Treatment of particle/gas partitioning using level III fugacity models in a six-compartment system

Autor: Li-Na Qiao, Robie W. Macdonald, Jining Liu, Peng-Tuan Hu, Meng Qin, Chongguo Tian, Lili Shi, Anatoly N. Nikolaev, Yi-Fan Li, Li-Yan Liu, Linjun Zhou, Pu-Fei Yang
Rok vydání: 2020
Předmět:
Zdroj: Chemosphere. 271
ISSN: 1879-1298
Popis: In this paper, two level III fugacity models are developed and applied using an environmental system containing six compartments, including air, aerosols, soil, water, suspended particulate matters (SPMs), and sediments, as a “unit world”. The first model, assumes equilibrium between air and aerosols and between water and SPMs. These assumptions lead to a four-fugacity model. The second model removes these two assumptions leading to a six-fugacity model. The two models, compared using four PBDE congeners, BDE-28, -99, −153, and −209, with a steady flux of gaseous congeners entering the air, lead to the following conclusions. 1. When the octanol-air partition coefficient (KOA) is less than 1011.4, the two models produce similar results; when KOA > 1011.4, and especially when KOA > 1012.5, the model results diverge significantly. 2. Chemicals are in an imposed equilibrium in the four-fugacity model, but in a steady state and not necessary an equilibrium in the six-fugacity model, between air and aerosols. 3. The results from the six-fugacity model indicate an internally consistent system with chemicals in steady state in all six compartments, whereas the four-fugacity model presents an internally inconsistent system where chemicals are in equilibrium but not a steady state between air and aerosols. 4. Chemicals are mass balanced in air and aerosols predicted by the six-fugacity model but not by the four-fugacity model. If the mass balance in air and aerosols is achieved in the four-fugacity model, the condition of equilibrium between air and aerosols will be no longer valid.
Databáze: OpenAIRE