2015
DOI: 10.1007/s10973-015-4996-z
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Thermal expansion behaviour of granites

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Cited by 33 publications
(14 citation statements)
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“…However, it should be noted that, different from the pure volume expansion of quartzite and granite, cracking of mineral particles and the formation of fractures in limestone are the most important factors for heat expansion of limestone (Chen et al 2009). Moreover, the anisotropic expansion behavior can be observed in these aggregates under elevated temperature (Chen et al 2009;Plevova et al 2016). Due to the thermal shrinkage of cement paste and the considerable thermal expansion of aggregates, a net expansion of concrete is exhibited and inner thermal stresses are generated.…”
Section: Thermal Expansionmentioning
confidence: 96%
“…However, it should be noted that, different from the pure volume expansion of quartzite and granite, cracking of mineral particles and the formation of fractures in limestone are the most important factors for heat expansion of limestone (Chen et al 2009). Moreover, the anisotropic expansion behavior can be observed in these aggregates under elevated temperature (Chen et al 2009;Plevova et al 2016). Due to the thermal shrinkage of cement paste and the considerable thermal expansion of aggregates, a net expansion of concrete is exhibited and inner thermal stresses are generated.…”
Section: Thermal Expansionmentioning
confidence: 96%
“…For temperature greater than 664 °C, the re-increase of TG curve may be due to the oxidation of some minerals in air atmosphere. In addition, the small endothermic peak representing α-β quartz phase transition at 573 °C is detected [19], which is visible on the DSC curve. This transition is accompanied by approximately 5 % of volume expansion which can induce numerous micro-cracks around the grain of quartz [26].…”
Section: Tg/dscmentioning
confidence: 98%
“…Sirdesai [18] demonstrated that the phase transition of quartz induced the sharply decrease of sandstone mechanical performances over 573 °C. Besides, mineral dehydration as temperature increased were also declared to weaken the rock structure [19][20][21][22]. Almost all literatures mentioned the deterioration of rock with temperature increasing is significantly related to the crystal mineral characteristics' changing at specific temperatures induced by either microwave irradiation or heat transfer.…”
Section: Introductionmentioning
confidence: 99%
“…4c, the light-colored minerals on the surface have turned to white, while dark minerals such as biotite turned to brown and the biotite layer demonstrate golden in the fractured area. This is because of the water losing in Fe-rich minerals [29]. Besides, it can be found that cracks initially appear around the biotite particles which are also split by cracks.…”
Section: Irradiating Outcomesmentioning
confidence: 98%
“…In the last phase (from 530 to 800 °C), the sharp decline in mass around 600 °C is identified as the process of dehydroxylation of biotite [28]. In the DSC curve, a small endothermic peak can be easily found at 573 °C, which is attributed to quartz α-β transition [29,30]. The stress increases due to the enlargement of volume in quartz mineral grains during the phase transition, on the other hand, its surface energy becomes very low in this course.…”
Section: Sample Propertiesmentioning
confidence: 99%