TY - GEN
T1 - Macro to atomistic examination of dynamic cleavage in single crystal silicon
AU - Sherman, Dov
PY - 2005
Y1 - 2005
N2 - A set of cleavage experiments with strip-shaped single-crystal silicon specimens subjected to three-point bending will be presented. The experiments enabled examination of the relationships between crack velocity, the crystallographic orientation, and the cleavage plane of propagation. Dynamic crack propagation experiments show that when a [001] silicon single crystal is fractured under three-point bending at measured velocity of up to 1500 m/sec, it prefers to cleave along the vertical (110) plane, while when the specimen is fractured under the same conditions but at a velocity higher than 2900 m/sec, it cleaves along the inclined (111) plane. At intermediate velocities, the crack will deflect from the (110) plane to the (111) plane. The deflection phenomenon presents an excellent opportunity to examine the upper crack tip's velocity limit. Analysis of the experimental results showed that the normalized crack tip velocity in the (110) plane with the Rayleigh surface wave speed yields ratio of up to 0.65 (in the [1 1 0] direction), which reduces to as low as 0.01 (in the [001] direction). It is suggested that the cause of the deflection phenomenon and the reasoning for the low limiting crack tip velocity is the anisotropic, velocity dependent, irreversible cleavage energy, resulted phonon radiation caused by anisotropic, velocity dependent lattice vibrations.
AB - A set of cleavage experiments with strip-shaped single-crystal silicon specimens subjected to three-point bending will be presented. The experiments enabled examination of the relationships between crack velocity, the crystallographic orientation, and the cleavage plane of propagation. Dynamic crack propagation experiments show that when a [001] silicon single crystal is fractured under three-point bending at measured velocity of up to 1500 m/sec, it prefers to cleave along the vertical (110) plane, while when the specimen is fractured under the same conditions but at a velocity higher than 2900 m/sec, it cleaves along the inclined (111) plane. At intermediate velocities, the crack will deflect from the (110) plane to the (111) plane. The deflection phenomenon presents an excellent opportunity to examine the upper crack tip's velocity limit. Analysis of the experimental results showed that the normalized crack tip velocity in the (110) plane with the Rayleigh surface wave speed yields ratio of up to 0.65 (in the [1 1 0] direction), which reduces to as low as 0.01 (in the [001] direction). It is suggested that the cause of the deflection phenomenon and the reasoning for the low limiting crack tip velocity is the anisotropic, velocity dependent, irreversible cleavage energy, resulted phonon radiation caused by anisotropic, velocity dependent lattice vibrations.
UR - http://www.scopus.com/inward/record.url?scp=84869795628&partnerID=8YFLogxK
M3 - פרסום בספר כנס
AN - SCOPUS:84869795628
SN - 9781617820632
T3 - 11th International Conference on Fracture 2005, ICF11
SP - 5379
EP - 5384
BT - 11th International Conference on Fracture 2005, ICF11
Y2 - 20 March 2005 through 25 March 2005
ER -