薄雾
硫酸盐
环境科学
相对湿度
大气科学
硝酸盐
环境化学
生态系统
硫酸盐气溶胶
气溶胶
中国
气候学
气象学
化学
生态学
地理
生物
地质学
考古
有机化学
作者
Gehui Wang,Renyi Zhang,Mario Gómez,Lingxiao Yang,Misti Levy Zamora,Min Hu,Yun Lin,Jianfei Peng,Song Guo,Jingjing Meng,Jianjun Li,Chunlei Cheng,Tafeng Hu,Yanqin Ren,Yuesi Wang,Jian Gao,Junji Cao,Zhisheng An,Weijian Zhou,Guohui Li
标识
DOI:10.1073/pnas.1616540113
摘要
Significance Exceedingly high levels of fine particulate matter (PM) occur frequently in China, but the mechanism of severe haze formation remains unclear. From atmospheric measurements in two Chinese megacities and laboratory experiments, we show that the oxidation of SO 2 by NO 2 occurs efficiently in aqueous media under two polluted conditions: first, during the formation of the 1952 London Fog via in-cloud oxidation; and second, on fine PM with NH 3 neutralization during severe haze in China. We suggest that effective haze mitigation is achievable by intervening in the sulfate formation process with NH 3 and NO 2 emission control measures. Hence, our results explain the outstanding sulfur problem during the historic London Fog formation and elucidate the chemical mechanism of severe haze in China.
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