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Development of fracture processes in Silesian Carboniferous sandstones

机译:西里西亚石炭系砂岩破裂过程的发展

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The development of fracture processes in selected Carboniferous rocks from the Upper Silesian Coal Basin is described, with particular regard to the behaviour of rock specimens in the post-failure stage. The fracture processes were monitored using the stress-strain relations, coupled with acoustic emission, recorded during loading. Energy accumulation and dissipation phenomena were observed during rock loading. Cracking was recorded on the stress-strain curves as deformation loops, accompanied by significant stress decreases, and as cyclic increases in acoustic emission activity. Observing and analysing stages of high acoustic emission and stress drops enabled determination of three ways ("schemes") in which fracture originated and developed during the post-critical stage. Scheme I is damage and movement of grains and rock cement, scheme II is destruction of single rock grains of particular resistance, and scheme III is a dislocational and slide deformation of the rock medium.
机译:描述了上西里西亚煤盆地中某些石炭系岩石破裂过程的发展,特别是考虑了断裂后阶段的岩石样本行为。使用应力-应变关系以及加载过程中记录的声发射来监测断裂过程。在岩石加载过程中观察到能量积累和耗散现象。应力-应变曲线上的裂纹被记录为变形环,伴随着应力的显着减小以及声发射活动的周期性增加。观察和分析高声发射和应力下降阶段可以确定在后临界阶段裂缝发生和发展的三种方式(“方案”)。方案I是谷物和岩石水泥的破坏和运动,方案II是具有特殊抵抗力的单个岩石颗粒的破坏,方案III是岩石介质的错位和滑动变形。

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