三水铝石
结晶度
勃姆石
材料科学
煅烧
热重分析
差示扫描量热法
粒径
分析化学(期刊)
矿物学
热分析
无定形固体
相(物质)
差热分析
粒子(生态学)
化学
结晶学
无机化学
高岭石
衍射
热的
色谱法
复合材料
物理化学
热力学
有机化学
铝
催化作用
物理
海洋学
地质学
光学
作者
Bogdan Ștefan Vasile,Gheorghe Dobra,S. Iliev,Lucian Cotet,Ionela Andreea Neacșu,Vasile-Adrian Surdu,Adrian Ionuț Nicoară,Alina Boiangiu,Laurențiu Filipescu
出处
期刊:Ceramics
[Multidisciplinary Digital Publishing Institute]
日期:2021-10-11
卷期号:4 (4): 564-575
被引量:19
标识
DOI:10.3390/ceramics4040040
摘要
In this paper, the thermal decomposition of crystalline Al(OH)3 was studied over the temperature range of 260–400 °C for particles with a size between 10 and 150 µm. The weight losses and thermal effects occurring in each of the dehydration process were assessed using thermogravimetry (TG) and differential scanning calorimetry (DSC) thermal analysis. X-ray diffraction (XRD) patterns, refined by the Rietveld method, were used for mineral phase identification, phase composition analysis, and crystallinity degree determination. Moreover, the particle size distributions and their corresponding D10, D50, and D90 numeric values were determined with a laser analyzer. We observed a strong relationship between the calcination temperature, the initial gibbsite grade particle size, and the crystallinity of the resulting powders. Hence, for all endothermic effects identified by DSC, the associated temperature values significantly decreased insofar as the particle dimensions decreased. When the gibbsite was calcined at a low temperature, we identified small amounts of boehmite phase along with amorphous new phases and unconverted gibbsite, while the powders calcined at 400 °C gradually yielded a mixture of boehmite and crystalized γ-Al2O3. The crystallinity % of all phase transition products declined with the increase in particle size or temperature for all the samples.
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