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The effect of experimental conditions on the microstructure of hematite particles precipitated by the forced hydrolysis of FeCl_3 solutions

机译:实验条件对FeCl_3溶液强迫水解沉淀赤铁矿颗粒微观结构的影响

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摘要

The effect of experimental conditions on the forced hydrolysis of FeCl _3 solutions and specifically the effect of amidosulphonic acid on the microstructure of precipitates were investigated. Precipitates were analyzed by XRD, ~(57)Fe M?ssbauer, FT-IR and UV/Vis/NIR spectroscopies, as well as FE-SEM. The phase transformation β-FeOOH → α-Fe _2O_3 was accelerated with an increase in the hydrolysis temperature, whereas an addition of amidosulphonic acid at the start of the hydrolysis of Fe~(3+) ions suppressed the phase transformation β-FeOOH → α-Fe_2O_3 or decreased crystallinity at 120 and 160 °C. The size and shape of hematite particles were strongly dependent on FeCl_3 concentration and temperature and the presence of sulfonate/sulfate groups. Preferential adsorption of sulfonate/sulfate groups influenced the hematite crystal growth direction. The aggregation effect was also noticed in the formation of hematite particles.
机译:研究了实验条件对FeCl_3溶液强制水解的影响,特别是氨基磺酸对沉淀物微观结构的影响。用XRD,〜(57)Fe M?ssbauer,FT-IR和UV / Vis / NIR光谱以及FE-SEM分析沉淀物。随着水解温度的升高,相转变β-FeOOH→α-Fe_2O_3加速,而在Fe〜(3+)离子水解开始时加入氨基磺酸抑制了相转变β-FeOOH→α -Fe_2O_3或在120和160°C下结晶度降低。赤铁矿颗粒的大小和形状在很大程度上取决于FeCl_3的浓度和温度以及磺酸盐/硫酸盐基团的存在。磺酸根/硫酸根的优先吸附影响了赤铁矿晶体的生长方向。在赤铁矿颗粒的形成中也注意到聚集作用。

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