2017
DOI: 10.1016/s1003-6326(17)60208-5
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Thermal decomposition kinetics of Algerian Tamazarte kaolinite by thermogravimetric analysis

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Cited by 14 publications
(9 citation statements)
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“…The As temperature increased from 100 C to 300 C, the area of inner-surface O-H groups (peak I) and that of inner-surface O-D groups (peak I 0 ) signicantly decreased, while the areas of peaks III and III 0 and peaks IV and IV 0 remained almost unchanged considering tting errors, whereas the peak II area slightly increased and the peak II 0 area at 200 C and 300 C became signicantly higher than that at 100 C. The area decrease of peaks I and I 0 and area increase of peaks II and II 0 indicated that peak I shied to peak II, and peak I 0 correspondingly changed into peak II 0 . Kristóf and Redaoui 41,42 reported that proton delocalization and predehydroxylation of kaolinite could occur between the temperatures of 30 C to 360 C. The results of Fig. 3 also proved that the kaolinite skeleton structure could be slightly affected as heating temperature increased from 30 C to 300 C, based on the changes of peak intensity at 757 cm À1 (Si-O-Al) and 670 cm À1 (Al-O).…”
Section: Physical and Chemical Properties Of Kaolinitementioning
confidence: 68%
“…The As temperature increased from 100 C to 300 C, the area of inner-surface O-H groups (peak I) and that of inner-surface O-D groups (peak I 0 ) signicantly decreased, while the areas of peaks III and III 0 and peaks IV and IV 0 remained almost unchanged considering tting errors, whereas the peak II area slightly increased and the peak II 0 area at 200 C and 300 C became signicantly higher than that at 100 C. The area decrease of peaks I and I 0 and area increase of peaks II and II 0 indicated that peak I shied to peak II, and peak I 0 correspondingly changed into peak II 0 . Kristóf and Redaoui 41,42 reported that proton delocalization and predehydroxylation of kaolinite could occur between the temperatures of 30 C to 360 C. The results of Fig. 3 also proved that the kaolinite skeleton structure could be slightly affected as heating temperature increased from 30 C to 300 C, based on the changes of peak intensity at 757 cm À1 (Si-O-Al) and 670 cm À1 (Al-O).…”
Section: Physical and Chemical Properties Of Kaolinitementioning
confidence: 68%
“…Based on the chemical compositions of the coal gangue and high alumina refractory solid wastes (Table 1), the main components are kaolinite, quartz, and alumina. When the samples were calcined, mullite was formed through the following reactions [18][19][20][21] :…”
Section: Phase and Microstructure Of The Mullite Powdermentioning
confidence: 99%
“…The expansion observed during stage D, between 840 and 983°C is due the structural reorganization of métakaolinite regarding the formation of a primary mullite phase or of a Al‐Si spinel phase 33 . The stage E, between 1000°C and 1200°C can be attributed to the occurrence of mullite (crystallization) and to the crystallization of cristobalite 34,35 . The curves of Figure 1 indicated that the presence of MgCO 3 tended to enhance the sintering shrinkages (‐ 0.5% for specimen with 12 mass% of magnesite sintered at 1200°C), this result appeared in agreement with results obtained from previous studies 36,37 .…”
Section: Resultsmentioning
confidence: 95%