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Comparison Between Stress and Strain Quantities of the Failure–Deformation Process of Fennoscandian Hard Rocks Using Geological Information

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Abstract

The aim of this paper was to compare the stress and strain quantities that are related to the failure–deformation process of hard rock. The data used here was obtained from laboratory uniaxial compression tests performed on different types of Fennoscandian hard rocks. The failure–deformation process quantities were compared at each deformation stage and for each single specimen. Moreover, geological information such as the rock origin process and the rock characteristics of the specimens were studied and linked to the stress and strain quantities. The purpose was to investigate the influence of the rock origin process and rock characteristics on these quantities. The main results of this study showed that the normalized crack damage lateral strain (ε 3cd/ε 3p ) and the volumetric strain (ε crv−ci and ε v−cd) quantities were strongly affected by the grain size. The normalized and volumetric quantities are weakly dependent on the mineral composition.

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References

  • Bieniawski ZT (1967) Mechanism of brittle rock fracture. Part I Theory of the fracture process. Int J Rock Mech Min Sci 4(4):395–406. doi:10.1016/0148-9062(67)90030-7

    Article  Google Scholar 

  • Brown ET (1981) Rock characterization testing and monitoring ISRM suggested methods. Pergamon Press, Oxford

    Google Scholar 

  • Carlsson B, Nordlund E, Andersson Y, Lindfors U (1999) The failure process and the acoustic emission of brittle rock under compression. In: Vouille G, Berest P (eds) 9th International Congress on Rock Mechanics, vol 2. Balkema, Paris, pp 569–572

    Google Scholar 

  • Diederichs MS (1999) Instability of hard rock masses: the role of tensile damage and relaxation. Doctoral thesis, University of Waterloo, Canada

  • Eberhardt E, Stead D, Stimpson B, Read RS (1998) Identifying crack initiation and propagation thresholds in brittle rock. Can Geotech J 35(2):222–233

    Article  Google Scholar 

  • Eberhardt E, Stead D, Stimpson B (1999a) Quantifying progressive pre-peak brittle fracture damage in rock during uniaxial compression. Int J Rock Mech Min 36(3):361–380. doi:10.1016/S0148-9062(99)00019-4

    Article  Google Scholar 

  • Eberhardt E, Stimpson B, Stead D (1999b) Effects of grain size on the initiation and propagation thresholds of stress-induced brittle fractures. Rock Mech Rock Eng 32(2):81–99

    Article  Google Scholar 

  • Einstein HH, Baucher GB (1983) Probabilistic and statistical methods in engineering geology. Specific methods and examples. Part 1: exploration. Rock Mech Rock Eng 16(1):39–72. doi:10.1007/BF01030217

    Article  Google Scholar 

  • Eloranta P, Hakala P (1998) Laboratory testing of Kivetty porphyritic granodiorite in borehole KI-KR10. Posiva 98-49, Finland

  • Eloranta P, Hakala P (1999a) Laboratory testing of Hästholmen pyterlite in borehole HH-KR6. Posiva 98-26, Finland

  • Eloranta P, Hakala P (1999b) Laboratory testing of Hästholmen equigranular rapakivi granite in borehole HH-KR6. Posiva 98-47, Finland

  • Hakala M, Heikkilä E (1997a) Laboratory testing of Olkiluoto mica gneiss in borehole OL-KR10. POSIVA-97-07, Finland

  • Hakala M, Heikkilä E (1997b) Summary report—development of laboratory tests and the stress-strain behaviour of Olkiluoto mica gneiss. POSIVA-97-04, Finland

  • Hatzor YH, Palchic V (1997) The influence of grain size and porosity on crack initiation stress and critical flaw length in dolomites. Int J Rock Mech Min 34(5):805–816. doi:10.1016/S1365-1609(96)00066-6

    Article  Google Scholar 

  • Heikkilä E, Hakala M (1998a) Laboratory testing of Kivetty granite in borehole KI-KR10. POSIVA-98-21e, Finland

  • Heikkilä E, Hakala M (1998b) Laboratory testing of Romuvaara tonalite gneiss in borehole RO-KR10. POSIVA-98-06e, Finland

  • Hudson JA, Harrison JP (1983) Engineering rock mechanics. An introduction to the principles. Pergamon, Oxford

  • Martin CD, Chandler NA (1994) The progressive fracture of Lac du Bonnet granite. Int J Rock Mech Min Sci Geomech Abstr 31(6):643–659. doi:10.1016/0148-9062(94)90005-1

    Article  Google Scholar 

  • Press F, Siever R (1986) Earth. W.H. Freeman and Company, New York

    Google Scholar 

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Acknowledgments

K. P. Hidalgo would like to express her gratitude to the Rock Engineering Research Foundation (BeFo), Trafikverket (The Swedish Transport Administration), and the Swedish Nuclear Fuel and Waste Management Co. (SKB) for financial support for this research project. The authors also acknowledge the support through the Centre of Advanced Mining and Metallurgy (CAMM) at Luleå University of Technology (LTU). K. P. Hidalgo also wishes to thank her assistant supervisor, Adjunct Professor Jonny Sjöberg at Itasca Consultants AB, Sweden, for his suggestions and comments. The authors also thank Mikael Nilsson for checking the English.

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Correspondence to Kelvis Pérez Hidalgo.

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Pérez Hidalgo, K., Nordlund, E. Comparison Between Stress and Strain Quantities of the Failure–Deformation Process of Fennoscandian Hard Rocks Using Geological Information. Rock Mech Rock Eng 46, 41–51 (2013). https://doi.org/10.1007/s00603-012-0242-1

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  • DOI: https://doi.org/10.1007/s00603-012-0242-1

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