Abstract:Based on the negative ion concentration and meteorological data from January 2010 to June 2016 in Jiufeng Mountain, the characteristics of atmospheric negative ion concentration and its main influencing factors were statistically analyzed. The results show the annual variation of negative ion concentration in Jiufeng Mountain has a single peak and single valley feature, with lower concentrations from July to October, and the lowest concentration (520 per·cm-3) in September, with higher concentrations from April to June, and the highest concentration(1 227 per·cm-3) in June. The daily concentration is low in the day and high at night, with an obvious decrease after 07∶00 BST, the lowest point at 12∶00, and then gradually increasing. The negative ion concentrations of grade 4-8 accounted for 80.2% of the total, with respective proportions of 97.2%, 67.1%, 75.5%, and 87.6% in each season, with minor changes during winter and maximum changes during summer. The negative ion concentration was negatively correlated with wind speed, sunshine duration, and PM2.5 concentration, positively correlated with precipitation. The negative ion concentration significantly increased with moderate rainfall and above, with a concentration exceeding 1 000 per·cm-3, and is higher in thunderstorms than in light fog and haze days.