Abstract

Abstract. Gas/particle (G/P) partitioning of semi-volatile organic compounds (SVOCs) is an important process that primarily governs their atmospheric fate, long-range atmospheric transport, and their routes of entering the human body. All previous studies on this issue are hypothetically based on equilibrium conditions, the results of which do not predict results from monitoring studies well in most cases. In this study, a steady-state model instead of an equilibrium-state model for the investigation of the G/P partitioning behavior of polybrominated diphenyl ethers (PBDEs) was established, and an equation for calculating the partition coefficients under steady state (KPS) of PBDEs (log KPS = log KPE + logα) was developed in which an equilibrium term (log KPE = log KOA + logfOM −11.91 where fOM is organic matter content of the particles) and a non-equilibrium term (log α, caused by dry and wet depositions of particles), both being functions of log KOA (octanol–air partition coefficient), are included. It was found that the equilibrium is a special case of steady state when the non-equilibrium term equals zero. A criterion to classify the equilibrium and non-equilibrium status of PBDEs was also established using two threshold values of log KOA, log KOA1, and log KOA2, which divide the range of log KOA into three domains: equilibrium, non-equilibrium, and maximum partition domain. Accordingly, two threshold values of temperature t, tTH1 when log KOA = log KOA1 and tTH2 when log KOA = log KOA2, were identified, which divide the range of temperature also into the same three domains for each PBDE congener. We predicted the existence of the maximum partition domain (the values of log KPS reach a maximum constant of −1.53) that every PBDE congener can reach when log KOA ≥ log KOA2, or t ≤ tTH2. The novel equation developed in this study was applied to predict the G/P partition coefficients of PBDEs for our Chinese persistent organic pollutants (POPs) Soil and Air Monitoring Program, Phase 2 (China-SAMP-II) program and other monitoring programs worldwide, including in Asia, Europe, North America, and the Arctic, and the results matched well with all the monitoring data, except those obtained at e-waste sites due to the unpredictable PBDE emissions at these sites. This study provided evidence that the newly developed steady-state-based equation is superior to the equilibrium-state-based equation that has been used in describing the G/P partitioning behavior over decades. We suggest that the investigation on G/P partitioning behavior for PBDEs should be based onsteady-state, not equilibrium state, and equilibrium is just a special case of steady-state when non-equilibrium factors can be ignored. We also believe that our new equation provides a useful tool for environmental scientists in both monitoring and modeling research on G/P partitioning of PBDEs and can be extended to predict G/P partitioning behavior for other SVOCs as well.

Highlights

  • Atmospheric transport is a major mechanism of moving semi-volatile organic compounds (SVOCs), including persistent organic pollutants (POPs), from source regions to otherPublished by Copernicus Publications on behalf of the European Geosciences Union.Y.-F

  • The section At a Glance in the Supplement presents G/P partition coefficients of polybrominated diphenyl ethers (PBDEs) as functions of log KOA at ambient temperature ranging from −50 to +50 ◦C, which can be applied at any sites worldwide

  • The three squares in the panel designate the log KP–log KOA graphs with three different temperature ranges: 0 to +50, −30 to +30, and −50 to 0 ◦C, representing the tropical and subtropical climate zones, warm temperate climate zone, and boreal and tundra climate zones, respectively. Monitoring data, their regression data, and the predicted results log KPS and log KPE in the three different temperature zones are presented in the figure: the site Guangzhou, China, within the subtropical climate zone, shown in the top-left panel; the site Harbin, China, within the warm temperate climate zone, shown in the bottom panel; and the site Alert, Canada, within tundra climate zone, shown in the top-right panel, all introduced in the previous sections

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Summary

Introduction

Atmospheric transport is a major mechanism of moving semi-volatile organic compounds (SVOCs), including persistent organic pollutants (POPs), from source regions to other. Based on a large data set of more than 700 pairs of air samples in both gas and particle phases with a wide ambient temperature range of 60 ◦C from −22 to +38 ◦C obtained from our Chinese POPs Soil and Air Monitoring Program, Phase 2 (China-SAMP-II), we investigated the G/P partitioning behavior of PBDEs in Chinese air (Yang et al, 2013; Li and Jia, 2014). We derived for the first time empirical equations to predict the values of slopes and intercepts for both KOAbased and PL-based models as functions of temperature, and the predicted partition quotient (KP), without assuming an equilibrium status and free of artifacts (Li and Jia, 2014).

Equilibrium state and steady state
Basic equation
Non-equilibrium term log α
Threshold values of log KOA and temperature
Particle-phase fraction
Application of the equations
Conclusions and discussion
The maximum partition coefficient
Comparison to the empirical equations
Findings
The limitation of applications
Full Text
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