Relative contribution of combustion-related emissions to atmospheric soluble Fe deposition over oceans. Constant Fe solubilities (0.44 % for dust, 22.5 % for coal fly ash, 79 % for oil fly ash and 18 % for biomass fly ash) were applied to calculate the deposition of soluble Fe from the deposition of total Fe.  

Relative contribution of combustion-related emissions to atmospheric soluble Fe deposition over oceans. Constant Fe solubilities (0.44 % for dust, 22.5 % for coal fly ash, 79 % for oil fly ash and 18 % for biomass fly ash) were applied to calculate the deposition of soluble Fe from the deposition of total Fe.  

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Atmospheric deposition of iron (Fe) plays an important role in controlling oceanic primary productivity. However, the sources of Fe in the atmosphere are not well understood. In particular, the combustion sources of Fe and the subsequent deposition to the oceans have been accounted for in only few ocean biogeochemical models of the carbon cycle. He...

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... The presence of these elements in the air suggests an origin from the resuspension of dust by road-tire interactions (Gustafsson et al., 2008). Although Fe in the atmosphere is primarily derived from crustal sources, anthropogenic sources of Fe include fossil fuel combustion and biomass burning (Matsui et al., 2018), industrial and metallurgical processes (Wang et al., 2015), exhaust emissions (Salazar et al., 2020), and tire and brake wear (Wahid, 2018). ...
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... Iron (Fe) in marine aerosol have been widely studied over the past few decades in order to understand its critical role on enhancing the marine biological pump and impacting the marine primary productivity that subsequently alter the trend in global climate change (Jickells et al., 2005;Mahowald et al., 2010). Traditionally, dust emission has been regarded as the main contributor to atmospheric Fe, with global annual emission of approximately 40-100 Tg Fe Ito and Shi, 2016;Luo et al., 2008;Wang et al., 2015). However, marine phytoplankton mainly uptake dissolved Fe rather than particulate Fe (Gledhill and Buck, 2012;Wang et al., 2019), depending on Fe solubility that is prominently affecting its bioavailability. ...
... In addition, model simulations indicated that anthropogenic emissions contributed significantly to soluble Fe deposition flux, even dominating in some oceanic regions. For example, Wang et al. (2015) reported that anthropogenic emissions accounted for >80 % of soluble Fe deposition in the Northwest Pacific. Thus, anthropogenic Fe deposition had nonnegligible impacts on marine ecology and climate (Pinedo-Gonzalez et al., 2020;Tang et al., 2021). ...
... For NWP2, although it is far from the East Asian continent, coal combustion still accounted for about 20 % of the total Fe in PM 2.5 , which was comparable to the findings of Lin et al. (2015). Based on the CMAQ model simulation, Lin et al. (2015) found that in different seasons of 2007, the contribution of coal fly ash Fe to total Fe deposition in PM 10 in the open Northwest Pacific was 5-15 %. Wang et al. (2015) also reported that contribution of coal combustion to total Fe deposition exceeded 10 % in the sea area around NWP2 based on model simulation. ...
... Heavy metal exposures also obstruct the microbial (continued) . Suspended sediment Raiswell and Canfield (2012), Wang et al. (2015), Wells et al. (1995) . Aeolian dust transport . ...
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... In brief, their approach calculated the Fe emitted from biomass burning by estimating the fraction of fuel consumption based on a global 0.1° × 0.1° fuel data set, the completeness of plant consumption, the average Fe concentration in each given biome, and the amount of Fe lost to the residue ash phase. The authors of this study found that the fine fraction (PM1 in their study) of the plant matter accounted for only 17 Gg yr −1 while the coarse fraction accounted for 460 Gg yr −1 of global Fe (Wang et al., 2015). To our knowledge, this estimate has not been corroborated with field data. ...
... Here, we provide direct measurements of the fine fraction of Fe (PM 2.5 ) derived from burning plant material that is isolated from uplifted soil particles and compare our results to those ascertained using a mass-balance approach (Wang et al., 2015). We conducted small-scale biomass burning experiments of isolated plant matter because field studies from large burns cannot disentangle burning plant matter from soil-suspended particles. ...
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