“…In addition, we excluded volcanic activity as a potential source of excess sFe, considering that it would not have affected the chemical composition of aerosol samples, as mentioned above. The potential Fe sources are distinctly divided into three groups according to the Al, K, and V concentrations in aerosols from previous studies: high K/Al and low V/Al (Group 1: biomass burning and steel plant), ,− low K/Al and high V/Al (Group 2: heavy fuel oil), ,, and low K/Al and low V/Al (Group 3: crust, solid waste, coal, and road dust) ,− (Figure a). In Group 1, higher K concentrations are generally observed in biomass burning and steel plants because K is abundant in the cytoplasm of the plant , and is a major component of recycled materials used in the main process of steel plants, such as sintering. ,, Additionally, Group 1 can be divided into two subgroups according to the type of biomass burning and the process of steel plants (Group 1–1: agricultural biomass burning and sintering dust from steel plant; Group 1–2: woody biomass burning and nonsintering dust from steel plant).…”