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Urban fine particulate matter: Chemical composition and possible origins.

机译:城市细颗粒物:化学成分和可能的来源。

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摘要

Fine aerosol plays an important role in the atmosphere's radiative transfer. Elevated fine aerosol concentration in urban areas can result in visibility reduction and human respiratory diseases. To study the chemical composition and possible origins of fine particulate matter (PM 2.5) in the Baltimore-Washington (B-W) corridor, chemically speciated PM2.5 and trace gases (including NH3, HNO3, CO, SO2, NOy) have been measured at Fort Meade (FME: 39.10°N, 76.74°W; elevation 46 m MSL), Maryland over a three-year period (1999–2002) including nine seasonally-representative months. FME is suburban, located in the middle of the B-W corridor, and generally downwind of the highly industrialized Midwest. The PM2.5 shows an annual mean concentration of ∼13 μg m−3. On average, over 90% of the PM2.5 mass can be attributed to sulfate, nitrate, ammonium, carbonaceous material, and crustal material. The PM 2.5 reconstructed mass is found ±15% different from its gravimetric mass. Ammonium sulfate dominates (>50%) in the summertime high PM episodes while organic matter also contributes (∼30%). By comparing the FME data with concurrent measurements at upwind and downwind sites, sulfate and crustal material are found to be more regional than other major components.; The inorganic fraction of fine aerosol is studied using a thermodynamic model, ISORROPIA. FME changes from an ammonia-poor environment in summer to an ammonia-rich environment in winter. ISORROPIA also estimates the aerosol water content; water can contribute to >50% of the atmospheric extinction in the visible region on humid days.; The elemental carbon (EC)/CO ratio observed at FME is compared to those from individual vehicles, tunnel studies, and biomass burning to estimate the contribution from each potential source. Ambient temperature appears to influence emission factors. Based on a well-established CO emission inventory, the EC/CO ratio leads to an estimate of EC emission at 0.32 ± 0.12 Tg (EC) yr−1 for North America.; Using a factor analysis module, UNMIX, six factors that contribute to the PM2.5 mass are resolved; these include regional sulfate, local sulfate, wood smoke, mobile, secondary nitrate, and copper/iron processing industry. The six factors are studied further using an ensemble back trajectory method to identify the possible source locations. Regional sulfate and wood smoke are more regional than other factors and associated with westerly and southerly transport, respectively. This study suggests that the local contribution to the PM2.5 mass can vary from 30% in summer to >60% in winter.
机译:优良的气溶胶在大气的辐射传递中起着重要作用。城市地区气溶胶浓度的升高会导致能见度降低和人类呼吸系统疾病。研究巴尔的摩-华盛顿(BW)走廊的细颗粒物(PM 2.5 ),化学形态的PM 2.5 和痕量气体(包括NH)的化学成分和可能的起源在米德堡(FME)测量了 3 ,HNO 3 ,CO,SO 2 ,NO y 39.10°N,76.74°W;海拔46 m MSL),马里兰州,为期三年(1999年至2002年),包括9个季节代表性月份。 FME位于郊区,位于B-W走廊的中间,通常处于高度工业化的中西部的顺风地区。 PM 2.5 的年平均浓度约为13μgm -3 。平均而言,PM 2.5 质量的90%以上可归因于硫酸盐,硝酸盐,铵,碳质物质和地壳物质。发现PM 2.5 重构质量与其重量分析质量相差<±15%。在夏季高PM事件中,硫酸铵占主导地位(> 50%),而有机物也占主导地位(〜30%)。通过将FME数据与顺风和顺风位置的同时测量值进行比较,发现硫酸盐和地壳物质比其他主要成分更具区域性。使用热力学模型ISORROPIA研究了精细气溶胶的无机部分。 FME从夏季的低氨环境到冬季的高氨环境变化。 ISORROPIA还估算了气溶胶水含量;在潮湿的日子里,水可以造成可见区域大气消灭的50%以上。将在FME处观察到的元素碳(EC)/ CO比值与来自各个车辆,隧道研究和生物质燃烧的元素碳比值进行比较,以估算每种潜在来源的贡献。环境温度似乎会影响排放因子。基于完善的一氧化碳排放清单,EC / CO比值导致北美的EC排放估计为0.32±0.12 Tg(EC)yr -1 。使用因子分析模块UNMIX,解决了导致PM 2.5 质量的六个因子。这些包括区域硫酸盐,局部硫酸盐,木烟,移动硝酸盐,仲硝酸盐和铜/铁加工工业。使用集合后向轨迹方法进一步研究了这六个因素,以识别可能的震源位置。区域性硫酸盐和木材烟雾比其他因素更具区域性,分别与西风和南风运输有关。这项研究表明,局部对PM 2.5 质量的贡献范围从夏季的<30%到冬季的> 60%不等。

著录项

  • 作者

    Chen, Lung-Wen Antony.;

  • 作者单位

    University of Maryland College Park.;

  • 授予单位 University of Maryland College Park.;
  • 学科 Geophysics.; Environmental Sciences.
  • 学位 Ph.D.
  • 年度 2002
  • 页码 219 p.
  • 总页数 219
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 地球物理学;环境科学基础理论;
  • 关键词

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