通过TG-DSC和SEM对仲钼酸铵在空气中热分解过程进行分析,结果表明:仲钼酸铵在空气中的热分解过程经历了3个阶段:室温至222.6℃之间仲钼酸铵失去结晶水;从222.6~240.7℃之间仲钼酸铵热分解了部分氨根离子;从240.7~248.7℃之间氨根离子完全分解,同时有亚稳态的氧化钼生成.从248.7~322.5℃之间亚稳态的氧化钼发生相变生成了稳态的三氧化钼.与此同时,仲钼酸铵在热分解温度300℃以下时,其热分解产物的形貌几乎没有太大的变化;在300℃以上时,其热分解产物的形貌由原来不规则的块体向不规则的片状转变,最后转变为了较规则的片状三氧化钼.这主要是由于随着热分解温度的进一步升高,热分解产物之间的相互作用、迁移和重组加剧,以及在高温下三氧化钼的挥发与沉积所致.
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