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Investigation of Ilmenite Reduction Behaviour Using In-situ Synchrotron Radiation based X-ray Powder Diffraction

机译:基于X射线粉末衍射原位同步辐射的钛铁矿还原行为研究

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Reduction of weathered mineral ores can initiate phase transformation which can affect either their activation or deactivation, subsequently influencing the extent of extraction of desired metals in a leaching reagent. The reduction of ilmenite ores for one occurs as a series of parallel, solid state reactions which at present has no known mechanisms, although the evidence of their effects is abundant. Understanding these reactions may well be the key to uncovering the mechanism of ilmenite activation, hence enabling precise control of its reaction process to maximize yield of TiO2 extraction. However, documenting the solid state reactions in the reduction of ilmenite is challenging due to the ore complexity, the number of simultaneous reactions and the difficulty of capturing critical intermediate reactions and phase transformations during processing.The phase transformations of ilmenite minerals reduced at temperatures up to 850°C were investigated in this study. Mineral transformations were studied in-situ using synchrotron radiation based X-ray powder diffraction with temperature resolved tests. The effect of the extent of reduction and specific mineral transformations were verified by leaching reduced ore with sulphuric acid. The results suggest that transformation of major mineral phases occurs within of specific window of operation and thermal treatment appears to influence the extent of activation and leachability of ilmenire minerals.
机译:风化矿物矿石的还原可以引发相变,这可能会影响其活化或失活,从而影响到浸出试剂中所需金属的提取程度。钛铁矿矿石的还原是通过一系列平行的固态反应发生的,虽然目前尚无已知的机理,但其作用的证据十分丰富。了解这些反应很可能是揭示钛铁矿活化机理的关键,因此可以精确控制其反应过程,以最大程度地萃取TiO2。然而,由于矿石的复杂性,同时发生的反应数量以及在加工过程中难以捕获关键的中间反应和相变,因此记录钛铁矿还原过程中的固态反应是一项挑战。在这项研究中研究了850°C。使用基于同步辐射的X射线粉末衍射和温度分辨测试对矿物转化进行了原位研究。还原程度和特定矿物转化的影响通过用硫酸浸出还原矿石来验证。结果表明,主要矿物相的转变发生在特定的操作窗口内,热处理似乎影响了钛铁矿矿物的活化程度和浸出率。

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