Water-soluble organic nitrogen in the aerosols and rainwater at an urban site in Japan: Implications for the nitrogen composition in the atmospheric deposition. (October 2018)

• Record Type: Journal Article
• Authors: Matsumoto, Kiyoshi; Takusagawa, Fumi; Suzuki, Haruka; Horiuchi, Ken
• Is Part Of: Atmospheric environment. Volume 191(2018)
• Page Start: 267
• Page End: 272
• Publication Date: 2018-10
• Subjects: Water-soluble organic nitrogen -- Nitrogen deposition -- Dry deposition -- Wet deposition -- Aerosols; Air -- Pollution -- Periodicals; Air -- Pollution -- Meteorological aspects -- Periodicals; 551.51
• DOI: 10.1016/j.atmosenv.2018.07.056
• Languages: English
• ISSNs: 1352-2310

Abstract

Abstract: Simultaneous measurements of the water-soluble organic nitrogen (WSON) in the aerosols and rainwater were conducted to clarify the deposition pathway of the atmospheric WSON. In the aerosols, about 10% of the water-soluble total nitrogen (WSTN) was in an organic form, and a large portion (about 81% on average) of the WSON was distributed in the fine-mode range. Concentrations of the fine-mode WSON were associated with the acidity of the fine particles, suggesting the secondary production of the WSON in the acid fine particles. On the other hand, it was suggested that the coarse-mode WSON was derived from bio-particles, such as plant debris, although its concentrations were low and widely scattered. Dry deposition amounts of the WSON estimated from the concentrations and dry deposition velocities of the particulate WSON suggested that almost all of the dry deposition of the particulate WSON was derived from the coarse-mode particles. The contribution of the fine-mode particles to the dry deposition was negligible. About 10% of the WSTN in the bulk precipitation was in an organic form. The bulk deposition amounts of the WSON were largely dependent on the rainfall amounts and coarse-mode WSON concentrations. Although about 30% of the WSON in the bulk deposition was from the dry deposition, the wet deposition significantly contributed to the WSON deposition, especially in the rainy season. Wet deposition is the major removal process of WSON from spring to autumn; however, in winter, dry and wet deposition are comparable. Highlights: About 10% of the WSTN in the aerosols was in an organic form. The WSON in fine particles was associated with the acidity of the particles. About 10% of the WSTN in the bulk precipitation was in an organic form. Almost all of the dry deposition of the WSON was derived from the coarse particles. Wet deposition is a major process for the WSON deposition.