2016
DOI: 10.1007/s00603-016-1047-4
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Effect of Varied Durations of Thermal Treatment on the Tensile Strength of Red Sandstone

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Cited by 118 publications
(41 citation statements)
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“…It can also be seen that, the duration and the nature of the thermal treatment provided to a certain rock type can widely affect the mechanical properties. Long and constant exposure lead to deeper and profound extension of the cracks [10]. In this study, since the rock was heated for a period of 5 days, the thermal treatment brought about a definite change to the microstructure as seen in figure 4.…”
Section: Resultsmentioning
confidence: 62%
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“…It can also be seen that, the duration and the nature of the thermal treatment provided to a certain rock type can widely affect the mechanical properties. Long and constant exposure lead to deeper and profound extension of the cracks [10]. In this study, since the rock was heated for a period of 5 days, the thermal treatment brought about a definite change to the microstructure as seen in figure 4.…”
Section: Resultsmentioning
confidence: 62%
“…However, the studies carried out on sedimentary rocks affirm with the decrease of the mechanical properties after a certain temperature limit. This limit, also known as the critical temperature zone (CTZ), indicate the deterioration of internal structure of rock due to extensive expansion and creation of inter and intragranularmicrocracks [8,10]. The CTZ for Dholpur sandstone can therefore be confirmed at temperatures between 300-500°C.…”
Section: Resultsmentioning
confidence: 99%
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“…More and more researchers have studied the influence of temperature on the physical and mechanical properties of salt rock. It was found that both uniaxial compressive strength and axial strain increase with the increasing temperature; however, the tangent modulus decreases with the increasing temperature . By extension, researchers studied the influence of high temperature on the peak strength, elastic modulus, and damage characteristics and compared the stress‐strain curves of different sandstones between normal temperature and the high temperature of 950°C .…”
Section: Introductionmentioning
confidence: 99%
“…Bauer and Johnson [4] showed that the thermal expansion of quartz and feldspar play an important role in initiation and propagation of thermal cracks which is the main reason for weakening the rock at higher temperatures. Sirdesai et al [19] concluded that the main reason for the changes in rock's characteristics upon heating is due to the minerals expansion. The change in the pores and micro-fracturing caused by the thermal expansion, leads to the alteration of rock's tensile strength.…”
Section: Introductionmentioning
confidence: 99%