为研究日喀则不同粒径大气颗粒物中水溶性无机离子的组成特征,利用Andersen分级撞击式采样器在夏、冬季进行大气颗粒物分级采样,采用离子色谱测定NH+4、Ca2+、K+、Mg2+、Na+、SO2-4、NO-3和Cl-等8种离子浓度.结果表明,夏、冬季总离子浓度分别为9648±3030、4925±1138 ng·m-3.夏季离子浓度高低顺序为Cl-﹥Ca2+﹥NH+4﹥Na+﹥SO2-4﹥NO-3﹥K+﹥Mg2+,Cl-、Ca2+、NH+4和Na+占总离子浓度的比重为74.9%;冬季水溶性无机离子浓度高低顺序为Cl-﹥SO2-4﹥NH+4﹥NO-3﹥Ca2+﹥Na+﹥K+﹥Mg2+,Cl-、SO2-4、NH+4和NO-3占总离子浓度的比重为88.0%.夏、冬季大气颗粒物中所有水溶性无机离子的粒径分布均成双峰型.夏季,大气颗粒物中SO2-4与Mg2+(r=0.951)、Ca2+(r=0.947),NO-3与Mg2+(r=0.904)、Ca2+(r=0.843),在0.01水平(双侧)上均显著相关;冬季,细粒子中K+与Cl-(r=0.740)、SO2-4(r=0.929)及NO-3(r=0.920),在0.01水平(双侧)上显著相关.
To investigate the size distributions of water-soluble inorganic ions in PM in Shigatse,samples were collected by Thermo Scientific Andersen impactor in summer and winter. Eight watersoluble inorganic ions,including NH+4,Ca2 +,K+,Mg2 +,Na+,SO2-4,NO-3and Cl-were analyzed by IC. The results showed that concentrations of all ions were 9648 ± 3030 ng·m- 3in winter and 4925 ± 1138 ng·m- 3in summer. Variations of ion concentrations were observed in the following order: Cl-﹥ Ca2 +﹥ NH+4﹥ Na+﹥ SO2-4﹥ NO-3﹥ K+﹥ Mg2 +in summer,and Cl-﹥ SO2-4﹥ NH+4﹥ NO-3﹥ Ca2 +﹥ Na+﹥ K+﹥ Mg2 +in winter. Concentrations of Cl-,Ca2 +,NH+4and Na+accounted for 74. 9% of all the ions in PM in summer,and those of Cl-,SO2-4,NH+4and NO-3accounted for 88. 0% of all the ions in PM in winter. Correlations of SO2-4and Mg2 +( r = 0. 951),Ca2 +( r = 0. 947) were significant at the 0. 01 level,and those of NO-3and Mg2 +( r =0. 904),Ca2 +( r = 0. 843) were also significant at the 0. 01 level in summe. Correlations of K+and Cl-( r = 0. 740),SO2-4( r = 0. 929),NO-3( r = 0. 920) were significant at the 0. 01 level.