块(置换群论)
地质学
岩体分类
断裂(地质)
岩土工程
数学
几何学
作者
Kaixing Wang,Bin Wu,Pan Yishan,A. P. Khmelinin,А. И. Чанышев
标识
DOI:10.1134/s1062739124020030
摘要
This article experimentally investigates the characteristics of $$P$$ -wave propagation in block rock mass when blocks fracture transversely and longitudinally. The velocity of $$P$$ -wave, rock block acceleration, kinetic energy, displacement response, and the time–frequency response of rock block were analyzed. The results show that when the rock block fractures, the $$P$$ -wave velocity decreases, the acceleration response duration time increases, and the maximum acceleration and kinetic energy decrease. However, transverse fractures show a more evident decrease in the acceleration and kinetic energy near the fracture area, and longitudinal fractures show a more evident decrease in the displacement amplitude far from the fracture area. On transverse fractures, the dominant frequency of acceleration and kinetic energy leads to a low value near the fracture area, but the dominant frequency of displacement—to a high value. Longitudinal fracture leads to a dominant frequency of block response occurrence time delayed far from the fracture area.
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