<p>Greigite (Fe<sub>3</sub>S<sub>4</sub>) is a ferrimagnetic mineral widespread in sedimentary environments, commonly found in lacustrine and marine sediments that records ancient geomagnetic field variations and environmental processes. However, its magnetic properties are not yet well understood due to the lack of a single crystal greigite suitable for magnetic measurements. In particular, the dependency of its magnetic properties with respect to structural and morphological properties remains uncertain.</p><p>In the present study, we analyzed the structural and magnetic properties of synthetic, polycrystalline greigite formed by controlled colloidal synthesis [Rhodes et al. 2017]. X-ray diffractometry and transition electron microscopy reveal that greigite forms flakes of about 100 nm that consist of epitaxial intergrown nanoparticles with a mean coherence length of 19 nm. Therefore, our synthetic greigite can be considered as polycrystalline flakes with a nanotexture.</p><p>The saturation magnetization (M<sub>s</sub>) of the nanotextured greigite is 32.7 Am<sup>2</sup>kg<sup>-1 </sup>and the coercivity is B<sub>c</sub> = 41 mT. The M<sub>s</sub> is about 45% below the value for relatively large, synthetic crystal and this in turn is probably caused by the nanotexture, e.g., interfaces between nanocrystallites. The ratios M<sub>r.</sub>/M<sub>S</sub> = 0.54 and B<sub>ar</sub>/B<sub>Sc</sub> = 1.33 indicate single-domain (SD) particles with pre-dominant uniaxial anisotropy [Roberts 1995]. The FORC diagram at room temperature shows an oval contour plot supporting that the flakes are nanotextured with interacting SD particles. The hysteresis parameters B<sub>c</sub> and M<sub>S</sub> continuously increase upon cooling to 10 K.</p><p>Low-temperature cycling of the magnetization between 300 and 10 K in fields between 10 mT and 1000 mT shows the expected behavior for ferrimagnets with the superposition of the cooling and warming curves at fields B &#179; 500 mT. At weaker fields a slight magnetic induction upon warming is found and the relative increase in magnetization is field dependent. This irreversibility most likely stems from the magnetization of the nanoparticle interfaces and their interactions in the flakes.</p><p>Ferromagnetic resonance spectroscopy (FMR) at room temperature shows a resonance field B<sub>res</sub>= 213 mT and linewidth DB = 160 mT. Upon cooling the B<sub>res</sub> decreases continuously down to 50 K followed by a pronounced shift to lower values down to 10 K. The shift goes along with markedly linewidth broadening. The discontinuity of the spectral parameters at T < 50 K points to a change in the effective anisotropy of the flakes most likely due to changes of the magnetocrystalline and the interaction anisotropies in the nanotexture, because the shape anisotropy of the polycrystalline flakes undergoes no significant change.&#160;</p><p>In summary, the magnetic properties of greigite can be critically affected by the nanotexture. The response of the nanotexture to the magnetization and anisotropy properties can be taken to identify and characterize greigite nanoparticles in natural environments and to critically evaluate their use for paleomagnetic studies.</p><p>Rhodes, Jordan M., et al. "Phase-controlled colloidal syntheses of iron sulfide nanocrystals via sulfur precursor reactivity and direct pyrite precipitation."&#160;Chemistry of Materials&#160;29.19 (2017): 8521-8530.</p><p>Roberts, Andrew P. "Magnetic properties of sedimentary greigite (Fe3S4)."&#160;Earth and Planetary Science Letters&#160;134.3-4 (1995): 227-236.</p>
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