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首页> 外文期刊>Fuel >Phase-mineral and chemical composition of coal fly ashes as a basis for their multicomponent utilization. 4. Characterization of heavy concentrates and improved fly ash residues
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Phase-mineral and chemical composition of coal fly ashes as a basis for their multicomponent utilization. 4. Characterization of heavy concentrates and improved fly ash residues

机译:粉煤灰的相矿物学和化学组成是其多组分利用的基础。 4.表征重精矿和改进的粉煤灰残留物

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The phase-mineral and chemical composition of heavy concentrates (HCc) and improved fly ash residues (IFAs) recovered from five fly ashes (FAs) produced in four large Spanish thermo-electric power stations was characterized. The HCs were separated by sink-float separation in bromoform, while the IFAs are residues after the isolation of ceramic cenosphere, salt, magnetic, char and heavy concentrates. The HCs recovered are in the range 0.02-0.28 percent and their phase-mineral composition (in decreasing order of significance) commonly includes aluminosilicate glass, hematite, magnetite, larnite, quartz, periclase, mullite, corundum, lime, char, melilite, rutile, plagioclase, wollastonite, fenian spinel, and anhydrite. Numerous accessory minerals of Ba, Ce, Cl, Cr, Cu, F, Fe, La, Mn, P, Pb, Th, Ti, Y, and Zr, are also typical components of HCs. These fractions are enriched in As, Ca, Cr, Cu, Gd, Mg, Mn, Mo, Fe, Ni, Pb, S, Se, Ti, V, Zn, and Zr in comparison with the FAs. The IFAs isolated are in the range 71.5-97.1 percent and their phase-mineral composition (in decresing order of significance) normally includes aluminosilicate glass, mullite, quartz, char, kaolinite, plagioclase, cristobalite, wollastonite, hematite, anhydrite, K-feldspar, melilite, and corundum. The contents of most elements in IFAs are similar to FAs as Ag, Ba, Cl, Cs, Ge, Mo, S, Sb, and Sc are significantly depleted in these residues. The IFAs have an improved composition in comparison with the FAs because they are: more homogeneous and finer-grained products; abundant in pozzolan and inert constituents; and depleted in harmful components. Some genetic features, properties, possible environmental concern, and potential utilization directions related to the HCs and IFAs are described. A basis for the advanced, multicomponent, wasteless, and environmentally safety utilization of various FAs is also discussed.
机译:从西班牙四个大型火力发电厂生产的五个粉煤灰(FA)中回收的重精矿(HCc)和改进的粉煤灰残余物(IFA)的相矿物学和化学组成进行了表征。通过在溴仿中的沉浮分离法分离出HC,而IFA是分离陶瓷空心层,盐,磁性,炭和重浓缩物后的残留物。回收的HC含量在0.02-0.28%的范围内,并且其相-矿物组成(按重要性降序排列)通常包括铝硅酸盐玻璃,赤铁矿,磁铁矿,褐铁矿,石英,钙镁石,莫来石,刚玉,石灰,炭,硅镁石,金红石,斜长石,硅灰石,石尖晶石和硬石膏。 HCs的典型成分还包括大量的Ba,Ce,Cl,Cr,Cu,F,Fe,La,Mn,P,Pb,Th,Ti,Y和Zr辅助矿物。与FA相比,这些馏分富含As,Ca,Cr,Cu,Gd,Mg,Mn,Mo,Fe,Ni,Pb,S,Se,Ti,V,Zn和Zr。分离出的IFA范围为71.5-97.1%,其相矿物组成(按降序排列)通常包括铝硅酸盐玻璃,莫来石,石英,炭,高岭石,斜长石,方石英,硅灰石,赤铁矿,硬石膏,钾长石,陨石和刚玉。 IFA中大多数元素的含量与FA相似,因为这些残基中的Ag,Ba,Cl,Cs,Ge,Mo,S,Sb和Sc显着减少。与FA相比,IFA的成分有所改善,因为它们具有:更均质和更细粒度的产品;火山灰和惰性成分丰富;并且耗尽了有害成分。描述了与HC和IFA相关的一些遗传特征,特性,可能的环境问题以及潜在的利用方向。还讨论了各种FA先进,多组分,无浪费和环境安全的利用基础。

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