岩体弹性波速度是组成岩体的岩石性质、岩体结构、赋存环境的综合反映。
Rock mass elastic wave velocity is the synthesized reflection of rock quality, rock mass structure, and rock mass existing environment.
同时,也为进一步建立岩体结构合理的损伤演化方程、本构关系和研究岩石破坏机理提供了科学依据。
At the same time, some scientific hypotheses of the damage evolution equations and stress-strain relationship as well as the failure mechanism of rock mass are also proposed.
对于深埋岩石工程,岩体的地应力状态直接关系到工程的稳定性。
To the deep rock engineering, stress state of rock mass directly influences the stability of project.
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