Dependence of electrical properties of epitaxial Pb(Zr,Ti)O3 thick films on crystal orientation and Zr∕(Zr+Ti) ratio

2005 ◽  
Vol 98 (9) ◽  
pp. 094106 ◽  
Author(s):  
Shintaro Yokoyama ◽  
Yoshihisa Honda ◽  
Hitoshi Morioka ◽  
Shoji Okamoto ◽  
Hiroshi Funakubo ◽  
...  
2014 ◽  
Vol 115 (13) ◽  
pp. 134101
Author(s):  
Tingting Jia ◽  
Hideo Kimura ◽  
Hongyang Zhao ◽  
Qiwen Yao ◽  
Zhenxiang Cheng ◽  
...  

2018 ◽  
Vol 57 (5-6) ◽  
pp. 285-292 ◽  
Author(s):  
A. V. Paustovsky ◽  
V. E. Sheludko ◽  
E. Ya. Telnikov ◽  
A. K. Marchuk ◽  
V. V. Kremenitsky ◽  
...  

Author(s):  
Cesar R. Foschini ◽  
B.D. Stojanovic ◽  
José A. Varela ◽  
V.B. Pavlovic ◽  
V.M. Pavlovic ◽  
...  

2012 ◽  
Vol 41 (11) ◽  
pp. 3077-3081 ◽  
Author(s):  
Fang Fu ◽  
Jiwei Zhai ◽  
Zhengkui Xu ◽  
Wangfeng Bai ◽  
Lingbing Kong

1979 ◽  
Vol 23 (89) ◽  
pp. 223-232 ◽  
Author(s):  
A. H. W. Woodruff ◽  
C. S. M. Doake

Abstract Polar ice is now thought to be marginally birefringent at radio echo-sounding frequencies. An experiment on the polarization behaviour of 60 MHz radio echoes from the bed of both ice shelf and land ice in Antarctica showed a marked difference in the returned polarization. It appears that differences in electrical properties or roughness of the reflecting boundary cannot explain our results. We suggest that there is a large change in the birefringence of the ice sheet at the hinge zone, caused by the effect of tidal strain on crystal orientation. This would imply a minimum value of the radio-frequency anisotropy in permittivity for the single crystal of (0.52±0.8)%. Therefore polarization changes could allow floating and grounded ice to be distinguished.


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