In order to study particulate matter transport and transformation in the Megacity environment, fine particulate carbon was measured simultaneously at two supersites, suburban T1 and rural T2, downwind of Mexico City during the MILAGRO field campaign in March 2006. Organic carbon (OC), element carbon (EC), and total carbon (TC=OC+EC) were determined in near real-time using a Sunset semicontinuous OCEC field analyzer. The semi-empirical EC tracer method was used to derive primary organic carbon (POC) and secondary organic carbon (SOC). Diurnal variations of primary and secondary carbon were observed at T1 and T2, which resulted from boundary layer inversion and impacted by local traffic patterns. The majority of organic carbon particles at T1 and T2 were secondary. The SOC_(TC)% (SOC%=SOC/TC x 100%) at T1 ranged from 0.5-93.8% with an average of 63.5±17.2%. The SOC_(TC)% at T2 ranged from 9.3-98.1% with an average of 67.4±12.4%. The average EC to PM_(2.5) percentage (EC_(PM)%=EC/PM_(2.5) x 100%) and OC_(PM)% were 6.0% and 20.0% over the whole sampling time at Tl. The POC to PM percentage (POC_(PM)%) and SOC_(PM)% were 3.7% and 16.3%, respectively at the same site. The maximum EC_(PM)% was 21.2%, and the maximum OC _(PM)% was 57.2% at T1. The maximum POC_(PM)% was 12.9%, and the maximum SOC_(PM)% was 49.7% at T1. Comparison of SOC and POC at T1 and T2 showed similar characteristics under favorable meteorological conditions, which indicated that transport from T1 towards T2 took place. Strong correlations between EC and carbon monoxide (CO) and odd nitrogen species (NO and NO_x) were observed at T1. This indicated that EC had nearby sources, such as local traffic emissions. The EC/CO ratio derived by linear regression analysis, with units of μgC/m~3 and μg/m~3, respectively, was 0.004 at T1. Correlations were also seen between OC and SOC vs. the sum of oxidants, such as O_3 and NO_2, suggesting the secondary nature of carbons observed at T1.
展开▼
