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Verification of numerical modeling results using analytical solution for oxygen diffusion process in sulfide waste dump

机译:使用硫化物废料蒸馏氧扩散过程的分析解决方案验证数值模拟结果

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Weathering of pyrite -containing rocks causes the well-known problem of acid rock drainage. Depending on the rate of pyrite oxidation, availability of water and oxidants and buffering capacity of surrounding rocks and sediments, the pH of the drainage is often very low When the pyrite or other sulfide mineral exposure by the atmosphere and water, the acid mine drainage was generated. Oxygen can be transported into the waste deposit by three mechanisms: (1) advective transport with water, (2) free ore forced air convection and (3) diffusion in the gaseous and aqueous phases through pores in waste material In generally, the pyrite oxidation and acid generation were controlled by oxygen diffusion. So, in this research was attempted that variation of oxygen concentration in waste dump depths was investigated and the analytical and numerical models results (obtained using PHOENICS software) were compared. The obtained results can use for controlling and reducing the environmental impacts.
机译:黄铁矿岩石的风化导致酸岩排水的众所周知的问题。取决于黄铁矿氧化,水和氧化剂的可用性和周围岩石和沉积物的缓冲能力,当大气和水的硫化石或其他硫化物矿物暴露时,引流的pH通常非常低,酸性矿矿物排水生成。氧气可以通过三种机制运输到废沉积中:(1)与水,(2)游离矿石的平均运输,(3)在气态和水相中通过废料中的孔隙中的扩散,通常是硫铁矿氧化通过氧气扩散控制酸产生。因此,在该研究中,研究了废物倾卸深度中氧浓度的变化,并比较了分析和数值模型(使用噬菌体软件获得)。所获得的结果可用于控制和降低环境影响。

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