Size-resolved chemical composition, effective density, and optical properties of biomass burning particles

• Published in: Atmospheric chemistry and physics Vol. 17; no. 12; pp. 7481 - 7493
• Main Authors: Zhai, Jinghao, Lu, Xiaohui, Li, Ling, Zhang, Qi, Zhang, Ci, Chen, Hong, Yang, Xin, Chen, Jianmin
• Format: Journal Article
• Language: English
• Published: Katlenburg-Lindau Copernicus GmbH 21.06.2017; Copernicus Publications
• Subjects: Absorption; Aerosol effects; Aerosols; Albedo; Atmospheric chemistry; Biomass; Biomass burning; Black carbon; Burning; Carbon; Chemical composition; Chemical research; Climate; Climate effects; Combustion; Components; Composition effects; Density; Density distribution; Distribution; Global climate; Heating; Influence; Inorganic salts; Internet; Mass spectrometry; Mass spectroscopy; Optical properties; Organic carbon; Oryza; Particle mass; Particle size; Particulate matter; Physicochemical processes; Physicochemical properties; Potassium; Potassium salts; Properties; Salts; Scattering; Separation; Soot; Straw; Wavelengths
• ISSN: 1680-7324; 1680-7316; 1680-7324
• DOI: 10.5194/acp-17-7481-2017

Biomass burning aerosol has an important impact on the global radiative budget. A better understanding of the correlations between the mixing states of biomass burning particles and their optical properties is the goal of a number of current studies. In this work, the effective density, chemical composition, and optical properties of rice straw burning particles in the size range of 50–400 nm were measured using a suite of online methods. We found that the major components of particles produced by burning rice straw included black carbon (BC), organic carbon (OC), and potassium salts, but the mixing states of particles were strongly size dependent. Particles of 50 nm had the smallest effective density (1.16 g cm−3) due to a relatively large proportion of aggregate BC. The average effective densities of 100–400 nm particles ranged from 1.35 to 1.51 g cm−3 with OC and inorganic salts as dominant components. Both density distribution and single-particle mass spectrometry showed more complex mixing states in larger particles. Upon heating, the separation of the effective density distribution modes confirmed the external mixing state of less-volatile BC or soot and potassium salts. The size-resolved optical properties of biomass burning particles were investigated at two wavelengths (λ =  450 and 530 nm). The single-scattering albedo (SSA) showed the lowest value for 50 nm particles (0.741 ± 0.007 and 0.889 ± 0.006) because of the larger proportion of BC content. Brown carbon played an important role for the SSA of 100–400 nm particles. The Ångström absorption exponent (AAE) values for all particles were above 1.6, indicating the significant presence of brown carbon in all sizes. Concurrent measurements in our work provide a basis for discussing the physicochemical properties of biomass burning aerosol and its effects on the global climate and atmospheric environment.