Interface excess and polymorphic stability of nanosized zirconia-magnesia

被引:26
作者
Castro, Ricardo H. R. [1 ]
Marcos, Paulo J. B. [2 ]
Lorriaux, Annick [3 ]
Steil, Marlu C. [4 ]
Gengembre, Leon [3 ]
Roussel, Pascal [3 ]
Gouvea, Douglas [5 ]
机构
[1] FEI Univ Ctr, Dept Mat Engn, BR-09850901 Sao Bernardo Do Campo, SP, Brazil
[2] Fac Tecnol Sao Paulo, BR-01124060 Sao Paulo, Brazil
[3] Ecole Natl Super Chim Lille Bat C7A, CNRS, UMR 8181, Unite Catalyse & Chim Solide, F-59652 Villeneuve Dascq, France
[4] Univ Grenoble 1, LEPMI, CNRS, INPG, F-38402 St Martin Dheres, France
[5] Univ Sao Paulo, Dept Met & Mat Engn, BR-05508900 Sao Paulo, Brazil
关键词
D O I
10.1021/cm703599r
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
Controlling the phase stability of ZrO2 nanoparticles is of major importance in the development of new ZrO2-based nanotechnologies. Because of the fact that in nanoparticles the surface accounts for a larger fraction of the total atoms, the relative phase stability can be controlled throughout the surface composition, which can be toned by surface excess of one of the components of the system., The objective of this work is to delineate a relationship between surface excess (or solid solution) of MgO relative to ZrO2 and the polymorphic stability of (ZrO2)(1-x) - (MgO), nanopowders, where 0.0 <= x <= 0.6. The nanopowders were prepared by a liquid precursor method at 500 degrees C and characterized by N-2 adsorption (BET), X-ray diffraction (XRD), X-Ray photoelectron spectroscopy (XPS), and Raman spectroscopy. For pure ZrO2 samples, both tetragonal and monoclinic polymorphs were detected, as expected considering the literature. For MgO molar fractions varying from 0.05 to 0.10, extensive solid solution could not be detected, and a ZrO2 surface energy reduction, caused by Mg surface excess detected by XPS, promoted tetragonal polymorph thermodynamic stabilization with relation to monoclinic. For MgO molar fractions higher than 0.10 and up to 0.40, Mg solid solution could be detected and induced cubic phase stabilization. MgO periclase was observed only at x = 0.6. A discussion based on the relationship between the surface excess, surface energy, and polymorph stability is presented.
引用
收藏
页码:3505 / 3511
页数:7
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