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THE MODIFICATION OF PYRITE AND ARSENOPYRITE SPECIFIC SURFACE AND POROSITY AT THERMAL DECOMPOSITION

机译:热分解过程中黄铁矿和亚砷铁矿比表面积的改性和孔隙率

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The paper contains the results of studying about modification of pyrite and arsenopyrite specific surface and porosity at their thermal decomposition. The studying of specific surface was carry out by B.E.T. - adsorption of nitrogen at his boiling-point. In our work were using the electron-microscopical, X-ray structure analysis and chemical analysis. There was established that the decomposition of pyrite and arsenopyrite accompany by increasing of pores volume from 0.303 • 10~(-3) to 1.23 • 10~(-3) at increasing of pyrite degree of decomposition about 41 % and then decrease about 0.131 • 10~(-3)m~3/g at degree of decomposition near 100 %. The surface area of pores increase from 0.31 to 1.085 m /g with following lowering due to enlargement and confluence of minor, small pores. Increasing of porosity accompany with increasing of particles windage that appear the result of heightened dust-furnace partially decomposing pyrite and arsenopyrite particles by air flow from furnace reaction zone. This explains heightened contention of sulfide sulfur in roast dust of sulfide concentrate.
机译:本文包含有关黄铁矿和毒砂的比表面积和热分解时的孔隙率的改性的研究结果。比表面积的研究是由B.E.T. -在沸点处吸收氮。在我们的工作中,使用了电子显微镜,X射线结构分析和化学分析。确定黄铁矿和毒砂的分解伴随着孔体积从0.303•10〜(-3)增加到1.23•10〜(-3),同时黄铁矿分解度增加约41%,然后降低约0.131•。分解度接近100%时为10〜(-3)m〜3 / g。孔的表面积从0.31增加到1.085 m 2 / g,随后由于小孔的扩大和汇合而降低。孔隙率的增加伴随着颗粒风阻的增加,这似乎是由于炉子反应区的空气流使粉尘炉部分分解了黄铁矿和毒砂的结果所致。这解释了硫化物精矿的焙烧粉尘中硫化物硫的含量增加。

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