钼酸盐
蒸发
热重分析
热重分析
钼
氧化物
产量(工程)
材料科学
氧化钼
大气温度范围
无机化学
氧化钙
冶金
化学
有机化学
热力学
物理
作者
A. Chychko,Lisong Teng,S. Seetharaman
标识
DOI:10.1002/srin.201000055
摘要
Abstract The evaporation rate of molybdenum oxide from mixtures with CaO or MgO was studied in the temperature range 300‐1573 K. The investigations were carried out using high temperature X‐ray diffraction and thermogravimetry. Further, additions of these precursors to molten steel in the laboratory scale and the Mo yield achieved were determined. The X‐ray studies show that the calcium molybdate is formed from the oxide mixture in the temperature interval 773‐873 K, which precedes the beginning of evaporation of MoO 3 . Results of thermogravimetric studies with mixtures CaO and MgO with MoO 3 as well as the compounds CaMoO 4 and MgMoO 4 confirm the above results. Addition of various molybdenum precursors, viz. the mixtures of carbon with pure MoO 3 , CaMoO 4 and MgMoO 4 , as well as oxide mixtures (CaO + MoO 3 , MgO + MoO 3 ) show that the highest yield was observed for CaMoO 4 + C and MoO 3 + C mixtures, while MgO + C + MoO 3 mixture showed much lower yield.
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