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Technogenic Magnetic Particles in Alkaline Dusts from Power and Cement Plants

机译:发电厂和水泥厂产生的碱性粉尘中的技术性磁性颗粒

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During this study, we investigated the min-eralogical characterization of technogenic magnetic particles (TMPs) contained in alkaline industrial dust and fly ash emitted by coal burning power plants and cement plants. The reaction of tested dust samples varied between values of pH 8 and pH 12. Their magnetic properties were characterized by measurement of magnetic susceptibility (x), frequency dependence of magnetic susceptibility (Xfd), and temperature dependence of magnetic susceptibility. Mineralogical and geochemical analyses included scanning electron microscopy with energy dispersive spectroscopy, mi-croprobe analysis and X-ray diffraction. The TMPs in fly ash from hard coal combustion have the form of typical magnetic spherules with a smooth or corrugated surface as well as a skeletal morphology, composed of iron oxides (magnetite, maghemite, and magnesio-ferrite) that occurred in the form of incrustation on the surface of mullite, amorphous silica, or aluminosilicate particles. The TMPs observed in fly ash from lignite combustion have a similar morphological form but a different mineralogical composition. Instead of magnetite and magnesioferrite, maghemite and hematite with lower x values were the prevailing magnetic minerals, which explains the much lower magnetic susceptibility of this kind of ash in comparison with the ash from hard coal combustion, and probably results from the lower temperature of lignite combustion. Morphology and mineralogical composition of TMPs in cement dust is more diverse. The magnetic fraction of cement dust occurs mostly in the form of angular and octahedral grains of a significantly finer granulation (<20 μm); however, spherules are also present. A very characteristic magnetic form for cement dust is calcium ferrite (CaFe_3O_5). The greatest impact on the magnetic susceptibility of cement dust results from iron-bearing additives (often waste materials from other branches of industry), which should be considered the most dangerous to the environment. Stoichiometric analysis of micro-particles confirmed the presence of heavy metals such as Pb, Mn, Cd, and Zn connected with TMPs, which are carriers of magnetic signals in atmospheric dust. Therefore, in some cases, their presence in topsoil when detected by magnetic measurement can be treated as an indicator of inorganic soil contamination.
机译:在这项研究中,我们调查了燃煤电厂和水泥厂排放的碱性工业粉尘和飞灰中所含技术磁粉(TMP)的最小能谱特征。被测粉尘样品的反应在pH 8和pH 12的值之间变化。通过测量磁化率(x),磁化率的频率依赖性(Xfd)和磁化率的温度依赖性来表征其磁性能。矿物学和地球化学分析包括具有能量色散谱的扫描电子显微镜,微型探针分析和X射线衍射。硬煤燃烧产生的粉煤灰中的TMP具有典型的磁性小球,其表面光滑或呈波纹状,且具有骨骼形态,由以硬壳形式出现的氧化铁(磁铁矿,磁赤铁矿和镁铁氧体)组成莫来石,无定形二氧化硅或铝硅酸盐颗粒的表面。褐煤燃烧产生的飞灰中观察到的TMP具有相似的形态形式,但矿物组成不同。具有较低x值的磁赤铁矿和赤铁矿代替了磁铁矿和镁铁矿,是主要的磁性矿物,这解释了这种灰的磁化率与硬煤燃烧的灰相比要低得多,并且可能是褐煤温度较低的结果燃烧。水泥粉尘中TMP的形态和矿物学组成更为多样。水泥粉尘的磁性部分主要以角粒和八面体颗粒的形式出现,其颗粒明显更细(<20μm)。但是,也存在小球。水泥粉尘的一种非常典型的磁性形式是铁酸钙(CaFe_3O_5)。含铁添加剂(通常是其他行业的废料)对水泥粉尘的磁化率影响最大,应将其视为对环境最危险的物质。微粒的化学计量分析证实,存在与TMP连接的重金属,例如Pb,Mn,Cd和Zn,这些金属是大气尘埃中磁信号的载体。因此,在某些情况下,当通过磁力测量检测到它们在表土中的存在时,可以将其视为无机土壤污染的指标。

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