氧化物体系 FeO-MnO-MgO-SiO2 的相图。报告 1.二元氧化物体系 MnO-SiO2 和 MgO-SiO2

L. Makrovets
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引用次数: 0

摘要

锰和硅几乎存在于所有钢材中,镁可以从衬里和镁渣中进入金属,也可以以合金的形式引入,因此了解液态和固态硅酸盐溶液的热力学和相平衡可以预测钢材中非金属夹杂物的出现。FeO-MnO-MgO-SiO2体系包括六个氧化物体系的双相图和四个三相图。以前曾研究过 FeO-MnO、FeO-MgO、FeO-SiO2 和 MnO-MgO 氧化物体系的二元相图。在这项工作中,考虑了 MnO-SiO2 和 MgO-SiO2 系统的相图,计算了锰和镁硅酸盐熔化的液相线和热力学数据--锰(Mn2SiO4 和 MnSiO3)和镁(Mg2SiO4 和 MgSiO3)的正硅酸盐和偏硅酸盐的熔化焓和熔化熵。亚规则离子溶液理论考虑了配位数对熔体成分的依赖性,用于计算氧化物熔体成分的活度,准确地描述了两种不相溶液体的图表,并与文献中提供的实验数据相一致。所获得的关于 MnO-SiO2 和 MgO-SiO2 系统亚规则离子溶液理论能量参数的数据,以及关于锰和镁硅酸盐形成的热力学数据,使得研究属于 FeO-MgO-MnO-SiO2 系统的三元氧化物系统成为可能。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Phase diagrams of oxide system FeO–MnO–MgO–SiO2. Report 1. Binary oxide systems MnO–SiO2 and MgO–SiO2
Manganese and silicon are present in almost any steel, and magnesium can enter the metal from the lining and magnesian slags or be introduced in the form of an alloy, so knowledge of the thermodynamics and phase equilibria of liquid and solid silicate solutions allows to predict the appearance of non-metallic inclusions in steel. The FeO–MnO–MgO–SiO2 system includes six double and four triple phase diagrams of oxide systems. The binary phase diagrams of FeO–MnO, FeO–MgO, FeO–SiO2, and MnO–MgO oxide systems were previously studied. In this work, the phase diagrams of the MnO–SiO2 and MgO–SiO2 systems were considered, the liquidus lines and thermodynamic data on the melting of manganese and magnesium silicates – the enthalpies and entropies of melting of ortho- and metasilicates of manganese (Mn2SiO4 and MnSiO3) and magnesium (Mg2SiO4 and MgSiO3) were calculated. The theory of subregular ionic solutions, which takes into account the dependence of the coordination number on the melt composition, is used to calculate the activities of the components of the oxide melt and accurately describes the diagrams with two immiscible liquids and is consistent with the experimental data presented in the literature. The obtained data on the energy parameters of the theory of subregular ionic solutions for the systems MnO–SiO2 and MgO–SiO2, as well as the thermodynamic data on the formation of manganese and magnesium silicates, make it possible to proceed to the study of ternary oxide systems belonging to the FeO–MgO–MnO–SiO2 system.
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