Jeong Cheol-Heon, Hopke Philip K, Chalupa David, Utell Mark
Department of Civil and Environmental Engineering, Center for Air Resources Engineering and Science, Clarkson University, Potsdam, New York 13699-5708, USA.
Environ Sci Technol. 2004 Apr 1;38(7):1933-40. doi: 10.1021/es034811p.
Number concentrations and size distributions of particles in the size range of 0.010-0.500 microm were measured in Rochester, NY, from December 2001 to December 2002. The relationships between the number concentrations, gaseous pollutants, and meteorological parameters were examined during particle nucleation events. More than 70% of measured total number concentration was associated with ultrafine particles (UFP, 0.011-0.050 microm). Morning nucleation events typically peaking UFP number concentrations at around 08:00 were apparent in winter months with CO increases. These particles appear to be formed following direct emissions from motorvehicles during morning rush hour. There were also often observed increases in this smaller-sized range particles in the late afternoon during the afternoon rush hour, particularly in winter when the mixing heights remain lowerthan in summer. Strong afternoon nucleation events (> 30,000 cm(-3)) peaking at around 13: 00 were more likely to occur in spiring and summer months. During the prominent nucleation events, peaks of SO2 were strongly associated with the number concentrations of UFP, whereas there were no significant correlations between these events and PM2.5 and CO. Increased SO2 concentrations were observed when the wind direction was northwesterly where three SO2 sources were located. It is hypothesized that UFP formed during the events are sulfuric acid and water from the oxidation of SO2. There were also a more limited number of nucleation events followed by particle growth up to approximately 0.1 microm over periods of up to 18 h. The nucleation and growth events tended to be common in spring months especially in April.
2001年12月至2002年12月期间,在纽约州罗切斯特市测量了粒径范围为0.010 - 0.500微米的颗粒物的数量浓度和粒径分布。在颗粒物成核事件期间,研究了数量浓度、气态污染物和气象参数之间的关系。超过70%的测量总数量浓度与超细颗粒物(UFP,0.011 - 0.050微米)有关。在冬季,随着一氧化碳增加,早晨的成核事件通常在08:00左右达到UFP数量浓度峰值。这些颗粒物似乎是在早晨高峰时段机动车直接排放后形成的。在下午高峰时段的傍晚,也经常观察到这个较小粒径范围内的颗粒物增加,特别是在冬季,此时混合高度低于夏季。强烈的下午成核事件(> 30,000 cm⁻³)在13:00左右达到峰值,更有可能在春季和夏季发生。在显著的成核事件期间,二氧化硫峰值与UFP数量浓度密切相关,而这些事件与PM2.5和一氧化碳之间没有显著相关性。当风向为西北风且有三个二氧化硫源时,观察到二氧化硫浓度增加。据推测,事件期间形成的UFP是二氧化硫氧化产生的硫酸和水。也有数量更有限的成核事件,随后在长达18小时的时间内颗粒物生长至约0.1微米。成核和生长事件在春季尤其是4月较为常见。