Abstract
The AE energy characteristics of granite specimens were tested experimentally under uniaxial compression to investigate the variation regulation of acoustic emission (AE) energy during the granite failure process. The results show that the AE energy accompanies rock deformation and failure during the entire loading process. With stress increase, AE energy of granite specimens is in dynamic variation. There is a fine corresponding relationship between AE energy and stress. Under low stress levels, AE energy is relative low and remains stable. As stress increases, in the plastic deformation stage, AE energy rapidly increases and remains at a high level indicating intense energy which is released before rock failure. This phenomenon could be considered as the precursor for rock failure. Moreover, the corresponding time point where the AE energy release rate reaches the maximum is determined as the critical point for predicting rock failure. Then AE energy sharply decreases in the failure stage and rock instability occurs.
Kurzfassung
Um das Variationsgesetz der Schallemissionsenergie während des Versagens von Granit zu untersuchen, wurden experimentelle Untersuchungen zu den Charakteristika der Schallemissionsenergie von Granitproben unter einachsiger Druckbeanspruchung durchgeführt. Die Ergebnisse zeigen, dass die Schallemissionsenergie die Gesteinsverformung und das Versagen während des gesamten Belastungsprozesses begleitet. Wenn die Spannung zunimmt, ist die Schallemissionsenergie unter dynamischer Variation. Es besteht eine Abhängigkeit zwischen der Schallemissionsenergie und der Spannung. Bei niedrigen Spannungsniveaus ist die Schallemissionsenergie klein und bleibt stabil. Wenn die Spannung zunimmt, steigt die Schallemissionsernergie im Bereich der plastischen Verformung rapide an und verbleibt auf hohem Niveau, was darauf hindeutet, dass seine intensive Energie freigesetzt wird, bevor das Gestein versagt. Dieses Phänomen kann als Vorankündigung für das Gesteinsversagen gedeutet werden. Darüber hinaus wurde der entsprechende Zeitpunkt, an dem die Freisetzungsrate der Schallemissionsernergie den maximalen Wert erreicht, als kritischer Punkt zur Vorhersage des Gesteinsversagens ermittelt. Danach nimmt die Schallemissionsenergie im Versagensstadium rapide ab und es tritt Instabilität des Gesteins auf.
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