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High-Phosphorus Fuel Combustion: Effect of Oxyfuel Conditions on PM10 Emission from Homo- and Heterogeneous Phases

机译:高磷燃料燃烧:含氧燃料条件对均相和非均相PM10排放的影响

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摘要

Volatiles and char were prepared from the pyrolysis of a biosolid (with a phosphorus content of similar to 2.3 wt %) at 1000 degrees C and then combusted separately in air and oxyfuel (30% O-2 in CO2) in a drop-tube furnace at 1300 degrees C. The aim is to understand the effect of oxyfuel conditions on the emission of particulate matter with aerodynamic diameters of <10 mu m (PM10) from separated combustion in homo- and heterogeneous phases, respectively. For volatiles combustion in homogeneous phase that leads to only PM1 (dominantly PM0.1) emission, a change from air to oxyfuel results in an increase in PM1 emission as a result of a higher yield of Na, K, S, and P, likely resulting from enhanced sulfation of alkali species under oxyfuel conditions (with a higher O-2 content), but leads to a negligible effect on the release of trace elements (As, Cd, Pb, V, and Zn). On the contrary, for char combustion in heterogeneous phase that contributes to both PM1 and PM1-10 emissions, a change from air to oxyfuel conditions leads to a reduction in PM1 emission but little change in the PM1-10 yield. Such a reduction in PM1 is contributed by reductions in the yields of Na, K, and P, most likely as a result of part of volatilized P to react with CaO to form non-volatile Ca3PO4. For trace elements during char combustion in heterogeneous phase, oxyfuel conditions lead to reductions in As and Cr released as PM1 (most likely as a result of the enhanced formation of Al/Fe/Ca arsenate and iron chromate) but have little effect on the release of Co, Cu, Mn, Ti, and V. The results show that P plays an important role in PM10 emission. For volatiles combustion in homogeneous phase, P is present in PM0.1 (contributes to most of the PM1 formed) in the form of both (Na,K)PO3 and P4O10 that is slightly favored under the oxyfuel conditions as a result of a higher O-2 content. However, for char combustion in heterogeneous phase, P is present in PM0.1 dominantly as (Na,K)PO3, with little P4O10 under both air and oxyfuel conditions. Phosphorus in PM1-10, which is only produced during char combustion, is in the form of Mg-3(PO4)(2) and Ca-3(PO4)(2) under both air and oxyfuel conditions.
机译:挥发物和木炭是由生物固体(磷含量接近2.3 wt%)在1000摄氏度下热解制备的,然后在滴管炉中分别在空气和含氧燃料(CO 2中的30%O-2)中燃烧。旨在了解含氧燃料条件对分别来自均相和异相燃烧的空气动力学直径小于10微米(PM10)的颗粒物排放的影响。对于仅导致PM1(主要为PM0.1)排放的均相中的挥发物燃烧,由于Na,K,S和P的产率更高,从空气变为含氧燃料会导致PM1排放增加这是由于在含氧燃料条件下(具有较高的O-2含量)碱性物质的硫酸盐化作用增强所致,但对微量元素(砷,镉,铅,钒和锌)的释放影响可忽略不计。相反,对于异质相中的焦炭燃烧,这会同时导致PM1和PM1-10排放,从空气状态变为含氧燃料条件会导致PM1排放量减少,但PM1-10收率变化很小。 PM1的这种减少归因于Na,K和P收率的降低,这很可能是部分挥发的P与CaO反应形成非挥发性Ca3PO4的结果。对于异相煤焦燃烧过程中的痕量元素,含氧燃料条件导致以PM1形式释放的As和Cr减少(很可能是由于Al / Fe / Ca砷酸根和铬酸铁形成的增加),但对释放的影响很小结果表明,P在PM10排放中起重要作用。对于均相中的挥发物燃烧,P以(Na,K)PO3和P4O10的形式存在于PM0.1中(占形成的大多数PM1的形式),由于较高的含氧量,P在氧气燃料条件下略受青睐O-2含量。但是,对于非均相的焦炭燃烧,P在PM0.1中主要以(Na,K)PO3的形式存在,在空气和含氧燃料条件下P4O10很少。 PM1-10中的磷仅在焦炭燃烧过程中产生,在空气和含氧燃料条件下均以Mg-3(PO4)(2)和Ca-3(PO4)(2)的形式存在。

著录项

  • 来源
    《Energy & fuels》 |2017年第3期|2317-2323|共7页
  • 作者

    Liaw Sui Boon; Wu Hongwei;

  • 作者单位

    Curtin Univ, Dept Chem Engn, GPO Box U1987, Perth, WA 6845, Australia;

    Curtin Univ, Dept Chem Engn, GPO Box U1987, Perth, WA 6845, Australia;

  • 收录信息 美国《科学引文索引》(SCI);美国《工程索引》(EI);美国《生物学医学文摘》(MEDLINE);
  • 原文格式 PDF
  • 正文语种 eng
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