Numéro |
J. Phys. IV France
Volume 112, October 2003
|
|
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Page(s) | 541 - 544 | |
DOI | https://doi.org/10.1051/jp4:2003943 |
J. Phys. IV France 112 (2003) 541
DOI: 10.1051/jp4:2003943
Compressive stresses and stabilisation in Cu-Al-Ni single crystals
C. Picornell, J. Pons and E. CesariDepartament de Fisica, Universitat de les llles Balears, Ctra. de Valldemossa km. 7.5, 07071 Palma de Mallorca, Spain
Abstract
Cu-AI-Ni single crystals which present
(quenched samples) or
(aged at 570K samples) thermally induced martensitic transformations, were submitted to compressive stresses at different
temperatures. The test temperatures were chosen in order to have martensite-martensite stress induced transformations. The
characteristics of the martensitic transformation and structural changes before and after the compression tests have been
studied by means of calorimetry (DSC) and TEM. The obtained results show that when applying compressive stresses in both ensembles
of samples, a non-twinned
martensite appears. In the quenched samples it is formed through the
beta phase already present at room temperature. In the aged samples the non twinned
phase is stress induced from the
thermally formed (internally twinned). The amount of non twinned
phase increases with the applied deformation, for low strain values it coexists with the
or
(twinned) phases and is the only present phase for higher applied strain values. In all the cases a notable martensite stabilisation
is observed in the first thermal induced transformation after the mechanical test only when the stress-strain loops are not
closed, that means when a permanent strain remains in the material after unloading. The degree of mechanical stabilisation
is more important as higher is the applied deformation and as much amount of
phase mechanically formed (non twinned) is still present in the material and it is slightly dependent on the test temperature
if lower than A
f The stress induced stabilisation mechanism is related to the presence of this non twinned martensite and its difficult retransformation
to the parent phase.
© EDP Sciences 2003