Sodium mobility in the NASICON series Na1+xZr2-xInx(PO4)3

被引:62
作者
Losilla, ER
Aranda, MAG
Bruque, S [1 ]
Sanz, J
París, MA
Campo, J
West, AR
机构
[1] Univ Malaga, Dept Quim Inorgan Cristalog & Mineral, Malaga 29071, Spain
[2] CSIC, Inst Ciencia Mat, E-28049 Madrid, Spain
关键词
D O I
10.1021/cm000122q
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
Rhombohedral Na1+xZr2-xInx(PO4)(3) (x = 0, 0.2, 0.4, 0.8, 1.0, 1.2, 1.6, and 1.8) NASICON materials have been studied by XRPD, variable-temperature NPD, (31)Ip and variable-temperature Na-23 MAS NMR, and impedance spectroscopies. Relative P-31 MAS NMR peak intensities of the five detected signals, attributed to the environments [P(OZr)(4-n)(OIn)(n) (n = 0-4)], are close to those expected for a random distribution of octahedral cations. This local probe allows us to rule out the existence of segregated metal-rich nanoregions. Combined NPD and XRPD Rietveld studies showed that the occupation of M2 sites by the extra Na+ cations produces a slight distortion of the structure. Low temperatures freeze Na mobilities and permit the assignment of the resulting NMR bands to Na+ in the M1 and M2 sites. The mobility of Na at room temperature increases with the Na content. For samples with x < 0.8, Na ions are relatively localized; however, for x greater than or equal to 0.8, Na mobility increases, yielding a unique signal in the Na-23 NMR spectra. The increase of Na mobility causes spatial disorder at the M1 site as deduced from the variable-temperature NPD study. At low temperatures, the activation energies do not change significantly. So, the observed increase in bulk conductivity by 2 orders of magnitude in the low-temperature regime is ascribed to an increase of mobile carrier, Na+, concentration. However, at higher temperatures a new regime has been identified by NPD, Na-23 NIAS NMR, and Arrhenius plots of f(max) data in Z " spectra and is associated with more extended sodium motion. The onset temperature for the curvature in the Z " f(max) Arrhenius plots, when reaching the high-temperature regime, depends on sodium content.
引用
收藏
页码:2134 / 2142
页数:9
相关论文
共 23 条
[1]  
BROCHU R, 1979, CR ACAD SCI C CHIM, V289, P85
[2]  
CABEZA A, 1998, ADV XRAY ANAL, V42, P228
[3]   SODIUM MOTION IN THE NASICON RELATED NA1+XZR2-XINX(PO4)3 SOLID-SOLUTION - AN NMR-STUDY [J].
CHERKAOUI, F ;
VILLENEUVE, G ;
DELMAS, C ;
HAGENMULLER, P .
JOURNAL OF SOLID STATE CHEMISTRY, 1986, 65 (03) :293-300
[4]  
DAVIS BL, 1986, POWDER DIFFR, V1, P240
[5]   CRYSTAL-CHEMISTRY OF THE NA1+XZR2-XLX(PO4)3 (L = CR, IN, YB) SOLID-SOLUTIONS [J].
DELMAS, C ;
OLAZCUAGA, R ;
LEFLEM, G ;
HAGENMULLER, P ;
CHERKAOUI, F ;
BROCHU, R .
MATERIALS RESEARCH BULLETIN, 1981, 16 (03) :285-290
[6]   IONIC-CONDUCTIVITY IN NASICON-TYPE PHASES NA1+XZR2-XCRX(PO4)3,NA1+XZR2-XINX(PO4)3,NA1+XZR2-XYBX(PO4)3 [J].
DELMAS, C ;
VIALA, JC ;
OLAZCUAGA, R ;
LEFLEM, G ;
HAGENMULLER, P ;
CHERKAOUI, F ;
BROCHU, R .
SOLID STATE IONICS, 1981, 3-4 (AUG) :209-214
[7]   A CORRECTION FOR POWDER DIFFRACTION PEAK ASYMMETRY DUE TO AXIAL DIVERGENCE [J].
FINGER, LW ;
COX, DE ;
JEPHCOAT, AP .
JOURNAL OF APPLIED CRYSTALLOGRAPHY, 1994, 27 :892-900
[8]   CRYSTAL-STRUCTURES AND CRYSTAL-CHEMISTRY IN SYSTEM NA1+XZR2SIXP3-XO12 [J].
HONG, HYP .
MATERIALS RESEARCH BULLETIN, 1976, 11 (02) :173-182
[9]   NA-23 NMR-STUDY OF THE NASICON SYSTEM NA1+XZR2(PO4)3-X(SIO4)X [J].
JAGER, C ;
BARTH, S ;
FELTZ, A .
CHEMICAL PHYSICS LETTERS, 1989, 154 (01) :45-48
[10]  
KHOLER H, 1983, SOLID STATE IONICS, V9, P795