Splitting of permittivity maximum of NH4HSeO4under mechanical stress and electric field

1994 ◽  
Vol 46 (3) ◽  
pp. 175-183 ◽  
Author(s):  
R. Styrkowiec ◽  
W. A. Syslo
2008 ◽  
Vol 55-57 ◽  
pp. 281-284 ◽  
Author(s):  
N. Wongdamnern ◽  
Athipong Ngamjarurojana ◽  
Supon Ananta ◽  
Yongyut Laosiritaworn ◽  
Rattikorn Yimnirun

Effects of electric field-amplitude and mechanical stress on hysteresis area were investigated in partially depoled hard PZT bulk ceramic. At any compressive stress, the hysteresis area was found to depend on the field-amplitude with a same set of exponents to the power-law scaling. Consequently, inclusion of compressive stresses into the power-law was also obtained in the form of < A – Aσ=0 > α E05.1σ1.19 which indicated the difference of the energy dissipation between the under-stress and stress-free conditions.


1999 ◽  
Vol 229 (1) ◽  
pp. 89-94
Author(s):  
Ho-Young Ahn ◽  
Yong-Chan Cho ◽  
Sang-Eon Park ◽  
Se-Young Jeong

2003 ◽  
Author(s):  
Sung H. Jang ◽  
Young S. Kim ◽  
Sang Ki Lee ◽  
Hoon C. Park ◽  
Kwang J. Yoon

1978 ◽  
Vol 20 (84) ◽  
pp. 543-546
Author(s):  
D.M. Joncich ◽  
J. Holder ◽  
A.V. Granato

AbstractA direct determination of the upper limit for the electric charge density along dislocations in ice has been carried out by measuring the simultaneous effects of an electric field and a mechanical stress on the movement of a low-angle tilt boundary in an ice single crystal. The determination is independent of the geometry of the dislocations or the distribution of the charge along them. No measurable effects of the electric field on boundary motion were found, requiring that the charge density be less than one unit of charge for every 300 atomic lengths of dislocation. This estimate is less than large previous estimates, but is consistent with smaller proposed values.


1978 ◽  
Vol 20 (84) ◽  
pp. 543-546
Author(s):  
D.M. Joncich ◽  
J. Holder ◽  
A.V. Granato

AbstractA direct determination of the upper limit for the electric charge density along dislocations in ice has been carried out by measuring the simultaneous effects of an electric field and a mechanical stress on the movement of a low-angle tilt boundary in an ice single crystal. The determination is independent of the geometry of the dislocations or the distribution of the charge along them. No measurable effects of the electric field on boundary motion were found, requiring that the charge density be less than one unit of charge for every 300 atomic lengths of dislocation. This estimate is less than large previous estimates, but is consistent with smaller proposed values.


In a previous communication, the writer discussed the double refraction of a medium composed of similar particles arranged in rectangular order, the results being applied especially to the effects produced in colloidal solutions by mechanical stress and by a magnetic field; the present paper is the discussion of a similar problem, using a simpler method of procedure suggested by Professor Larmor. The object is to investigate to what extent it is possible to consider double refraction, whether produced artificially or occurring in natural crystals, as due simply to an æolotropic distribution of similar particles; the questions which arise when one considers whether the æolotropy occurs naturally or is produced by the action of mechanical, electric, or magnetic force are not specially considered, but the various cases are classified in the first section. In the next sections we consider a medium composed of a homogeneous assemblage of optically isotropic molecules and obtain an expression giving the dispersion of the double refraction. This is applied first to artificial double refraction produced by mechanical stress and by an electric field; then on the same basis the dispersion in quartz is examined. Certain divergences in natural crystals and especially such anomalous cases as apophylite and vesuvian lead to an extension of the theory. This is, briefly, an æolotropic distribution of optically æolotropic molecules, each of which disperses regularly; it is examined first in relation to uniaxal crystals and finally in general for biaxal crystals, and is found to contain the possibility of all the varieties of dispersion of double refraction which occur in natural crystals.


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