Figure 6
From: Divergent Evolution of Carbonaceous Aerosols during Dispersal of East Asian Haze

Comparison of ∆13C (=δ13Cobserved − δ13Csource-predicted) versus ∆14C of WSOC and WIOC at Beijing and KCOG. ∆13C denotes the difference in δ13C between δ13C signals of observed and source mixture predicted by MCMC simulations for each WSOC (or WIOC) sample (that is, ∆13C = δ13Cobserved − δ13Csource-predicted). The dual-isotope signatures of the original sources are marked by grey shade (dark grey and light grey represent 1σ and 2σ numerical spread, respectively), including coal, fossil fuel, and biomass/biogenic sources. The δ13C source endmember databases are found in Table S3.