P1C-5 Shear Strain Imaging with Shear Deformation

Author(s):  
T. Varghese ◽  
M. Rao ◽  
E. L. Madsen
2010 ◽  
Vol 36 (11) ◽  
pp. 1813-1824 ◽  
Author(s):  
Haiyan Xu ◽  
Min Rao ◽  
Tomy Varghese ◽  
Amy Sommer ◽  
Sara Baker ◽  
...  

2007 ◽  
Vol 539-543 ◽  
pp. 2872-2877 ◽  
Author(s):  
Young Hoon Chung ◽  
Jong Woo Park ◽  
Kyong Hwan Lee

As the surface friction between feeding rolls and metal sheet generates the feeding power of ECAR, the generated feeding power is low, and the friction between the metal sheet and ECAR die should be minimized. However, for obtaining a large shear deformation by ECAR, the metal sheet should be tightly contacted with the wall of ECAR die. In this condition, the thickness of the metal sheet is continuously increased during ECAR. A new ECAR apparatus is developed for maximizing the shear deformation and obtaining sheet thickness uniformity, and succeeding continuous ECAR with such a limited feeding power. By controlling the outlet gap of the ECAR die with elastic unit, the thickness of the metal sheet is kept uniform. Detailed thickness control mechanism during the new ECAR process is analyzed. A sheet of Al 6063 alloy that is 1-pass deformed with the new ECAR apparatus shows below ±0.037 mm of thickness variation and 0.61 of shear strain.


2008 ◽  
Vol 35 (2) ◽  
pp. 412-423 ◽  
Author(s):  
Min Rao ◽  
Tomy Varghese ◽  
Ernest L. Madsen

Author(s):  
Haiyan Xu ◽  
Tomy Varghese ◽  
Jingfeng Jiang ◽  
Timothy J. Hall ◽  
James A Zagzebski

Author(s):  
Tim Idzenga ◽  
Hendrik H.G. Hansen ◽  
Johan M. Thijssen ◽  
Chris L. de Korte

2010 ◽  
Vol 4 (4) ◽  
pp. 151
Author(s):  
T. Idzenga ◽  
H.H.G. Hansen ◽  
R.G.P. Lopata ◽  
C.L. De Korte

1958 ◽  
Vol 3 (24) ◽  
pp. 271-278 ◽  
Author(s):  
George P. Rigsby

Apparatus was built for deforming ice crystals under hydrostatic pressures up to 350 atmospheres. Single crystals were placed in the mounts in such a way that the deformation occurred by gliding on the basal glide plane. It was found that the shear strain rate increased as the pressure was increased at constant temperature, but that the rate is practically independent of hydrostatic pressure when the difference between the ice temperature and the melting temperature is kept constant.


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