4.7 Article

An experimental study of the mechanical properties of granite after high temperature exposure based on mineral characteristics

Journal

ENGINEERING GEOLOGY
Volume 220, Issue -, Pages 234-242

Publisher

ELSEVIER SCIENCE BV
DOI: 10.1016/j.enggeo.2017.02.010

Keywords

Mineral characteristic; Rock mechanics; Scanning electron microscopy; Phlogopite; High temperature; Fracture toughness

Funding

  1. K.C. Wong Education Foundation (KCWEF)
  2. DAAD-CSC Program (PPP)
  3. Natural Science Foundation of Shanghai [14ZR1428200]
  4. National Natural Science Foundation of China [10872133, 51608323]
  5. Yangfan Project of Science and Technology Commission of Shanghai Municipality [15YF1408200]

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The macroscopic mechanical properties of granite collected from the Fujian Province, China were measured using uniaxial compression and three-point bending after the granite was exposed to high temperatures. The stress strain relationship was measured and mechanical properties including the Young's modulus, uniaxial compressive strength (UCS) and fracture toughness were calculated. In general, the uniaxial compressive strength (UCS), Young's modulus and fracture toughness of the granite specimens decrease with an increase in heat treatment temperature up to 800 degrees C, above which there is no obvious change. The microstructure of the failed specimens was explored using scanning electron microscopy (SEM) and stereomicroscopy. After heat treatment, the minerals within the granite were analysed using X-ray diffraction. The failure mechanisms and the mechanical characteristics of the granite are explained in terms of the microstructure and the minerals present. The results of the experiments indicate that the crystal structure of the phlogopite in granite transforms to a more stable structure between 400 degrees C and 600 degrees C with an associated increase in volume. A dehydroxylation reaction also occurs in the phlogopite at 400 degrees C, after which the uniaxial compressive strength (UCS) decreases and the ductility increases. Using SEM and stereomicroscopy, it was observed that the connection between the minerals within the granite becomes weaker with increasing heat treatment temperature. Intercrystalline cracking is the main failure mode for samples exposed to temperatures below 800 degrees C, whereas transcrystalline cracking can be observed in samples exposed to 1000 degrees C. (C) 2017 Elsevier B.V. All rights reserved.

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