首页> 外文期刊>Iranian journal of chemistry & chemical engineering >Thermodynamic Modeling and Experimental Studies of Bayerite Precipitation from Aluminate Solution: Temperature and pH Effect
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Thermodynamic Modeling and Experimental Studies of Bayerite Precipitation from Aluminate Solution: Temperature and pH Effect

机译:铝酸盐溶液中Bayerite沉淀的热力学建模和实验研究:温度和pH值影响

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摘要

Bayerite is one of the phases of aluminum hydroxide which is precipitated by the carbonation of aluminate solutions obtained from sintered nepheline syenite leaching. In this study, the conditions for the bayerite formation were predicted by thermodynamic modeling of the carbonation process and the Bromley- Zemaitis model was used for this purpose. Carbonation experiments were carried out at pH 11 and the temperature range of 50- 90 degrees C based on the data obtained from thermodynamic modeling results. XRD analysis of products showed that bayerite was the predominant phase at all temperatures. SEM and LDS analysis indicated that the bayerite precipitates had uniform morphology and bimodal particle size distribution with mean particle size of 4.6 mu m at 50 degrees C to 12.9 mu m at 90 degrees C. It was found that the d(50) increased slowly at the precipitation temperature ranging from 80 to 90 degrees C, from 12.6 to 12.9 mu m and the effect of temperature was on the shape of particles. XRF analysis of the products indicated that the amount of Al2O3 and SiO2 in the bayerites decrease by increasing the temperature. According to the thermodynamic modeling data and experimental results, the temperature of 80 degrees C and pH 11 were determined as optimal conditions for bayerite precipitation.
机译:钙铝石是氢氧化铝的相之一,其是通过从烧结的霞石正长岩浸出获得的铝酸盐溶液的碳酸化而沉淀的。在这项研究中,通过碳酸化过程的热力学模型预测了钙锰矿形成的条件,并为此使用了Bromley-Zemaitis模型。基于从热力学建模结果获得的数据,在pH 11和50-90摄氏度的温度范围内进行了碳酸化实验。产品的X射线衍射分析表明,在所有温度下,钠铝石是主要相。 SEM和LDS分析表明,三羟铝石沉淀具有均匀的形貌和双峰粒径分布,在50℃时平均粒径为4.6μm,在90℃时平均粒径为12.9μm。发现d(50)在50℃缓慢增加。沉淀温度在80至90摄氏度,12.6至12.9微米之间,并且温度对颗粒的形状有影响。产物的XRF分析表明,三方石中Al2O3和SiO2的含量随着温度的升高而降低。根据热力学模型数据和实验结果,确定80℃的温度和11的pH值是钙铝石沉淀的最佳条件。

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