Symmetry and light stuffing of Ho2Ti2O7, Er2Ti2O7, and Yb2Ti2O7 characterized by synchrotron x-ray diffraction

被引:33
作者
Baroudi, Kristen [1 ]
Gaulin, Bruce D. [2 ,3 ,4 ]
Lapidus, Saul H. [5 ]
Gaudet, Jonathan [2 ]
Cava, R. J. [1 ]
机构
[1] Princeton Univ, Dept Chem, Princeton, NJ 08544 USA
[2] McMaster Univ, Dept Phys & Astron, Hamilton, ON L8S 4M1, Canada
[3] McMaster Univ, Brockhouse Inst Mat Res, Hamilton, ON L8S 4M1, Canada
[4] Canadian Inst Adv Res, Toronto, ON M5G 1Z8, Canada
[5] Argonne Natl Lab, Adv Photon Source, Xray Sci Div, Argonne, IL 60439 USA
来源
PHYSICAL REVIEW B | 2015年 / 92卷 / 02期
基金
加拿大自然科学与工程研究理事会;
关键词
FRUSTRATED PYROCHLORE ANTIFERROMAGNET; SINGLE-CRYSTAL GROWTH; FLOATING-ZONE METHOD; SPIN ICE; EARTH; TB2TI2O7; OXIDES;
D O I
10.1103/PhysRevB.92.024110
中图分类号
T [工业技术];
学科分类号
08 ;
摘要
The Ho2Ti2O7, Er2Ti2O7, and Yb2Ti2O7 pyrochlores were studied by synchrotron x-ray diffraction to determine whether the (002) peak, forbidden in the pyrochlore space group Fd-3m but observed in single crystal neutron scattering measurements, is present due to a deviation of their pyrochlore structure from Fd-3m symmetry. Synchrotron diffraction measurements on precisely synthesized stoichiometric and nonstoichiometric powders and a crushed floating zone crystal of Ho2Ti2O7 revealed that the (002) reflection is absent in all cases to a sensitivity of approximately one part in 30 000 of the strongest x-ray diffraction peak. This indicates to high sensitivity that the space group of the crystal structure of these rare earth titanate pyrochlores is Fd-3m, and that, thus, the (002) peak observed in the neutron scattering experiments has a nonstructural origin. The cell parameters and internal strain for lightly stuffed Ho2+xTi2-xO7 are also presented.
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页数:7
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