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岩体二次应力
岩体开挖后原始应力大小和方向发生变化的应力。在岩体中开挖坑硐后,打破了岩体原始应力的平衡状态,在坑硐附近一定范围的岩体中发生应力重新分布,形成二次应力场,岩体二次应力分布,与岩体原始应力的主应力方向、大小和坑硐的几何形状及岩体结构有关
expl.
induced stress in rock mass
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