scholarly journals Numerical modelling of micro-machining of f.c.c. single crystal: Influence of strain gradients

2014 ◽  
Vol 94 ◽  
pp. 273-278 ◽  
Author(s):  
Murat Demiral ◽  
Anish Roy ◽  
Tamer El Sayed ◽  
Vadim V. Silberschmidt
2020 ◽  
Vol 106 ◽  
pp. 107822
Author(s):  
Sarthak Mohapatra ◽  
P.K. Sahu ◽  
S. Rath ◽  
N.V.L. Narasimha Murty

2016 ◽  
Vol 861 ◽  
pp. 3-8 ◽  
Author(s):  
Shao Chuan Feng ◽  
Chuan Zhen Huang ◽  
Jun Wang ◽  
Hong Tao Zhu ◽  
Peng Yao ◽  
...  

Single crystal silicon carbide (SiC) is a new semiconductor material that has a great potential to be widely used. However, SiC is a kind of difficult-to-machine material due to its extreme hardness and brittleness. The present study investigated the machinability of single crystal SiC using dry laser and three different water-laser co-machining processes. The results indicate that using the hybrid laser-waterjet micro-machining to micro-groove single crystal SiC can derive the clean and straight edges and thermal damage-free grooves.


1996 ◽  
Vol 440 ◽  
Author(s):  
H. E. Schaffer ◽  
D. M. Lipkin ◽  
F. Adar ◽  
D. R. Clarke

AbstractMicroscopic examination of the surface of single crystal (111) NiAl during various stages of oxidation at 1100 C in air shows the development of islands composed of rings of different colors.These islands appear to grow in size and eventually impinge with increased exposure. Microscopic fluorescence mapping of the surfaces of three single crystals subjected to varied exposure times provides an identification of the composition of the islands and the surrounding area as two different allotropes of alurninum oxide.Additionally, analysis of the map spectra demonstrates the decrease of intensity of their characteristic fluorescence bands in the island centers with increasing island size, which we refer to as “volcanic” intensity topography. Thus, the observed color variation is an interference effect, due to varied films thicknesses through the islands. Finally, the energies of the fluorescent bands are seen to shift as a function of distance from the island center, indicating the development of strain gradients across the islands.


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