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氧化硅包敷对铁黄脱水过程的影响 被引量:9

Effect of Silica Coating on Geothite Dehydration Process
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摘要 本文采用DTA、TG、HTXTD和TEM研究了SiO2包敷α-FeOOH粒子的脱水过程。从DTA和TG曲线算得的动力学参数表明,SiO2包敷α-FeOOH粒子的脱水过程近似为一级反应,其活化能大于未处理的α-FeOOH粒子的活化能。HTXRD和TEM的测量结果表明,α-FeOOH热分解成α-Fe2O3同时形成晶核和条形微孔,这可能是X射线衍射峰展宽的主要原因。随着温度增加,微孔织构转变为中孔或大孔织构,大约在800℃以上逐渐消失。对于SiO2包敷α-FeOOH,其相应的热变化温度移向高温。 Abstract The dehydration process of SiO2 coated α-FeOOH has been investigated by DTA, TG, HTXRD and TEa measurementS. The kinetic parameters caculated from DTA and TG curves indicate that the dehydstien proess of SiO2 coatde α-FeOOH is about first order reaction, and its apparent activation energy is higher than that of the untreated α-FeOOH. The results from HTXRD and TEM measurements show that the thermal decomposition of α-FeOOH into α-Fe2O3 leads to the simultaneous formation of the crystal nuclei and of the slit--shaped micropores, which may be the main reason to broad X-ray diffraction lines. With the temperature increasing, the microporous texture is changed into a mesoporous or macroporous texture, and it almost disappears at the temperature above 800℃ or so. In the case of silica coated αFeOOH, its thermal variation temperature shifts to the high temperature
出处 《Chinese Journal of Chemical Physics》 SCIE CAS CSCD 1995年第5期416-423,共8页 化学物理学报(英文)
基金 国家教委重大资助
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