Abstract
Iron (Fe) in aerosol particles is a major external source of micronutrients for marine ecosystems, and poses a potential threat to human health. To understand these impacts of aerosol Fe, it is essential to quantify the sources of dissolved and total Fe. In this study, we applied a receptor modelling for the first time to apportion the sources of dissolved and total Fe in fine particles collected under five different weather conditions in Hangzhou megacity of Eastern China, which is upwind of East Asian outflow. Results showed that Fe solubility (dissolved to total Fe) was the largest in fog days (6.3 ± 2.6 %), followed by haze (4.6 ± 1.9 %), dust (2.1 ± 0.7 %), clear (1.7 ± 0.6 %), and rain (0.8 ± 0.3 %) days. Positive Matrix Factorisation (PMF) analysis suggested that industrial and traffic emissions were the two dominant primary sources of dissolved and total Fe during haze and fog days, but dust was the dominant source in dust days. About 15 % of dissolved Fe was associated with secondary sources during haze and fog days, although it was less than 5 % during dust and clear days. Transmission electron microscopy analysis of individual particles showed that approximately 76 % and 87 % of Fe-containing particles were internally mixed with acidic sulfates and nitrates in haze and fog days, respectively. Our results indicated that aqueous surface of aerosol particles promotes heterogeneous reactions between acidic species and Fe aerosol, contributing to higher Fe solubility during fog and haze days.
Highlights
The deposition of atmospheric aerosols is a major external source of iron (Fe) in the ocean (Li et al, 2017; Pinedo-González et al, 2020; Yang et al, 2020)
About 15% of dissolved Fe was associated with secondary sources during haze and fog days, it was less than 5% during dust and clear days
Our results indicated that aqueous surface of aerosol particles promotes heterogeneous reactions between acidic species and Fe aerosol, contributing to higher Fe solubility during fog and haze days
Summary
The deposition of atmospheric aerosols is a major external source of iron (Fe) in the ocean (Li et al, 2017; Pinedo-González et al, 2020; Yang et al, 2020). Atmospheric Fe-containing particles have an adverse effect on human health by generating reactive oxygen species (ROS) (Abbaspour et al, 2014), and can convert S(IV) to S(VI) by catalytic oxidation for 35 atmospheric sulfate (SO42-) production (Alexander et al, 2009). These roles of Fe largely depend on the atmospheric Fe solubility (Shi et al, 2012; Baker et al, 2021). Field observations on atmospheric Fe solubility are still limited, and the available data show a wide range of Fe solubility (0.02 % to 98 %) in different atmospheric environments (Schroth et al, 2009; Shi et al, 2012; Oakes et al, 2012; Myriokefalitakis et al, 2015)
Sign-in/Register to view highlights & summary Sign-in/Register to access full text options 
Free) 
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a call
