“…Therefore, BDE congener specific transport and plant uptake mechanisms (soil-air-plant vs. soil-soil moisture-root-plant) strongly differ and depend on compound physical parameters (vapor pressure, K OW value, K OA value, Henry coefficient, air to plant distribution coefficient), meteorological parameters (temperature, wind velocity, rainfall, temporal rainfall distribution, deposition kinetics of gaseous BDEs, deposition kinetics of particulate BDEs), long range transport, plant specific characteristics (species, lipid content, carbohydrate content, fiber content, leaf morphology, non-lipid plant parts, bark consistency), and rhizosphere parameters (Klinčić et al 2020;Yogui et al 2011;Zhao et al 2009;Zhu et al 2015). Under aspects of transport, low brominated BDEs (Br 2 -Br 3 ) are mainly and medium brominated BDEs (Br 4 -Br 5 ), depending on the study, are minorly to dominantly distributed as gaseous compounds (BDE-15: 100%; BDE-28: 35-60%), while transmission and deposition of higher brominated congeners (Br 6 -Br 10 ) are obligatorily characterized by adsorption of BDEs on a particulate phase (Dreyer et al 2018;Gao et al 2019;Yogui et al 2011;Zhao et al 2009;Zhu et al 2020). Due to the lower-range transport of the particulate phase, spectrum and concentrations of BDEs in soil and plant samples taken out of densely populated regions are more or less in agreement with the BDE emission spectrum, while the spectrum of detected PBDEs in sparsely populated regions is dominated by low brominated congeners like BDE-47 (51.2%) and BDE-99 (17.8%;Zhao et al 2009).…”