赤铁矿
分散性
摩尔浓度
铁
化学
化学工程
产量(工程)
硫酸盐
核化学
材料科学
无机化学
色谱法
矿物学
分析化学(期刊)
高分子化学
水溶液
有机化学
冶金
工程类
作者
Tadao Sugimoto,Mohammad Mansoob Khan,Atsushi Muramatsu
标识
DOI:10.1016/0927-7757(93)80285-m
摘要
Recently, it has been found that monodisperse pseudocubic hematite particles 1.65 μm in mean edge length can be obtained in large quantities of the order of the molality with a yield close to 100%, by adding 100 ml of 5.4 N NaOH to 100 ml of well-stirred 2.0 M FeCl3 and aging the resulting condensed gel of Fe(OH)3 for 8 days at 100°C. The method was provisionally referred to as the gel—sol method. As an application of this technique, when 90 ml of 6.0 N NaOH and 10 ml of sulfate or phosphate solution were added instead of 100 ml of 5.4 N NaOH, the pseudocubic particles turned into peanut-type particles via an ellipsoidal shape with increasing concentration of the additives.
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