Brown carbon (BrC) is a nonnegligible chemical component of organic aerosols and has great influences on radiative forcing, regional and global climates, and even human health (Lin et al., 2018). BrC can be released from a variety of emission sources such as traffic, biomass burning, and coal combustion, and formed from secondary transformation (Fleming et al., 2020;Soleimanian et al., 2020). BrC formed through different mechanisms could have unique light absorption capacities (Lei et al., 2019;Lukacs et al., 2007). The formations of BrC with sulfur (S), nitrogen (N), and oxygen (O)-containing precursors simulated in chamber experiments have been widely reported in the last decade (