11.07.2015 Views

Recent developments in the research of shape memory alloys

Recent developments in the research of shape memory alloys

Recent developments in the research of shape memory alloys

SHOW MORE
SHOW LESS
  • No tags were found...

You also want an ePaper? Increase the reach of your titles

YUMPU automatically turns print PDFs into web optimized ePapers that Google loves.

K. Otsuka, X. Ren/Intermetallics 7 (1999) 511±528 521Fig. 16. Mechanism <strong>of</strong> <strong>the</strong> rubber-like behavior and martensite stabilization phenomenon. The illustrations show <strong>the</strong> statistical atomic con®guration(conditional probabilities around an A atom) <strong>of</strong> an imperfectly-ordered AB compound <strong>in</strong>, (a) equilibrium parent phase; (b) martensite immediatelyafter transformed from (a); (c) equilibrium martensite; (d) stress-<strong>in</strong>duced martensite doma<strong>in</strong> (tw<strong>in</strong>) immediately formed from (c); (e) equilibriumstate <strong>of</strong> <strong>the</strong> stress-<strong>in</strong>duced doma<strong>in</strong>; and (f) parent immediately transformed from (c), respectively. P: <strong>the</strong> parent phase, and M: martensite. P i B (orP i A ) is <strong>the</strong> conditional probability <strong>of</strong> B atom (or A atom) occupy<strong>in</strong>g i-site (i=1,2,3,...8) if an A atom is at O-site. The relative values <strong>of</strong> P i B and P iAare <strong>in</strong>dicated by <strong>the</strong> black and grey areas, respectively [86].same four-fold symmetry accord<strong>in</strong>g to SC-SRO pr<strong>in</strong>ciple,i.e., P 1 B =P 2 B =P 3 B =P 4 B , and P 5 B =P 6 B =P 7 B =P 8 B ,etc., where P i B (i=1,2,3,...) are conditional probabilities,as de®ned <strong>in</strong> Fig. 16.When <strong>the</strong> parent phase shown <strong>in</strong> Fig. 16(a) transformsdi€usionlessly <strong>in</strong>to martensite, all <strong>the</strong> probabilitiesmust rema<strong>in</strong> unchanged despite <strong>the</strong> symmetrychange, as shown <strong>in</strong> Fig. 16(b). That is, P 1 B =P 2 B =P 3 B =P 4 B , and P 5 B =P 6 B =P 7 B =P 8 B , etc.. However, thishigh-symmetry con®guration is no longer a stable con-®guration for <strong>the</strong> lower symmetry martensite structureaccord<strong>in</strong>g to <strong>the</strong> SC±SRO pr<strong>in</strong>ciple. Then dur<strong>in</strong>g ag<strong>in</strong>g,such a con®guration gradually changes <strong>in</strong>to a stable onethat conforms to martensite symmetry, as shown <strong>in</strong>Fig. 16(c). Because <strong>the</strong> equilibrium martensite structureshould be ma<strong>in</strong>ta<strong>in</strong>ed (for stable martensite), this processproceeds by atomic rearrangement or relaxationwith<strong>in</strong> <strong>the</strong> same sublattice. This is <strong>the</strong> only way that amartensite can lower its free energy without alter<strong>in</strong>g <strong>the</strong>average structure (equilibrium phase).When <strong>the</strong> stabilized (or aged) martensite [Fig. 16(c)] isdeformed, it changes <strong>in</strong>to ano<strong>the</strong>r doma<strong>in</strong> (or tw<strong>in</strong>) as aresult <strong>of</strong> <strong>the</strong> accommodation <strong>of</strong> <strong>the</strong> stra<strong>in</strong>. Because thistw<strong>in</strong>n<strong>in</strong>g process is also di€usionless, <strong>the</strong> atomic occupationprobabilities shown <strong>in</strong> Fig. 16(c) is <strong>in</strong>herited to<strong>the</strong> new doma<strong>in</strong>, as shown <strong>in</strong> Fig. 16(d). Such a con®guration,however, is not <strong>the</strong> stable one for <strong>the</strong> newdoma<strong>in</strong>, which is shown <strong>in</strong> Fig. 16(e). Therefore, adriv<strong>in</strong>g force that tries to restore <strong>the</strong> orig<strong>in</strong>al doma<strong>in</strong>[Fig. 16(c)] engenders. When <strong>the</strong> external stress isreleased immediately after <strong>the</strong> load<strong>in</strong>g, this restor<strong>in</strong>gforce reverts <strong>the</strong> new doma<strong>in</strong> [Fig. 16(d)] to <strong>the</strong> orig<strong>in</strong>alone [Fig. 16(c)] by detw<strong>in</strong>n<strong>in</strong>g. This is <strong>the</strong> orig<strong>in</strong> <strong>of</strong> <strong>the</strong>rubber-like behavior. If <strong>the</strong> stress is held for some time,atomic con®guration <strong>in</strong> Fig. 16(d) have enough time tochange <strong>in</strong>to a stable con®guration [Fig. 16(e)], <strong>the</strong>n noRLB will occur.When <strong>the</strong> stabilized martensite [Fig. 16(c)] is heatedup and transforms back (di€usionlessly) <strong>in</strong>to <strong>the</strong> parent,<strong>the</strong> stable SRO con®guration for <strong>the</strong> martensite is<strong>in</strong>herited <strong>in</strong>to <strong>the</strong> parent [Fig. 16(f)]. From <strong>the</strong> abovementionedsymmetry-conform<strong>in</strong>g pr<strong>in</strong>ciple <strong>of</strong> SRO, it isobvious that Fig. 16(f) is not a stable con®guration for<strong>the</strong> parent. From a <strong>the</strong>rmodynamic po<strong>in</strong>t <strong>of</strong> view, thiscorresponds to an <strong>in</strong>creased reverse transformationtemperature. This is <strong>the</strong> orig<strong>in</strong> <strong>of</strong> martensite stabilization.The SC±SRO model can be easily extended <strong>in</strong>to disordered<strong>alloys</strong> by consider<strong>in</strong>g <strong>the</strong> existence <strong>of</strong> only onesublattice. In this case, <strong>the</strong> present model reduces toChristian's model [88], which was later elaborated byOtsuka and Wayman [6]. This model expla<strong>in</strong>ed <strong>the</strong>rubber-like elasticity <strong>in</strong> disordered <strong>alloys</strong> such as In±Tl.The largest advantage <strong>of</strong> <strong>the</strong> SC±SRO model comparedwith previous models is its generality. It not onlyexpla<strong>in</strong>s why ag<strong>in</strong>g does not cause a change <strong>of</strong> averagestructure <strong>of</strong> martensite, but also uni®ed <strong>the</strong> orig<strong>in</strong> <strong>of</strong>ag<strong>in</strong>g e€ect for both ordered and disordered martensites.

Hooray! Your file is uploaded and ready to be published.

Saved successfully!

Ooh no, something went wrong!