Chemical and structural variations at augite (100) deformation twin boundaries

2007 ◽  
Vol 92 (11-12) ◽  
pp. 1833-1837 ◽  
Author(s):  
S. Zhang ◽  
D. R. Veblen
2004 ◽  
Vol 819 ◽  
Author(s):  
Randall S. Hay

AbstractMonazite (LaPO4) was indented at room temperature. Deformation twin boundaries and stacking faults were characterized by high resolution transmission electron microscopy. Kinked deformation twins were also characterized and analyzed. Three types of stacking faults associated with climb-dissociated partial dislocations were observed. Two were found on twin boundaries, and a third in the lattice. Formation mechanisms are discussed. The superimposition of stacking faults along twin boundaries during deformation twinning and the glide of climb-dissociated partial dislocations allowed by stacking fault migration are discussed. The possible relationship between the formation mechanisms for these defects and the low- temperature recrystallization and self-annealing of defects in monazite is considered.


2015 ◽  
Vol 107 (9) ◽  
pp. 091901 ◽  
Author(s):  
S. B. Jin ◽  
K. Zhang ◽  
R. Bjørge ◽  
N. R. Tao ◽  
K. Marthinsen ◽  
...  

2006 ◽  
Vol 438-440 ◽  
pp. 495-499 ◽  
Author(s):  
M. Nishida ◽  
M. Matsuda ◽  
T. Fujimoto ◽  
K. Tanka ◽  
A. Kakisaka ◽  
...  

2004 ◽  
Vol 821 ◽  
Author(s):  
Randall S. Hay

AbstractMonazite (LaPO4) was indented at room temperature. Deformation twin boundaries and stacking faults were characterized by high resolution transmission electron microscopy. Kinked deformation twins were also characterized and analyzed. Three types of stacking faults associated with climb-dissociated partial dislocations were observed. Two were found on twin boundaries, and a third in the lattice. Formation mechanisms are discussed. The superimposition of stacking faults along twin boundaries during deformation twinning and the glide of climb-dissociated partial dislocations allowed by stacking fault migration are discussed. The possible relationship between the formation mechanisms for these defects and the low- temperature recrystallization and self-annealing of defects in monazite is considered.


2000 ◽  
Vol 45 (6) ◽  
pp. 320-325 ◽  
Author(s):  
L.C Zhang ◽  
J.G Wang ◽  
G.L Chen ◽  
G Sauthoff

2021 ◽  
Vol 11 (1) ◽  
Author(s):  
Chang-Yu Hung ◽  
Tomotsugu Shimokawa ◽  
Yu Bai ◽  
Nobuhiro Tsuji ◽  
Mitsuhiro Murayama

AbstractSome of ultrafine-grained (UFG) metals including UFG twinning induced plasticity (TWIP) steels have been found to overcome the paradox of strength and ductility in metals benefiting from their unique deformation modes. Here, this study provides insights into the atomistic process of deformation twin nucleation at Σ3{111} twin boundaries, the dominant type of grain boundary in this UFG high manganese TWIP steel. In response to the applied tensile stresses, grain boundary sliding takes place which changes the structure of coherent Σ3{111} twin boundary from atomistically smooth to partly defective. High resolution transmission electron microscopy demonstrates that the formation of disconnection on Σ3{111} twin boundaries is associated with the motion of Shockley partial dislocations on the boundaries. The twin boundary disconnections act as preferential nucleation sites for deformation twin that is a characteristic difference from the coarse-grained counterpart, and is likely correlated with the lethargy of grain interior dislocation activities, frequently seen in UFG metals. The deformation twin nucleation behavior will be discussed based on in-situ TEM deformation experiments and nanoscale strain distribution analyses results.


1973 ◽  
Vol 21 (11) ◽  
pp. 1515-1521 ◽  
Author(s):  
O.P Bhandari ◽  
R.L Bertolotti ◽  
W.D Scott

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