Optimization of Dissolution of Ulexite in Disodium Hydrogen Phosphate

B. O. Kaya, S. Kuşlu, T. Çalban
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Abstract

The study aimed to investigate the optimization of the dissolution of ulexite minerals in disodium hydrogen phosphate solutions by using a factorial experimental design. The study used the solid-liquid ratio, reaction temperature, the concentration of disodium hydrogen phosphate solutions and reaction time as parameters. 2 n factorial experimental design and orthogonal central composite experimental design methods were used. The optimum conditions for maximum ulexite dissolution were: Solid-liquid ratio of 1/8 g mL -1 , a reaction temperature of 65 °C, a concentration of disodium hydrogen phosphate of 2 M, and a reaction time of 4 hours. Under these optimum conditions, the dissolute B 2 O 3 was 98.16 % in disodium hydrogen phosphate solutions. The complete model, including all parameters, was obtained using the 2. degree variables of the model experiment and internal interactions was found to be as follows. Ŷk.model = 80,45 + 11,31X 1 + 5,70X 2 – 1,10X 3 – 7,29X 4 – 11,27X 12 - 1,34X 22 + 2,37X 32 – 4,33X 42 + 3,25 X 1 X 2 – 7,45 X 1 X 3 + 14,00 X 1 X 4 + 4,30 X 2 X 3 - 7,80X 2 X 4 + 7,17X 3 X 4
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磷酸氢二钠溶出无绿石的优化研究
采用析因试验设计,研究了无辉石矿物在磷酸氢二钠溶液中的溶出效果。研究以料液比、反应温度、磷酸氢二钠溶液浓度和反应时间为参数。采用2 n因子试验设计和正交中心复合试验设计方法。最佳溶出条件为:料液比为1/8 g mL -1,反应温度为65℃,磷酸氢二钠浓度为2 M,反应时间为4 h。在此条件下,b2o3在磷酸氢二钠溶液中的溶解率为98.16%。用2。模型实验和内部相互作用的程度变量如下:Ŷk。模型= 80、45 + 11,31 × 1 + 5,70 × 2 - 1,10 × 3 - 7,29 × 4 - 11,27 × 12 - 1,34 × 22 + 2,37 × 32 - 4,33 × 42 + 3,25 × 1 × 2 - 7,45 × 1 × 3 + 14,00 × 1 × 4 + 4,30 × 2 × 3 - 7,80 × 2 × 4 + 7,17 × 3 × 4
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