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Solubility of oxygen in iron-silicon melts in equilibrium with silica at 1 873 K

机译:在1 873 K时,氧在铁硅中的溶解度与二氧化硅达到平衡

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The solubility of oxygen in iron-silicon melts in equilibrium with silica was measured within the range from 0.1 up to 70 mass percent Si at 1 873 K. The experimental procedure involved alloys melting in silica crucibles under argon atmosphere. The sampling was made by melt sucking into quartz tubes, equipped with copper chillers. The oxygen content of analytical samples was determined with inert gas fusion analysis after careful sample preparation. The results obtained were treated by thermodynamic model, which allowed to calculated the activity and solubility of oxygen in Fe-Si melts up to 100 mass percent Si. The isotherm of oxygen solubility exhibits both intermediate minimum and maximum at 20 and 85 mass percent Si, respectively. The corresponding values of oxygen saturated contents are as follows: 1.4 and 94 mug/g. The activity coefficient of oxygen shows alternating deviations from the additive behaviour. These are positive in the iron rich melts, containing up to 45 mass percent Si. In the melts with higher silicon content the deviations from additivity are negative. The following values of interaction parameters were calculated: epsilon_(O(Fe))~Si =12.9 + - 2.7 and epsilon_(O(Si))~Fe = -6.5 + - 2.0.
机译:在1873 K时,测量了氧在与二氧化硅平衡的铁硅熔体中的溶解度,范围为0.1至70质量%Si。该实验程序涉及在氩气氛下在硅坩埚中熔化合金。通过将熔体吸入装有铜冷却器的石英管中进行采样。仔细准备样品后,通过惰性气体熔融分析确定分析样品的氧含量。通过热力学模型处理获得的结果,该模型允许计算氧在Fe-Si熔体中达到100质量%Si的活性和溶解度。氧溶解度的等温线分别在20和85质量%的Si处表现出中间的最小值和最大值。氧饱和含量的相应值如下:1.4和94马克杯/克。氧的活度系数显示出与添加剂行为的交替偏离。这些在富含铁的熔体中是阳性的,其铁含量最高为45质量%。在硅含量较高的熔体中,与可加性的偏差为负。计算以下相互作用参数值:ε_(O(Fe))〜Si = 12.9 +-2.7和ε_(O(Si))〜Fe = -6.5 +-2.0。

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