Effect of Ag addition on phase transitions of the Cu–22.26 at.%Al–9.93 at.%Mn alloy
Highlights
► A kinetic mechanism for the dissolution of DO3 phase is suggested. ► The intermediate phase interferes on the kinetics of the DO3 phase dissolution. ► The presence of Ag changes the stability of intermediate phase.
Introduction
Alloys of the Cu–Al–Mn system are Hume–Rothery alloys. The phase stability of these materials is largely dominated by the average number of conduction electrons per atom, denoted as e/a. Within a certain range of compositions around the Cu-rich region (far from the Cu2AlMn Heusler stoichiometry) the system undergoes a martensitic transition associated with shape-memory properties [1]. The Cu-rich portion of the Cu–Mn–Al system has been fully investigated at temperatures above 723 K. It was found that the addition of Mn expands the high temperature β phase field of the Cu–Al system. The β phase stability compositional range increases with temperature, and includes the composition of the well-known Heusler alloy Cu2MnAl at temperatures above 923 K. At 673 K the equilibrium phases in these alloys are: Cu3Mn2Al, γ and βMn [2]. At temperatures lower than 600 K, a spinodal decomposition can occur between a non-magnetic (DO3) Cu3Al-rich phase and a (L21) Cu2AlMn-rich phase, which orders ferromagnetically. The kinetics of this process is slow and this decomposition is avoided for typical cooling rates. Associated with this spinodal decomposition some authors have reported the appearance of superparamagnetism at low temperatures [3].
Silver additions to Cu–Al alloys increase its hardness [4], stress corrosion resistance [5] and modify the aging characteristics of the alloys [6], with no ternary intermediate phases being observed [7], [8]. It is expected that Ag additions to Cu–Al–Mn alloys present a similar effect, thus improving some properties of the system mainly its corrosion resistance, apart from allowing the study of the effect of Ag presence on the characteristics temperatures and mechanism of phase transitions. In this work, the influence of addition of 1.53 at.%Ag to the Cu–22.26 at.%Al–9.93 at.%Mn alloy was studied using differential scanning calorimetry (DSC) at different heating rates, microhardness changes with temperature, magnetization changes with temperature, scanning electron microscopy (SEM) and energy dispersion X-ray spectroscopy (EDXS). The purpose of this work is to study the phase transitions in the Cu–Al–Mn and Cu–Al–Mn–Ag alloys after slow cooling at about 5 K/h, correlating with the presence of Ag and its influence on the ternary system.
Section snippets
Experimental procedure
The Cu–22.26 at.%Al–9.93 at.%Mn and Cu–22.49 at.%Al–10.01 at.%Mn–1.53 at.%Ag alloys were prepared in an arc furnace under argon atmosphere using 99.95% copper, 99.97% aluminum, 99.995% manganese and 99.98% silver as starting materials. Cylindrical samples with 2.0 cm diameter and 6.0 cm length were cut in disks of 2.0 mm thickness. The samples were maintained for 120 h at 1123 K and then cooled at 5.0 K/h down to room temperature. The DSC curves were obtained using a DSC Q20 TA Instruments at different
Results and discussion
Fig. 1 shows the DSC curves obtained at different heating rates for the Cu–22.26 at.%Al–9.93 at.%Mn and Cu–22.49 at.%Al–10.01 at.%Mn–1.53 at.%Ag alloys. These alloys were initially maintained at 1123 K for 120 h and then cooled at 5.0 K/h down to room temperature. The curves of Fig. 1a, corresponding to the Cu–22.26 at.%Al–9.93 at.%Mn alloy, show three thermal events. The endothermic peak P1, at about 520 K, is shifted to higher temperatures with the increase of the heating rate. This thermal event is
Conclusions
The phase transitions in the Cu–22.49 at.%Al–10.01 at.%Mn–1.53 at.%Ag alloy were analyzed and a kinetics mechanism for the DO3 phase dissolution was suggested. The results indicated that the DO3 phase interferes in the microhardness values of the Cu–22.49 at.%Al–10.01 at.%Mn–1.53 at.%Ag alloy. The α + T3-Cu3Mn2Al + γ → β + γ + T3-Cu3Mn2Al transition is dominant at lower heating rates while L21(p) → B2 transition is dominant at higher heating rates. The (Ag–Cu)-rich precipitates dissolution occurs in the same
Acknowledgments
The authors thank FAPESP (proc. 2011/11041-4), CNPq (proc. 482348/2010-0) and LME/LNLS for technical support during electron microscopy work (JSM-5900LV).
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