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Relationship between point load strength and uniaxial compressive strength of hydrothermally altered soft rocks

机译:水热蚀变软岩单点抗压强度与单轴抗压强度的关系

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We clarified relationships between point load strength (PLS) and uniaxial compressive strength (UCS) in hydrothermally altered soft rocks found in northeastern Hokkaido, Japan, using axial and irregular lump PLS test specimens. The numbers of specimens tested were 1,755 and 2,123 rock specimens for the axial and irregular lump PLS tests, respectively, and 329 rock specimens for the UCS test. The rock specimens underwent PLS and UCS tests using a laboratory testing machine with specimens in forced-dry and forced-wet states. The correlations between the PLS and the UCS were linear. The UCS was 11.1 times larger than the axial PLS, and 4.7 times larger than the irregular lump PLS, respectively, in soft rocks with a UCS below 25MPa.We could calculate the UCS from PLS tests on soft rocks only when their UCSs were below 25MPa.
机译:我们使用轴向和不规则块状PLS试样阐明了在日本北海道东北部发现的热液蚀变软岩中的点载荷强度(PLS)和单轴抗压强度(UCS)之间的关系。对于轴向和不规则块状PLS测试,测试的样本数量分别为1,755和2,123;对于UCS测试,测试的样本数量为329。岩石样本使用实验室测试机进行了PLS和UCS测试,样本处于强迫干燥和强迫湿润状态。 PLS和UCS之间的相关是线性的。 UCS低于25MPa的软岩的UCS分别是轴向PLS的11.1倍和不规则块状PLS的4.7倍,只有当UCS低于25MPa时,我们才能通过PLS试验计算出UCS 。

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