Quantitative measurements of the generation of hydroxyl radicals by soot particles in a surrogate lung fluid
Quantitative measurements of the generation of hydroxyl radicals by soot particles in a surrogate lung fluid
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DOI:
10.1016/j.atmosenv.2005.11.015
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发表时间:
2006-02-01
影响因子:
5
通讯作者:
Kennedy, IM
中科院分区:
文献类型:
--
作者:
Jung, H;Guo, B;Kennedy, IM
Epidemiological and toxicological studies have shown a relation between the inhalation of atmospheric particles and adverse cardiopulmonary health effects. The generation of reactive oxygen species (ROS) by particles is one current hypothesis for their toxic effects. Thus a quantitative measurement of ROS is important since that will be an index to assess the oxidative stress that particles may cause in the lung. We have developed a technique to quantitatively and specifically measure (OH)-O-center dot (the strongest biological ROS) in an aqueous, buffered extract solution as a surrogate lung fluid (SLF). Using this technique we quantitatively measured (OH)-O-center dot formation in SLF containing hydrogen peroxide (HOOH) for samples of flame soot particles, carbon black, and ambient fine particles (PM2.5). We have found that (OH)-O-center dot is formed by flame soot, independent of transition metals, with a dose-dependent linear response that depends upon HOOH concentration. Experiments with carbon black revealed that its mass-normalized (OH)-O-center dot generation was similar to 10 times lower than that of flame soot, suggesting that carbon black is not a good surrogate for soot particles in health effect studies, at least in terms of oxidative stress. Mass-normalized (OH)-O-center dot generation by ambient PM2.5 was 6-30 times larger than that of flame soot. While much of the PM2.5 reactivity was suppressed by pretreating samples with a transition metal chelator, there was a significant fraction of reactivity which was not affected. Our results suggest that the in vivo generation of free radicals, specifically (OH)-O-center dot, by inhalation of PM2.5 is partially due to carbonaceous soot as well as transition metals. (c) 2005 Elsevier Ltd. All rights reserved.