明矾石
无水的
石英
吸热过程
明矾
碱金属
矿物学
热分解
化学
无机化学
地质学
材料科学
冶金
有机化学
地震学
热液循环
吸附
作者
M.-A. Kashkai,I. A. Babaev
出处
期刊:Mineralogical Magazine
[The Mineralogical Society]
日期:1969-03-01
卷期号:37 (285): 128-134
被引量:22
标识
DOI:10.1180/minmag.1969.037.285.13
摘要
Summary The thermal decomposition of alunite and of mixtures of alunite with dickite or quartz or both has been studied, and X-ray determinations of the products at various stages of the decomposition have been made. Between 600 and 700°C the product from alunite is a mixture of anhydrous alum and amorphous alumina; between 700 and 770°C the anhydrous alum breaks down into aluminium sulphate and alkali sulphate; then in the prominent 850°C endothermic reaction three-quarters of the sulphate is lost, leaving a mixture of alkali sulphate and γ -alumina. The area of the 850 °C endothermic peak may be used as a measure of the percentage of alunite in alunitized rocks (alunite-quartz-dickite mixtures).
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