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Thermodynamic simulation of silicon and iron reduction and zinc and lead distillation in zincoligonite ore-carbon systems

机译:锌橄榄石矿石-碳体系中硅铁还原及锌铅蒸馏的热力学模拟

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This article is devoted to theoretical investigations into the thermodynamic simulation of a zincoligonite ore (Zhairem deposite, Kazakhstan)-carbon systems in the temperature ranges from 1000 to 3000 K and pressure range from 0.001 to 0.1 MPa using the Astra bundled software based on the entropy maximum principle. It is revealed that an increase in the amount of deoxidizer in the charge results in a decrease in the degree of conversion of silicon to elemental Si because of an increase in its conversion to carbides. The lower deoxidizer content results in an increase in the silicon fraction converted to SiO at the practically complete absence of reduced elemental Si. When reducing pressure in the system from 0.1 to 0.001 MPa, temperatures for the complete conversion of zinc (1500-1200 K) and lead (1900-1500 K) and for the beginning of silicon formation (2300-1900 K) decrease. The noticeable (> 50%) formation of elemental Si at P = 0.001 MPa can be attained at T a parts per thousand 2450 K.
机译:本文致力于使用基于熵的Astra捆绑软件对锌橄榄石矿石(哈萨克斯坦Zhairem矿床)-碳系统在1000至3000 K温度范围和0.001至0.1 MPa压力范围内的热力学模拟进行理论研究。最大原则。可以看出,由于装料中脱氧剂的量增加,导致硅向元素Si的转化率降低,这是因为硅向碳化硅的转化率增加。较低的脱氧剂含量导致在几乎完全没有还原的元素Si的情况下转化为SiO的硅部分增加。当将系统压力从0.1 MPa降低到0.001 MPa时,用于锌(1500-1200 K)和铅(1900-1500 K)完全转化以及开始形成硅(2300-1900 K)的温度降低。在P = 0.001 MPa时,可以达到T(千分之千)2450 K的显着(> 50%)形成元素Si。

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