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In Situ Capturing and Absorption of Sulfur Gases Formedduring Thermal Treatment of South African Coals

机译:原位捕获和吸收形成的硫气南非煤炭热处理过程中

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摘要

The objective of this study, the first of its kind on these specific South African low-sulfur coals, was to capture H2S and SO2 produced under inert and oxidizing conditions from sulfur compounds present in the coals. The capturing agents were calcium and magnesium oxides formed during the transformation of calcite and dolomite. The effectiveness of two different scrubbing solutions (0.15 M cadmium acetate and 1.1 M potassium hydroxide) for absorption of volatilized H2S and SO2 was also investigated. The bituminous coal (coal A) contained dolomite, calcite, pyrite, and organic sulfur. Lignite (coal B) had a high organic sulfur content and contained gypsum, no or low dolomite and pyrite contents, and no calcite. A third sample (coal C) was prepared by adding 5 wt % potassium carbonate to coal A. Under oxidizing conditions and at elevated temperatures, FeS2 produced Fe2O3, FeO, and SO2. It transformed to FeS and released H2S under inert conditions. Organic sulfur interacted with organically bound calcium and magnesium at 400 °C in an inert atmosphere to form calcium sulfate and oldhamite ((Ca,Mg)S). CaO, produced fromcalcite or dolomite, reacted with SO2 and O2 at 950 °C to form calcium sulfate. Treatment of lignite at400–950 °C resulted in 96–98% evolution of sulfuras gases. Hydrogen sulfide formation increased with the increasingthermal treatment temperature under inert conditions for the threecoals. Under oxidizing conditions, sulfur dioxide formation decreasedwith the increasing temperature when heating coals B and C. The lowestratio (0.01) of H2S to SO2 was achieved duringthermal treatment of the blend of coal and potassium carbonate (coalC), implying that almost all of sulfur was retained in the coal Cash/char samples. In situ capturing of sulfur gases by CaO and MgOand by the added K2CO3 in coal C to form calcium/magnesium/potassiumsulfates and potassium/calcium/magnesium aluminosilicate glasses duringutilization of these and similar coals could reduce the percentageof sulfur volatilized from the coals by 54–100%, thereby potentiallydecreasing their impact on the environment.
机译:这项研究的目标是针对这些特定的南非低硫煤进行的首次此类研究,目的是捕获煤中存在的硫化合物,在惰性和氧化条件下产生的H2S和SO2。捕获剂是在方解石和白云石转变过程中形成的钙和镁氧化物。还研究了两种不同的洗涤溶液(0.15 M醋酸镉和1.1 M氢氧化钾)对挥发的H2S和SO2吸收的有效性。烟煤(煤A)包含白云石,方解石,黄铁矿和有机硫。褐煤(煤B)具有高的有机硫含量并且包含石膏,没有或具有低的白云石和黄铁矿含量,并且没有方解石。通过向煤A中添加5 wt%的碳酸钾来制备第三种样品(煤C)。在氧化条件和升高的温度下,FeS2生成Fe2O3,FeO和SO2。它在惰性条件下转化为FeS并释放出H2S。在惰性气氛中,有机硫在400°C下与有机结合的钙和镁相互作用,形成硫酸钙和菱铁矿((Ca,Mg)S)。 CaO,由方解石或白云石,在950°C下与SO2和O2反应形成硫酸钙。褐煤的处理400–950°C导致产生96–98%的硫作为气体。硫化氢的形成随着增加而增加惰性条件下的三种热处理温度煤。在氧化条件下,二氧化硫的形成减少随煤B和C的加热温度升高而降低。H2S与SO2的比率(0.01)在煤和碳酸钾(煤)混合物的热处理C),这意味着几乎所有的硫都保留在煤C中灰/炭样品。 CaO和MgO原位捕获硫气并通过在煤C中添加K2CO3形成钙/镁/钾硫酸盐和钾/钙/镁铝硅酸盐玻璃这些和类似煤炭的利用可能会降低百分比煤中挥发的硫有54-100%,因此有可能减少对环境的影响。

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