2006
DOI: 10.1016/j.msea.2006.05.048
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Effect of heat treatment atmosphere on the multistage martensitic transformation in aged Ni-rich Ti–Ni alloys

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Cited by 20 publications
(12 citation statements)
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“…Details such as heat treatment atmosphere are described elsewhere. 6,11,15,16) Some specimens were aged at 773 K for 3.6 ks and then quenched into ice water. The solution-treated and aged specimens were subjected to thermal cycling in the temperature range between 77 and 373 K by alternately dipping them into liquid nitrogen and boiling water for 1 min at a time.…”
Section: Methodsmentioning
confidence: 99%
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“…Details such as heat treatment atmosphere are described elsewhere. 6,11,15,16) Some specimens were aged at 773 K for 3.6 ks and then quenched into ice water. The solution-treated and aged specimens were subjected to thermal cycling in the temperature range between 77 and 373 K by alternately dipping them into liquid nitrogen and boiling water for 1 min at a time.…”
Section: Methodsmentioning
confidence: 99%
“…These differences between M1*, M2* and M3* are attributable to the heterogeneous microstructure with variations in size and distribution density of Ti 3 Ni 4 precipitates in the aged specimen, as mentioned above. 39,11,1416) After 100 thermal cycles, ¦A1*, ¦(A2* + AR*) and ¦A3* are 3, 3 and 11 K, respectively. These results suggest that the influence of thermal cycling is also more pronounced in forward transformation than in reverse transformation in the aged specimen with heterogeneous microstructure.…”
Section: Methodsmentioning
confidence: 99%
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“…The path of the martensitic phase transition was * david.holec@unileoben.ac.at shown to change once oxygen was a part of a residual gas during the heat treatment. In order to explain the observed effects, Fujishima et al [14] and recently also Ravari et al [15] suggested a link between the precipitation of the Ni 4 Ti 3 phase and the composition of the heat treatment atmosphere. While the scenario proposed by Nishida et al [13] focused on the role of the residual oxygen, some other gaseous components, that may have contributed to the overall pressure of residual gasses and thus to the varying PTTs, were not taken into account.…”
Section: Introductionmentioning
confidence: 99%