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首页> 外文期刊>Energy & fuels >A Novel Two-Stage Alumina Reactor System for Burning Volatiles Generated in Situ from Biosolid: Effect of Pyrolysis Temperature and Combustion Conditions on PM_1 Emission
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A Novel Two-Stage Alumina Reactor System for Burning Volatiles Generated in Situ from Biosolid: Effect of Pyrolysis Temperature and Combustion Conditions on PM_1 Emission

机译:一种新型的两阶段氧化铝反应器系统,用于燃烧生物固体原位挥发物:热解温度和燃烧条件对PM_1排放的影响

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摘要

A novel two-stage alumina reactor system is developed for studying particulate matter (PM) emission from in situ volatiles combustion. It enables the generation of in situ volatiles at different pyrolysis temperatures (up to 1300 degrees C) and the subsequent combustion of in situ volatiles in air and oxyfuel at 1300 degrees C. It is found that the PM emitted from volatiles combustion contains only PM with aerodynamic diameter 1 mu m (PM1) and has a unimodal distribution. An increase in pyrolysis temperature from 1100 to 1300 degrees C results in a substantial increase in PM1 yield and a shift of fine mode diameter from 0.043 to 0.108 Jim. The PM1 emitted from the volatiles generated at 1100 degrees C mainly consists of Na, K, S, and P. For PM, emitted from the volatiles generated at 1300 degrees C, there are substantial increases in the yield of Na, K, and P; in addition, Mg and Si are present in PM1 because of the release of these inorganic species from biosolid into the volatiles. For trace elements, increasing pyrolysis temperature from 1100 to 1300 degrees C not only increases the As and Cd yields in PM1 but also results in the presence of Cr, Cu, and Mn in PM, because of increasing As and Cd volatility and the release of Cr, Cu, and Mn from biosolid into the volatiles. The yields of V and Pb remained unchanged, and there is no Ti, Ni, and Co present in the PM1. Changing the combustion atmosphere from air to oxyfuel causes a slight increase in PM, yield due to increased formation of alkali sulfates and enhanced formation of P4010 but results in no changes in the yields and particle size distributions of trace elements. Further analysis indicates the Na, K, S, and CI are present in the PM1 emitted from the combustion of volatiles produced at 1100 degrees C in the form of Na and K sulfates and Cl while P is present in the form of P4O10. The P in PM1 is present in the forms of Na, K, and Mg metaphosphates and P4O10 where higher proportion of P4O10 is formed in PM1 when pyrolysis temperature increases to 1300 degrees C. It is also evident that (Na, K)PO3 and P4O10 vapors can react with the alumina reactor tube to form alkali aluminophosphate glass which is then retained in the furnace, leading to only a fraction of Na and K in the volatiles being collected as PM1 after combustion.
机译:开发了一种新颖的两级氧化铝反应器系统,用于研究原位挥发物燃烧产生的颗粒物(PM)排放。它可以在不同的热解温度(最高1300摄氏度)下生成原位挥发物,并随后在1300摄氏度下在空气和含氧燃料中原位挥发物燃烧。发现挥发物燃烧释放出的PM仅含有PM空气动力学直径小于1微米(PM1),具有单峰分布。热解温度从1100摄氏度增加到1300摄氏度,导致PM1产量大幅增加,精细模式直径从0.043吉姆转变为0.108吉姆。在1100摄氏度时产生的挥发物释放出的PM1主要由Na,K,S和P组成。对于PM,在1300摄氏度时产生的挥发物排放出的PM中,Na,K和P的产率显着增加;另外,由于这些无机物从生物固体释放到挥发物中,所以PM1中存在Mg和Si。对于痕量元素,将热解温度从1100摄氏度提高到1300摄氏度,不仅会增加PM1中的As和Cd收率,而且还会导致PM中存在Cr,Cu和Mn,这是因为As和Cd的挥发性增加以及Pd的释放。 Cr,Cu和Mn从生物固体进入挥发物。 V和Pb的产率保持不变,并且PM1中没有Ti,Ni和Co。将燃烧气氛从空气变为含氧燃料会导致PM略有增加,由于增加了碱金属硫酸盐的形成并增加了P4010的形成,导致收率略有增加,但不会导致微量元素的收率和粒度分布发生变化。进一步的分析表明,Na,K,S和CI存在于1100℃燃烧生成的挥发物的燃烧中,并以Na和K硫酸盐和Cl的形式存在,而P以P4O10的形式存在。 PM1中的P以Na,K和Mg偏磷酸盐和P4O10的形式存在,当热解温度升高到1300摄氏度时,PM1中P4O10的比例较高。很明显(Na,K)PO3和P4O10蒸汽可与氧化铝反应器管反应形成碱金属铝磷酸盐玻璃,然后将其保留在炉中,导致燃烧后仅将一部分挥发分的Na和K收集为PM1。

著录项

  • 来源
    《Energy & fuels》 |2018年第9期|9438-9447|共10页
  • 作者单位
  • 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
  • 中图分类
  • 关键词

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