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Thermal damage pattern and thresholds of granite

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Abstract

High temperature may lead to the development of new microcracks or growth of pre-existing microcracks within granite, varying its physical and mechanical properties. Experiments were conducted to study the evolution of the physical and mechanical properties of granite specimens from room temperature to 800 °C. The specimens were heated in heating furnace and uniaxial compression tests were done using MTS servo-controlled testing machine. The results indicate five phases in the variation of physical and mechanical properties with temperature: from room temperature to 100, 100–300, 300–400, 400–600, and 600–800 °C. The first phase corresponds to the vaporization-escaping interval of adhered water, bound water, and structural water. Larger changes of physical and mechanical parameters in the temperature range of 300–600 °C, mostly 400–600 °C, are probably caused by the transition from the brittle state to plasticity (or ductility) of granite, and 400 °C may be a critical threshold of its thermal damage. These results confirm the important link among physical and mechanical properties in response to thermal treatment.

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References

  • Albaric J, Déverchère J, Petit C, Perrot J, Gall BL (2009) Crustal rheology and depth distribution of earthquakes: insights from the central and southern East African rift system. Tectonophysics 468:28–41

    Article  Google Scholar 

  • Alm O, Jaktlund LL, Kou SQ (1985) The influence of microcrack density on the elastic and fracture mechanical properties of stropa granite. Phys Earth Planet Inter 40:161–171

    Article  Google Scholar 

  • Anderson CA, Bridwell RJ (1980) A finite element method for studying the transient non-linear thermal creep of geological structures. Int J Rock Mech Min Sci Geomech Abstr 4:255–276

    Google Scholar 

  • Bauer S J, Johnson B (1979) Effects of slow uniform heating on the physical properties of the westerly and charcoal granites. In: Proceedings of the 20th US symposium on rock mechanic, Austin, 4–6 June 1979, pp 7–18

  • Björnsson A (2008) Temperature of the Icelandic crust: inferred from electrical conductivity, temperature surface gradient, and maximum depth of earthquakes. Tectonophysics 447:136–141

    Article  Google Scholar 

  • Blanpied ML, Marone CJ, Lockner DA, Byerlee JD, King DP (1998) Quantitative measure of the variation in fault rheology due to fluid-rock interactions. J Geophys Res 103(B5):9691–9712

    Article  Google Scholar 

  • Chaki S, Takarli M, Agbodjan WP (2008) Influence of thermal damage on physical properties of a granite rock: porosity, permeability and ultrasonic wave evolutions. Constr Build Mater 22:1456–1461

    Article  Google Scholar 

  • Chen Y, Wang CY (1980) Thermally induced acoustic emission in Westerly granite. Geophys Res Lett 7(12):1089–1092

    Article  Google Scholar 

  • Chen Y, Wu XD, Zhang FQ (1999) Experimental research on rock thermal cracking (in Chinese). Chinese Sci Bull 44(8):880–883

    Article  Google Scholar 

  • Chen YL, Ni J, Shao W, Azzam R (2012) Experimental study on the influence of temperature on the mechanical properties of granite under un-axial compression and fatigue loading. Int J Rock Mech Min 56:62–66

    Google Scholar 

  • Craig TJ, Copley A, Jackson J (2012) Thermal and tectonic consequences of India underthrusting Tibet. Earth Planet Sci Lett 353–354:231–239

    Article  Google Scholar 

  • Du SJ, Liu H, Zhi HT, Chen HH (2004) Testing study on mechanical properties of post-high-temperature granite (in Chinese). Chin J Rock Mech Eng 23(14):2359–2364

    Google Scholar 

  • Dwivedi RD, Goel PK, Prasad VVR, Sinha Amalendu (2008) Thermo-mechanical properties of Indian and other granites. Int J Rock Mech Min 45:303–315

    Article  Google Scholar 

  • Etienne FH, Poupert R (1989) Thermally induced microcracking in granites: characterization and analysis. Int J Rock Mech Min Sci 26(2):125–134

    Article  Google Scholar 

  • Foulger GR (1995) The Hengill geothermal area, Iceland: variation of temperature gradients deduced from the maximum depth of seismogenesis. J Volcanol Geoth Res 65:119–133

    Article  Google Scholar 

  • Fredrich JT, Wong T (1986) Micromechanics of thermally induced cracking in three crustal rocks. J Geophys Res 91(B12):12743–12764

    Article  Google Scholar 

  • Géraud Y (1994) Variations of connected porosity and inferred permeability in a thermally cracked granite. Geophys Res Lett 21(11):979–982

    Article  Google Scholar 

  • Géraud Y, Mazerolle F, Raynaud S (1992) Comparison between connected and overall porosity of thermally stressed granites. J Struct Geol 14(8/9):981–990

    Article  Google Scholar 

  • Glover PWJ, Baud P, Darot M, Meredith PG, Boon SA, LeRavalec M, Zoussi S, Reuschlé T (1995) α/β phase transition in quartz monitored using acoustic emissions. Geophys J Int 120:775–782

    Article  Google Scholar 

  • Hajpal M (2002) Changes in sandstone of historical monuments exposed to fire or high temperature. Fire Technol 38(4):373–382

    Article  Google Scholar 

  • Heuze FE (1983) High-temperature mechanical, physical and thermal properties of granitic rocks—a review. Int J Rock Mech Min Sci Geomech Abstr 20(1):3–10

    Article  Google Scholar 

  • Jana J, Agnes K (2012) Thermally induced alterations of minerals during measurements of the temperature dependence of magnetic susceptibility: a case study from the hydrothermally altered soultz-sous-Forêts granite, France. Int J Earth Sci 101:819–839

    Article  Google Scholar 

  • Jason DP, Carlson SR, Young RP, Hutchins DA (1993) Ultrasonic imaging and acoustic emission monitoring of thermally induced microcracks in Lac du Bonnet Granite. J Geophys Res Solid Earth 98(B12):22231–22243

    Article  Google Scholar 

  • Jones C, Keaney G, Meredith PG et al (1997) Acoustic emission and fluid permeability measurements on thermally cracked rocks. Phys Chem Earth 22:813–817

    Google Scholar 

  • Knapp RB, Norton D (1981) Preliminary numerical analysis of processes related to magma crystallisation and stress evolution in cooling pluton environments. Am J Sci 281:35–68

    Article  Google Scholar 

  • Koide H, Bhattacharji S (1975) Formation of fractures around magmatic intrusions and their role in ore localization. Econ Geol 70:781–799

    Article  Google Scholar 

  • Liu JR, Qin JS, Wu XD (2005) Experimental study on relation between temperature and rock permeability (in Chinese). J China Univ Pet Nat Sci 24(12):51–53

    Google Scholar 

  • Lockner DA, Summers R, Byerlee JD (1986) Effects of temperature and sliding rate on frictional strength of granite. Pure appl Geophys 124(3):446–468

    Google Scholar 

  • Lokajícek T, Rudajev V, Dwivedi RD et al (2012) Influence of thermal heating on elastic wave velocities in granulite. Int J Rock Mech Min 54:1–8

    Google Scholar 

  • Mereer JJ (1973) Finite element approach to the modeling of hydrothermal systems. PhD dissertation, University of Illinois, Urbana

  • Nasseri MHB, Schubnel A, Young RP (2007) Coupled evolutions of fracture toughness and elastic wave velocities at high crack density in thermally treated westerly granite. Int J Rock Mech Min Sci 44:601–616

    Article  Google Scholar 

  • Nasseri MHB, Tatone BSA, Grasselli G, Young RP (2009) Fracture toughness and fracture roughness interrelationship in thermally treated Westerly granite. Pure Appl Geophys 166:801–822

    Article  Google Scholar 

  • Parish DK, Krivz AI, Carter NI (1976) Finite element folds of similar geometry. Tectonophysics 32:183–207

    Article  Google Scholar 

  • Pracht WE (1971) A numerical method for calculating transient creep flows. J Comp Phys 7:46–60

    Article  Google Scholar 

  • Ramdani F (1998) Geodynamic implications of intermediate-depth earthquakes and volcanism in the intraplate Atlas mountains (Morocco). Phys Earth Planet Inter 108:245–260

    Article  Google Scholar 

  • Rao GMN, Murthy CR (2001) Dual role of microcracks: toughening and degradation. Can J Earth Sci 38(2):427–440

    Google Scholar 

  • Shimamoto T, Hara I (1976) Geometry and strain distribution of single-layer folds. Tectonophysics 30:1–34

    Article  Google Scholar 

  • Stesky RM (1978) Mechanisms of high temperature frictional sliding in Westerly granite. Can J Earth Sci 15:361–375

    Article  Google Scholar 

  • Sun Q, Zhang ZZ, Xue L, Zhu SY (2013) Physical–mechanical properties variation of rock with phase transformation under high temperature. (in Chinese). Chin J Rock Mech Eng 32(5):935–942

    Google Scholar 

  • Xi BP, Zhao JC, Zhao YS, Zhu HH, Wu JW (2011) Key technologies of hot dry rock drilling during construction (in Chinese). Chin J Rock Mech Eng 30(11):2234–2243

    Google Scholar 

  • Xu XC, Liu QS (2000) A preliminary study on basic mechanical properties for granite at high temperature (in Chinese). Chin J Geotech Eng 22(3):332–335

    Google Scholar 

  • Xu XL, Gao F, Shen XM, Jin CH (2010) Research on mechanical characteristics and micropore structure of granite under high-temperature (in Chinese). Rock Soil Mech 31(6):1752–1758

    Google Scholar 

  • Yang SF, Chen H, Jiang JS, Zhu GQ, Xie HS, Hou W, Zhang YM, Xu HG (1997) Testing study on elastic wave velocities and electrical conductivity of crustal rocks (in Chinese). Sci China Ser D 27(1):33–38

    Google Scholar 

  • Yin TB (2012) Study on dynamic behavior of rocks considering thermal effect (in Chinese). Ph.D. Thesis, Central south university, Changsha

  • Zhang ZX, Yu J, Kou SQ, Lindqvist PA (2001) Effects of high temperatures on dynamic rock fracture. Int J Rock Mech Min 38(2):211–225

    Article  Google Scholar 

  • Zhang Y, Zhao YS, Wan ZJ, Qu F, Dong FK, Feng ZJ (2008) Experimental study on effect pore pressure on feldspar fine sandstone permeability under different temperatures (in Chinese). Chinese J Rock Mech Eng 27(1):53–58

    Article  Google Scholar 

  • Zhang Y, Zhao YS, Wu G (2010) Meso-structure and pattern of thermal cracking of Luhui granite (in Chinese). J Lanzhou Univ Technol 36(6):115–118

    Google Scholar 

  • Zhi LP, Xu JY, Liu ZQ, Liu S, Chen TF (2012) Research on ultrasonic characteristics and Brazilian splitting-tensile test of granite under post-high temperature (in Chinese). Rock Soil Mech 33(s1):61–66

    Google Scholar 

Download references

Acknowledgments

This research was supported by the State Basic Research and Development Program of China (No. 2013CB036003), the Priority Academic Program Development of Jiangsu Higher Education Institutions, Transport project (2013318J12330), and the National Science Youth Foundation of China (Grant No.41102201, No.41302233, No.51309222).

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Correspondence to Qiang Sun.

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Sun, Q., Zhang, W., Xue, L. et al. Thermal damage pattern and thresholds of granite. Environ Earth Sci 74, 2341–2349 (2015). https://doi.org/10.1007/s12665-015-4234-9

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