THE BOND-ANGLE DEPENDENCE OF THE ASYMMETRY PARAMETER OF THE O-17 ELECTRIC-FIELD GRADIENT TENSOR

被引:28
作者
STERNBERG, U
机构
[1] Friedrich-Schiller-Universität Jena, Institut für Optik und Quantenelektronik, O- 6900 Jena
关键词
ELECTRIC FIELD GRADIENT; ASYMMETRY PARAMETER; O-17; NQR; NMR; BOND ANGLE; ICE POLYMORPHS; SILICATES;
D O I
10.1016/0926-2040(93)90023-G
中图分类号
O64 [物理化学(理论化学)、化学物理学];
学科分类号
070304 ; 081704 ;
摘要
From Primarily geometric starting points, simple formulae for the bond angle dependence of the O-17 quadrupolar asymmetry parameter eta were derived. Expressions for the bond angle dependence of the components of the electric field gradient (EFG) were first derived by Vega. Poplett used these expressions to discuss the O-17 NQR results obtained for the water molecule. The formulae presented in this paper were derived essentially from other starting points and contain only the bond angle of a A-O-17-A oxygen bridge and all details concerning the electron distribution within the bonds will cancel out. Since no assumptions concerning the p-orbital occupancies had to be invoked, these geometric eta formulae are valid for most bridging oxygens. A necessary prerequisite of the eta formulae was that the electron distribution around the oxygen atom under study should exhibit C2v or D2 symmetry. The formulae were applied to explain the data of water molecules in the gaseous state, of various ice polymorphs and of crystal water. As supposed, the theory worked best for the free water molecule because of its perfect C2v symmetry. The differences between experiment and theory for water in solid compounds were mostly smaller than 6%. In the case of silicates and zeolites it was demonstrated that the eta formulae correctly described the experimental trends of the O-17 NMR measurements of these substances. It could be demonstrated that reliable A-O-A-bond angles could be obtained from an eta measurement independent of the bond partner A. Comparing calculated eta values with ab initio calculations of this parameter, the largest difference was observed in the case of a Si-O-Si bond angle near 90-degrees. The eta formulae gave slightly lower eta values than ab initio calculations but the general trends were correctly reflected.
引用
收藏
页码:181 / 190
页数:10
相关论文
共 29 条
  • [1] ACHLAMA M, 1977, CHEM PHYS LETT, V48, P501
  • [2] CRYSTAL-STRUCTURES OF CA-RICH CLINOPYROXENES ON THE CAMGSI2O6-MG2SI2O6 JOIN
    BRUNO, E
    CARBONIN, S
    MOLIN, G
    [J]. TSCHERMAKS MINERALOGISCHE UND PETROGRAPHISCHE MITTEILUNGEN, 1982, 29 (04): : 223 - 240
  • [3] NUCLEAR-QUADRUPOLE RESONANCE OF D-2 AND O-17 IN ICE-II
    EDMONDS, DT
    GOREN, SD
    MACKAY, AL
    WHITE, AAL
    SHERMAN, WF
    [J]. JOURNAL OF MAGNETIC RESONANCE, 1976, 23 (03) : 505 - 514
  • [4] NUCLEAR-QUADRUPOLE RESONANCE OF D-2 AND O-17 IN ICE-V, ICE-VI, ICE-VIII, AND ICE-IX
    EDMONDS, DT
    GOREN, SD
    WHITE, AAL
    SHERMAN, WF
    [J]. JOURNAL OF MAGNETIC RESONANCE, 1977, 27 (01) : 35 - 44
  • [5] CORRECTIONS TO THE O-H BOND LENGTHS AND H-O-H ANGLES OF THE WATER-MOLECULES IN CRYSTALLINE HYDRATES APPLICATION TO BA(CLO3)2.H2O AND K2C2O4H2O
    ERIKSSON, A
    BERGLUND, B
    TEGENFELDT, J
    LINDGREN, J
    [J]. JOURNAL OF MOLECULAR STRUCTURE, 1979, 52 (01) : 107 - 112
  • [6] QUANTIFICATION OF THE DISORDER IN NETWORK-MODIFIED SILICATE-GLASSES
    FARNAN, I
    GRANDINETTI, PJ
    BALTISBERGER, JH
    STEBBINS, JF
    WERNER, U
    EASTMAN, MA
    PINES, A
    [J]. NATURE, 1992, 358 (6381) : 31 - 35
  • [7] HOY AR, 1979, J MOL SPECTROSC, V24, P1
  • [8] PURE NUCLEAR QUADRUPOLE-RESONANCE OF NATURALLY ABUNDANT O-17 IN ORGANIC SOLIDS
    HSIEH, Y
    HAHN, EL
    KOO, JC
    [J]. CHEMICAL PHYSICS LETTERS, 1972, 13 (06) : 563 - &
  • [9] ORDERED PROTON CONFIGURATION IN ICE-II, FROM SINGLE-CRYSTAL NEUTRON DIFFRACTION
    KAMB, B
    HAMILTON, WC
    LAPLACA, SJ
    PRAKASH, A
    [J]. JOURNAL OF CHEMICAL PHYSICS, 1971, 55 (04) : 1934 - +
  • [10] STRUCTURE AND HYDROGEN ORDERING IN ICE-VI, ICE-VII, AND ICE-VIII BY NEUTRON POWDER DIFFRACTION
    KUHS, WF
    FINNEY, JL
    VETTIER, C
    BLISS, DV
    [J]. JOURNAL OF CHEMICAL PHYSICS, 1984, 81 (08) : 3612 - 3623