Yao Qing, Liu Zi-Rui, Han Su-Qin, Cai Zi-Ying, Liu Jing-le, Huang Xiao-Juan, Liu Jing-Yun, Wang Yue-Si
Tianjin Meteorological Institute, Tianjin 300074, China.
Tianjin Environmental Meteorological Center, Tianjin 300074, China.
Huan Jing Ke Xue. 2017 Dec 8;38(12):4958-4967. doi: 10.13227/j.hjkx.201702097.
To characterize the size distribution of water-soluble inorganic ions (WSⅡ) during a heavy pollution episode, particle samples were collected by an Andersen cascade sampler in Tianjin in January 2014, and the concentrations of eight WSⅡ (Na, NH, K, Mg, Ca, Cl, NO, and SO) during a typical haze episode were analyzed by ion chromatography. The sources and formation mechanisms of WSⅡ were analyzed based on their size distributions. The results showed that the daily average concentrations of PM and PM were (138±100) μg·m and (227±142) μg·m, respectively, and the average concentration of total WSⅡ concentrations (TWSⅡ) in the coarse and fine particles were (34.07+6.16) μg·m and (104.16+51.76) μg·m, respectively. The concentrations of SO, NO, and NH in the fine particles were much higher than concentrations of the other ions, and there were strong correlations between these three ions. The TWSⅡ on clear days, light pollution days, and heavy pollution days were (41.55±12.41) μg·m, (94.46±31.19) μg·m, and (147.55±27.76) μg·m, respectively. On clear days, SO showed a unimodal distribution, peaking at 0.43-0.65 μm; and NO showed a trimodal distribution, peaking at 0.43-0.65 μm, 2.1-3.3 μm, and 5.8-9.0 μm. NH had a bimodal distribution, peaking at 0.43-0.65 μm and 4.7-5.8 μm. On heavy pollution days, however, the size distributions of these three secondary inorganic ions switched to a unimodal size distribution, peaking at 0.65-1.1 μm. Unimodal NH mainly coexisted with SO and NO, and the excess NH was found to be combined with Cl in the fine particles. In the coarse particles, NH completely coexisted with SO and NO.
为了表征重污染事件期间水溶性无机离子(WSⅡ)的粒径分布,于2014年1月在天津用安德森级联采样器采集了颗粒物样本,并通过离子色谱法分析了典型霾污染事件期间8种WSⅡ(Na、NH、K、Mg、Ca、Cl、NO和SO)的浓度。基于WSⅡ的粒径分布分析了其来源和形成机制。结果表明,PM和PM的日均浓度分别为(138±100)μg·m和(227±142)μg·m,粗颗粒和细颗粒中总WSⅡ浓度(TWSⅡ)的平均浓度分别为(34.07+6.16)μg·m和(104.16+51.76)μg·m。细颗粒中SO、NO和NH的浓度远高于其他离子的浓度,且这三种离子之间存在很强的相关性。晴天、轻度污染天和重度污染天的TWSⅡ分别为(41.55±12.41)μg·m、(94.46±31.19)μg·m和(147.55±27.76)μg·m。晴天时,SO呈单峰分布,在0.43 - 0.65μm处达到峰值;NO呈三峰分布,在0.43 - 0.65μm、2.1 - 3.3μm和5.8 - 9.0μm处达到峰值。NH呈双峰分布,在0.43 - 0.65μm和4.7 - 5.8μm处达到峰值。然而,在重度污染天,这三种二次无机离子的粒径分布转变为单峰粒径分布,在0.65 - 1.1μm处达到峰值。单峰的NH主要与SO和NO共存,且发现细颗粒中过量的NH与Cl结合。在粗颗粒中,NH完全与SO和NO共存。