2022
DOI: 10.12911/22998993/150682
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The Behavior of Jordanian Oil Shale during Combustion Process from the El-Lajjun Deposit

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“…The peaks at these locations vary in intensity between the two samples, which is attributed to the discrepancies in the quartz and feldspar content as well as the types and quantities of the clay minerals. The peaks at 715 cm −1 and 1799 cm −1 and the peaks at 876 cm −1 and 1447 cm −1 are derived from calcites [34]. The peak at 1447 cm −1 in the MP samples also has the contribution of the deformation vibration peaks of methylene (-CH 2 -) [35].…”
Section: Thermogravimetric Analysismentioning
confidence: 92%
“…The peaks at these locations vary in intensity between the two samples, which is attributed to the discrepancies in the quartz and feldspar content as well as the types and quantities of the clay minerals. The peaks at 715 cm −1 and 1799 cm −1 and the peaks at 876 cm −1 and 1447 cm −1 are derived from calcites [34]. The peak at 1447 cm −1 in the MP samples also has the contribution of the deformation vibration peaks of methylene (-CH 2 -) [35].…”
Section: Thermogravimetric Analysismentioning
confidence: 92%