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磷酸分解磷矿石的动力学 被引量:17

Reaction Kinetics of Phosphate Ore in Phosphoric Acid
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摘要 采用间歇反应器,在反应温度6080℃,磷酸浓度2040%P2O5,磷矿粒径0.1380.7mm,搅拌速度500转/分的条件下,研究了磷酸分解上蒜磷矿的酸解反应动力学。研究表明,在上述条件下,该过程的速率控制步骤为氢离子通过Ca(H2PO4)2的固态膜向反应界面的扩散。并建立了酸解过程的动力学模型,该模型在α=0.05上显著。表观活化能Ea=10.08kJ·mol-1。 The experiments were carried out in a batch reactor. The reaction temperature was varied from 60 to 80℃, the initial phosphoric acid concentration 20 to 40 wt%P 2O 5, the initial mean particle size 0.138 to 0.7 mm, and the stirrer speed was 500 rpm. Under such conditions, the acidulation process of Shangsuan phosphate ore in phosphoric acid was investigated. The results showed that the rate determining step of the digestion process was the diffusion of hydrogen ions away from the bulk of the solution through the coating layer of Ca(H 2PO 4) 2 into the reaction surface. By applying the unreacted shrinking core model, a rate equation for the digestion process was fitted to experimental results as follows:1-3(1-x B) 2/3 +2(1-x B)=144.2 exp (-1.008×10 4RT)C 2.075 A0 R -0.1799 s exp (-1τ)\ \ The apparent activation energy E a was 10.08 kJ·mol -1
出处 《高校化学工程学报》 EI CAS CSCD 北大核心 1998年第3期265-270,共6页 Journal of Chemical Engineering of Chinese Universities
关键词 磷酸 酸解反应 缩芯模型 动力学 磷矿 Phosphoric acid, Acidulation reaction, Unreacted shrinking core model
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  • 1王建华,化学反应工程,1988年

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