2015
DOI: 10.1016/j.ijrmms.2015.01.006
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The rock stress memory unrecoverable by the Kaiser effect method

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Cited by 26 publications
(6 citation statements)
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“…There were no apparent AE events in different cycles at the same level, and numerous events occurred only when the load in first cycle was greater than the maximum load of the previous level (A and B in Figure 6(b)). The Kaiser effect was clear 33 for sandstones under tiered cyclic loading and unloading and appeared in every cycle. Stress continued to increase after the end of the cyclic loading and unloading, and the number of AE events increased sharply when the rock approached its peak stress value.…”
Section: Evolution Of Acoustic-emission Eventsmentioning
confidence: 94%
“…There were no apparent AE events in different cycles at the same level, and numerous events occurred only when the load in first cycle was greater than the maximum load of the previous level (A and B in Figure 6(b)). The Kaiser effect was clear 33 for sandstones under tiered cyclic loading and unloading and appeared in every cycle. Stress continued to increase after the end of the cyclic loading and unloading, and the number of AE events increased sharply when the rock approached its peak stress value.…”
Section: Evolution Of Acoustic-emission Eventsmentioning
confidence: 94%
“…The above results suggest that TMM could be used as an oriented core method in the future. However, as stated by Lavrov (2003), Ljunggren et al (2003), andHsieh et al (2015), there are several factors that can affect the results of stress measurements by oriented core methods. It was necessary to investigate the effects prior to any practical use of TMM or any other oriented core method.…”
Section: Influences Of Various Factorsmentioning
confidence: 99%
“…When the dilatation of the rock occurs due to the applied stress, the Kaiser effect disappears. Usually the dilatancy stress (crack initiation stress) does not exceed 70-80% of the uniaxial compressive strength (σ c ) [23][24][25][26]. When the first loading stress level is less than 30% of σ c in the compaction stage of stress-strain curve of the rock, the Kaiser effect can be easily misjudged due to the acoustic emission generated from closure of original fissures and sliding friction between particles in the rock.…”
Section: Introductionmentioning
confidence: 99%
“…The influence of short delay duration on Kaiser effect is small. As time passes (long delay time), the Kaiser effect of some rocks will disappear gradually [23][24][25][26][27]. (3) The loading rate and lithology can affect the evolution of Felicity rate and occurrence of the Kaiser effect.…”
Section: Introductionmentioning
confidence: 99%