Chow Judith C, Watson John G, Chen L W Antony, Arnott W Patrick, Moosmüller Hans, Fung Kochy
Desert Research Institute, Reno, Nevada 89512, USA.
Environ Sci Technol. 2004 Aug 15;38(16):4414-22. doi: 10.1021/es034936u.
Charring of organic carbon (OC) during thermal/optical analysis is monitored by the change in a laser signal either reflected from or transmitted through a filter punch. Elemental carbon (EC) in suspended particulate matter collected on quartz-fiber filters is defined as the carbon that evolves after the detected optical signal attains the value it had prior to commencement of heating, with the rest of the carbon classified as organic carbon (OC). Heretofore, operational definitions of EC were believed to be caused by different temperature protocols rather than by the method of monitoring charring. This work demonstrates that thermal/ optical reflectance (TOR) corrections yield equivalent OC/ EC splits for widely divergent temperature protocols. EC results determined by simultaneous thermal/optical transmittance (TOT) corrections are 30% lower than TOR for the same temperature protocol and 70-80% lower than TOR for a protocol with higher heating temperatures and shorter residence times. This is true for 58 urban samples from Fresno, CA, as well as for 30 samples from the nonurban IMPROVE network that are individually dominated by wildfire, vehicle exhaust, secondary organic aerosol, and calcium carbonate contributions. Visual examination of filter darkening at different temperature stages shows that substantial charring takes place within the filter, possibly due to adsorbed organic gases or diffusion of vaporized particles. The filter transmittance is more influenced by the within-filter char, whereas the filter reflectance is dominated by charring of the near-surface deposit that appears to evolve first when oxygen is added to helium in the analysis atmosphere for these samples. The amounts of charred OC (POC) and EC are also estimated from incremental absorbance. Small amounts of POC are found to dominate the incremental absorbance. EC estimated from absorbance are found to agree better with EC from the reflectance charring correction than with EC from the transmittance charring correction.
在热/光分析过程中,通过从滤膜打孔处反射或透过的激光信号变化来监测有机碳(OC)的炭化情况。收集在石英纤维滤膜上的悬浮颗粒物中的元素碳(EC)定义为,在检测到的光信号达到加热开始前的值之后释放出的碳,其余的碳归类为有机碳(OC)。在此之前,人们认为EC的操作定义是由不同的温度方案引起的,而不是由监测炭化的方法导致的。这项研究表明,对于差异很大的温度方案,热/光反射率(TOR)校正能产生等效的OC/EC划分。在相同温度方案下,通过同步热/光透射率(TOT)校正确定的EC结果比TOR低30%,而在加热温度更高且停留时间更短的方案中,比TOR低70 - 80%。对于来自加利福尼亚州弗雷斯诺的58个城市样本以及来自非城市IMPROVE网络的30个样本(这些样本分别主要受野火、车辆尾气、二次有机气溶胶和碳酸钙的影响)来说都是如此。对不同温度阶段滤膜变黑情况的目视检查表明,滤膜内部会发生大量炭化,这可能是由于吸附的有机气体或汽化颗粒的扩散所致。滤膜透射率受滤膜内部炭化的影响更大,而滤膜反射率则主要由近表面沉积物的炭化决定,对于这些样本,在分析气氛中向氦气中添加氧气时,近表面沉积物的炭化似乎最先发生。烧焦的OC(POC)和EC的量也通过增量吸光度来估算。发现少量的POC主导了增量吸光度。通过吸光度估算的EC与通过反射率炭化校正得到的EC比与通过透射率炭化校正得到的EC更吻合。