2021
DOI: 10.1007/s10973-021-11083-9
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Young’s modulus of illitic clay in the temperature region of quartz transition

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(2 citation statements)
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“…After a linear decrease, f0 increased at ~573 °C due to quartz modification transition. The further decrease of f0 and the increase of δ are attributed to the dehydroxylation of illite [16]. At 733 °C, f0 reached its local minima and δ its local maxima.…”
Section: Measurement Examplementioning
confidence: 95%
See 1 more Smart Citation
“…After a linear decrease, f0 increased at ~573 °C due to quartz modification transition. The further decrease of f0 and the increase of δ are attributed to the dehydroxylation of illite [16]. At 733 °C, f0 reached its local minima and δ its local maxima.…”
Section: Measurement Examplementioning
confidence: 95%
“…At 573 °C, a deteriorating effect of quartz was manifested during cooling. Due to the extraordinary temperature dependence of the elastic properties of quartz during its modification transition [17] and because of the rapid change in its thermal expansion coefficient, the course of f0 showed its typical V-shaped minima followed by a substantial decrease [16]. The modification transition of quartz was also reflected in δ.…”
Section: Measurement Examplementioning
confidence: 99%