ON THE NATURE OF MANGANESE IONS IN THE BETA-CA2SIO4 STRUCTURE DETECTED BY HIGH-FIELD ESR

被引:4
|
作者
LUCK, R
STOSSER, R
POLUEKTOV, OG
GRINBERG, OY
LEBEDEV, YS
机构
[1] ZENT INST ANORGAN CHEM,BERLIN,GERMANY
[2] ACAD SCI USSR,INST CHEM PHYS,MOSCOW V-71,USSR
来源
关键词
BETA-DICALCIUM SILICATE; MANGANESE IONS; HIGH FIELD ESR; ESR FINE-STRUCTURE AND HYPERFINE-STRUCTURE TRANSITIONS;
D O I
10.1002/zaac.19926070133
中图分类号
O61 [无机化学];
学科分类号
070301 ; 081704 ;
摘要
The stabilization effect of dopants of the structure of beta-dicalcium silicate using manganese in different oxidation states was investigated in detail by ESR at 3.2 cm (X-band), 8 mm (Q-band) and by high field ESR at 2 mm (W-band). The assignment of the signals was supported by corresponding single crystal measurements using X-Band and Q-band. If there are only low manganese concentrations on forming the microcrystallites the incorporated Mn2+ will be localized on less distorted sites of the lattice. Increasing the manganese concentration the Mn2+ spectra are superimposed by the fine structure of Mn2+ and of Mn4+ ions occupying distorted lattice sites with axial and rhombic symmetry. This pattern of the cation substitution represents the typical transition metal behaviour and obviously favours the formation of regular crystalline units from the melt on compensating of nonequivalent distances and charges.
引用
收藏
页码:183 / 187
页数:5
相关论文
共 50 条
  • [1] STUDIES OF THE STABILITY OF BETA-CA2SIO4 DOPED BY MINOR IONS
    LAI, GC
    NOJIRI, T
    NAKANO, K
    CEMENT AND CONCRETE RESEARCH, 1992, 22 (05) : 743 - 754
  • [2] POLYMORPHISM AND TRANSFORMATION OF BETA-CA2SIO4
    HANIC, F
    KAPRALIK, I
    FIGUS, V
    STRACELSKY, J
    TRANSACTIONS AND JOURNAL OF THE BRITISH CERAMIC SOCIETY, 1983, 82 (06): : 205 - 207
  • [3] KINETICS AND MECHANISM OF HYDRATION OF BETA-CA2SIO4
    DANILOV, VV
    SYCHEV, MM
    KORNEEV, VI
    SAMIGULLINA, GV
    INORGANIC MATERIALS, 1976, 12 (04) : 571 - 576
  • [4] EFFECT OF NA, K AND FE ON THE FORMATION OF ALPHA-CA2SIO4 AND BETA-CA2SIO4
    SUZUKI, K
    ITO, S
    NISHIKAWA, T
    SHINNO, I
    CEMENT AND CONCRETE RESEARCH, 1986, 16 (06) : 885 - 892
  • [5] CALORIMETRIC STUDIES OF BETA-CA2SIO4 HYDRATION IN SOLUTIONS OF ELECTROLYTES
    GAWLICKI, M
    JOURNAL OF THERMAL ANALYSIS, 1995, 45 (04): : 823 - 828
  • [6] Anisotropic thermal expansion of beta-Ca2SiO4 monoclinic crystal
    Fukuda, K
    Maki, I
    Ito, S
    JOURNAL OF THE AMERICAN CERAMIC SOCIETY, 1997, 80 (06) : 1595 - 1598
  • [7] THE CRYSTALLOGRAPHIC ORIENTATION-RELATIONSHIP BETWEEN BETA-CA2SIO4 AND GAMMA-CA2SIO4 DETERMINED BY HRTEM
    EBERHARD, E
    FROHLICH, A
    RAHMAN, SH
    NEUES JAHRBUCH FUR MINERALOGIE-ABHANDLUNGEN, 1991, 163 (01): : 87 - 92
  • [8] LOW-TEMPERATURE SYNTHESIS OF BETA-CA2SIO4 FROM HILLEBRANDITE
    ISHIDA, H
    MABUCHI, K
    SASAKI, K
    MITSUDA, T
    JOURNAL OF THE AMERICAN CERAMIC SOCIETY, 1992, 75 (09) : 2427 - 2432
  • [9] ELECTRON-MICROSCOPIC OBSERVATIONS OF THE PHASE-TRANSITION BETA-CA2SIO4 TO GAMMA-CA2SIO4
    RAHMAN, SH
    FROHLICH, A
    ZEITSCHRIFT FUR KRISTALLOGRAPHIE, 1988, 182 (1-4): : 116 - 118
  • [10] THERMAL-DECOMPOSITION OF CACO3 AND FORMATION OF BETA-CA2SIO4
    GHOSH, SN
    PAUL, AK
    THAKUR, AK
    JOURNAL OF MATERIALS SCIENCE, 1978, 13 (07) : 1602 - 1606