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Conducting Elevated Temperature Normal and Combined Pressure-Shear Plate Impact Experiments Via a Breech-end Sabot Heater System
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Effect of Elevated Temperature on Rhyolitic Rocks' Properties.

Haitham M Ahmed1, Mohammed A Hefni1, Hussin A M Ahmed1

  • 1Mining Engineering Department, King Abdulaziz University, Jeddah 21589, Saudi Arabia.

Materials (Basel, Switzerland)
|May 20, 2022
PubMed
Summary

High temperatures impact rhyolitic rock properties. Below 600°C, rock hardens, but above this, mechanical strength (uniaxial compressive strength and elastic modulus) significantly decreases, with microcracking observed.

Keywords:
failure modesheat treatmentmicrostructurerhyolitic rocksrock physical and mechanical behavior

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Area of Science:

  • Geotechnical Engineering
  • Materials Science
  • Rock Mechanics

Background:

  • Understanding thermophysical and mechanical properties of rocks at high temperatures is crucial for underground geotechnical applications.
  • Rhyolitic turf rock's response to elevated temperatures requires detailed investigation for safe and efficient design.

Purpose of the Study:

  • To investigate the impact of high temperatures on the physical and mechanical properties of rhyolitic turf rock.
  • To analyze microstructural changes in rhyolite rock after thermal exposure.

Main Methods:

  • Heating intact cylindrical rhyolite core samples to temperatures of 200, 400, 600, and 800 °C.
  • Determining uniaxial compressive strength (UCS) and elastic modulus of heated and unheated samples.
  • Analyzing physical properties (density, color, absorption) and microstructural characteristics using SEM.

Main Results:

  • Rhyolitic rock exhibited hardening below 600 °C.
  • Above 600 °C, UCS and elastic modulus decreased, reaching 78.0% and 75.9% of original values at 800 °C.
  • Density and pore volume remained largely unaffected, while color changes occurred at ≥400 °C, with microcracking and surface cracks evident at 600 °C.

Conclusions:

  • High temperatures significantly alter the mechanical properties of rhyolitic rock, with degradation occurring above 600 °C.
  • Thermal exposure induces microstructural damage, including particle displacement and cracking, affecting rock integrity.
  • While density is stable, observable color changes and microstructural alterations necessitate careful consideration in high-temperature geotechnical designs.