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TakedownIf you consider content in White Rose Research Online to be in breach of UK law, please notify us by emailing eprints@whiterose.ac.uk including the URL of the record and the reason for the withdrawal request. The main focus of their paper is the errors that occur during the determination of fractional solubility (using distilled water or DI leaches) due to the dissolution of <0.45 µm particles during storage of the leaches. We agree that such dissolution errors are important, but go further here in choosing to emphasise the fundamental role of mineralogy, which lies at the heart of the errors in this methodology. Our view is that DI leach errors need to be considered in relation to the forms of iron in dust samples and their mineralogical associations.
Comments onThe DI technique leaches dust at pH 5.6 through a <0.45 µm filter in a flow through system (Buck et al., 2006;. This minimises Fe losses due to precipitation of Fe ( Mineralogy may also provide important insights into potential bioavailability (Raiswell et al., 2016). Most dFe is considered to be bioavailable because organically boundFe can be taken up by phytoplankton through several known pathways (Shaked and Lis, 2012;Meskhidze et al.,2016). However the iron dissolved by the DI leach is mainly inorganic (see above) and only the highly reactive and/or amorphous phases are likely to be bioavailable. For example there is experimental evidence to suggest that poorly crystalline or amorphous phases such as ferrihydrite can be used by plankton (Wells et al., 1983;Rich and Morel, 1990; Kuma and Matsunga, 1995;Nodwell and Price, 2001). By contrast the more crystalline phases may not be readily bioavailable unless modified by dissolution or grazing (Barbeau et al., 1996;Shaked and Lis, 2012). Thus using a technique that extracts only adsorbed or amorphous iron phases (such as ferrihydrite), and excludes contributions from crystalline phases would produce a closer correspondence between dFe and the DI leach.Iron mineralogy has often been peripheral to the dust research agenda although it plays a crucial role in atmospheric processes such as radiative forcing and ice nucleation (Mahowald, 2013). Unfortunately observations of dust iron minerals are scarce although models such as those presented by Scanza et al.(2015), Perlwitz et al.(2015) and Journet et al.(2014) are now trying explicitly to represent dust mineralogy and their impacts on the climate s...