| Project/Area Number |
59420037
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| Research Category |
Grant-in-Aid for General Scientific Research (A)
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| Allocation Type | Single-year Grants |
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| Research Field |
資源開発工学
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| Research Institution | Kyoto University |
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Principal Investigator |
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| Project Period (FY) |
1984 – 1985
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| Project Status |
Completed (Fiscal Year 1985)
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| Budget Amount *help |
¥21,300,000 (Direct Cost: ¥21,300,000)
Fiscal Year 1985: ¥3,000,000 (Direct Cost: ¥3,000,000)
Fiscal Year 1984: ¥18,300,000 (Direct Cost: ¥18,300,000)
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| Keywords | Application of AE Measurement / Prediction of Microcracking / Localization of Dilatancy / AE震源決定 |
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| Research Abstract |
An experimental research has been carried out for the application of acoustic emission (AE) measurement to predict microcracking in rock.
The localization of dilatancy during creep of Oshima granite under uniaxial compression was investigated by locating hypocenters of AE events. It was found that the mechanical behavior of Oshima granite was controlled by the localization of microcracks. During the loading up to the creep stress, the hypocenters of AE events were randomly distributed throughout the specimen. As soon as the creep began, abrupt migration and clustering of AE hypocenters into several near-surface zones were observed. AE events formed volumetric concentrations. This migration and clustering strongly suggested the rapid localized development of dilatancy at the beginning of the primary creep.
By the end of the primary creep, AE events began to concentrate into one of these cluster, while the activity of others gradually decayed. In the most active cluster, clustering of AE events by itself gave rise to more AE events preceding faulting. The shape of this cluster was spheroidal with the long axis parallel to the loading axis. The development of localized dilatancy identified by hypocenter locations was also confirmed by the surface strain mapping.
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