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Fundamental Investigation of Reduction and Dissolution Behavior of Manganese Ore at High Temperature

机译:高温下锰矿矿石还原及溶出行为的根本调查

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The high temperature reduction behavior of manganese ore was investigated with the aim of utilizing ore as a more economical manganese source in the steelmaking process. The melting temperature and phase change behaviors of raw and sintered manganese ores were measured by high temperature X-ray diffraction and DTA in the temperature range from 303K to 1773K under atmospheric and vacuum conditions. The melting temperatures of the raw and sintered manganese ores were 1688K and 1732K, respectively. The main manganese compounds in the raw and sintered manganese ores were CaMn_6SiO_(12) and MnO, Mn_3O_4 respectively. Under a vacuum (0.13kPa), both the raw and sintered manganese ores were reduced to MnO above 1473K, whereas under the atmospheric condition (101.3kPa), the manganese ores were reduced to Mn_3O_4 rather than MnO. The obtained results were discussed from a thermodynamic viewpoint.
机译:研究了锰矿矿石的高温降温行为,目的是利用矿石作为炼钢过程中更经济的锰来源。通过高温X射线衍射和DTA在大气和真空条件下通过高温X射线衍射和DTA测量原料和烧结锰矿矿石的熔化温度和相变行为。原料和烧结锰矿矿石的熔化温度分别为1688K和1732K。原料和烧结锰矿石中的主要锰化合物分别是Camn_6siO_(12)和MnO,Mn_3O_4。在真空(0.13kPa)下,将原料和烧结锰矿矿石均低于1473K以上的MNO,而在大气条件下(101.3kPa),锰矿石将锰矿矿石还原成Mn_3O_4而不是MNO。从热力学观点讨论了所得结果。

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