自形成MnFe2O4磁性液体的制备和磁性

用化学共沉淀法制备MnFe2O4纳米微粒,并且采用自形成法制备了粒子型磁性液体.在这种磁性液体中,通过适当的酸蚀,Mn2+和Fe3+离子从MnFe2O4纳米微粒溶解并吸附在磁性微粒表面以阻止微粒团聚.微粒和磁性液体都呈磁滞回线.这种磁化性质可能来源于在高场下产生的不可逆团聚.

Abstract：

MnFe2O4 nanoparticles are prepared by chemical coprecipitation method. Based on the MnFe2O4 nanoparticles, a self-formed ionic ferrofluid is synthesized. In the ferrofluid, Mn2+ and Fe3+ ions dissolved from the MnFe2O4 nanoparticles via suitable acid attack are adsorbed on the surface of the magnetic particles, thus preventing the particles from aggregating. The average thickness of ionized layers of the ferrofluid particles is about 1 to 2 nm.Both the particles and the ferrofluids have hysteresis behavior. The behavior may result from irreversible aggregation induced under high magnetic field.     

ZnFe2O4基磁凝胶的制备及磁性

用自形成法制备ZnFe2O4磁凝胶,并进一步研究包裹ZnFe2O4的γ-Fe2O3磁凝胶的制备,用振动样品磁强计(VSM)对ZnFe2O4和包裹ZnFe2O4的γ-Fe2O3磁性微粒及配制的胶体处在溶胶和凝胶的磁性测量.结果表明ZnFe2O4磁性微粒和胶体呈顺磁性,而包裹ZnFe2O4的γ-Fe2O3磁性微粒和胶体呈亚铁磁性.ZnFe2O4凝胶较其溶胶易磁化,而ZnFe2O4/γ-Fe2O3凝胶较其溶胶难磁化.从微观机制上解释了产生这些磁性差异的原因.

Abstract：

ZnFe2O4 magnetic gel is prepared by the self-formed method, and the preparation of γ-Fe2O3 coated with ZnFe2O4 is studied. The magnetization of ZnFe2O4 and γ-Fe2O3 nanoparticles coated with ZnFe2O4 and their gels and sols are measured by a vibrating sample magnetometer(VSM). The results show that the ZnFe2O4 powder and its colloid are paramagnetic, while the γ-Fe2O3 magnetic particles coated with ZnFe2O4 and colloid show ferrimagnetism. ZnFe2O4 gel is easier to be magnetized than sol. However, ZnFe2O4/γ-Fe2O3 gel is harder magnetized than sol. The reason for the difference in magnetization is interpreted microscopically.     

自形成MnFe2O4磁性液体的磁性研究

采用共沉淀法制备MnFe2O4磁性纳米微粒,并配制自形成磁性液体.测量了微粒粒径,以及MnFe2O4磁性纳米微粒、自形成磁性液体的磁性.磁性液体呈现出微粒所具有的矫顽力,其比饱和磁化强度与剩余磁化强度之比都是3∶1的关系.在高场下的磁化性质随v变化.通过分析得出自形成MnFe2O4磁性液体的磁性除与微粒磁性、微粒体积分数v以及基液磁性有关外,还受微粒表面非磁性层的影响.     

自形成MnFe2O4磁性液体的磁性研究

采用共沉淀法制备MnFe2O4磁性纳米微粒,并配制自形成磁性液体．测量了微粒粒径,以及MnFe2O4磁性纳米微粒、自形成磁性液体的磁性．磁性液体呈现出微粒所具有的矫顽力,其比饱和磁化强度与剩余磁化强度之比都是3：1的关系．在高场下的磁化性质随声。变化．通过分析得出自形成MnFe2O4磁性液体的磁性除与微粒磁性、微粒体积分数Фv 以及基液磁性有关外,还受微粒表面非磁性层的影响．     

- F e 2O 3/N i 2O 3复合磁性纳米微粒及磁性液体的磁化特性

采用化学共沉淀法制备了γ-Fe2O3/Ni2O3复合磁性纳米微粒,并用Massart法合成了γ-Fe2O3/Ni2O3复合磁性微粒的磁性液体.用振动样品磁强计(VSM)测量了磁性微粒及不同体积分数的磁性液体的磁化曲线.结果表明,磁性液体的饱和磁化强度与磁性液体中微粒的体积分数v、微粒表面的非磁性层以及基液的磁性有关;不同体积分数的磁性液体的饱和磁化强度实际测量值与相应的理论值吻合较好.由此可判断:γ-Fe2O3/Ni2O3复合磁性微粒较其它单相纳米微粒更适于合成磁性液体.     

水甘油基γ-Fe2O3/Ni2O3 复合微粒磁性液体的磁化性质

采用化学诱导相变法制备了γ-Fe2O3/Ni2O3 复合磁性纳米微粒,并用类似自形成离子型磁性液体的制备方 法合成了水甘油基γ-Fe2O3/Ni2O3 磁性液体.用振动样品磁强计(VSM)测量了γ-Fe2O3/Ni2O3 复合磁性微粒、不 同比例水甘油基磁性液体的磁化性质.结果表明,相同体积分数的水甘油基γ-Fe2O3/Ni2O3 磁性液体,由于基液 的不同其饱和磁化强度也不同,纯水基磁性液体的约化饱和磁化强度与磁性纳米微粒的磁化强度吻合得比甘油基 磁性液体好.     

CuFe2O4纳米微粒及其自形成磁性液体的磁性研究

对用共沉淀法制备的CuFe2O4磁性纳米微粒及其合成的自形成磁性液体在室温下进行磁性测量.其结果表明CuFe2O4微粒的饱和磁化强度较小,粉末与自形成磁性液体均呈超顺磁性-无剩磁、无矫顽力.用Langevin理论对测得的磁性进行了对比分析,从微粒间的相互作用解释了粉末和磁性液体的实测磁化曲线与Langevin理论的不同偏离现象.     

CuFe2O4纳米微粒及其自形成磁性液体的磁性研究

对用其沉淀法制备的CuFe2O4磁性纳米微粒及其合成的自形成磁性液体在室温下进行磁性测量.其结果表明CuFe2O4微粒的饱和磁化强度较小,粉末与自形成磁性液体均呈超顺磁性-无剩磁、无矫顽力.用Langevin理论对测得的磁性进行了对比分析,从微粒间的相互作用解释了粉末和磁性液体的实测磁化曲线与Langevin理论的不同偏离现象.     

由Ni2O3/Fe2O3复合纳米微粒构成的离子型磁性液体的磁化性质研究

采用Massart法合成了Ni2O3/Fe2O3复合微粒磁性液体,并用振动样品磁强计(VSM)对磁性微粒及其磁性液体的磁化性质进行了测量.用Langevin理论进行了磁性液体磁化曲线的拟合.实验结果表明,磁性液体的实际测量的比饱和磁化强度小于理论值,并且磁性液体的初始磁化率大于Langevin理论曲线的初始磁化率.用零场下磁性液体中的微粒自组装结构对实验现象进行了解释.     

COFe2O4-p-NiFe2O4二元离子型磁性液体的制备及其场致光透射驰豫

介绍了CoFe2O4-p-NiF2O4二元离子型磁性液体的制备方法,用X射线衍射仪、透射电子显微镜、振动样品磁强计分别对NiFe2O4微粒前驱体(p.NiFe2O4)和COFe2O4微粒的结构、粒径和磁性进行了测量与分析,研究了CoFe2O4-p-NiFe2O4二元离子型磁性液体在平行于激光照射方向具有不同梯度的外磁场作用下的场致透光的驰豫时间,并从微观结构上分析了产生驰豫时间差异的原因.     

超声辅助磁性纳米四氧化三铁催化过氧化氢降解亚甲蓝染料的研

建立了一种基于超声辅助磁性四氧化三铁纳米微粒催化过氧化氢降解亚甲蓝染料的方法,研究了四氧化三铁纳米微粒浓度、过氧化氢浓度、pH值、反应时间、超声时间和温度等对催化降解反应的影响.结果表明,当四氧化三铁纳米粒子浓度为600mg/L,过氧化氢浓度为0.32mol/L,pH值为5,超声时间为3min,温度为30℃,反应时间为2h时,模拟染料废水中亚甲蓝的去除率最高可达到95%.     

0.8ZnFe2O4-0.2MnFe2O4纳米颗粒磁化性质的实验研究

对采用化学共沉淀法制备的ZnFe2O4,MnFe2O4以及两者混合的3种纳米颗粒体系的磁化性质进行了实验研究.在室温下测量了它们的磁化曲线,结果表明ZnFe2O4颗粒是顺磁性的,MnFe2O4及0.8Zn Fe2O40.2MnFe2O4混合颗粒呈超顺磁性.MnFe2O4颗粒的实验曲线和无相互作用的Langevin理论曲线间有较大偏差.混合颗粒体系的磁化强度不等于单独两种颗粒的磁化强度的简单相加.应用偶极子相互作用和颗粒团聚效应解释了MnFe2O4颗粒和混合颗粒体系的磁化性质.     

0.8ZnFe2O4-0.2MnFe2O4纳米颗粒磁化性质的实验研究

对采用化学共沉淀法制备的ZnFe2O4,MnFe2O4以及两者混合的3种纳米颗粒体的磁化性质进行了实验研究．在室温下测量了它们的磁化曲线,结果表明ZnFe2O4颗粒是顺磁性的,MnFe2O4及0.8Zn Fe2O4-0.2MnFe2O4混合颗粒呈超顺磁性．MnFe2O4颗粒的实验曲线和无相互作用的Langevin理论曲线间有较大偏差．混合颗粒体系的磁化强度不等于单独两种颗粒的磁化强度的简单相加．应用偶极子相互作用和颗粒团聚效应解释了MnFe2O4颗粒和混合颗粒体系的磁化性质．     

Multiferroic BaTiO3-CoFe2O4 Nanostructures

We report on the coupling between ferroelectric and magnetic order parameters in a nanostructured BaTiO3-CoFe2O4 ferroelectromagnet. This facilitates the interconversion of energies stored in electric and magnetic fields and plays an important role in many devices, including transducers, field sensors, etc. Such nanostructures were deposited on single-crystal SrTiO3 (001) substrates by pulsed laser deposition from a single Ba-Ti-Co-Fe-oxide target. The films are epitaxial in-plane as well as out-of-plane with self-assembled hexagonal arrays of CoFe2O4 nanopillars embedded in a BaTiO3 matrix. The CoFe2O4 nanopillars have uniform size and average spacing of 20 to 30 nanometers. Temperature-dependent magnetic measurements illustrate the coupling between the two order parameters, which is manifested as a change in magnetization at the ferroelectric Curie temperature. Thermodynamic analyses show that the magnetoelectric coupling in such a nanostructure can be understood on the basis of the strong elastic interactions between the two phases.     

Chemico-Viscous Remanent Magnetization in the Fe3O4-yFe2O3 System

The chemical remanent magnetization (CRM) acquired when single-domain size magnetite (Fe(3)0(4)) oxidizes to maghemite (gammaFe(2)O(3)) in a 50-microtesla field at a series of 13 temperatures from 1000 to 6560C is of similar intensity to viscous remanent magnetization (VRM) acquired under the same field and temperature conditions by unoxidized magnetite. The remanences of the oxidized and unoxidized phases also have similar resistances to demagnetization. These similarities imply that the remanence of the oxidized material is a chemico-viscous remanent magnetization (CVRM) having some of the characteristics of both classic growth CRM and thermally activated VRM. At low temperatures in partially oxidized grains, VRM of the magnetite core and growth CRM of the maghemite surface layer contribute about equally to CVRM. Near the Curie point, intensity of CVRM increases to a Hopkinson-type peak. High-temperature CVRM is more resistant to demagnetization than the thermoremanent magnetization (TRM) produced from cooling through the Curie point.     

COFe2O4-p-NiFe2O4二元离子型磁性液体的制备及其场致光透射驰豫

介绍了CoFe2O4-p-NiFe2O4二元离子型磁性液体的制备方法,用X射线衍射仪、透射电子显微镜、振动样品磁强计分别对NiFe2O4微粒前驱体（p-NiFe2O4）和CoFez04微粒的结构、粒径和磁性进行了测量与分析。研究了CoFe2O4-p-NiFe2O4二元离子型磁性液体在平行于激光照射方向具有不同梯度的外磁场作用下的场致透光的驰豫时间,并从微观结构上分析了产生驰豫时间差异的原因。