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A reaction rate model for pyrite oxidation considering the influence of water content and temperature

机译:考虑水含量和温度影响的黄铁矿氧化反应速率模型

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Natural oxidation of pyrite in refractory gold bearing rock stockpiles may facilitate the recovery of gold contained in mined low-grade material that was originally sub-economic due to the cost of pre-treatment to oxidise fresh pyrite. The evaluation of this potential requires the oxidation level of pyrite under various conditions. This paper proposes a reaction rate model for prolonged natural oxidation of pyrite under various water saturation conditions and temperatures and a circum-neutral to alkaline pH. The application is to a natural pre-treatment process for refractory gold ore to liberate the gold content encapsulated in pyrite crystals and allow effective cyanidation for gold extraction. The proposed model is based on the shrinking core model with half-order surface reaction on the pyrite surface. It assumes that, in unsaturated water conditions and at circum-neutral to alkaline pH, a diffusion barrier forms on the fresh pyrite surface during the reaction, which prohibits the diffusion of oxygen to the reacting sites and lowers the reaction rate over time. The diffusion barrier may consist of a thin solution film, some precipitations of soluble oxidation products and/or insoluble oxidation products depending on the water saturation and pH. The diffusivity of this diffusion barrier for oxygen is determined as a function of water saturation and temperature. In this model, the concept of effective oxygen concentration is also proposed to represent the change in oxygen concentration at the particle surface due to water; an exponential relationship is found to be appropriate. Based on the reaction rate data reported in the literature, the reaction rate constant in the model for the surface reaction is determined as 5 x 10(-8)mol(0.5).m(-0.5).s(-1) while the diffusion coefficient is 1.2 x 10(-15)m(2).s(-1) for water saturation of 25% and above and 4.7 x 10(-19) m(2).s (-1) for 0.1% water saturation. This rate model can be used for predicting and modelling the level of pyrite oxidation in rock piles or mine tailings where various unsaturated water conditions and circum-neutral to alkaline pH apply.
机译:耐火金轴承岩石库存中的硫铁矿的自然氧化可以促进所占用的低级材料中的金的回收,原本是由于预处理到氧化新鲜黄铁矿的成本。对该潜力的评价需要在各种条件下氧化水平。本文提出了一种反应速率模型,其在各种水饱和条件下延长硫铁矿的延长自然氧化和温度和环状pH值。该应用对于难治性金矿石的天然预处理方法,以释放包封在硫铁矿晶体中的金含量,并允许有效的金色氰化。所提出的模型基于缩收核模型,在硫铁矿表面上具有半阶表面反应。它假设在不饱和水条件和环形中性至碱性pH下,在反应过程中,在新鲜的硫铁矿表面上形成扩散阻挡层,这禁止氧气扩散到反应位置并随时间降低反应速率。扩散屏障可以由薄溶液膜组成,根据水饱和度和pH值,可溶性氧化产物和/或不溶性氧化产物的一些沉淀。该扩散屏障的氧气的扩散性被确定为水饱和度和温度的函数。在该模型中,还提出了有效氧浓度的概念,以表示由于水引起的颗粒表面上的氧浓度的变化;发现指数关系是合适的。基于文献中报道的反应速率数据,表面反应模型中的反应速率常数确定为5×10(-8)摩尔(0.5)。(-0.5)。(-1)扩散系数为1.2×10( - 15)m(2)。(-1)水饱和度为25%及以上,4.7×10(-19)m(2)。(-1)0.1%水饱和。该速率模型可用于预测和建模岩桩或矿井尾矿中的硫铁矿水平,其中各种不饱和水条件和碱性至碱性pH施用。

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