rheologic model
Recently Published Documents


TOTAL DOCUMENTS

11
(FIVE YEARS 0)

H-INDEX

3
(FIVE YEARS 0)

2006 ◽  
Vol 163 (9) ◽  
pp. 1991-2009
Author(s):  
Zhiping Song ◽  
Xiangchu Yin ◽  
Shirong Mei ◽  
Yucang Wang ◽  
Can Yin ◽  
...  

2006 ◽  
Vol 19 (1) ◽  
pp. 20-29
Author(s):  
Zhi-ping Song ◽  
Shi-rong Mei ◽  
Xiang-chu Yin

2004 ◽  
Vol 17 (2) ◽  
pp. 131-143 ◽  
Author(s):  
Song Zhi-Ping ◽  
Yin Xiang-Chu ◽  
Mei Shi-Rong

2003 ◽  
Vol 16 (6) ◽  
pp. 588-597 ◽  
Author(s):  
Song Zhi-ping ◽  
Xiang-chu Yin ◽  
Shi-rong Mei

1994 ◽  
Vol 365 ◽  
Author(s):  
B.G. Nair ◽  
R.F. Cooper ◽  
J.N. Almquist ◽  
M.E. Plesha

ABSTRACTThe elevated temperature rheology of continuous SiC (Nicalon®) calcium aluminosilicate glass-ceramic matrix composites is evaluated in uniaxial compression creep experiments (-σ1 = 20-to-40 MPa; T = 1300–1320°C). The steady state strain rate is demonstrated.to be highly sensitive to the orientation of the reinforcement relative to the maximum compressional stress, with highest bulk specimen strain rates noted for conditions in vWhich the sliding between the fiber and the matrix is optimized as a kinetic flow response (i.e., a fiber orientation of approximately 40-50° from σ1). One further discovers that the temperature sensitivity (i.e., activation energy) of flow increases as the amount of interface flow/sliding increases. The experimental results suggest that the high-temperature, low-stress interface response in this composite system is related to the ductile flow of the “Planar” SiO2 reaction-layer interphase that exists (in addition to the well-recognized planar carbon interphase) in these materials. The results of these simple experiments are used to calibrate a microscale-to-macroscale rheologic model in which the fibermatrix interface is described by a viscous constitutive relationship.


Radiocarbon ◽  
1986 ◽  
Vol 28 (2A) ◽  
pp. 417-423 ◽  
Author(s):  
Michael Andree ◽  
Juerg Beer ◽  
H P Loetscher ◽  
Ernst Moor ◽  
Hans Oeschger ◽  
...  

Results of 14C/12C ratio measurements on CO2 extracted from air bubbles in polar ice are presented. The samples investigated originate from the Dye 3, South Greenland, deep ice core and span approximately the last 10,000 years. The results are calibrated with tree-ring records. The 14C ages are compared with information obtained from seasonal variations of ice-core parameters and rheologic model calculation.


Sign in / Sign up

Export Citation Format

Share Document