Fu Xiaoxin, Wang Xinming, Liu Tengyu, He Quanfu, Zhang Zhou, Zhang Yanli, Song Wei, Dai Qunwei, Chen Shu, Dong Faqin
Key Laboratory of Solid Waste Treatment and Resource Recycle, Ministry of Education, Southwest University of Science and Technology, Mianyang 621010, China.
State Key Laboratory of Organic Geochemistry and Guangdong Key Laboratory of Environmental Protection and Resources Utilization, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China.
Sci Total Environ. 2024 Mar 25;918:170512. doi: 10.1016/j.scitotenv.2024.170512. Epub 2024 Jan 28.
Wintertime fine particle (PM) pollution remains to be perplexing air quality problems in many parts of China. In this study, PM compositions and aerosol acidity at different pollution levels at an urban cite in the southwest China's Sichuan Basin were investigated during a sustained winter haze episode. Organic matter was the most abundant component of PM, followed by nitrate, sulfate and ammonium. Shares of organic aerosol in PM mass decreased with the elevated PM levels, while the enhancements of sulfate and secondary organic aerosol were much less than that of nitrate and ammonium during heavy pollution with increased ratios of nitrate to sulfate, implying a significant role of nitrate in the haze formation. Results also suggest the nighttime chemistry might contribute substantially to the formation of nitrate under severe pollutions. The daily average aerosol pH showed a decreasing trend with the elevated levels of PM, and this increased aerosl acidity was mainly due to the fast rising secondary inorganic aerosol (SIA) concentration, with the increase in hydronium ion concentration in air (H) surpassing the dilution effect of elevated aerosol liquid water content (LWC). Thermodynamic model calculations revealed that the air environment was NH-rich with total NH (NH + NH) greater than required NH, and the aerosol pH exponentially declined with the decreasing excess NH (p < 0.01). This study demonstrated that under air stagnation and NH-rich environment during winter, the raised relative humidity (RH) would lead to an increase in LWC and thereby facilitate the aqueous chemistry processes with the neutralization capacity of NH to form sulfate and nitrate, which would further increase the LWC and lower the pH. This self-amplifying SIA formation might be crucial to the severe PM pollution and haze events during winter, and therefore cutting both NO and NH emissions would benefit stopping the self-amplification.
冬季细颗粒物(PM)污染仍是中国许多地区令人困惑的空气质量问题。本研究在持续的冬季雾霾期间,对中国西南部四川盆地某城市不同污染水平下的PM成分和气溶胶酸度进行了调查。有机物是PM中含量最丰富的成分,其次是硝酸盐、硫酸盐和铵盐。随着PM水平升高,有机气溶胶在PM质量中的占比下降,而在重度污染期间,硫酸盐和二次有机气溶胶的增加量远小于硝酸盐和铵盐,且硝酸盐与硫酸盐的比例增加,这意味着硝酸盐在雾霾形成中起重要作用。结果还表明,夜间化学过程可能在严重污染下对硝酸盐的形成有很大贡献。日均气溶胶pH值随PM水平升高呈下降趋势,气溶胶酸度增加主要是由于二次无机气溶胶(SIA)浓度快速上升,空气中水合氢离子浓度(H)的增加超过了气溶胶液态水含量(LWC)升高的稀释作用。热力学模型计算表明,空气环境呈富氨状态,总氨(NH₃ + NH₄⁺)大于所需氨,气溶胶pH值随过量氨的减少呈指数下降(p < 0.01)。本研究表明,在冬季空气停滞和富氨环境下,相对湿度(RH)升高会导致LWC增加,从而促进与氨中和能力相关的水相化学过程,形成硫酸盐和硝酸盐,这将进一步增加LWC并降低pH值。这种自增强的SIA形成可能对冬季严重的PM污染和雾霾事件至关重要,因此减少氮氧化物和氨的排放都将有助于阻止这种自增强过程。