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Memory Effects in Rock Salt Under Triaxial Stress State and Their Use for Stress Measurement in a Rock Mass

机译:三轴应力状态下岩盐中的记忆效应及其在岩体应力测量中的应用

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Regularities of memory effects in rock salt specimens under triaxial stress state were investigated. Each specimen was subjected to two loading cycles. The first cycle was axisymmetric triaxial compression (#sigma#_1>#sigma_2=#sigma#_3). The second cycle was uniaxial compression in the direction of #sigma#_1 of the first cycle. Distinct acoustic emission (AE) and deformation memory effects were observed in the second cycle at the stress value equal to a linear combination of the first cycle principal stresses given by #sigma#_1-(k+1)_#sigma#_3, where k is about 0.5-0.6 for rock salt. Anomalies in deformation curves were found to be more reliable than the AE methods in distinguishing memory symptoms. The necessary pre-requisite for memory formation in the first cycle was that #sigma#_1 exceeded the elastic limit, corresponding to the given confining stress #sigma#_3. Inflections in uniaxial stress versus axial strain and lateral strain curves, in the second cycle, were observed at equal stress values if in the first cycle #sigma#_1 exceeded the elastic limit and memory-forming damage was induced. If there was no memory-forming damage, those inflections were seen at different stress values. This characteristic was used to distinguish between true memory effects and natural characteristic points in deformation curves derived from rock salt testing. A new memory symptom was established, namely a turn point in curve "uniaxial stress versus differential coefficient of lateral strains". The results form a basis for application of the memory effects for stress measurement in rock salt masses.
机译:研究了三轴应力状态下岩盐标本的记忆效应规律。每个样品经受两个加载循环。第一个周期是轴对称三轴压缩(#sigma#_1>#sigma_2 =#sigma#_3)。第二个循环是在第一个循环的#sigma#_1方向上进行单轴压缩。在第二循环中,在应力值等于由#sigma#_1-(k + 1)_#sigma#_3给出的第一循环主应力的线性组合的应力值下,观察到了明显的声发射(AE)和变形记忆效应。对于岩盐,k约为0.5-0.6。发现变形曲线异常在分辨记忆症状方面比AE方法更可靠。在第一个循环中形成记忆的必要前提是#sigma#_1超过了弹性极限,对应于给定的限制应力#sigma#_3。如果在第一个循环中#sigma#_1超过了弹性极限,并且诱发了记忆形成损伤,则在第二个循环中,在相同的应力值下观察到了单轴应力与轴向应变和横向应变曲线的变化。如果没有形成记忆的损伤,则可以在不同的应力值下看到这些变形。该特性用于区分真实的记忆效果和岩盐测试得出的变形曲线中的自然特性点。建立了新的记忆症状,即曲线“单轴应力与横向应变的微分系数”的转折点。这些结果为将记忆效应应用到岩盐岩体应力测量中奠定了基础。

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