BeAl2O4:Cr3+的能谱及R1和R2线压力移位的理论计算

采用强场方案和三角基,通过对角化三角畸变立方场的d3电子组态完全能量矩阵,拟合得到BeAl2O4:Cr3+的能谱和波函数.利用获得的波函数,计算出了基态g因子和R1 、R2线能谱压致移位值,计算值和实验结果相符合.各参数对能级压力移位率的影响也被定量计算,揭示了R1和R2线压力移位的物理起源.     

可调谐激光晶体GSGG∶Cr3+在低温下光谱压致移位的理论研究

采用单组态坐标模型,应用由对角化d3能量矩阵而获得的波函数,同时考虑了自旋-轨道相互作用和电-声子耦合,并定量计入了4T2与2T1各电子态对R线的影响以及局域压缩率和整体压缩率之间的差异,从微观的角度,研究了GSGG∶Cr3+低温下光谱结构的特点以及压力导致的R1线和4T2宽带的移位.理论计算的结果与实验符合较好,R线的常压位置及其分裂、R1线的压致移位及其"反转"现象和4T2宽带的压致移位都得到了合理的解释.     

KAl(MoO4)2晶体中掺杂Cr3+的能谱和g因子的理论计算*

采用强场方案和三角基，通过对角化三角畸变的立方晶场下的d3 完全能量矩阵，计算出了KAl(MoO4)2:Cr3+ 的能谱和波函数。使用对角化完全能量矩阵所获得的波函数，进一步计算了KAl(MoO4)2:Cr3+ 的基态g 因子。计算结果与光谱，EPR谱实验数据很好地符合。研究表明,利用对角化完全能量矩阵获得的波函数对 g 因子所作的计算为整个理论计算及波函数的归属提供了重要判据,充分体现了将能谱和g 因子作统一计算的重要性和必要性.     

YGG:Cr3+低温常压下的能谱和g因子的理论计算

采用对角化由强场方案和无耦合的三角基建立的三角畸变八面体场中的d3离子完全能量矩阵,对YGG:Cr3+在低温常压下的能谱及波函数进行了拟合计算,并分析了各参数对部分能级的影响,定量地显示了能级分裂的影响因素.同时,使用对角化完全能量矩阵所获得的基态波函数,进一步计算了YGG:Cr3+的基态g因子.各项计算结果均与实验符合很好.     

MgO:Cr3+和MgO:V2+的能谱随温度移位的拟合计算

全面计入电-声子耦合导致的热移位(其中包括~2T_1贡献的单声子项,Raman项,光学支项)与热膨胀导致的热移位,对MgO:Cr~(3+)与MgO:V~(1+)的R线热移位作了理论计算,结果与热移位、热膨胀系数,高压移位、声子谱与光谱、晶体密度、弹性常数与晶格常数等大量实验数据符合得很好.进而,将完全的d~3能量矩阵对角化,得到能谱与波函数,再通过电-声子相互作用矩阵元等一系列计算,从微观上算出单声子项的参量,结果与拟合实验得到的值符合得很好.结果表明:单声子项起主导作用(导致红移),而Raman项(导致 关键词：     

YGG:Cr3+低温常压下的能谱及g因子理论计算

采用对角化由强场方案和无耦合的三角基建立的三角畸变八面体场中的d3离子完全能量矩阵,对YGG:Cr3+在低温常压下的能谱及波函数进行了拟合计算,并分析了各参数对部分能级的影响,定量地显示了能级分裂的影响因素。同时,使用对角化完全能量矩阵所获得的基态波函数,进一步计算了YGG:Cr3+的基态g因子。各项计算结果均与实验符合很好。     

LiNbO_3:Ni~(2+)的常压能谱和g因子

采用强场方案,通过将d8完全能量矩阵对角化,统一计算了LiNbO3:Ni2+的常压能谱和g因子,计算结果与大量实验数据符合很好.给出了各个能级对不同参量的变化率.研究表明,利用对角化完全能量矩阵获得的波函数对g因子所作的计算为整个理论计算及波函数的归属提供了重要判据,充分体现了将能谱和g因子作统一计算的重要性和必要性. 关键词： 晶场 能谱 g因子     

LaAlO3: Cr3+低温常压下的能谱和顺磁 g 因子的统一解释

利用配位场理论,在强场方案下,建立了包括立方晶场、库仑相互作用、自旋-轨道耦合、低对称场的d³完全能量矩阵,对LaAlO₃：Cr³⁺在低温常压下的能谱进行了拟合,确定了相应的参量,得到了与实验值比较相符的能谱,并利用所得的波函数计算了LaAlO₃：Cr³⁺基态的 g 因子,与实验结果相吻合. 根据所得参量分析了Cr³⁺与配位体之间相互作用的特性.     

Paul阱中两个Bi+共线的能量本征态性质

通过对Paul阱中共线两Bi 形成的系统波函数、能谱和相对距离的平均值的精确计算,计算得到的频率、能量是目前的离子阱实验能达到的值;并且对共线两个Bi 的相对几率分布和系统能量本征态进行分析.     

两体自旋轨道耦合力与f7/2壳层能谱

本文采用中心力加两体自旋轨道耦合力作为剩余相互作用,计算了 f_7/2壳层原子核的能谱.交换参数可调.径向波函数采用谐振子波函数.计算值和实验值的符合程度令人满意.因而表明在剩余相互作用中,两体自旋轨道相互作用的影响不可忽视.     

Energy Spectra,g Factors and Their Pressure—induced and ／or Thermal Shifts of SrTiO3：Cr^3＋ and SrTiO3：Mn^4＋ Ⅱ：Pressure Effects on Ground_State g Factor and Splittings of t2^32E and t2^34A2 of Sr

By using the wavefunctions obtained from diagonalizing the complete d^3 energy matrix at normal and various pressures,the g factor of the ground state of SrTiO3:Cr^3 and its pressure-induced shift have been microscopically calculated.Only by taking the local strains around Cr^3 in SrTiO3:Cr^3 (which are about twice the bulk ones)and corresponding P-χ dependence,can we obtain a good agreement etween the calculated result of pressure-induced shift of ground-state g factor and the experimental one.The physical origins of this pressure-induced shift have been explained.It is found that the change of Dq^-1 with pressure makes main contribution to the pressure-induced shift of ground-state g factor of SrTiO3:Cr^3 .By using the wavefunctions obtained from diagonalizing the complete d^3 energy matrix at normal pressure,the relevant matrix elements and accordingly strain-induced splittings of t2^32E and t2^34A2 of SrTiO3:Cr^3 have been calculated.The important results of Yc.Zc,Pc and Qc have also been evaluated.It is the admixtures of basic wavefunctions resulted from the spin-orbit interaction and /or Coulomb interaction and /or Kramers degeneracy that make the strain-induced splittings of the levels nonzero.It is found that there are nonvanishing matrix elements of operators T2ξ between wavefuncgtions with positive Ms and those with negative Ms′ and those with negative ms′,which have important effects on the strain-induced splittings of the levels.     

Energy Spectrum and g Factor of MgO:Cr3+ and Their Pressure-Induced Shifts

The unified calculation of the whole energy spectrum and g factor of the ground state for MgO:Cr³⁺ at normal pressure and their pressure-induced shifts has been carried out on the basis of the theory of pressure-induced shifts and the diagonalization of the complete d³ energy matrix in a regular octahedral field. All the calculated results are in very good agreement with a lot of experimental data. For the first time, by using the wavefunctions obtained by diagonalization of the complete energy matrix, the pressure-induced shifts of g factor have satisfactorily been calculated and explained by microscopic theory. The rates of change of levels with respect to various parameters and the contributions to levels from various parameters have been calculated. The distinct differences in magnitude and/or sign of pressure-induced shifts of various levels are immediately determined by their characteristic dependencies on the parameters of interactions. The pressure-induced shifts of levels and g factor have provided important criteria for the correctness of the calculations and assignments of the energy spectrum and wavefunctions, and it is quite necessary and important to carry out the unified calculation of the whole energy spectrum and g factor at normal pressure and their pressure-induced shifts.     

Theoretical Calculation of Energy Spectrum of YGG：Cr^3＋ and Thermal Shifts of Its R-Lines

With the strong-field scheme and trigonal bases, the complete d3 energy matrix in a trigonally distorted cubic-field has been constructed. By diagonalizing this matrix, the energy spectrum of YGG：Cr^3＋ at normal pressure and low temperature has been calculated. The g factor of the ground-state has been evaluated in terms of the energy spectrum. At the same time, by using the wavefunctions obtained from diagonalizing the complete d^3 energy matrix and Thermal Shifts theory, we calculate the thermal shifts of the sharp lines of YGG：Cr^3＋ and determine the relevant parameters. The calculated results are all in good agreement with the optical-spectrum and EPR experimental data. It is demonstrated that the obtained wavefunctions and the values of parameters are reasonable.     

Theoretical Calculations of Strain—Induced Splittings and／or Shifts of t2^32E and t2^34A2 Levels for MgO：Cr^3＋

Under various uniaxial stresses, both strains with low symmetry and isotropic strains of crystals take place. The former gives the strain-induced low-symmetry crystal fields and accordingly splittings of levels; the latter gives the isotropic parts of strain-induced crystal fields and accordingly shifts of levels. By using the wavefunctions obtained from the diagonalization of the complete d^3$ energy matrix in a regular octahedral field, the relevant matrix elements and accordingly strain-induced splittings and/or shifts of t₂³²E and t₂³⁴A₂ for MgO:Cr³⁺ have been calculated. Their physical origins have been thoroughly analyzed and revealed. It is the admixtures of basic wavefunctions resulted from the spin-orbit interaction and/or Coulomb interaction and/or Kramers degeneracy that make strain-induced splittings of levels nonzero. In contrast with this, strain-induced shifts come mainly from the zero-order approximate wavefunctions. It is found that there are nonvanishing matrix elements of operators T₂ξ, T₂η and T₂ζ between wavefunctions with positive M_s and those with negative M_s', which have important effects on strain-induced splittings of levels. The shifts of t₂³²E under both hydrostatic pressure and uniaxial pressure have been uniformly calculated. The important results of Y_c, Z_c, P_c, Q_c and 〈t₂|| C(A₁)|| t₂〉have been evaluated.     

Theoretical Studies of Energy Spectra and g Factors of Cr3+-Doped YAl3(BO3)4

With the strong-field scheme and trigonal bases, by diagonalizing the complete d³ energy matrix in a trigonally distorted cubic-field, the energy spectra and wavefunctions of YAl₃(BO₃)₄:Cr³⁺ have been calculated. The rates of change of levels with respect to various parameters and the contributions to levels from various parameters are calculated, and the physical origins of various levels or splittings have been clearly and quantitatively shown. By using the wavefunctions obtained from diagonalizing the complete energy matrix, the g factors of the ground state of YAl₃(BO₃)₄:Cr³⁺ have been evaluated. The calculated results are in good agreement with the optical-spectral and EPR experimental data. It is demonstrated that the bonding between Cr³⁺ and ligands (O^2-) is ionic.     

Thermal Shift Calculations (Ⅱ): The Theoretical Calculation of R Line Thermal Shift of MgO:Cr3+

By making use of the theory for thermal shift of crystal field spectra of rare earth or transition metalions, taking into account all the contributions adequately, we calculated R line thermal shift of MgO:Cr³⁺ by fitting experimental data. The results show a good agreement with thermal shift experimental data and a series of other experimental data of MgO:Cr³⁺. Values of the most important parameters are calculated theoretically with wavefunctions obtained from diagonalization of complete d³ energy matrices. They are in good agreement with those from fitting experimental data.     

Complete Ligand-Field Calculations of Energy Spectrum and g Factor of CaO:Ni2+ and Their Pressure-Induced Shifts

The calculations of the whole energy spectrum and the g factor of the ground state for CaO:Ni²⁺ at ,normal pressure and their pressure-induced shifts have been carried out on the basis of the theory of pressure-induced shifts and the diagonalization of the complete d⁸ energy matrix in a regular octahedral field. The calculated results are in very good agreement with experimental data. The physical essentials of the pressure-induced shifts of typical levels and g factor for the ground state have been revealed by using the wavefunctions and energy spectra at various pressures.     

Complete Ligand-Field Calculation of Energy Spectrum and g Factor of MgO:Ni2+ and Their Pressure Effects

The unified calculation of the whole energy spectrum and g factor of ground state for MgO:Ni²⁺ at normal pressure and their pressure-induced shifts has been carried out on the basis of the theory of pressure-induced shifts and the diagonalization of the complete d⁸ energy matrix in a regular octahedral field. A11 the calculated results are in excellent agreement with a lot of experimental data. For the first time, by using the wavefunctions obtained by diagonalization of the complete energy matrix, the pressure-induced shift-of g factor has satisfactorily been calculated and explained by microscopic theory The contributions to typical levels from various parameters have been calculated. The distinct differences of pressure-induced shifts of various levels are immediately determined by their characteristic dependencies on the parameters of interactions. The pressure-induced shifts of levels have provided important criteria for the correctness of the calcutation and assignment of them.