Yin Han-Mei, Chen Jun-Hui, Feng Xiao-Qiong, Jian Tao, Qian Jun, Liu Zheng
Sichuan Academy of Environmental Sciences, Chengdu 610041, China.
Huan Jing Ke Xue. 2020 Sep 8;41(9):3889-3898. doi: 10.13227/j.hjkx.202003042.
Water-soluble ions in PM were serially on-line monitored using the MARGA sampling and measurement system in Chengdu in 2019. Pollution characteristics of water-soluble ions were analyzed using the meteorological monitoring data. The results show that variations in the concentrations of eight water-soluble ions were consistent with the variations in PM in Chengdu. The annual average mass concentration of the total water-soluble ions was (20.2±12.7) μg ·m, accounting for 48.6% of the PM mass, which indicates that water-soluble ions were the major components of PM. The mass concentrations of all the ions were in the order of NO > SO > NH > Cl > Ca > K > Mg > Na. The annual average mass concentration of secondary ions was (20.2±12.7) μg ·m, accounting for 87.2% of total water-soluble ions. The concentrations of total water-soluble ions in different seasons were in the order of winter > spring ≈ autumn > summer. Monthly variations in total water-soluble ion concentrations followed a U-shaped curve; mass concentrations were the highest in January and December and lowest from June to August. Monthly variations in the concentrations of NO, SO, NH, Cl, Na, and K were consistent with the total water-soluble ion concentrations, while the concentrations of Ca and Mg were the highest in June. Visibility declined with the increase in the concentration of water-soluble ions, especially secondary water-soluble ions regardless of the rainfall. Light rain (accumulated rainfall in 24 h <10 mm) had no scavenging effect on water-soluble ions, while moderate and heavy rainfall had a significant effect. There was a significant positive correlation between NO, SO, and NH (all the correlation coefficients were over 0.7), indicating that the mechanisms of evolution of secondary water-soluble ions in the atmosphere are highly similar to each other. The annual mean values of SOR and NOR were 0.42 and 0.12, respectively, which were negatively correlated with temperature and O and positively correlated with humidity, indicating that the main source of SO was heterogeneous oxidation reactions in the liquid phase and the main source of NO was heterogeneous oxidation reactions at night. The annual mean values of CE/AE and NR were 1.2 and 1.1, respectively, indicating that most aerosols in the study area were relatively alkaline. The atmospheric environment of Chengdu is rich in ammonia; thus, (NH) SO and NHNO were the main forms of secondary ions.
2019年在成都使用MARGA采样和测量系统对PM中的水溶性离子进行了连续在线监测。利用气象监测数据对水溶性离子的污染特征进行了分析。结果表明,成都8种水溶性离子浓度的变化与PM的变化一致。水溶性离子总量的年平均质量浓度为(20.2±12.7)μg·m,占PM质量的48.6%,表明水溶性离子是PM的主要成分。所有离子的质量浓度顺序为NO>SO>NH>Cl>Ca>K>Mg>Na。二次离子的年平均质量浓度为(20.2±12.7)μg·m,占水溶性离子总量的87.2%。不同季节水溶性离子总量浓度顺序为冬季>春季≈秋季>夏季。水溶性离子总量的月变化呈U形曲线;1月和12月质量浓度最高,6月至8月最低。NO、SO、NH、Cl、Na和K浓度的月变化与水溶性离子总量浓度一致,而Ca和Mg浓度在6月最高。能见度随水溶性离子浓度的增加而下降,尤其是二次水溶性离子,与降雨无关。小雨(24小时累计降雨量<10毫米)对水溶性离子没有清除作用,而中雨和大雨有显著作用。NO、SO和NH之间存在显著正相关(所有相关系数均超过0.7),表明大气中二次水溶性离子的演化机制彼此高度相似。SOR和NOR的年平均值分别为0.42和0.12,与温度和O呈负相关,与湿度呈正相关,表明SO的主要来源是液相中的非均相氧化反应,NO的主要来源是夜间的非均相氧化反应。CE/AE和NR的年平均值分别为1.2和1.1,表明研究区域内的大多数气溶胶相对呈碱性。成都的大气环境中氨含量丰富;因此,(NH)SO和NHNO是二次离子的主要形式。