2019
DOI: 10.1088/2053-1591/ab3093
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Evaluation of red clay and ball clay drying using transient three-dimensional mathematical modeling: volumetric shrinkage and moisture content

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Cited by 6 publications
(1 citation statement)
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“…The diffraction peaks observed in the C1-S 10% sample were more prominent than those in the other samples. This might be related to an increase in the temperature of the system owing to the high content of organics and higher humidity of the mixture [51,52]. The diffractograms of the samples produced with C2 showed peaks of quartz and hematite because kaolinite and mica were consumed with increasing temperature (480 °C and 850-940 °C, respectively).…”
Section: Mineralogical Propertiesmentioning
confidence: 99%
“…The diffraction peaks observed in the C1-S 10% sample were more prominent than those in the other samples. This might be related to an increase in the temperature of the system owing to the high content of organics and higher humidity of the mixture [51,52]. The diffractograms of the samples produced with C2 showed peaks of quartz and hematite because kaolinite and mica were consumed with increasing temperature (480 °C and 850-940 °C, respectively).…”
Section: Mineralogical Propertiesmentioning
confidence: 99%