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Dipolar structures in magnetite ferrofluids studied with small-angle neutron scattering with and without applied magnetic field

机译:磁铁矿铁磁流体中的偶极结构研究了小角度中子散射,有或没有施加磁场

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摘要

Field-induced structure formation in a ferrofluid with well-defined magnetite nanoparticles with a permanent magnetic dipole moment was studied with small-angle neutron scattering (SANS) as a function of the magnetic interactions. The interactions were tuned by adjusting the size of the well-defined, single-magnetic-domain magnetite (Fe3O4) particles and by applying an external magnetic field. For decreasing particle dipole moments, the data show a progressive distortion of the hexagonal symmetry, resulting from the formation of magnetic sheets. The SANS data show qualitative agreement with recent cryogenic transmission electron microscopy results obtained in 2D [Klokkenburg et al., Phys. Rev. Lett. 97, 185702 (2006)] on the same ferrofluids.
机译:利用小角中子散射(SANS)研究了具有明确定义的具有永久磁偶极矩的磁铁矿纳米颗粒的铁磁流体中的场致结构形成,该函数是磁相互作用的函数。通过调整明确定义的单磁畴磁铁矿(Fe3O4)颗粒的大小并施加外部磁场,可以调节相互作用。为了减小粒子偶极矩,数据显示了由于形成磁性片而导致的六边形对称性的逐渐变形。 SANS数据显示与2D中获得的最新低温透射电子显微镜结果在质量上一致[Klokkenburg等,Phys。牧师97,185702(2006)]上的相同铁磁流体。

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