氧化铁浓度对feo - 2o3 - rp2o6 (R=Mg, Ca, Ba)类玻璃高熔体与气相的氧化还原平衡的影响

哲郎 吉田, 有次 岡田, 碩 平島
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引用次数: 1

摘要

为了阐明高浓度过渡金属离子在高粘性气相氧化物熔体中的氧化还原平衡,本文研究了铁浓度对FeO-Fe2O3-RP2O6体系(R=Mg, Ca, Ba)在1200℃、氧分压约为10-3.6 atm的CO2气氛下氧化还原平衡的影响。[Fe2+]/[Fe3+]比值在低氧化铁浓度下下降,随着氧化铁浓度的增加达到最小值后上升。由于R被Mg、Ca、Ba交换,这些比值在低氧化铁水平下减小,在高氧化铁水平下增大。通过这种交换,[Fe2+]/[Fe3+]比值的最小值向低氧化铁浓度转移。从这些实验结果可以看出,在低氧化铁浓度下,自由亚铁离子与氧化铁离子(fe2 ++1/4 O2+(x-1/2)O2-=FeOx(2x-3))的反应主要起氧化还原平衡的作用,而在高氧化铁浓度下,铁离子与氧化铁离子(feoy (2y-2)-+1/4 O2=FeOx(2x-3)-+{1/2-(x-y)}O2的反应主要起氧化还原平衡的作用。结合上述两种氧化还原反应得到的[Fe2+]/[Fe3+]与[O2-]氧离子浓度的关系,与各熔体中氧化铁浓度与[Fe2+]/[Fe3+]比值关系的实验结果一致,即氧离子浓度随氧化铁浓度的增加而增加。通过在氧化还原平衡中淬火熔体得到的玻璃红外光谱,可以识别出氧离子浓度的增加。对比FeO-Fe2O3-RP2O6玻璃与RP2O6玻璃的红外光谱,发现氧化铁浓度的增加对应于RP2O6玻璃中Mg、Ca、Ba与R的交换,熔体碱度的增加。这种增加似乎伴随着熔体中磷氧化离子形式(例如,链长)的变化。从上述玻璃的光学吸收光谱中亚铁离子对吸收峰的移位发现熔体中氧化亚铁离子的形成是可能的。本文对各种离子的活性讨论不成功。
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FeO-Fe2O3-RP2O6 (R=Mg, Ca, Ba) 系ガラス熔融体と気相との酸化還元平衡に及ぼす酸化鉄濃度の影響
To elucidate the redox equilibrium of high concentration transition metal ions in a highly viscous oxide melts with gas phase, the effect of iron concentration on the redox equilibriums in the oxide melts of FeO-Fe2O3-RP2O6 system (R=Mg, Ca, Ba) at 1200°C with CO2 atmosphere, which oxygen partial pressure is about 10-3.6 atm, was studied in this report.The [Fe2+]/[Fe3+] ratios decreased at low iron oxide concentration and then increased after reaching their minimum values, as iron oxide concentration increased. These ratios also decreased at low iron oxide level and increased at high iron oxide level, as R was exchanged by Mg, Ca, Ba. The minimum values of [Fe2+]/[Fe3+] ratios shifted to the low iron oxide concentration by these exchange.It is discussed from these experimental results that the reaction between free ferrous ion and ferric oxiacid ion such asFe2++1/4 O2+(x-1/2)O2-=FeOx(2x-3)-contributes mainly to the redox equilibrium at the low iron oxide concentration, and that the reaction between oxiacid ions of ferrous and ferric ions such asFeOy(2y-2)-+1/4 O2=FeOx(2x-3)-+{1/2-(x-y)}O2-contributes mainly at the high iron oxide concentration.The relation between [Fe2+]/[Fe3+] and [O2-], oxygen ion concentration, given by the combination of the above two redox reactions, agrees with the experimental results about the relation between iron oxide concentration and [Fe2+]/[Fe3+] ratios in various melts, if the oxygen ion concentration increases with the increase of iron oxide concentration.The increase of oxygen ion concentration was recognized from the infra-red spectrums of glasses, obtained by quenching the melts in the redox equilibrium. Comparing the I. R. spectrums of FeO-Fe2O3-RP2O6 glasses with RP2O6 glasses, it was observed that the increase of iron oxide concentration corresponded to the exchanging R by Mg, Ca, Ba in RP2O6 glasses, the increase of basicity in the melts. This increase seemed to accompany with the change of the form (for example, chain length) of the phosphorus oxiacid ions in the melts. The formation of ferrous oxiacid ion in the melt was found to be possible from the shift of absorption peak by ferrous ion in the optical absorption spectrum in the above glass.Discussion about activities of various ions was not successful in this paper.
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