Estimating the maximum size of explosive iron sulfide particles

N. Poletaev
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引用次数: 1

Abstract

Introduction. There are estimates of the maximum size dcr of explosive particles of the two types of sulfide ores. The estimates are based on a qualitative approach to the dispersion analysis of combustible ore specimens (Soundararajan, Amyotte & Pegg, 1996): 49 μm < dcr, PO < 63 μm for pyrrhotite (PO) and 85 μm < dcr, PY < 145 μm for pyrite (PY). The task was to refine these estimates using the quantitative method of the mentioned analysis, taking into account the lower explosive limit (LEL) of flame propagation in terms of ore suspensions. Experimental data processing method. Continuous functions F of particle size distribution d were constructed for the two polydisperse specimens of pyrrhotite (LELPO,1 = 475 g/m3 and LELPO,2 = 1,375 g/m3) and two polydisperse specimens of pyrite (LELPY,1 = 375 g/m3 and LELPY,2 = 500 g/m3). The obtained functions FPO,1(d), FPO,2(d), FPY,1(d) and FPY,2(d) were converted using Rosin – Rammler distributions, filling the gaps between the discrete data of the grain-size analysis of the specimens. dcr rating. The procedure for estimating dcr (Poletaev, 2014) was employed to find the values of dcr, PO and dcr, PY using the following equations: FPO,1(dcr, PO)/FPO,2(dcr, PO) = LELPO,2/LELPO,1 and FPY,1(dcr, PY)/FPY,2(dcr, PY) = LELPY,2/LELPY,1. The solutions were presented in the visual graphic format.Discussion of the results. Due to the low values of explosion parameters of pyrrhotite and pyrite in a 20‑liter chamber (maximum explosion pressure Pmax ≤ 350 kPa, index Kst ≤ 2 MPa ∙ m/s), the validity of classifying ores as explosive dusts was discussed. Low explosion values have proven that sulfur is the main fuel in the air suspension. The explosiveness of ores is proven empirically (Selle & Zehr, 1954) by estimating the combustion temperature, which exceeds 1,000 °С.Conclusions. The values of dcr for sulfide ores have been refined: for pyrrhotite, dcr = 40 μm; for pyrite dcr = 107 μm. In the air suspensions of ores, only sulfur is burnt out, which substantially reduces the explosiveness of ores.
估计爆炸性硫化铁颗粒的最大尺寸
介绍。对这两种硫化物矿石的爆炸颗粒的最大尺寸dcr进行了估计。这些估计是基于可燃矿石样品色散分析的定性方法(Soundararajan, Amyotte & Pegg, 1996):磁黄铁矿(PO) 49 μm < dcr, PO < 63 μm,黄铁矿(PY) 85 μm < dcr, PY < 145 μm。任务是使用上述分析的定量方法来改进这些估计,同时考虑到矿石悬浮物火焰传播的爆炸下限(LEL)。实验数据处理方法。对两种磁黄铁矿多分散试样(LELPO,1 = 475 g/m3和LELPO,2 = 1375 g/m3)和两种黄铁矿多分散试样(LELPY,1 = 375 g/m3和LELPY,2 = 500 g/m3)构建粒径分布d的连续函数F。得到的函数FPO,1(d), FPO,2(d), FPY,1(d)和FPY,2(d)用Rosin - Rammler分布进行转换,填补了试样粒度分析离散数据之间的空白。dcr评级。采用估计dcr (Poletaev, 2014)的方法,利用以下方程求出dcr, PO和dcr, PY的值:FPO,1(dcr, PO)/FPO,2(dcr, PO) = LELPO,2/LELPO,1和FPY,1(dcr, PY)/FPY,2(dcr, PY) = LELPY,2/LELPY,1。解决方案以可视化图形的形式呈现。结果的讨论。由于磁黄铁矿和黄铁矿在20升硐室中爆炸参数值较低(最大爆炸压力Pmax≤350 kPa,指标Kst≤2 MPa∙m/s),讨论了将矿石分类为爆炸性粉尘的有效性。低爆炸值证明了硫是空气悬架的主要燃料。矿石的爆炸性是经验证明(Selle & Zehr, 1954)通过估计燃烧温度,超过1000°С.Conclusions。对硫化物矿石的dcr值进行了细化:磁黄铁矿的dcr = 40 μm;黄铁矿DCR = 107 μm。在矿石的空气悬浮液中,只有硫被燃烧掉,这大大降低了矿石的爆炸性。
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