Biomass burning organic aerosols (BBOA) emitted from wildfires and prescribed forest and agricultural burns have diverse composition and undergo complex reactions and transformations in the atmosphere, leading to profound impacts on air quality, climate, and atmospheric chemistry. BBOA emission characteristics are strongly dependent on regional vegetation, with different biofuels resulting in substantially different component profiles. Understanding the composition and emission profiles of BBOA from various biomass fuels is crucial for predicting the impact and atmospheric consequences of wild and prescribed fires. This study focuses on characterizing smoldering-phase BBOA emissions from Peat, Sage, Grass, and Ponderosa Pine biofuels burned in controlled laboratory experiments. Employing ultraperformance liquid chromatography coupled to a photodiode array detector and high-resolution mass spectrometer for advanced molecular characterization, we introduce a novel "fractionation" method for data analysis to extract pertinent high-level optical and compositional information. The physicochemical properties unique to each biofuel-specific BBOA are investigated. We report the mass absorption coefficient at 405 nm (MAC 405nm ) and absorption Ångstrom exponent (AAE) values of the investigated BBOA to classify their brown carbon (BrC) characteristics. Peat BBOA, characterized by the lowest MAC 405nm (0.76 m 2 /g) and the highest AAE 280−360nm (6.09), is classified as "weakly absorbing" BrC. Ponderosa Pine BBOA falls within the same category with MAC 405nm (1.39 m 2 /g) and AAE 280−360nm (5.08). Sage BBOA, displaying MAC 405nm (2.18 m 2 /g) and AAE 280−360nm (4.87), is classified as "moderately absorbing" BrC. Grass BBOA, with the highest MAC 405nm (2.45 m 2 /g) and the lowest AAE 280−360nm (4.56), is also categorized as "moderately absorbing" BrC, exhibiting the strongest absorption. We estimate the values of the volatility, viscosity, and e-folding times of BBOA with respect to atmospheric dilution to assess its atmospheric evolution and lifetimes. This comprehensive analysis provides valuable insights into the molecular characteristics and atmospheric behavior of BBOA from distinct biomass types. We demonstrate that close to emission sources, where atmospheric BBOA mass loadings are elevated, particle viscosity is anticipated to be around 10 4 −10 6 Pa s, corresponding to mixing time scales within individual particles on the order of minutes or single hours. However, with atmospheric dilution, the viscosity of BBOA particles may increase by 2−3 orders of magnitude, reaching conditions akin to solid glass with significantly longer mixing times (many days and weeks). These estimates suggest that atmospheric transport of BBOA substantially suppresses its multiphase chemistry, yet they may transition into efficient ice nucleating particles.