Results of our aerosol study, performed during 1983-1984 in Beijing, demonstrate that ambient carbonaceous aerosols are derived principally from coal combustion. Different SO2 oxidation processes have been observed in summer and winter. The winter sulfate appears to be produced locally and associated with products of incomplete combustion. © 1986.
CITATION STYLE
Dod, R. L., Giauque, R. D., Novakov, T., Weihan, S., Quipeng, Z., & Wenzhi, S. (1986). Sulfate and carbonaceous aerosols in Beijing China. Atmospheric Environment (1967). https://doi.org/10.1016/0004-6981(86)90317-3
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