花岗岩破裂过程中的声发射活动性研究

    STUDY ON THE AE ACTIVITY DURING THE FAILURE PROCESS OF GRANITE SAMPLES

    • 摘要: 当岩石受外力或内力作用产生变形或断裂时,产生声发射现象。声发射技术是一个用来研究岩石裂纹扩展过程的很好的工具。本文应用声发射技术,研究了单轴加载条件下花岗岩试样破裂失稳过程,应用单纯形方法对声发射事件进行定位,对加载过程中花岗岩的声发射活动性进行了分析。研究结果表明:声发射次数随着应变的增加而增加;通过声发射事件定位技术,在开始加载时,声发射事件分布的很散乱,但是随着荷载的增加,声发射事件逐步聚集,直至宏观发生破坏;声发射次数随时间变化出现逐渐增加趋势,但岩石宏观破坏之后,其声发射活动并没有立即停止,而有增加的趋势,这主要是由于应力场寻求新的平衡,声发射次数仍然增加。可见,声发射事件随时间的变化,可以很好的反映岩石宏观失稳破裂之后,其内部应力场达到新的应力平衡过程。

       

      Abstract: The rock sample will generate acoustic emission when the rock sample suffering the external or internal loading.AE technique is a good tool which is used to study the process of crack expansion.In this paper,AE technique was employed to study the failure process of granite samples under uniaxial compression loading,and analyze the AE activity of granite samples during the total loading process.The testing result indicated the AE events gradually increased with the strain changing.The Simplex technique was used to locate the position of AE events.From the result of AE location,we found the AE events distribute randomly in the initial loading.With the loading increasing,the AE events gradually congregated up to the rock failure.The AE events gradually increase with the time changing.After the granite samples failure the AE events continue to increase,which is mainly due to the internal stress achieving the new balance.From the result,we can conclude that AE events with time changing can be used to disclosure how to attain the new balance of the internal stress field after the rock sample marco-failure.

       

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