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High-TemperatureMagnetism as a Probe for Structural and Compositional Uniformity inLigand-Capped Magnetite Nanoparticles

机译:高温磁性作为结构和组成均匀性的探究配体包覆的磁铁矿纳米颗粒

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摘要

To investigate magnetostructural relationships in colloidal magnetite (Fe3O4) nanoparticles (NPs) at high temperature (300–900 K), we measured the temperature dependence of magnetization (M) of oleate-capped magnetite NPs ca. 20 nm in size. Magnetometry revealed an unusual irreversible high-temperature dependence of M for these NPs, with dip and loop features observed during heating–cooling cycles. Detailed characterizations of as-synthesized and annealed Fe3O4 NPs as well as reference ligand-free Fe3O4 NPs indicate that both types of features in M(T) are related to thermal decomposition of the capping ligands. The ligand decomposition upon the initial heating induces a reduction of Fe3+ to Fe2+ and the associated dip in M, leading to more structurally and compositionally uniform magnetite NPs. Having lost the protective ligands, the NPs continually sinter during subsequent heating cycles, resulting in divergent M curves featuring loops. The increase in M with sintering proceeds not only through elimination of a magnetically dead layer on the particle surface, as a result of a decrease in specific surface area with increasing size, but also through an uncommonlyinvoked effect resulting from a significant change in Fe3+/Fe2+ ratio with heat treatment. The interpretation ofirreversible features in M(T) indicatesthat reversible M(T) behavior, conversely,can be expected only for ligand-free, structurally and compositionallyuniform magnetite NPs, suggesting a general applicability of high-temperature M(T) measurements as an analytical methodfor probing the structure and composition of magnetic nanomaterials.
机译:为了研究高温(300–900 K)下胶体磁铁矿(Fe3O4)纳米颗粒(NPs)的磁结构关系,我们测量了油酸封端磁铁矿NPs的磁化强度(M)。尺寸为20 nm。磁力计揭示了这些NP对M的异常的不可逆高温依赖性,在加热-冷却循环中观察到了倾角和回线特征。合成和退火的Fe3O4 NP以及不含参比的Fe3O4 NP的详细特征表明,M(T)中的两种特征都与封盖配体的热分解有关。初始加热时,配体分解会导致Fe 3 + 还原为Fe 2 + 并伴随M的下降,从而导致结构和组成上更均匀的磁铁矿NP。失去保护性配体后,NP在随后的加热循环中不断烧结,从而形成带有环的发散的M曲线。烧结引起的M的增加不仅通过消除颗粒表面上的磁死层(由于比表面积随尺寸增加而减小)而进行,而且还通过不常见的方式进行。热处理引起的Fe 3 + / Fe 2 + 比率的显着变化所产生的激活效应。的解释M(T)中的不可逆特征表示相反,可逆的M(T)行为只能预期在结构和组成上都不含配体均匀的磁铁矿纳米颗粒,表明高温M(T)测量作为分析方法的一般适用性用于探测磁性纳米材料的结构和组成。

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