Combustion iron distribution and deposition

By C. Luo, N. Mahowald, Tami C. Bond, P. Chuang, P. Artaxo, R. Siefert, Ying Chen, J. Schauer. 2007

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Iron, phosphorus, and nitrogen supply ratios define the biogeography of nitrogen fixation (2013, methodology): “2009) and reanalysis estimates of annual mean atmospheric Fe flux (Luo et al. 2008).”
Interconnection of nitrogen fixers and iron in the Pacific Ocean: Theory and numerical simulations (2012, methodology): “The aeolian iron supply has changed markedly across the last glacial maximum [Mahowald et al., 2006], preindustrial and modern day [Luo et al., 2008;Mahowald et al., 2009] and is likely to change in the future [Mahowald and Luo, 2003; Tegen et al., 2004].”
Modelling spatial and temporal patterns in size-structured marine plankton communities: top -down and bottom -up controls (2014, background): “Iron chemistry includes explicit complexation with an organic ligand, scavenging by particles (Parekh et al ., 2005) and representation of aeolian (Luo et al ., 2008) and sedimentary (Elrod et al ., 2004) sources.”
A size‐structured food‐web model for the global ocean (2012, background): “where Fatmos and Fsediment are the local atmospheric and sedimentary fluxes of bioavailable iron across the ocean surface and ocean bottom, respectively (Luo et al. 2008; Dutkiewicz et al. 2012).”