI)之间的比率。自1960年代以来,它一直被用于根据PLI估算UCS。许多研究人员针对不同地质起源的各种岩石类型(例如火成岩,沉积岩和变质岩)研究了UCS和PLI之间的关系。在这项研究中,评估了火成岩(碎屑岩,火山岩和深成岩),沉积岩(化学和碎屑岩)和变质岩(叶状和非叶状)子类别的k值。为此,对从世界各地出版的文献中提取的总共410个岩石样品的UCS和PLI数据,以及从土耳其东部黑海地区采集的80个岩石样品的这项工作中获得的UCS和PLI数据进行了评估,以便:确定不同岩石类别的k值。使用零截距回归分析,公式化和图形方法获得强度转换因子。这项研究证实,没有适用于所有岩石类别的单个k值。根据统计分析,所研究岩石的k在12.98至18.55之间变化。这些发现表明,这项工作中得出的k值可以可靠地用于估计具有特定岩性的岩石样品的强度。

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