2018
DOI: 10.1016/j.jallcom.2018.05.010
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Effects of calcination on silica phase transition in diatomite

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Cited by 72 publications
(28 citation statements)
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“…19 The amorphous phase of opal (SiO 2 $nH 2 O) is reected by the peak at 21 , which can be seen in the XRD pattern of diatomite. 9 The typical characteristic peaks of hydroxides at 9.96 , 20.05 and 30.24 are attributable to the Cu/Al-LDH structure, which is similar to the result we previously reported. 16 Thus, we conclude that diatomaceous earth has no impact on the hydrothermal preparation of copper aluminium hydroxides.…”
Section: Catalytic Ldpe Pyrolysissupporting
confidence: 89%
See 1 more Smart Citation
“…19 The amorphous phase of opal (SiO 2 $nH 2 O) is reected by the peak at 21 , which can be seen in the XRD pattern of diatomite. 9 The typical characteristic peaks of hydroxides at 9.96 , 20.05 and 30.24 are attributable to the Cu/Al-LDH structure, which is similar to the result we previously reported. 16 Thus, we conclude that diatomaceous earth has no impact on the hydrothermal preparation of copper aluminium hydroxides.…”
Section: Catalytic Ldpe Pyrolysissupporting
confidence: 89%
“…8 Diatomite is a fossil of single-cell aquatic plants (algae), which consists of a porous diatom skeleton and an Si-O tetrahedral interconnected network with excellent features such as low density, high surface area and large adsorption capacity. [9][10][11][12][13] Layered double hydroxides (LDH) which are one type of layered materials with many outstanding catalytic behaviors, such as activity, selectivity and stability of active sites that have been extensively studied. [14][15][16][17][18][19][20][21] LDH has been applied as an adsorbent and precursor of well-mixed oxides in various catalytic reactions.…”
Section: Introductionmentioning
confidence: 99%
“…The literature results indicated that such a calcination temperature slightly exceeds the temperature of the structural transition from β and α quartz (573°C), simultaneously being considerably lower than the temperatures of significant alterations of other minerals. During such a calcination, the surface-bound water and an organic substance should be removed, whereas clay minerals dehydroxylated and partly decomposed (Yılmaz & Ediz 2008, Zhi-Yang et al 2009, Ediz et al 2010, Posi et al 2014, Zheng et al 2018. Melting of clay minerals in pores was also reported to start at 600°C (Zhi-Yang et al 2009).…”
Section: Methodsmentioning
confidence: 99%
“…Los prototipos sinterizados por encima de 950 °C (Fig. 7c) presentaron una superficie más consolidada, sus cambios morfológicos obedecen a dos aspectos: las transformaciones de fase que suceden por encima de los 900 °C y la posterior aglomeración de partículas que origina un cuerpo cerámico mucho más denso [39,40]. Para este rango de temperaturas se observó en la superficie poros interconectados y aislados.…”
Section: Análisis Microestructuralunclassified