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Removal of Phosphorus from High-phosphorus Iron Ore with Preliminary Reduction Treatment and Physical Concentration

机译:初步还原处理和物理浓缩去除高磷铁矿石中的磷

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Fundamental experiments were conducted with the aim of crude separation of the phosphorus contained in high-P iron ore prior to the ironmaking process. By reducing high-P iron ore with lime and graphite at an appropriate blending ratio and temperature, a reduction product was obtained consisting of a P-concentrated phase, metallic Fe with low P, and an Fe oxide-containing phase. The reduction product was pulverized by electrical pulse disintegration, and a magnetic separation experiment was performed for each particle group. As a result, 57.5% of the P contained in the reduction product was removed by removing particles of 250 μ m or less. Samples simulating the constituent phases of the reduction products were synthesized and subjected to magnetization measurement. It was assumed that the Fe oxide-containing phase was paramagnetic and the P-concentrated phase was diamagnetic. We calculated the magnetic and drag forces acting on the paramagnetic particles in wet magnetic separation. When the magnetic field gradient was low, the magnetic forces acting on the fine particles were low, and attraction was difficult due to the drag force of water.
机译:进行基础实验的目的是在炼铁过程之前粗分离高磷铁矿石中所含的磷。通过在适当的混合比和温度下用石灰和石墨还原高磷铁矿石,可以得到还原产物,该还原产物由P富集相,低P的金属Fe和含Fe氧化物相组成。通过电脉冲分解将还原产物粉碎,并且对每个颗粒组进行磁分离实验。结果,通过除去250μm或更小的颗粒,除去了还原产物中所含的P的57.5%。合成模拟还原产物的组成相的样品,并进行磁化强度测量。假定含Fe氧化物的相是顺磁性的,而P-浓缩相是抗磁性的。我们计算了湿法磁选中作用在顺磁性颗粒上的磁力和阻力。当磁场梯度低时,作用在细颗粒上的磁力低,并且由于水的阻力而难以吸引。

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