JOURNALOFIRON ANDSTEELRESEARCH,INTERNATIONAL2 0 1 6,2 3( 9):9 4 0 G 9 4 8
Con s t i t u t i v eMod e lo fWa rm De f o rma t i onBe ha v i o ro f Me d i um Ca r bonS t e e l Hong G b i nLI1 2 , Yun G l iFENG2 , TaoYAN3 , En G l i nYU1 ,
( i ve r s i t 1.Na t i ona lEng i ne e r i ngRe s e a r chCen t e rf o rEqu i tandTe chno l ogyo fCo l dS t r i l l i ng,YanshanUn y, pmen pRo Qi nhuangdao066004,Hebe i,Ch i na; 2.Co l l egeo fMe t a l l u r r r t hCh i naUn i ve r s i t fSc i enc eand gyandEne gy,No yo Te chno l ogy,Tangshan063009,Hebe i,Ch i na; 3.Equ i tManu f a c t u r i ngCo l l ege,Hebe iUn i ve r s i t f pmen yo Eng i ne e r i ng,Handan056038,Hebe i,Ch i na) Ab s t r a c t:Thec omp r e s s i vebehav i o r so fmed i umc a r bons t e e lspe c imenswe r ei nve s t i t edove rawi der angeo ft emG ga r a t u r e sands t r a i nr a t e sus i ngaGl e eb l e G 3500t he rmo G s imu l a t i onma ch i ne.Ther e su l t sshowt ha tt hef l ows t r e s si n G pe c r e a s edwi t hs t r a i na tf i r s t,andt heng r adua l l c r e a s eda f t e rr e a ch i ngape akva l ue.Thef l ows t r e s ss o f t en i ngr a t e yde a tah i t r a i nr a t ewa sl a r rt hant ha ta tal ows t r a i nr a t e.Thee f f e c t so fde f o rma t i onhe a t i ngandf r i c t i ononf l ow ghs ge s t r e s swe r eana l z ed.Anewf r i c t i onc o r r e c t i onme t hod,whe r e i nt hee f f e c to fs t r a i nonf r i c t i ona lc oe f f i c i en twa sc on G y , s i de r ed wa se s t ab l i shedhe r e.Thes t r e s s e sr e v i s edbyt henew me t hodde v i a t edf r omt heme a su r eds t r e s s e swi t hi n G c r e a s i ngs t r a i n.Me anwh i l e,t heappa r en tf r i c t i ona lc oe f f i c i en tva r i a t i onl aw wi t hs t r a i nwa sob t a i ned.Thef r i c t i ona l c oe f f i c i en ti nc r e a s eda st hes t r a i ni nc r e a s edandt hens l i t l c r e a s eda f t e rma i n t a i n i ngac ons t an tva l ue.Thes t r e s s gh yde wa sc o r r e c t edbyc ons i de r i ngde f o rma t i onhe a t i ng.Thea c cur a cyo ft het empe r a t ur ecor r e c t i onme t hodwa sve r i f i ed us i ngaspe c i a lexpe r imen t.Ther e su l t so ft heve r i f i c a t i onexpe r imen tshowt ha tt het empe r a t u r ec o r r e c t i on me t hod exh i b i t edagooda c cu r a cyi nc a l cu l a t i ngt heva r i a t i ono fs t r e s sc aus edbyde f o rma t i onhe a t i ng.Ac ons t i t u t i vemode l c ons i de r i ngs t r a i nwa sp r opo s edhe r et ode s c r i bet hede f o rma t i onbehav i o r s.Compa r edwi t hexpe r imen t a lda t a,t he mod i f i edc ons t i t u t i vemode lexh i b i t edagooda c cu r a cya st oc ons t i t u t i vec o r r e l a t i on. Ke r d s:f r i c t i onc o r r e c t i on;t empe r a t u r ec o r r e c t i on;de f o rma t i onhe a t i ng;f l ows t r e s s;c ons t i t u t i vemode l ywo
Du r i ngap l a s t i cde f o rma t i on p r o c e s s,t he mi G [ ] c r os t ruc t u r a levo l u t i ono fa l l oysi sc omp l ex1G3 . I ti s we l l Gknownt ha tt het he rmo Gme chan i c a lpa r ame t e r s wi l la f f e c tt he mi c r o s t ruc t u r a levo l u t i on,f l ow be G [ ] hav i o randp r ope r t i e so fa l l oys4G6 .Fu t he rmo r e,t he f l ow behav i o ri sa l s oi n f l uenc ed by t he ma t e r i a l r ope r t i e s.Att hei n i t i a ls t age o fde f o rma t i on,a p wo rk G ha r den i ngbehav i o ro c cu r r ede spe c i a l l o ra l G yf l oyswi t hl ame l l a rs t ruc t u r eo rl ows t a ck i ngf au l ten G [] e rgy,sucha seu t e c t o i ds t e e landt i t an i um a l l oy7 . Thedynami cr e c ove r e c r t a l l i z a t i onhaves i G yandr ys g n i f i c an te f f e c t si ns o f t en i ng;howeve r,t he wo rk ha rden i ng wi l ll e adt os t r a i nha r den i ng.The r e f o r e, t het he rma lp l a s t i cf o rmi ngbehav i o ri sac ompe t i t i ve r oc e s sbe twe en wo rk ha r den i ng anddynami cso f G p
t en i ng me chan i sms.Thus,i ti sne c e s s a r odeve l op yt asu i t ab l econs t i t u t i veequa t i ont ode s c r i bet hecomG l excompe t i t i vep r oc e s s. p Thei so t he rma ls t r e s s G s t r a i nda t aa r er equ i r ed [ ,] f o rt hecons t i t u t i vebehav i o rana l i s8 9 .Howeve r, ys whent hes t r a i nr a t ei s mo r et hanac e r t a i nva l ue, -1 sucha s0 8s ,t hea c t ua lt empe r a t ur eo faspe c i G
menmayva r i a t ef r omt hep r e s e tt empe r a G yanddev t ur eduet ot hep l a s t i cde f o rma t i onhe a t i nggene r a t ed [ ] f r om p l a s t i cwo r k10 . I na dd i t i on,t hei n t e r f a c i a lf r i c t i on i si n e v i t ab l edu r i ng d e f o rma t i onb e twe e nt hes e c ime n p andd i e s.Event houghl ubr i c a t i oni sus edt o mi n i G mi z et hei n t e r f a c i a lf r i c t i on,t hee f f e c to fl ubr i c a t i on ont hei n t e r f a c i a lf r i c t i oni sno ta lwaysve r s G ygoode c i a l l i ngl a r f o rma t i ons.Be c aus et hef r i c G pe ydur gede
Founda t i onI t em: I t em Spons o r edbyNa t i ona lNa t ur a lSc i enc eFounda t i ono fCh i na ( 51474092);I r onandS t e e lJ o i n tFundso fHebe iPr ov i nc eo f Ch i n a( E2015209243);I nno v a t i onT e am Le a d i ngT a l e n ti nUn i ve r s i t i e sCu l t i va t i onP l ano fHebe iPr ov i nc eo fCh i na ( LJRC007) B i o r aphy: Hong G b i nLI,Ma s t e r; E Gma i l: l i hongb i nxp@126 c om; Re c e i v e dDa t e:De c embe r30,2015 g Co r r e s i ngAu t ho r:En G l i nYU,Do c t o r,Pr o f e s s o r; E Gma i l:yuen l i n@ysu edu cn pond
I s sue9 Cons t i t u t i veMode lo fWa rm De f o rma t i onBehav i o ro fMed i um Ca r bonS t e e l
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t i on wi l lc aus ei nhomogeneousde f o rma t i on o ft he [ ] spe c imens11 ,s omee r r o r so c cu ri nt hec a l cu l a t i on o fcons t i t u t i vemode lpa r ame t e r s.The r e f o r e,Evans [ [ 12] 13] , andScha rn i ng Me nge ta l a swe l la sEb r ah imi [ ] and Na a f i z adeh14 p r e s en t ed wayst or emovet he j e f f e c to fi n t e r f a c i a lf r i c t i on ont he me a su r edf l ow s t r e s s.Ba s edont her e su l t so fRe f s [ 12, 15],Mo G [ 16] s t a f a e iand Ka z emi n e z h a d c o r r e c t e dt h ef l ows t r e s s,
duc t edonaGl e eb l e G 3500t he rmo Gme chan i c a ls imu l a G t o ra tf ourd i f f e r en tde f o rma t i ont empe r a t ur e s( 550, 600,650,and700 ℃ )andf i ved i f f e r en ts t r a i nr a t e s -1 ( , , , , ) , 0 001 0 01 0 1 1 and10s r e spe c t i ve l y. Thespe c imens we r ecomp r e s s edt oas t r a i no f0 8 andhe a t e dt ot hed e s i e df o rmi ngt empe r a t ur ea ta gn -1 , he a t i ngr a t eo f10℃ s t he nhe l df o r3mi nt oe l imi G n a t et het he rma lg r ad i en tbe f o r ede f o rma t i on.The compa r edt hed i f f e r enc ei nf l ow s t r e s sc o r r e c t edby f l ows t r e s scur ve swe r ea c i r edau t oma t i c a l l i ng qu yus [ [ 12] 13] , Evansand Scha rn i ng and Meng e ta l and t het he rmo Gme chan i c a ls imu l a t o r.Toob t a i nt hede G co r r e c t edt hes t r e s so ft head i aba t i che a t i nge f f e c t. f o rmedmi c r o s t r u c t u r e,t hes e c ime n swe r eimme d i a t e G p [ ] [ ] L i ne ta l 17 a nd Zh a ng e ta l 18 c o r r e c t e dt h ef l ow l nco l dwa t e ra f t e rcomp r e s s i on. yquenchedi s t r e s sba s edont her e su l t sr e r t e di nRe f [ 14].The po 2 Re s u l t sandDi s c u s s i on abov e Gmen t i oned me t hodsr equ i r eaf r i c t i onf r a c t i on t oco r r e c tt hef l ow s t r e s s.Howeve r,t hef r i c t i on 2 1 Ana l s i so ff l ows t r e s sa ndmi c r o s t r u c t u r a le v o l u t i o n y [ 19] f r a c t i onva r i e swi t hs t r a i n andi sd i f f i cu l tt ocon G F i 2showst hef l ows t r e s s e so fmed i um c a r G g f i rma c cu r a t e l r e f o r e,i ti sne c e s s a r oc o r r e c t bons t e e ldur i ng wa rm de f o rma t i on.Theva l ue so f y.The yt t hes t r e s scu r vei nt e rmso fde f o rma t i onhe a t i ngand t hes t r e s s e swe r eobv i ous l f f e c t edbyt hede f o rma G ya i n t e r f a c i a lf r i c t i onwh i l ec ons i de r i ngt hes t r a i n. t i ont emp e r a t u r eands t r a i nr a t e.Thes t r e s si n c r e a s e d Thes t udya imst oempha s i z et hene c e s s i t f wi t hi nc r e a s i ngs t r a i nr a t eandde c r e a s i ng de f o rma G yo , f l ows t r e s sc o r r e c t i onsf o rmed i umc a rbons t e e land t i ont empe r a t ur e.I n gene r a l t heva r i a t i onsi nt he t oe s t ab l i shac ons t i t u t i ver e l a t i ont ode s c r i bewa rm f l ows t r e s swi t ht empe r a t ur eands t r a i nr a t ewe r ea t G de f o rma t i onbehav i o rbyc ons i de r i ngt hec ompens a G t r i bu t edt ot hee vo l u t i ono fd e f o rma t i onme c han i sms. t i ono ft hes t r a i nr a t e. Att he beg i nn i ng o f de f o rma t i on,t hef l ow s t r e s si nc r e a s edr ap i d l e a ched a max imum; y andr
1 Exp e r imen t a l
Theexpe r imen t a lma t e r i a lwa sa med i um c a r G bons t e e lwi t hchemi c a lc ompo s i t i onso fC0 46,S i 0 23,Mn0 72,P0 03,S0 03,Ni0 02,Cr0 02, Cu0 03,and Feba l anc e( i n ma s s% ).Cy l i nd r i c a l
t hent heme chan i sm o fso f t en i ngde c r e a s edwi t hi n G c r e a s i ngt empe r a t ur eandde c r e a s i ngs t r a i nr a t e.The
spe c imenswi t had i ame t e ro f10mmandahe i to f gh 15 mm we r ema ch i nedf r om aho tr o l l edba rwi t ha d i ame t e ro f13 mm.Thei n i t i a l mi c r o s t ruc t u r ei s showni nF i 1,wh i chshowst ha tt heda rka r e ai s g a r l i t e( P)andt hewh i t ea r e ai sf e r r i t e( F).The pe , me ang r a i ns i z ei sabou t20μm me a su r edbyt hei n G t e r c ep tme t hod.Wa rmcompr e s s i ont e s t swe r econ G
F i 1 I n i t i a lmi c r o s t r u c t u r eo fme d i umc a r bon g s t e e lf o rc omp r e s s i ont e s t
F i 2 F l ows t r e s so fme d i umc a r bons t e e lme a s u r e d g du r i ngwa rmc omp r e s s i on
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J ou r na lo fI r onandS t e e lRe s e a r ch,I n t e r na t i ona l Vo l 23
s t r e s scu r ve sf o rah i t r a i nr a t eandl owt empe r a G ghs t ur eexh i b i t ed add i t i ona lf l ow s o f t en i ng a f t e rt he aks t r e s s.Th i si si nc on t r a s t wi t ht he gene r a l pe e f f e c tru l eo ft empe r a t u r eands t r a i nr a t eont hef l ow s t r e s s. I ti sc aus edbyt he mi c r o s t ruc t u r a lva r i a t i on o f med i um c a rbon s t e e l.No rma l med i um c a rbon s t e e li sc ompo s edo ftwo pha s e s:po l lf e r r i t e ygona andl ame l l a rc emen t i t e.Du r i ngde f o rma t i on,t hel a G [ ] me l l a rc eme n t i t eb e nd s,f r a c t u r e so rd e c ompo s e s20 , wh i l et hef e r r i t er e c ove r so rr e c r t a l l i z e s.The s e ys va r i a t i onsi nt hetwopha s e sl e adt ot hede c r e a s eo f , t hef l ows t r e s s.Atah i t r a i nr a t e dynami cr e G ghs cove r l lo c cu ri nf e r r i t eandt hec emen t i t e wi l l y wi bendo rf r a c t u r e.Th i si sj us tano t he rc emen t i t edy G
nami csphe r o i d i z a t i onme chan i smt ha ti sdemons t r a G [ ] t edbyRa s t ega r ie ta l 21 . I tc aus e st hes t r e s st ode G c r e a s ebeyondt hepe aks t r e s swi t hah i t r a i nr a t e. ghs , Atal ows t r a i nr a t et hedynami cr e c r t a l l i z a t i ono f ys f e r r i t eoc cur r ed,andc emen t i t ede compos ed,f o rmG i ngs eve r a lsma l lpa r t i c l e s.Thepa r t i c l e swou l dp i n t hed i s l oc a t i onso rg r a i nbounda r i e sdur i ngde f o rma G t i on.Thepa r t i c l e sp l ayedt her o l eo fs t r eng t hen i ng, andhenc e,t heso f t en i ngo ft hes t r e s swa sno tobv i G , ous t houghdynami cr e c r t a l l i z a t i ono ff e r r i t eoc G ys cur r eda tal ow s t r a i nr a t e.Cemen t i t ef r a c t ur eand ( de compos i t i on we r e obs e r ved s i ng l ea r r ow i n F i 3( a)and3( b)),andf e r r i t edynami cr e c r t a l G gs ys l i z a t i onoc cur r ed ( doub l ea r r owi nF i 3( b)). g
( a)600°C,10s-1; ( b)600°C,0 01s-1.
F i 3 Cemen t i t ef r a c t u r eandd e c ompo s i t i ona td i f f e r en ts t r a i nr a t e s g
2 2 Fr i c t i onc o r r e c t i ono ff l ows t r e s sc u r v e As chema t i cd i ag r am o ft he de f o rma t i oni s showni nF i 4. g
( a)Be f o r ec omp r e s s i on; ( b)Af t e rc omp r e s s i on.
F i 4 S ch ema t i cd i a r amo fs e c imenc omp r e s s i ont e s t g g p
Du r i ngt hep l a s t i cde f o rma t i on,f r i c t i oni suna G vo i dab l aus edbyt her e l a t i ve mo t i onbe twe ent he yc spe c imensandd i e s.Thef r i c t i onbe twe ent hespe c i G mensandanv i l swou l di n f l uenc et hede f o rma t i ono f me t a l s. I nt h i sexpe r imen t,t hef r i c t i onbe twe enspe c i G
mensandanv i l sa f f e c t edt hes t r i c a lde f o rma G ymme t i ono ft hespe c imen.Thes t r a i n G s t r e s sda t ar e co rded byt het e s t i ngs t emcon t a i nedt hei n f l uenc eo ff r i c G ys , t i on.Thus t hef l ows t r e s sa c i r edbyt e s t i ngsys G qu t e rmshou l dbe mod i f i edbye l imi na t i ngt hef r i c t i on i n f l uenc e.Thef l ows t r e s sc anbemod i f i edus i ngt he [ ] me t hodr e r t e di nRe f s 12 G 14 .Thef o l l owi nge a G po qu t i on shavebe enus edi nRe f [ 12]: σ0 ( σ= 1) 1+ ( 2/3 3) m( R0/h0) exp( 3 ε/2) andi nRe f [ 13]:
σ0 ( σ= 2) 1+ ( 2mRe/3 3h) whe r e, σi st hef r i c t i onco r r e c t ed; σ0i st heme a sur ed ; ; f l ows t r e s s e s εi st het rues t r a i n mi st hef r i c t i ona l coe f f i c i en t;h0i st hei n i t i a lhe i to fspe c imens;hi s gh t hespe c imenshe i i ngde f o rma t i on;Rei san ghtdur equ i va l en tr ad i us;andR0i st hei n i t i a lr ad i us. [ ] Ebr ah imiand Na a f i z adeh14 expr e s s edt hei n G j t e r f a c i a lf r i c t i onco r r e c t edequa t i ona sf o l l ows:
I s sue9 Cons t i t u t i veMode lo fWa rm De f o rma t i onBehav i o ro fMed i um Ca r bonS t e e l
σ0C2 ( σ= [ ( ) 3) 2 exp C -C -1] whe r e,C i st hec o r r e c t i onc oe f f i c i en to fi n t e r f a c i a l , : f r i c t i on wh i chi sexp r e s s eda s ( C =2m/h 4) 0 5 ( Re=R0/( 5) h0/h) [ , ] , I nRe f s 12 13 m wa sc ons i de r edt obe0 2. I nRe f [ 14],m wa seva l ua t edus i ngt hef o l l owi ng : expr e s s i on ( Re/h) b ( 6) m = ( 2 4/ 3)- ( b/3 3) ΔRh b=4 ReΔh ΔR =R M -RT
( 7) ( 8)
h0 ( 9) RT = 3 R2 R2M 0 -2 h ( Δh=h0 -h 10) whe r e,R M i st he max imumr ad i us;RT i st hehe ad r ad i us;andbi st hebu l kc oe f f i c i en t. F i 5showst ha tt hemax imum d i ame t e rchan G g sdu r i ngt hec omp r e s s i ont e s t;henc e,i ti sne c e s G ge s a r oc o r r e c tt hef r i c t i onus i ngt her e a l G t imeR M yt andt hehe i tdu r i ngde f o rma t i on. gh Du r i ngt hepr o c e s so fde f o rma t i on,t hei n t e r f a G c i a lf r i c t i oni sa f f e c t edbyt hede f o rma t i on.Ther e a l G t ime ma x imum r a d i u s wa s me a s u r e du s i nga Gl e e b l e G 3500C GGauges ens o r.Theva l ueo fR M i sshowni n F i 5. I tc anbes e ent ha tt hed i f f e r enc eo fR M unde r g , d i f f e r en tc ond i t i onsi si ns i i f i c an t. I nt h i sc a s et he gn e f f e c t so ft hef o rmi ngt empe r a t u r eands t r a i nr a t eon RM c anbeneg l e c t ed.
943
F i 5 Va r i a t i oni nRM du r i ngd e f o rma t i on g
anbec a l G Ac co rd i ngt oEq ( 6),t heva l ueo fm c cu l a t edus i ngR M andh.Theva l ue so fC andm a r e showni nF i 6.Theva l ueo fC i nc r e a s ed wi t ht he g sshowni n s t r a i n.Thef i t t i ngf o rmu l af o rC andm i n i t i a l l n G Eq s ( 11)and ( 12).Theva l ueo fm i yi c r e a s edt oape akva l ue ( 0 25)t henr ema i nedcon G , s t an t.Af t e rt ha ti tde c r e a s eds l i t l t hi nc r e a s G gh y wi i ngs t r a i n.Atas t r a i no f0 8,t heva l ueo fm wa s 0 19andshowedl i t t l ed i f f e r enc ewi t ht heva l ueus ed [ , ] i nRe f s 12 13 .Theconc en t r a t i ono fl ubr i c an tde G c r e a s edwi t hi nc r e a s i ngs t r a i n,andt hef r i c t i ona lco G [ ] e f f i c i en ti nc r e a s ed19 .Thei nc r e a s eo ff r i c t i ons t r e s s wa sc aus ed by t hei nc r e a s e si n bo t hf r i c t i on and s t r e s swi t hs t r a i n.Onc et hef r i c t i ons t r e s sexc e eded , t hey i e l ds t r e s so ft hespe c imen t her e l a t i veg l i de be twe ent hespe c imensandd i e ss t opped.Thec l i n G y de rp r o f i l ei sshowni nF i 7,andt hef r i c t i ona lcoe f G g ( ) f i c i en tob t a i nedbyEq 12 de c r e a s ed.
( a)Re l a t i onbe twe enC andε; ( b)Re l a t i onbe twe enm andε.
F i 6 Re l a t i onb e twe enC,m ,andε g
( C =-0 654 ε-0 180 ε2 11) 2 3 m =-0 109-5 162 ε-31 155 ε -98 494 ε- ( 168 719 ε4 -146 602 ε5 -50 557 ε6 12) Thec o r r e c t edr e su l t sus i ng d i f f e r en t me t hods a r eshowni nF i 8.Thed i f f e r enc ebe twe enc o r r e c G g
t edandunco r r e c t edcur ve sg r adua l l nc r e a s ed wi t h yi [ 16] s t r a i n . I ti squ i t econs i s t en twi t ht hea c t ua ls i t ua G t i ono facomp r e s s i ont e s t.Atas t r a i no f0 8,t he s t r e s sco r r e c t edby Eq ( 3)wi t ht her e a l G t ime R M wa sequa lt ot heone sco r r e c t edbyEq ( 3)wi t ht he
944
J ou r na lo fI r onandS t e e lRe s e a r ch,I n t e r na t i ona l Vo l 23
F i 7 S imp l er ep r e s en t a t i ono fup t u rn i ng g
F i 8 Compa r i s ono fme a s u r e dandc o r r e c t e dc u r v e s g
f i na lR M .Bu tf o rt hewho l ep r o c e s s,t hes t r e s sco r G ( ) r e c t edby Eq 3 wi t ht her e a l G t imeR M wa s mo r e cons i s t en twi t ht her e a ls t r e s st h a nt h a tw i t ht h ef i n a l
R M .The pr ed i c t edf r i c t i on l e s ss t r e s sc a l cu l a t ed by Eq ( 2)wa sl e s st hant ha tc a l cu l a t edbyEq ( 1).The s t r e s sc a l cu l a t edbyEq ( 1)i sc l os et ot ha tob t a i ned ( ) byEq 3 wi t ht her e a l G t imeR M .Thef r i c t i onf a c t o r wa scons i de r edt obe0 2i nRe f s [ 12, 13],bu tQi an [ ] e ta l 10 cons i de r edt ha tt hef r i c t i onf a c t o rwa s0 3. , I nf a c tt hef r i c t i onf a c t o rva r i eddur i ngt hef o rmi ng. Fo r t una t e l hef r i c t i onf a c t o rc anbededuc edf r om y,t Eq ( 6)by me a sur i ngt her e a l G t imeva l ueo fR M . 2 3 An a l s i so ft emp e r a t u r ev a r i a t i o nd u r i n e f o rma t i o n y gd Mos to ft heene r st r ans f o rmedi n t ohe a t gy wa wh i l eaf r a c t i ono ft heene r ss t o r edi nt hespe c G gywa [ 22] imensi nt hef o rm o fd i s t o r t i on ene r ft he gy .I , s t r a i nr a t ei sh i ri tc aus e sani nc r e a s ei ns t r e s s ghe andade c r e a s ei nt hede f o rma t i ont ime;henc e,mos t o ft hede f o rma t i onhe a tc anno tber emovedf r omt he spe c imens.Thes amp l et empe r a t ur et heni nc r e a s e s duet ot hede f o rma t i on he a t i ng.I nt h i sc a s e,t he t empe r a t ur eva r i a t i onmaybes i i f i c an t. gn , Fo rt hecomp r e s s i ont e s t s t het empe r a t ur ei s showni nF i 9.Thet empe r a t ur ei nc r e a s edwi t hi n G g c r e a s i ngs t r a i nandde c r e a s i ngde f o rma t i ont empe r a G t ur e.Fur t he rmo r e,t het empe r a t ur eva r i a t i ona ta s t r a i nr a t eo f0 1s-1 wa sve r l landcou l dbei G ysma g
F i 9 Cu r v e so ft emp e r a t u r ev a r i a t i ondu r i ngd e f o rma t i on g [ ] no r ed16 ,a sshowni nF i 9( b). g An Ar rhen i us G t t i oni sa lwaysus edt o ypeequa de s c r i bet het he rma lde f o rma t i onbehav i o ro ft hea l G l oys.Thet empe r a t u r eva r i a t i ondu r i ngde f o rma t i on i sco r r e c t edbyus i ng Ar rhen i usequa t i onandZene r G [ ] Ho l l omi npa r ame t e ra sf o l l ows23 : æ ö çQ ÷ ( ÷÷ Z =̇ 13) εexpçç R è Tø ( Z =A1σn1 ( α σ<1 2) 14) ( ( Z =A2exp( σ) α σ>1 2) 15) β n ( ) ( ) ( Z =As i nhα σ Fo ra l lσ 16) whe r e,A1 ,A2 ,A ,n1 ,n andβ a r e ma t e r i a l spa G
̇ r ame t e r s;αi st hes t r e s smu l t i l i e r( α=β/n1 ); s εi p ; t hes t r a i nr a t e Qi st heappa r en ta c t i va t i onene r gy; Ri st heun i ve r s a lga scons t an t;andT i st heabso G l u t et empe r a t ur e. By subs t i t u t i ng Eq ( 13)i n t o Eq s ( 14)and ( 15)andt hent ak i ngt hel oga r i t hmandr e a r r ang i ng Eq s ( 14)and ( 15),t hef o l l owi ngequa t i onsc anbe ob t a i ned: é æ öù ê ΔT ç Q ÷ú ê x ç ÷ ú ( Δσ=σ e α σ<1 2) ( 17) pç êê n T +ΔT )÷ø úúû ë è 1RTT ( Q æç ΔT ö÷ ÷ Δσ= çç +ΔT ÷ø è βR T
( α σ>1 2) ( 18)
I s sue9 Cons t i t u t i veMode lo fWa rm De f o rma t i onBehav i o ro fMed i um Ca r bonS t e e l
Ac c o r d i ngt oRe f [ 24],αi sabou t0 003,and i ti se a s oge tt ha ti ft hes t r e s si sg r e a t e rt han350 yt MPa.Eq ( 17)i ssu i t ab l ef o rde f o rma t i onc ond i t i on -1 -1 -1 , , , sucha s700 ℃ 10s o r1s and650 ℃ 1s . Ot he rwi s e,Eq ( 18) i ssu i t ab l ef o rde f o rma t i onconG d i t i onss u c ha s550℃ ,10s-1o r1s-1 ,600℃ ,10s-1 o r1s-1 ,and650 ℃ ,10s-1 .Thepa r ame t e rc a l cu l a G t i onpr o c e s si sshowna sf o l l ows. Ba s edont he me a su r edda t a,as t r a i no f0 4 wa st aken a s an c a s et o de s c r i bet he c a l cu l a t i on oc e s so ft hema t e r i a lc ons t an t s.Us i ngt hena t ur a l pr ( ) ( ) , l oga r i t hmf o rEqs 14 and 15 t hef o l l owi ngr e G l a t i onc anbeob t a i ned: ̇ ( l n nA1 +n1l σ ε=l n 19) ̇ ( ε=l nA2 +β σ 20) l n Then,subs t i t u t i ng t hef l ow s t r e s so fs t r a i n , 0 4 wh i ch wa s ob t a i ned du r i ng t he c omp r e s s i on t e s t,ands t r a i nr a t ei n t oEq s ( 19)and ( 20),i tc an tt her e l a t i onbe twe ent hef l ow s t r e s sands t r a i n ge , r a t ej us ta sshowni nF i 10. g ̇ εandl I ti sobv i oust ha tt hel i ne so ft heσG l n n σG
̇ l n εc anbec ons i de r edt obepa r a l l e l,andt hen1andβ
945
equa lt ot hes l opo ft hepa r a l l e ll i ne s,r e spe c t i ve l y. Cons i de r i ngt hee f f e c to ft empe r a t ur eonn1 andβ, t a i nedbyl i ne a rf i t t i ng t heme anva l ue so fn1andβob -1 , me t hoda r e10 567and0 035 MPa r e spe c t i ve l y. The r e f o r e,αi scons i de r edt obe0 0033. Fo ra l lt hes t r e s sl eve l s,Eq ( 15)c anbed i f f e r G , en t i a t edandt hus d l n[ s i nh( α σ)] ( 21) Q =R n d( 1/T ) ̇ d( l n ε) ( n= { [ ( )]} 22) σ dl ns i nhα Bysubs t i t u t i ngt het empe r a t ur e s,s t r a i nr a t e s ( ) ( ) ands t r e s s e s a tas t r a i no f0 4 i n t oEq s 21 and ( 22),t her e su l t s we r eob t a i nedanda r eshowni n
F i 11. g Theva l ue so fn and Q a r ec a l cu l a t edt o be 7 677and384 810kJmo l-1 ,r e spe c t i ve l y. Thed a t awi t hc o r r e c t e dt emp e r a t u r e sa r es howni n F i 12.F i 12( a)showst her e su l t sco r r e c t edf o r g g t empe r a t ur e.Thed i f f e r enc ebe twe enr e su l t sco r r e c G t edbyEq s ( 17)and ( 18)i sve r l i t;t hus,t he ys gh e f f e c to fus i ng d i f f e r en tequa t i onsi sneg l i i b l e.I n g t h i sr e s e a r ch,Eq ( 18)i sus edt oco r r e c tf o rt hei n G
̇ ̇ ( a)l n σG l n ε; ( b)σG l n ε.
F i 10 Re l a t i onb e twe ent h es t r a i nr a t eandf l ows t r e s s g
F i 11 Ca l c u l a t i on so fQ andn g
946
J ou r na lo fI r onandS t e e lRe s e a r ch,I n t e r na t i ona l Vo l 23
( a)10s-1; ( b)Compa r i s onbe twe enme a sur edandc o r r e c t eds t r e s s e s.
F i 12 Cu r v e so fs t r e s sc o r r e c t e df o rd e f o rma t i onh e a t i ng g
f l uenc eo fde f o rma t i onhe a t i ng. F i 12( b)showst he g compa r i s onbe twe ent h et emp e r a t u r ec o r r e c t e ds t r e s s ( ) ba s edonEq 18 andt he me a su r eds t r e s swi t hi n G c r e a s i ngt empe r a t u r ef r om550t o700 ℃ du r i ngde G f o rma t i onwi t has t r a i nr a t eo f0 01s-1 .Thec o r r e c G t eds t r e s sva l ue sc o i nc i de we l l wi t ht he me a sur ed s t r e s s.
2 4 Con s t i t u t i v ee t i on so ff l ows t r e s sf o rme d i um qua c a r bons t e e l Ba s edont hes t r e s sc o r r e c t edf o rf r i c t i onand de f o rma t i on he a t i ng,t he p r o c e s so fe s t ab l i sh i ng cons t i t u t i veequa t i onsi ss imi l a rt os e c t i on2 2. Ac c o r d i ngt ot hec a l cu l a t i onr e su l t s,t hev a l u e s o fα,n1 a ndβa r e0 0035,9 294,a nd0 033 MPa-1 ,
r e spe c t i ve l l ue so fn and Q a r e6 673and y.Theva 353 565kJmo l-1 ,r e spe c t i ve l y. Tak i ngt hel oga r i t hmo fbo t hs i de so fEq ( 16),
t hef o l l owi ngequa t i onc anbeob t a i ned ( l nZ =l nA +nl n[ s i nh( α σ)] 23) , Ba s edont heexpe r imen t a lr e su l t st heva l ue so f r et hei n t e r c ep tands l opeo fonl nAG l n l nA andn a [ s i nh( α σ)]p l o t,r e spe c t i ve l heva l ueo fA y.Thus,t 19 c anbee a s i l a l cu l a t edt obe1 338×10 . yc I ns imi l a r ways,t heva l ue so f ma t e r i a lcon G Q ,A ,n,andα)o ft hec ons t i t u t i veequa t i on s t an t s( we r ec ompu t edunde rd i f f e r en tde f o rma t i ons t r a i ns wi t h i nt her angeo f0 05-0 80i ni n t e r va l so f0 05. Ther e l a t i onbe twe enQ ,A ,n, α,andt hes t r a i nf o r , med i um c a rbons t e e lc an be po l a lf i t t ed a s ynomi showni nF i 13. g Asc anbes e eni nF i 13( a),t hea c t i veene r g gy , i n i t i a l l c r e a s edwi t hs t r a i nr e a chedi t smi n imum yde va l uea tas t r a i no f0 45, i n c r e a s e dupt o362 86k J mo l-1 a tas t r a i no f0 7,andf i na l l d e c r e a s e dt o y -1 357 32kJ mo l a tas t r a i no f0 8.Theva l ue sa r e l e s st hant ha tr epo r t edf o rmed i umc a rbons t e e lwi t h
F i 13 Va r i a t i on so fQ ( a),α ( b),n ( c),and g A( d)wi t hs t r a i nba s e donpo l a lf i t t i ng ynomi
I s sue9 Cons t i t u t i veMode lo fWa rm De f o rma t i onBehav i o ro fMed i um Ca r bonS t e e l
ama r t ens i t emi c r o s t ruc t u r e24 .Th i sr e f l e c t st hef a c t t ha ta i rc oo l ed med i um c a rbon s t e e lha sa be t t e r wo rkab i l i t hanquenchedmed i umc a rbons t e e l.Ac G yt ( ) , co rd i ngt oF i 13 b t heva l ueo fα i n i t i a l l G g y de c r e a s edt ot hemi n imumva l uea tas t r a i no f0 1,and i nc r e a s eds t e ad i l t hi nc r e a s i ngs t r a i n, l i ngi nt he ywi y -1 r ange o f0 0033 - 0 0038 MPa .Re f e r r i ng t o F i 13( c),t heva l ueo fni n i t i a l l c r e a s edwi t hi n G g yde c r e a s i ng s t r a i n,and r e a ched t he mi n imum,t hen s l i t l nc r e a s ed.Theva l ue so ft he s epa r ame t e r so f gh yi t hecons t i t u t i vemode la r es imi l a rt ot heda t ar epo r G [ ] t edbyL ie ta l 24 . anbe Ac c o r d i ngt oEq ( 16),t hef l ows t r e s sσc opo s eda saf unc t i ono ft heZene r GHo l l omon pa G pr , r ame t e r.The r e f o r et hep r opo s edc ons t i t u t i vemode l c anbesumma r i z eda sf o l l ows: [ ]
ö2 n éæ ù1 2 üï ê çZ ÷ ú 1 ìïï æçZ ö÷1 n ï ( níïï çç ÷÷ + êêê çç ÷÷ +1úúú ýïï σ= l 24) α î èA ø ë èA ø û þ Q=373 659+190 922 ε+562 370 ε2-123 956 ε3- /
/
/
947
ε4 -6628 ε5 -3 3670 855 475 646×103ε6 ( 25)
004+0 021 ε+0 158 ε2 +0 ε3 + α=0 566 ( 1 042 ε4 +0 948 ε5 +0 337 ε6 26) 2 3 n=11 213+71 501 ε+477 535 ε +1589 218 ε+ ( 2746 634 ε4 +2354 472 ε5 +791 082 ε6 27) A =6 130×1019 +5 56×1020ε+1 50×1020ε2 - 22 3 22 4 1 246×10 ε -4 76×10 ε -6 71× ( 1022ε5 -3 29×1022ε6 28)
2 5 Ve r i f i c a t i ono fde v e l ope dc on s t i t u t i v ee t i on s qua Tot e s tt heve r a c i t ft hedeve l opedcons t i t u G yo t i veequa t i on,t hec a l cu l a t edf l ow s t r e s sda t a wa s compa r ed wi t h me a sur emen t sove rt heen t i r et emG r a t ur eands t r a i nr a t er ang ei nv e s t i a t e d,a ss hown pe g i nF i 14. g Thec a l cu l a t edf l ows t r e s s e sp r ov i deagoodap G r ox ima t i ont ot heco r r e c t edva l ue s.Toeva l ua t et he p a c cur a c ft hede f o rma t i onc on s t i t u t i v ee a t i on,t he yo qu
F i 14 Compa r i s onb e twe enf r i c t i on G c o r r e c t e dandc a l c u l a t e df l ows t r e s s e s g
e r r o ra nda v e r a ea b s o l u t er e l a t i v ee r r o r( AARE),be G g twe ent hec a l cu l a t edf l ow s t r e s s( σc )andf r i c t i on co r r e c t edf l ows t r e s s( σe)c a nb ec a l c u l a t e da sf o l l ows: N
R2 =
∑( Ei -E )( Pi -P )
i=1 N
N
∑( Ei -E )∑ ( Pi -P )
i=1
2
i=1
( 29)
1 N Ei -Pi ( Rave= ∑ ×100% 30) Ni=1 Ei whe r e,E i st heexpe r imen t a lda t a;P i st hec a l cu G l a t edva l uebyt hedeve l opedcons t i t u t i veequa t i ons; r et heme anva l ue so fE andC ,r E andPa e spe c t i ve G ; l st henumbe ro fda t a. y andN i Ac co rd i ngt oEq s ( 29)and ( 30),t hemax imum
948
J ou r na lo fI r onandS t e e lRe s e a r ch,I n t e r na t i ona l Vo l 23
R2 wa s0 998 and t he AARE wa s0 547% ,a s showni nF i 15.Th i si nd i c a t e st ha tt he p r opos ed g cons t i t u t i veequa t i onp r ov i de sana c cu r a t ep r ed i c t i on o ft hes t r e s sf o rmed i umc a rbons t e e l.
F i 15 Co r r e l a t i onb e twe enc o r r e c t e dandp r e d i c t e d g f l ows t r e s sdu r i ngc omp r e s s i ont e s t
3 Conc l u s i on s ( 1)Thef l owcu r ve sa th i rs t r a i nr a t e sex G ghe h i b i t edanadd i t i ona ls o f t en i ngt endenc t i t e y.Cemen f r agmen t swe r eobs e r vedt ode f o rmi nt hes amp l e sa t , h i h e rs t r a i nr a t e s a n df e r r i t ed n a m i cr e c r s t a l l i G g y y z a t i ona swe l la sc emen t i t ede c ompo s i t i on we r eob G s e r ved. ( 2)Thef l ow s t r e s s wa ss i i f i c an t l n f l u G gn yi enc edbyde f o rma t i onhe a t i ngandf r i c t i on.Thede G f o rma t i onhe a t i ngc o r r e c t ed me t hodve r i f i edbyex G r imen t a lr e su l t sexh i b i t edagooda c cu r a c nc a l G pe yi , cu l a t i ngt heva r i a t i oni ns t r e s s.Thus anewf r i c t i on me t hod c ons i de r i ng s t r a i n wa se s t ab l i shed.The e f f e c to fs t r a i nont hef r i c t i onf a c t o rwa sobv i ous. ( 3)Ther e l i ab i l i t ft hec o r r e c t edc ons t i t u t i ve yo mode lwa seva l ua t edbys t a t i s t i c a lana l i s.Theco r G ys r e c t edc on s t i t u t i v emod e lp r o v i d e da na c c u r a t ee s t ima t e o ft hes t r e s s.The r e f o r e,t hedeve l opedc ons t i t u t i ve equa t i onsa r er e l i ab l ef o rf i n i t ee l emen tana l i sf o r ys wa rmde f o rma t i onc ond i t i ons.
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