Influence of contemporary carbon originating from the 2003 Siberian forest fire on organic carbon in PM2.5 in Nagoya, Japan

被引:20
作者
Ikemori, Fumikazu [1 ,2 ]
Honjyo, Koji [2 ]
Yamagami, Makiko [1 ]
Nakamura, Toshio [3 ]
机构
[1] Nagoya City Inst Environm Sci, Minami Ku, Nagoya, Aichi 4570841, Japan
[2] Nagoya Univ, Grad Sch Environm Studies, Chikusa Ku, Nagoya, Aichi 4648601, Japan
[3] Nagoya Univ, Ctr Chronol Res, Chikusa Ku, Nagoya, Aichi 4648602, Japan
关键词
Siberian forest fire; Radiocarbon; Contemporary carbon; Organic carbon; Long-range transport; PM2.5; LONG-RANGE TRANSPORT; BIOMASS BURNING EMISSIONS; PARTICULATE MATTER; SOURCE APPORTIONMENT; C-14; MEASUREMENTS; AIR-POLLUTION; TRACE GASES; AEROSOL; CLIMATE; HYDROCARBONS;
D O I
10.1016/j.scitotenv.2015.05.006
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
In May 2003, high concentrations of organic carbon (OC) in PM2.5 were measured in Nagoya, a representative metropolitan area in Japan. To investigate the influence of possible forest fires on PM2.5 in Japan via long-range aerosol transport, the radiocarbon (C-14) concentrations of PM2.5 samples from April 2003 to March 2004 were measured. C-14 concentrations in total carbon (TC) from May to early June showed higher values than those in other periods. The OC/elemental carbon (EC) ratios from May to early June were also significantly higher than the ones in other periods. In addition, OC concentrations from May to early June were typically high. These results indicate that the abundant OC fraction from May to early June in Nagoya consisted predominantly of contemporary carbon. Furthermore, simulations of diffusion and transport of organic matter (OM) in East Asia showed that abundant OM originating from East Siberia spread over East Asia and Japan in May and early June. Backward air mass trajectories from this time frame indicate that the air mass in Nagoya likely first passed through East Siberia where fire events were prevalent. However, the backward trajectories showed that the air mass after early June did not originate mainly from Siberia, and correspondingly, the C-14 and OC concentrations showed lower values than those from May to early June. Therefore, the authors conclude that contemporary carbon originating from the forest fire in East Siberia was transported to Nagoya, where it significantly contributed to the high observed concentrations of both OC and C-14. (C) 2015 Elsevier B.V. All rights reserved.
引用
收藏
页码:403 / 410
页数:8
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