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Fracture growth on Långören Island, Finland, on the hottest day on record in 2014 Rodrigo Alcaino-Olivares, Derek Hayden, Matthew A. Perras Department of Civil Engineering, York University, Toronto, Ontario, Canada Kerry Leith, Simon Loew Engineering Geology Group, ETHZ, Zurich, Switzerland ABSTRACT Cyclic variation of temperature and its potential effect on crack growth have recently been observed in a few select geological environments. The current research presents a site investigation on Långören Island (Finland) where acoustic emission, crack meter and weather parameters including air and rock temperature sensors were installed. In addition, laboratory tests for Indirect Tensile Strength and P-wave velocity were conducted. Results suggest that large temperature variations are affecting the shallow layer of the rock surface which can be associated with cumulative acoustic emission events. Laboratory tests indicate a variation in P-wave velocity at different orientations, suggesting that anisotropy could be the result of preferred micro-cracks orientations. Ongoing data collection and correlations between crack growth and the climatic variables will help improve our understanding of the crack growth mechanism.

MS Word Technical Paper Template - geoedmonton2018.ca file · Web viewFracture growth on Långören Island, Finland, on the hottest day on record in 2014. Rodrigo Alcaino-Olivares,

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Fracture growth on Långören Island, Finland, on the hottest day on record in 2014Rodrigo Alcaino-Olivares, Derek Hayden, Matthew A. PerrasDepartment of Civil Engineering, York University, Toronto, Ontario, CanadaKerry Leith, Simon LoewEngineering Geology Group, ETHZ, Zurich, Switzerland

ABSTRACTCyclic variation of temperature and its potential effect on crack growth have recently been observed in a few select geological environments. The current research presents a site investigation on Långören Island (Finland) where acoustic emission, crack meter and weather parameters including air and rock temperature sensors were installed. In addition, laboratory tests for Indirect Tensile Strength and P-wave velocity were conducted. Results suggest that large temperature variations are affecting the shallow layer of the rock surface which can be associated with cumulative acoustic emission events. Laboratory tests indicate a variation in P-wave velocity at different orientations, suggesting that anisotropy could be the result of preferred micro-cracks orientations. Ongoing data collection and correlations between crack growth and the climatic variables will help improve our understanding of the crack growth mechanism.