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Magnetic characterization of ferrihydrite nanoparticles synthesized by hydrolysis of Fe metal-organic precursor

机译:铁金属有机前驱体水解合成水铁矿纳米粒子的磁性表征

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We investigate the formation of ferrihydrite nanoparticles (NPs) by hydrolysis of the Fe(III) alkoxide Fe((OBu)-Bu-t)(3). Controlled amounts of water, up to 3.0 vol%, were added to the precursor solution yielding a series of hydrolyzed samples ranging from P0.0 (the unreacted precursor) to P3.0. X-ray diffraction (XRD) analysis evidenced the formation of high-crystalline ferrihydrite NP in sample P3.0, with grain size estimate of about 3.2 nm. The transition from the molecular precursor to the formation of crystalline magnetic NPs was followed through magnetization measurements M(T) and M(H), as well as Mossbauer spectroscopy (MS). M(T) measurements indicate a paramagnetic (PM) behavior for sample P0.0, characteristic of binuclear Fe-O-Fe units, which evolves to a superparamagnetic (SPM) behavior, with an energy barrier for the blocking process estimated for sample P3.0 as E-a = 4.9 x 10(-21) J (E-a/k(B) = 355 K), resulting in a high effective anisotropy constant K-eff = 290 kJ/m(3). Magnetization loops at 5 K progressively change from PM-like to ferromagnetic-like shape upon increasing the hydrolysis process, although hysteresis (H-c approximate to 500 Oe) only is apparent for P2.0 and higher. MS spectra at room temperature are PM/SPM doublets for all samples, while the MS spectra at T = 4.2 K reveal increasingly well-defined magnetic ordering as hydrolysis of the precursor stepwise progresses until well-crystallized ferrihydrite particles are formed.
机译:我们调查的Fe(III)醇盐Fe((OBu)-Bu-t)(3)的水解形成水铁矿纳米粒子(NPs)。将控制量的水(最多3.0%(体积))添加到前体溶液中,得到一系列水解样品,范围从P0.0(未反应的前体)到P3.0。 X射线衍射(XRD)分析表明样品P3.0中形成了高结晶亚铁水合物NP,晶粒尺寸估计约为3.2 nm。通过磁化测量M(T)和M(H)以及Mossbauer光谱法(MS)跟踪从分子前体到形成结晶磁性NP的过渡。 M(T)测量表明样品P0.0的顺磁性(PM)行为,双核Fe-O-Fe单元的特征,演变为超顺磁性(SPM)行为,并且对样品P3估计的阻挡过程具有能垒.0当Ea = 4.9 x 10(-21)J(Ea / k(B)= 355 K)时,导致高有效各向异性常数K-eff = 290 kJ / m(3)。尽管增加了磁滞现象(H-c大约为500 Oe),但在5 K时,磁化回路从PM状逐渐转变为铁磁状,尽管P2.0和更高的磁滞仅明显。对于所有样品,室温下的MS光谱都是PM / SPM的双峰,而T = 4.2 K时的MS光谱显示,随着前体的水解逐步进行直至形成结晶良好的三水铁矿颗粒,磁性越来越清晰。

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