(Fe1-xNix)2P电子结构与磁学特性的X射线近边吸收谱研究

利用X射线近边吸收谱对Fe₂P,Ni₂P及其掺杂物(Fe_1-xNi_x)₂P(x=01,025,05)中Fe,Ni,P的K边进行了研究.结合多重散射理论近边计算,讨论了金属原子不同位置格点3f,3g对近边谱特征的贡献,得出当Ni原子取代Fe原子时将优先占据Fe(3f)格点位置;根据第一性原理对能态的计算发现,不考虑磁性时不同格点P的pDOS未占据态电子结构与P-K近边吸收谱实验相符合;与考虑铁磁性Fe₂P 的DOS相比较后结果显示Fe₂P的磁性主要来源于Fe(3g)格点,铁磁性Ni₂P计算的Ni不同格点原子磁矩均接近于0,与它一般显顺磁性结论相一致. 关键词： X射线近边吸收谱 电子结构 多重散射理论 态密度     

High pressure X-ray diffraction study of SrMnO3 perovskite

Using a diamond anvil cell device and synchrotron radiation, the in-situ high-pressure structure of SrMnO₃ has been investigated. At pressure up to 28.6 GPa, no pressure-induced phase transition is observed. The lattice parameters as a function of pressure is reported, and the relationship of the axial compression coefficients is β_a>β_c. The isothermal bulk modulus K₂₉₈=266(4) GPa is also obtained by fitting the pressure-volume data using the Murnaghan equation of state.     

Quasi-hydrostatic Limit of LiF as a Pressure Transmitting Medium and Its Equation of States

Quasihydrostatic limit of LiF as a pressure transmitting medium is investigated by synchrotron radiation x-ray diffraction combined with the diamond anvil cells technique up to 60 GPa at room temperature. The equation-of- state parameters of LiF are determined to be Vo = 65.7（2）A3 Bo = 58（3） GPa and B＇0 = 4.9（2） in the silicon oil environment; Vo = 67.4（3） A3, Bo = 51（3） GPa and B＇0 = 4.7（2） without pressure transmitting medium. The full width at half maximum of LiF （111） peak increases with the increase of pressure in two independent experiments. The pressure distribution in the sample chamber is estimated by line-scanning x-ray diffraction measurements across the chamber＇s center, which presents as homogeneous with Pmax - Pmin Of about 1 GPa below 40 GPa.     

In situ high-pressure X-ray diffraction experiments and ab initio calculations of Co2P

In situ high-pressure experiments of Co2P are carried out by means of angle dispersive X-ray diffraction with diamond anvil cell technique. No phase transition is observed in the present pressure range up to 15 GPa at room temperature, even at high temperature and 15 GPa. Results of compression for Co2P are well presented by the second-order Birch-Murnaghan equation of state with V0 = 130.99(2)3 (1=0.1 nm) and K0 = 160(3) GPa. Axial compressibilities are described by compressional modulus of the axis: Ka = 123(2) GPa, Kb = 167(8) GPa and Kc = 220(7) GPa. Theoretical calculations further support the experimental results and indicate that C23-type Co2P is stable at high pressure compared with the C22-type phase.     

Pr1-x Srx MnO3体系中O1s2p2p俄歇过程特性研究

对于组份为x=0.0和x=0.3的巨磁电阻锰氧化物Pr_1-x Sr_x MnO₃(PSMO)体系在OK阈值,Mn L_2,3边的区域内进行了O1s2p2p俄歇谱随光子能量变化的实验研究.实验结果显示O1s2p2p俄歇峰发生分裂并且可将其拟合为3个子峰.PSMO在OK阈值或Mn L_2,3边以下进行激发时,其俄歇峰3个子峰的相对强度基本保持恒定,然而反映终态效应特性的总强度却有起伏发生.这一状况在Mn L_2,3边以上激发时表现更为显著,即组份为x=0.3的总强度为x=0.0的4倍.对这些现象在共价键图     

aodSrTi1-xRuxO3系列类钙钛矿结构氧化物的电子结构研究

利用同步辐射光电子能谱技术研究SrTi_1-xRu_xO₃系列类钙钛矿结构氧化物的电子结构. 通过测量该系列氧化物的光电子能谱(PES)和X射线吸收谱(XAS),得到了SrRuO₃在入射能量53eV时的共振光电子能谱(RPES),SrTi_1-xRu_xO₃中,随着x变化而变化的价带光电子能谱和O 1s的吸收谱.然后参照文献中局部密度近似方法(LDA)模拟计算的能带结构,进行初步的分析和解释.     

天然橄榄石单晶的压缩性北大核心CSCD

采用金刚石对顶砧高压装置和同步辐射X射线衍射技术,在常温下对两种天然橄榄石单晶(含铁的铁镁橄榄石(Mg_(1.83)Fe_(0.17))SiO_4和不含铁的纯镁橄榄石Mg_2SiO_4)进行了高压结构行为研究。实验结果表明,两种天然橄榄石单晶在最高压力为9.9GPa的条件下没有发生相变。采用二阶Birch-Murnaghan状态方程描述压力-晶胞体积(p-V)关系,获得了铁镁橄榄石和纯镁橄榄石在零压下的晶胞体积(0.292 9(3)、0.289 9(1)nm^3)和体积模量(140(3)、151(2)GPa)。两种镁橄榄石呈高度各向异性,轴压缩性表现为:b轴的压缩率最大,c轴次之,a轴的压缩率最小。随着铁组分的加入,橄榄石的体波速减小,两种橄榄石的体波速相差5.2%,该结果对于研究上地幔的物质构成和弹性波速具有一定的意义。     

Pressure-induced phase transition of B-type Y_2O_3

The synthesized monoclinic(B-type) phase of Y_2O_3 has been investigated by in situ angle-dispersive x-ray diffraction in a diamond anvil cell up to 44 GPa at room temperature. A phase transition occurs from monoclinic(B-type) to hexagonal(A-type) phase at 23.5 GPa and these two phases coexist even at the highest pressure. Parameters of isothermal equation of state are V_0= 69.0(1) ~3, K_0= 159(3) GPa, K_0= 4(fixed) for the B-type phase and V_0= 67.8(2) ~3, K_0= 156(3) GPa,K'_0= 4(fixed) for the A-type phase. The structural anisotropy increases with increasing pressure for both phases.     

钙钛矿型(Pbnm)化合物在高压下的结构变化

ABX₃型钙钛矿,最常见的结构为斜方晶系Pbnm,在高压下的结构变化具有多样性.本文简要介绍了3个参量(t,V_A/V_B,E_tot),描述ABX₃型钙钛矿结构的稳定性,全面总结了应用这3个参量建立的高压下钙钛矿结构(Pbnm)变化模型,基中有些模型对所有的钙钛矿结构都适合.通过举例,运用不同的模型对CaTiO₃(Pbnm)在高压下的结构变化进行综合分析,定性地得出随着压力的增加其结构的对称性应降低.     

(Fe1-xNix)2P电子结构与磁学特性的X射线近边吸收谱研究

利用X射线近边吸收谱对Fe2P,Ni2P及其掺杂物(Fe1-xNix)2P(x=0.1,0.25,0.5)中Fe,Ni,P的K边进行了研究.结合多重散射理论近边计算,讨论了金属原子不同位置格点3f,3g对近边谱特征的贡献,得出当Ni原子取代Fe原子时将优先占据Fe(3f)格点位置;根据第一性原理对能态的计算发现,不考虑磁性时不同格点P的pDOS未占据态电子结构与P-K近边吸收谱实验相符合;与考虑铁磁性Fe2P的DOS相比较后结果显示Fe2P的磁性主要来源于Fe(3g)格点,铁磁性Ni2P计算的Ni不同格点原子磁矩均接近于0,与它一般显顺磁性结论相一致.