2007
DOI: 10.1021/es070420p
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Comparison of Carbonaceous Aerosols in Tokyo before and after Implementation of Diesel Exhaust Restrictions

Abstract: We compared the status of carbonaceous aerosols in Tokyo before and after the implementation of a diesel vehicle regulation intended to reduce the quantity of particulate carbon from diesel engines in one of the largest scale ever attempts at vehicle exhaust control. Radiocarbon (14C) in elemental carbon (EC) and total carbon (TC) were analyzed to identify fossil fuel carbonaceous particles emitted from diesel-powered vehicles. One-sided paired-month t-tests showed no distinct difference in the absolute concen… Show more

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Cited by 19 publications
(16 citation statements)
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“…Heald et al (2008) compiled all the gas and particle phase organic measurements into the newly defined "Total Observed Organic Carbon", which had a daytime mean of 456ugCm-3 at TO and 17ugCm-3 for the C-130. The TO levels are an order-of-magnitude higher than those measured in Pittsburgh (28)(29)(30)(31)(32)(33)(34)(35)(36)(37)(38)(39)(40)(41)(42)(43)(44)(45), while those measured in the C-130 are typical of polluted airmasses in the US sampled from aircraft. The organic aerosol PM contribution increased from -3% of the TOOC at TO to 9% for the C-130, due to SOA formation and the larger contribution of biomass burning to regional airmasses.…”
Section: Voc Distributions and Patternsmentioning
confidence: 71%
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“…Heald et al (2008) compiled all the gas and particle phase organic measurements into the newly defined "Total Observed Organic Carbon", which had a daytime mean of 456ugCm-3 at TO and 17ugCm-3 for the C-130. The TO levels are an order-of-magnitude higher than those measured in Pittsburgh (28)(29)(30)(31)(32)(33)(34)(35)(36)(37)(38)(39)(40)(41)(42)(43)(44)(45), while those measured in the C-130 are typical of polluted airmasses in the US sampled from aircraft. The organic aerosol PM contribution increased from -3% of the TOOC at TO to 9% for the C-130, due to SOA formation and the larger contribution of biomass burning to regional airmasses.…”
Section: Voc Distributions and Patternsmentioning
confidence: 71%
“…During the MCMA-2006 field campaign, air flow trajectories within the Mexico City basin and the fate of the urban plume were simulated, and five types of wind circulation patterns were identified : Cold Surge, South Venting, 0 3 -North, 0 3 -South, and Convection (North and South). During the 31 days of the MCMA-2006 field campaign, three were Cold Surge (14,21,23 March), eight were South Venting (1)(2)(3)(4)(5)(6)(7)13 March), five were 03-South (8,12,(15)(16)(17), seven were 03-North (9)(10)(11)(18)(19)(20)22 March), and eight were Convection (24)(25)(26)(27)(28)(29)(30)(31). The prevailing meteorological conditions can strongly influence ambient pollutant concenti'ations for given emission levels and also determine the regional impacts of the urban plume .…”
Section: Measurement Sitesmentioning
confidence: 99%
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“…It is expected that the characteristics of carbonaceous aerosols in the Tokyo metropolitan area (TMA) will have significantly varied since the introduction of these regulations. Yamamoto et al (2007) (Yamamoto et al, 2007). Fushimi et al (2011) investigated the impacts of biogenic carbon on the mass of secondary organic aerosols (SOA) as well as their diurnal variations at sites outflow from the TMA in the summer of 2007.…”
Section: Introductionmentioning
confidence: 99%