Orbital Moment Determination in (MnxFe1-x)3O4 Nanoparticles

V. L. Pool
{"title":"Orbital Moment Determination in (MnxFe1-x)3O4 Nanoparticles","authors":"V. L. Pool","doi":"10.1063/1.3562905","DOIUrl":null,"url":null,"abstract":"JOURNAL OF APPLIED PHYSICS 109, 07B532 (2011) Orbital moment determination in (Mn x Fe 12x ) 3 O 4 nanoparticles V. L. Pool, 1,2,a) C. Jolley, 3,4 T. Douglas, 2,3 E. A. Arenholz, 5 and Y. U. Idzerda 1,2 Department of Physics, Montana State University, Bozeman, Montana 59717, USA Center for Bio-inspired Nanomaterials, Montana State University, Bozeman, Montana 59717, USA Department of Chemistry and Biochemistry, Montana State University, Bozeman, Montana 59717, USA Astrobiology Biogeocatalysis Research Center, Montana State University, Bozeman, Montana 59717, USA Advanced Light Source, Lawrence Berkeley National Labs, Berkeley, California 94720, USA (Presented 17 November 2010; received 24 September 2010; accepted 8 December 2010; published online 7 April 2011) Nanoparticles of (Mn x Fe 1Ax ) 3 O 4 with a concentration ranging from x ¼ 0 to 1 and a crystallite size of 14–15 nm were measured using X-ray absorption spectroscopy and X-ray magnetic circular dichroism to determine the ratio of the orbital moment to the spin moment for Mn and Fe. At low Mn concentrations, the Mn substitutes into the host Fe 3 O 4 spinel structure as Mn 2þ in the tetrahedral A-site. The net Fe moment, as identified by the X-ray dichrosim intensity, is found to increase at the lowest Mn concentrations then rapidly decrease until no dichroism is observed at 20% Mn. The average Fe orbit/spin moment ratio is determined to initially be negative and small for pure Fe 3 O 4 nanoparticles and quickly go to 0 by 5%–10% Mn addition. The average Mn moment is anti-aligned to the Fe moment with an orbit/spin moment ratio of 0.12 which gradually C decreases with Mn concentration. V 2011 American Institute of Physics. [doi:10.1063/1.3562905] I. INTRODUCTION The doping of spinel ferrite nanoparticles (c-Fe 2 O 3 and Fe 3 O 4 ) with magnetic and nonmagnetic substitutional transi- tion metals has demonstrated good control of both moment and anisotropy, 1 with magnetic behavior and dopant occu- pancy sites often quite different from the bulk behavior. One example is for the biomineralization of (Mn x Fe 1Ax ) 3 O 4 nano- particles inside protein cage structures, where Mn initially substitutes as Mn 2þ into the octahedral B-site causing the moment to decrease instead of as Mn 2þ in the tetrahedral A-site, 1 creating an enhanced moment as occurs in the bulk. 2 It is unclear whether these differences are due to the gentle synthesis conditions of biomineralization, the presence of the protein encapsulation, or the reduced dimensionality of nanoparticles. A comparison of dopant occupation sites and anisotropy energies of similar nanoparticles synthesized under different conditions would be useful. For noninteracting particles, frequency dependent ac- susceptibility measurements are a useful way to determine anisotropy energies. 1,3 A related parameter to the magneto- crystalline anisotropy energy is the elemental orbital mag- netic moment as determined from energy integration of the X-ray magnetic circular dichroism spectra (using the XMCD sum-rules). 4–7 Used predominantly for single crystal thin film geometries, this unique method for separating the orbital moment and the spin moment of each element has utility for nanoparticles, especially those found to be interacting. II. EXPERIMENTAL tein encapsulated particles (the synthesis route used in ref #1 but without inclusion of the protein). Solutions of 12.5 mM (NH 4 ) 2 Fe(SO 4 ) 2 .6H 2 O and 12.5 mM MnCl 2 were prepared using H 2 O that had been sparged with N 2 to remove dis- solved oxygen and mixed to obtain the desired [Fe 2þ ]: [Mn 2þ ] ratio. The 12.5 mM metal mixture and a deaerated 4.17 mM H 2 O 2 solution were added at a rate of 40 ml/h to a deaerated solution of 100 mM NaCl maintained at 65 C while the pH was maintained at 8.5 by addition of deaerated 100 mM NaOH using an autotitrator. Samples were centri- fuged and triple washed with de-ionized water in order to remove NaCl and unreacted metal ions. Samples used for X-ray absorption spectroscopy (XAS) and X-ray magnetic circular dichroism (XMCD) measurements were stored in an aqueous suspension and subsequently dried onto Formvar- coated TEM grids, while samples to be used for hard X-ray pair distribution function (PDF) analysis were immediately dried to powder using a vacuum lyophilizer. The XAS and XMCD measurements were conducted at beamline 4.0.2 of the Advanced Light Source of Berkeley National Laboratories simultaneously in transmission yield (using a Ga photodetector) and total electron yield (in the sample current mode). Absorption measurements were made at room temperature with the photon polarization set at 90% and an alternating applied magnetic field of 0.5 T. III. RESULTS Nanoparticles of (Mn x Fe 1Ax ) 3 O 4 were synthesized with x ¼ 0 to 1.0 by a chemical route identical to that used for pro- a) Author to whom correspondence should be addressed. Electronic mail: pool@physics.montana.edu. The Mn L 23 -edge XAS spectra for a representative sam- pling of different Mn concentrations are shown in Fig. 1. The spectra have had a linear background removed, been normalized to the integrated peak area (L 2 þ L 3 ), and were energy calibrated by comparing the peak position of a simul- taneously collected Mn 3 O 4 reference powder spectra (set to 640.05 eV). The evolution of the spectra show that as the Mn C V 2011 American Institute of Physics 0021-8979/2011/109(7)/07B532/3/$30.00 109, 07B532-1","PeriodicalId":17982,"journal":{"name":"Lawrence Berkeley National Laboratory","volume":"79 11 1","pages":""},"PeriodicalIF":0.0000,"publicationDate":"2011-04-07","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Lawrence Berkeley National Laboratory","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.1063/1.3562905","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 0

Abstract

JOURNAL OF APPLIED PHYSICS 109, 07B532 (2011) Orbital moment determination in (Mn x Fe 12x ) 3 O 4 nanoparticles V. L. Pool, 1,2,a) C. Jolley, 3,4 T. Douglas, 2,3 E. A. Arenholz, 5 and Y. U. Idzerda 1,2 Department of Physics, Montana State University, Bozeman, Montana 59717, USA Center for Bio-inspired Nanomaterials, Montana State University, Bozeman, Montana 59717, USA Department of Chemistry and Biochemistry, Montana State University, Bozeman, Montana 59717, USA Astrobiology Biogeocatalysis Research Center, Montana State University, Bozeman, Montana 59717, USA Advanced Light Source, Lawrence Berkeley National Labs, Berkeley, California 94720, USA (Presented 17 November 2010; received 24 September 2010; accepted 8 December 2010; published online 7 April 2011) Nanoparticles of (Mn x Fe 1Ax ) 3 O 4 with a concentration ranging from x ¼ 0 to 1 and a crystallite size of 14–15 nm were measured using X-ray absorption spectroscopy and X-ray magnetic circular dichroism to determine the ratio of the orbital moment to the spin moment for Mn and Fe. At low Mn concentrations, the Mn substitutes into the host Fe 3 O 4 spinel structure as Mn 2þ in the tetrahedral A-site. The net Fe moment, as identified by the X-ray dichrosim intensity, is found to increase at the lowest Mn concentrations then rapidly decrease until no dichroism is observed at 20% Mn. The average Fe orbit/spin moment ratio is determined to initially be negative and small for pure Fe 3 O 4 nanoparticles and quickly go to 0 by 5%–10% Mn addition. The average Mn moment is anti-aligned to the Fe moment with an orbit/spin moment ratio of 0.12 which gradually C decreases with Mn concentration. V 2011 American Institute of Physics. [doi:10.1063/1.3562905] I. INTRODUCTION The doping of spinel ferrite nanoparticles (c-Fe 2 O 3 and Fe 3 O 4 ) with magnetic and nonmagnetic substitutional transi- tion metals has demonstrated good control of both moment and anisotropy, 1 with magnetic behavior and dopant occu- pancy sites often quite different from the bulk behavior. One example is for the biomineralization of (Mn x Fe 1Ax ) 3 O 4 nano- particles inside protein cage structures, where Mn initially substitutes as Mn 2þ into the octahedral B-site causing the moment to decrease instead of as Mn 2þ in the tetrahedral A-site, 1 creating an enhanced moment as occurs in the bulk. 2 It is unclear whether these differences are due to the gentle synthesis conditions of biomineralization, the presence of the protein encapsulation, or the reduced dimensionality of nanoparticles. A comparison of dopant occupation sites and anisotropy energies of similar nanoparticles synthesized under different conditions would be useful. For noninteracting particles, frequency dependent ac- susceptibility measurements are a useful way to determine anisotropy energies. 1,3 A related parameter to the magneto- crystalline anisotropy energy is the elemental orbital mag- netic moment as determined from energy integration of the X-ray magnetic circular dichroism spectra (using the XMCD sum-rules). 4–7 Used predominantly for single crystal thin film geometries, this unique method for separating the orbital moment and the spin moment of each element has utility for nanoparticles, especially those found to be interacting. II. EXPERIMENTAL tein encapsulated particles (the synthesis route used in ref #1 but without inclusion of the protein). Solutions of 12.5 mM (NH 4 ) 2 Fe(SO 4 ) 2 .6H 2 O and 12.5 mM MnCl 2 were prepared using H 2 O that had been sparged with N 2 to remove dis- solved oxygen and mixed to obtain the desired [Fe 2þ ]: [Mn 2þ ] ratio. The 12.5 mM metal mixture and a deaerated 4.17 mM H 2 O 2 solution were added at a rate of 40 ml/h to a deaerated solution of 100 mM NaCl maintained at 65 C while the pH was maintained at 8.5 by addition of deaerated 100 mM NaOH using an autotitrator. Samples were centri- fuged and triple washed with de-ionized water in order to remove NaCl and unreacted metal ions. Samples used for X-ray absorption spectroscopy (XAS) and X-ray magnetic circular dichroism (XMCD) measurements were stored in an aqueous suspension and subsequently dried onto Formvar- coated TEM grids, while samples to be used for hard X-ray pair distribution function (PDF) analysis were immediately dried to powder using a vacuum lyophilizer. The XAS and XMCD measurements were conducted at beamline 4.0.2 of the Advanced Light Source of Berkeley National Laboratories simultaneously in transmission yield (using a Ga photodetector) and total electron yield (in the sample current mode). Absorption measurements were made at room temperature with the photon polarization set at 90% and an alternating applied magnetic field of 0.5 T. III. RESULTS Nanoparticles of (Mn x Fe 1Ax ) 3 O 4 were synthesized with x ¼ 0 to 1.0 by a chemical route identical to that used for pro- a) Author to whom correspondence should be addressed. Electronic mail: pool@physics.montana.edu. The Mn L 23 -edge XAS spectra for a representative sam- pling of different Mn concentrations are shown in Fig. 1. The spectra have had a linear background removed, been normalized to the integrated peak area (L 2 þ L 3 ), and were energy calibrated by comparing the peak position of a simul- taneously collected Mn 3 O 4 reference powder spectra (set to 640.05 eV). The evolution of the spectra show that as the Mn C V 2011 American Institute of Physics 0021-8979/2011/109(7)/07B532/3/$30.00 109, 07B532-1
(MnxFe1-x)3O4纳米粒子轨道矩的测定
V. L. Pool, 1,2,a) C. Jolley, 3,4 T. Douglas, 2,3 E. a . Arenholz, 5 and Y. U. Idzerda 1,2,美国蒙大拿州立大学物理系,波兹曼,蒙大拿州59717,美国蒙大拿州立大学生物启发纳米材料中心,波兹曼,蒙大拿州59717,美国蒙大拿州立大学化学与生物化学系,波兹曼,蒙大拿州59717,美国蒙大拿州立大学,波兹曼,蒙大拿州59717,美国蒙大拿州立大学,波兹曼,蒙大拿州59717,美国蒙大拿州立大学,波兹曼,蒙大拿州59717,美国天体生物学生物地理催化研究中心,蒙大拿州立大学,波兹曼,蒙大拿州59717,美国先进光源,劳伦斯伯克利国家实验室,伯克利,加州94720,美国(2010年11月17日提交;2010年9月24日收到;2010年12月8日接受;利用x射线吸收光谱和x射线磁圆二色性测量了浓度为x¼0 ~ 1、晶粒尺寸为14 ~ 15 nm的(Mn x Fe 1Ax) 3o 4纳米粒子,以确定Mn和Fe的轨道矩与自旋矩的比值。在低Mn浓度下,Mn在四面体a位上以Mn 2þ的形式取代宿主Fe 3o - 4尖晶石结构。通过x射线二色性强度确定的净铁矩在Mn浓度最低时增加,然后迅速下降,直到在Mn浓度为20%时没有二色性。纯fe3o4纳米粒子的平均Fe轨道/自旋矩比最初为负且较小,在添加5% ~ 10% Mn时,平均Fe轨道/自旋矩比迅速趋于0。Mn的平均矩与Fe的反向,轨道/自旋矩比为0.12,且随着Mn浓度的增加,轨道/自旋矩逐渐减小。V 2011美国物理研究所。[doi:10.1063/1.3562905]尖晶石铁氧体纳米粒子(c- fe2o3和fe2o3)与磁性和非磁性取代过渡金属的掺杂表现出对矩和各向异性的良好控制,其磁性行为和掺杂占据位置往往与体行为完全不同。一个例子是蛋白质笼结构内(Mn x Fe 1Ax) 3o - 4纳米颗粒的生物矿化,其中Mn最初以Mn 2þ的形式取代了八面体b位,导致力矩减小,而不是以Mn 2þ的形式取代了四面体a位,1产生了增强的力矩。目前尚不清楚这些差异是由于生物矿化的温和合成条件,蛋白质封装的存在,还是纳米颗粒的降低。比较不同条件下合成的类似纳米粒子的掺杂位置和各向异性能将是有用的。对于非相互作用粒子,频率相关的交流磁化率测量是确定各向异性能量的有效方法。与磁晶各向异性能量相关的一个参数是元素轨道磁矩,这是由x射线磁圆二色谱的能量积分确定的(使用XMCD求和规则)。主要用于单晶薄膜几何形状,这种分离每个元素的轨道力矩和自旋力矩的独特方法对纳米粒子,特别是那些发现相互作用的纳米粒子有实用价值。2实验蛋白包封颗粒(参考文献1中使用的合成路线,但不包含蛋白质)。在h2o中加入氮气去除溶解氧,并混合得到所需的[Fe 2þ]: [Mn 2þ]比例,制备12.5 mM (nh4) 2fe (so4) 2.6 h2o和12.5 mM MnCl 2溶液。将12.5 mM的金属混合物和4.17 mM的脱氧水溶液以40 ml/ H的速率加入到100 mM NaCl的脱氧水溶液中,在65℃下,通过自动滴定器添加脱氧水100 mM NaOH,将pH维持在8.5。样品经离心和去离子水三次洗涤,以去除NaCl和未反应的金属离子。用于x射线吸收光谱(XAS)和x射线磁圆二色性(XMCD)测量的样品存储在水悬浮液中,随后在Formvar涂层的TEM网格上干燥,而用于硬x射线对分布函数(PDF)分析的样品立即使用真空冻干机干燥成粉末。XAS和XMCD在伯克利国家实验室先进光源的光束线4.0.2处同时进行透射率(使用Ga光电探测器)和总电子产率(在样品电流模式下)的测量。在室温下,光子极化率设为90%,外加0.5 t的交变磁场下进行吸收测量。结果(Mn x Fe 1Ax) 3o - 4纳米颗粒在x¼0 ~ 1.0的浓度下合成,化学路线与pro- a相同。电子邮件:pool@physics.montana.edu。
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