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    蔡根才. QDTA/T/EGD/GC在线联同技术——Ⅷ.菱铁矿、高岭土及其混合矿物的热分解反应机理[J]. 华东理工大学学报(自然科学版), 1992, (3).
    引用本文: 蔡根才. QDTA/T/EGD/GC在线联同技术——Ⅷ.菱铁矿、高岭土及其混合矿物的热分解反应机理[J]. 华东理工大学学报(自然科学版), 1992, (3).

    QDTA/T/EGD/GC在线联同技术——Ⅷ.菱铁矿、高岭土及其混合矿物的热分解反应机理

    • 摘要: 从测得的DTA/EGD/GC曲线所提供的信息和数据表明:菱铁矿中含有微量高岭土,则在热分解逸出气的GC谱图中就有H_2峰出现。由于气相色谱对H_2的检出灵敏度特高,可作为对菱铁矿中含有羟基结构的微量粘土及其矿物杂质的检测方法,反之亦然。其检测极限低于X-射线衍射法。文中探讨了菱铁矿/高岭土混合矿物在N_2气氛下产生H_2的反应机理。

       

      Abstract: The information and data supplied by the detected DTA/EGD/GC curves shows: if the siderite involves micro kaolinite, H_2 peak will appear on the GC profile of the evolved gas of the thermal decomposition. The gas chromatography has extremely high sensibility to identify H_2, so it is a method to detect siderite which contains micro clays and impurity minerals with OH groups, vice versa. Its detection limits are lower than that of X-ray diffration. The reaction mechanism of producing H_2 by siderite/kaolinite mixed minerals under flowing nitrogen is discussed.

       

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