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Agglomerated superparamagnetic iron
oxide nanoparticles can easily and in large scale be
precipitated from iron salt solutions. Although the
process is well known, it is ambiguously either assumed
that magnetite or maghemite is obtained. The first part
of our study clarifies this question using X-ray absorption
spectroscopy. For further processing of the nanoparticles,
i.e., for giving them a surface functionality or
incorporating them into composites, it is important to
break the agglomerates and individualize the particles
at first. This can effectively be done with nitric acid
treatment. The influence of this process on the particles
chemistry and structure was analyzed in great detail
using X-ray diffraction, X-ray absorption, and smallangle
X-ray scattering. In contrast to our expectation,
no oxidation from magnetite (Fe3O4) to maghemite (γ-
Fe2O3) was found; the formal valence of the particles in
any case is magnetite (Fe3O4). Instead, an increase in
the particles' surface disorder was discovered from
X-ray absorption analyses and high-resolution transmission
electron microscopy. The acid treatment
roughens and distorts the surface of the nanoparticles
which is connected with an increased spin disorder.
Impact of organic phosphates on the structure and composition of short-range ordered iron nanophases
(2024)
Organic phosphates (OP) are important nutrient components for living cells in natural environments, where they readily interact with ubiquitous iron phases such as hydrous ferric oxide, ferrihydrite (FHY). FHY partakes in many key bio(geo)chemical reactions including iron-mediated carbon storage in soils, or iron-storage in living organisms. However, it is still unknown how OP affects the formation, structure and properties of FHY. Here, we document how β-glycerophosphate (GP), a model OP ligand, affects the structure and properties of GP–FHY nanoparticles synthesized by coprecipitation at variable nominal molar P/Fe ratios (0.01 to 0.5). All GP–FHY precipitates were characterized by a maximum solid P/Fe ratio of 0.22, irrespective of the nominal P/Fe ratio. With increasing nominal P/Fe ratio, the specific surface area of the GP–FHY precipitates decreased sharply from 290 to 3 m2 g−1, accompanied by the collapse of their pore structure. The Fe–P local bonding environment gradually transitioned from a bidentate binuclear geometry at low P/Fe ratios to monodentate mononuclear geometry at high P/Fe ratios. This transition was accompanied by a decrease in coordination number of edge-sharing Fe polyhedra, and the loss of the corner-sharing Fe polyhedra. We show that Fe(III) polymerization is impeded by GP, and that the GP–FHY structure is highly dependent on the P/Fe ratio. We discuss the role that natural OP-bearing Fe(III) nanophases have in biogeochemical reactions between Fe–P and C species in aquatic systems.