钙钛矿（La1-yTby)0.67Sr0.33MnO3的磁致伸缩效应

采用固相反应烧结法制备了（La_1-yTb_y)_0.67Sr_0.33MnO₃系列样品（y=0,0.05,0.15,0.20,0.25,0.33,0.40,0.50,0.60,1.00).X射线衍射表明,随着y值增大钙钛矿型晶体结构从菱面对称性向正交对称性转变.180K时,μ₀H=7T条件下,在y=0.40样品的巨磁电阻可达900％.μ₀H=1.7T时,y=0.20样品的室温磁致伸缩为-50×10^-6.210K时,y=0.33样品的磁致伸缩可达-130×10^-6. 关键词：     

TbyDy1-y(Fe1-xTx)2(T=Al,Mn)的磁致伸缩与内禀磁致伸缩特性

用直拉单晶生长系统制备Tb_yDy_1-x(Fe_1-xT_x)₂(T=Al,Mn)单晶,并测量其磁致伸缩.用电弧炉合成多晶Tb_yDy_1-y(Fe_1-xT_x)₂(T=Al,Mn),并用X射线衍射方法测量拟合得到内禀磁致伸缩.结果表明,Al和Mn替代后饱和磁场降低,说明Al和Mn的替代明显地降低了各向异性能.随Al和Mn替代量的增加,总的趋势是材料的内禀磁致伸缩λ₁₁₁降低.对Tb_0.5Dy_0.5(Fe_0.9Mn_0.1)₂单晶,在不加压情况下的磁致伸缩效果并不明显,但当施加压力时,磁致伸缩变化显著,尤其在12—26MPa压力下,磁致伸缩变化很大,且低场效果很好. 关键词：     

熔体快淬Pr(Fe1-xCox)2合金的结构和磁性

通过熔体快淬方法获得Pr(Fe_1-xCo_x)₂合金条带,经过X射线衍射、差示扫描量热计和磁性测量对其结构、磁性和热稳定性进行了研究.发现当Co的含量x大于0.2时才可能获得Pr(Fe,Co)₂立方Laves相化合物.对Pr(Fe_0.6Co_0.4)₂合金,在快淬速度为30m/s时,条带由Pr₂(Fe,Co)₁₇,Pr(Fe,Co)₂和富稀土相组成;在速度为40m/s时,获得了几乎单相的Pr(Fe_0.6Co_0.4)₂化合物,其居里温度为305℃;在速度为45m/s时,除了Pr(Fe_0.6Co_0.4)₂化合物外,还存在少量的非晶相.Pr(Fe_0.6Co_0.4)₂化合物在770℃以上发生分解.用40m/s快淬纳米晶粉胶粘磁体有大的磁致伸缩系数（λ_∥-λ_⊥=140×10^-6)和高的硬磁性能（_iH_c=398kA/m). 关键词：     

K0.5Na0.5NbO3-LiSbO3-BiFeO3/CuFe2O4复合陶瓷的制备与磁电性能研究

采用传统的固相法制备了(1-x)(K_0.5Na_0.5NbO₃-LiSbO₃-BiFeO₃)-xCuFe₂O₄ (x=0.1, 0.2, 0.3, 0.4) 磁电复合陶瓷, 并借助X射线衍射仪、扫描电镜和磁电耦合系数测试仪等对复合陶瓷的微结构和性能进行了分析. 结果表明, 复合陶瓷的K_0.5Na_0.5NbO₃-LiSbO₃-BiFeO₃和CuFe₂O₄物相之间发生了一定的离子相互扩散作用, 且两相的颗粒大小匹配性较好. 随着CuFe₂O₄含量增加, 复合陶瓷的压电系数从130 pC/N减小到30 pC/N, 饱和磁致伸缩系数从4.5×10^-6增加到12.4×10^-6左右, 磁电耦合系数表现出先增加后减小, 在x=0.3时获得最大的磁电耦合系数9.4 mV·cm^-1·Oe^-1. 关键词： 0.5Na_0.5NbO₃-LiSbO₃-BiFeO₃')" href="#">K_0.5Na_0.5NbO₃-LiSbO₃-BiFeO₃ 2O₄')" href="#">CuFe₂O₄ 磁电耦合     

Mn替代对Dy2AlFe16－xMnx化合物的结构和磁性的影响

通过X射线衍射及磁测量手段研究了Dy₂AlFe_16-xMn_x化 合物的结构和磁性.研究结果表明Dy₂AlFe_16-xMn_x化合 物具有六角相的Th₂Ni₁₇型结构.对x=1，2的样品采用X射线热膨胀 测定法在104—647K的温度范围内测量了其热膨胀性质，发现这些化合物在低温下存在热膨 胀反常现象，在居里点附近出现负膨胀性质.对自发磁致伸缩的研究结果表明Dy₂AlFe_16-xMn_x化合物中存在着较强的各向异性的自发磁致伸缩，随 着Mn含量的增加，其低温下的自发体磁致伸缩减弱.磁测量结果表明Mn的替代导致Dy_{2< /sub>AlFe16-xMnx化合物的居里温度及自发磁化强度急剧下降. 关键词： 2}AlFe_16-xMn_x化合物')" href="#">Dy₂AlFe_16-xMn_x化合物 反常热膨胀 自发磁致伸缩 自发磁化强度     

离轴磁场退火后Tb0.3Dy0.7Fe1.95〈110〉取向晶体的磁致伸缩"跳跃"效应

将〈110〉取向Tb_0.3Dy_0.7Fe_1.95合金棒放在与轴向成35°夹角的外磁场中退火处理,研究其在0—30 MPa预压应力σpre作用下的磁致伸缩效应.结果表明,σpre=0条件下的饱和磁致伸缩值λs由退火前的1023×10^-6提高到1650×10^-6;σpre 关键词： 磁致伸缩 磁场退火 磁致伸缩"跳跃"效应     

H2O2氧化法制备Fe3O4纳米颗粒及与共沉淀法制备该样品的比较

在近中性条件下，利用H₂Ｏ₂氧化Fe(OH)2胶体成功制备了Fe₃ Ｏ₄纳米颗粒.分别利用透射电镜(TEM)，x射线衍射仪(XRD)，振动样品磁强计(VSM)和超导量子干涉仪（SQUI D）对样品的形貌，结构，宏观磁性进行了表征和测量.TEM图像表明样品为球形颗粒，直径 大小约18nm，且分布较均匀.XRD结果表明样品为立方尖晶石结构.穆斯堡尔谱测量表明样品 室温下对应两套六线谱，样品的晶体结构存在缺陷，内磁场略小于块体Fe₃Ｏ4的值. 宏观磁测量表明样品的饱和磁化强度可达67×10^-3A·m²/g，在20 K出现了Verw ey转变.选择该法制备的Fe₃Ｏ₄纳米颗粒与共沉淀法得到的样品作 了磁性比较.宏观磁 测量表明共沉淀法制备的样品在外磁场为1T时仍未饱和，磁化强度仅为46×10^-3A·m²/g，在178K出现了超顺磁转变温度，且在测量温度范围内没有发现Verwe y转变. 关键词： 亚铁磁 超顺磁 穆斯堡尔谱     

Si-Al2O3复合薄膜的室温铁磁性

在Si-Al₂O₃复合薄膜中观察到室温铁磁性.Si的体积百分比为15 %的Si-Al₂O₃复合薄膜的磁性最强.Si的含量影响样品的磁有序,在样品中观察到了明显的磁畴.在不同气氛下,对样品进行快速热退火.退火样品的磁性测试结果的差别表明氧空位不是样品铁磁性的主要来源.我们认为铁磁性来源于Si与Al₂O₃基质界面之间的缺陷的磁耦合.改变Si的含量可以改变缺陷密度,从而控制铁磁耦合强度. 关键词： 2O₃薄膜')" href="#">Al₂O₃薄膜 室温铁磁性 掺杂 交换相互作用     

混合场中 (Pr1－yNdy)2/3Sr1/3MnO3体系磁转变行为研究

对(Pr1-yNdy)2/3Sr1/3MnO3(y=2/8,4/8,6/8)体系在42K—300K温度范围内混合场（即交流驱动场Hac与附加直流磁场H dc的叠加）下的磁转变行为进行了系统的实验研究. 结果表明，随着外加直流磁场强 度的增大，样品的直流磁化强度增大，交流磁化率逐渐减小；在混合场作用下，磁转变温度 （居里温度）附近样品交流磁化率的实部出现一个特征的尖峰. 对于(Pr1-yNdy)2/3Sr1/3MnO3体系，随着Nd掺杂量的增加，交流磁化率实部 的相对变化 (Eχ′=Δχ′/χ′dc)的峰值对应的温度降低，这一点与该系 统的磁电阻的变化规律一致. 对锰氧化物体系在混合场中的磁转变现象进行了讨论. 关键词： 锰氧化物 混合场 磁特性     

甩带Fe85Ga15合金的巨磁致伸缩研究

利用甩带快淬方法制备了Fe₈₅Ga₁₅合金样品.测量了样品在沿带片长度方向和厚度方向上的磁致伸缩，发现其值分别高达－1300ppm和＋1100ppm.巨大磁致伸 缩的获得来源于甩带样品的形状各向异性和合金内部生成的大量短程应变有序以及它们的择优取向.样 品温度特性的测量表明，在室温附近约60℃宽的温度范围，合金的磁致伸缩数值基本保持不 变；而在高温条件下，合金具有更大的磁致伸缩. 关键词： 磁致伸缩 Fe-Ga合金 甩带快淬     

Anomalous magnetostrictive effects in （La1—xTbx）2／3Sr1／3 MnO3

A series of (La_{1-x}Tb_x)_{2/3}Sr_{1/3}MnO_3 polycrystalline samples has been studied by means of x-ray diffraction, magnetostriction, and thermal expansion measurements. It has been found that this series undergoes a phase transition from a rhombohedral to an orthorhombic form at the doping level x≈0.20 at room temperature accompanied by an anisotropic magnetostriction up to －50×10^{-6} under a magnetic field of 1T. The linear and volume magnetostrictions vary with chemical composition, even change sign. At T=80K, the magnetostrictions for the samples of x=0.20 and 0.40 exhibit different behaviours. The sample of x=0.20 has positive volume and linear magnetostrictions and a negative anisotropic magnetostriction, while the sample of x=0.40 has an opposite behaviour. The magnitude of volume magnetostriction for both the samples is essential (～10^{-4}) at T=80K under a magnetic field of 4T. We conclude that these anomalous effects are due to the charge delocalization and the structural phase transition between orthorhombic and rhombohedral forms induced by the applied magnetic field.     

Irreversible magnetovolume effect in Nd7Rh3 single crystal

Magnetovolume effect in Nd₇Rh₃ single crystal has been studied by measuring the magnetostriction as a function of external magnetic field at 4.2 K. An irreversible magnetovolume effect having a negative remanent volume magnetostriction was observed when the external magnetic field was applied along the b-axis. The irreversible magnetostrictive effect takes place in the longitudinal magnetostriction along the b-axis. The remanent magnetostriction along the b-axis relaxes after removing external magnetic field for several hours and equilibrium state is stabilized.     

稀土掺杂La-Sr-Mn-O的室温磁致伸缩效应

采用两种不同的方法制备了不同稀土含量的(La_1-xR_x)_2/3Sr_1/3MnO₃(R=Sm,Tb)大块多晶样品,并研究了它们的晶体结构及室温下的磁致伸缩效应.分析表明,随Sm,Tb对La的替代,样品的晶体结构从菱面体相转变为正交相.在结构相转变点附近,样品在室温下的磁致伸缩效应出现极大值.样品在室温下的磁致伸缩主要来源于材料中的交换磁致伸缩. 关键词：     

过渡族元素掺杂BaTiO3-Tb1-xDyxFe2-y层状复合材料中的磁电效应

用溶胶-凝胶法制备1.0%mol Mn,Cr,Co掺杂 BaTiO₃(BTO)粉体,在1350℃下烧结成多晶陶瓷样品.X射线衍射和差示扫描量热分析表明,室温下掺杂BaTiO₃具有四方钙钛矿结构;居里点和相变潜热随Cr,Mn,Co掺杂逐渐降低.将掺杂BaTiO₃与Tb_1-xDy_xFe_2-y(TDF)胶合制成双层磁电复合材料,并研究了Cr:BTO-TDF,Mn∶BTO-TDF,Co:BTO-TDF层状复合材料中的磁电效应.实验表明,在340×80 A·m^-1偏置磁场下, Cr:BTO-TDF的横向磁电电压系数达到最大值586 mV·cm^-1·(80 A·m^-1)^-1.在400×80 A·m^-1偏置磁场下,Mn∶BTO-TDF和Co:BTO-TDF的横向磁电电压系数的最大值分别为480 mV·cm^-1·(80 A·m^-1)^-1和445mV·cm^-1·(80 A·m^-1)^-1.研究表明掺杂BaTiO₃-TDF层状复合材料中具有较强的磁电耦合.作为无铅压电材料,掺杂BaTiO₃制备的磁电效应器件颇具应用前景. 关键词： 磁电效应 双层复合材料 3')" href="#">掺杂BaTiO₃ 1-xDy_xFe_2-y')" href="#">Tb_1-xDy_xFe_2-y     

In替代(La2/3Ca1/3)(Mn(3-2x)/3In2x/3)O3体系巨磁电阻效应的研究

采用固态反应法制备了In替代的(La_2/3Ca_1/3)(Mn_(3-2x)/3In_2x/3)O₃(x=0.00，0.10，0.15)体系.通过测量其零场和1.6T磁场下样品的电阻-温度关系以及一定温度下磁电阻率与磁场的关系.发现随In³⁺替代量的增加其磁电阻峰和电阻峰均向低温方向移动，同时巨磁电阻效应减弱，磁电阻峰也展宽.这是由于In³⁺替代量的变化，引起 关键词：     

Reinvestigation of the magnetic structure of Ca3Mn2Ge3O12

Precise neutron diffraction experiments performed on powdered antiferromagnetic garnet Ca₃Mn₂Ge₃O₁₂ lead to a complex non collinear magnetic structure. In the absence of magnetic field, it is three dimensional with eight spin directions and belongs to ¹I_41/a. At a critical magnetic field spin-flop mechanism occurs with a lowering of the magnetic symmetry which becomes triclinic. In addition to tetragonal anisotropy, both single ion orthorhombic anisotropy and its antisymmetrical counterpart for definite pairs of ions are required to explain both the observed structure and its behaviour in a magnetic field.     

Magnetism in a UNi2/3Rh1/3Al single crystal

We report a magnetization, magnetostriction, electrical resistivity, specific heat and neutron scattering study of a UNi_2/3Rh_1/3Al single crystal, a solid solution of an antiferromagnet UNiAl and a ferromagnet URhAl. The huge uniaxial magnetic anisotropy confining the principal magnetic response to the c axis in the parent compounds persists also for the solid solution. The magnetization curve at 1.6 K has a pronounced S shape with an inflection at 12 T. The temperature dependence of magnetic susceptibility exhibits a maximum around 10 K and is magnetic history dependent at lower temperatures where the resistivity increases linearly with decreasing temperature. The low-temperature ρ(T) anomaly is removed in a magnetic field applied along c, which yields a large negative magnetoresistance amounting to m46 zin 14T (at 2 K). The C/T values exhibit a minimum around 12 K and below 8 K they become nearly constant (about 250 mJ mol^?1 K^?2), which is strongly affected by magnetic fields. Neutron scattering data confirm a non-magnetic ground state of UNi_2/3Rh_1/3Al. The bulk properties at low temperatures are tentatively attributed to the freezing of U magnetic moments with antiferromagnetic correlations. The additional intensities detected on top of nuclear reflections in neutron diffraction in a magnetic field applied along c are found to be proportional to the field-induced magnetization, which reflects field-induced ferromagnetic coupling of U magnetic moments. This scenario is corroborated also by finding low-temperature magnetostriction data that also scale with the square of magnetization.     

Magnetostriction in the rare-earth ferroborates RFe3(BO3)4, R=Pr and Tb

Recent experimental data for magnetostriction in the rare-earth (RE) ferroborates RFe₃(BO₃)₄ with R=Pr and Tb are discussed from a theoretical point of view. Multipole moments of RE ions are calculated in the framework of a crystal-field model for the RE ion and the molecular-field approximation. Quadrupole approximation is shown to be sufficient for interpretation of data for longitudinal magnetostriction at the magnetic field along the trigonal axis. Parameters of PrFe₃(BO₃)₄ are deduced when accounting for the experimental magnetization curves that manifest a spin-flop transition.     

Magnetostriction relative to pretransition in Ni50.5Mn24.5Ga25 single crystal

The strain behaviors as well as the structural and magnetic changes relative to the pretransition in the Ni_50.5Mn_24.5Ga₂₅ single crystals have been characterized by various methods, such as pretransition strain, magnetostriction, magnetization measurements, and TEM observations. A large magnetostriction up to 505 ppm measured in the [001] direction of the sample is obtained at the pretransition temperature with only a low magnetic field of about 1 kOe applied along the [010] direction. We found that not only the pretransition strain pronounces a more large change, but also the magnetostriction at a certain temperature exhibits a more large magnitude for field applied along the [010] direction than with field along the [001] direction. It is concluded that the magnetoelastic interaction is responsible for the premartensitic transition, and the magnetoelastic interaction in the [010] direction is stronger than that in the [001] direction.