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HAL Id: jpa-00221068

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Submitted on 1 Jan 1981

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publics ou privés.

INTERNAL STRESS MEASUREMENT IN

ALUMINIUM BY ”DIP-TEST” METHOD AND

CORRELATION WITH THE BORDONI

RELAXATION EVOLUTION

J. Chicois, A. Hamel, R. Fougères, C. Esnouf, Gilbert Fantozzi, J. Perez

To cite this version:

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JOURNAL DE PHYSIQUE

c'oZZoque C5, suppZ6ment au noIO, Tome 42, octobre 2982 page C5-169

I N T E R N A L STRESS

M E A S U R E M E N T I N A L U M I

N I U M BY

I'D

I P-TEST" METHOD A N D

CORRELATION WITH THE BORDONI RELAXATION EVOLUTION

J . C h i c o i s , A. Hamel, R. FougSres, C. ~ s n o u f

*,

G. ~ a n t o z z i * and J. ~ e r e z *

Laboratoire de Me'taZZurgie e t Traitements Thermiques, B6t. 303

* ~ r o u ~ e drEtudes de M6tallurgie Physique e t Physique des Mate'riaux, E.R.A. 963 BZt. 502, I n s t i t u t National d e s Sciences AppZiqu6es de Lyon

-

69621

Vi

Z Zeurbmzne Cedex, France

Abstract.- The Bordoni r e l a x a t i o n appears only w i t h a s u f f i c i e n t v a l u e of s t r e s s g i v e n by t h e Par6 c o n d i t i o n . We have made a d i r e c t measurement of in- t e r n a l s t r e s s i n o r d e r t o know i t s e v o l u t i o n d u r i n g p l a s t i c deformation o r a n n e a l i n g . T h i s e v o l u t i o n i s compared w i t h t h e behaviour of t h e Bordoni r e l a - x a t i o n : v a r i a t i o n of t h e r e l a x a t i o n s t r e n g t h on t h e one hand and non l i n e a r p r o p e r t i e s on t h e o t h e r hand.

1 . I n t r o d u c t i o n . - It i s w e l l e s t a b l i s h e d t h a t t h e Bordoni r e l a x a t i o n s t r e n g t h i s r e - l a t e d t o t h e s t r e s s amplitude ( 1 ) . Indeed, t h e Bordoni peaks appear only when t h e Par6 c o n d i t i o n i s f u l l f i l l e d : ob2L = 2Wk (1) w i t h 0 = oi + u (ai i n t e r n a l , om ap-

m

p l i e d s t r e s s ) , L = d i s l o c a t i o n l e n g t h and 2Wk = double-kink n u c l e a t i o n energy. Du- r i n g p l a s t i c d e f o r m a t i o n o r a n n e a l i n g , t h e h e i g h t of t h e Bordoni peaks changes and t h i s change c a n b e due e i t h e r t o t h e v a r i a t i o n of d i s l o c a t i o n l e n g t h o r t h e v a r i a - t i o n of i n t e r n a l s t r e s s . T h i s second v a r i a t i o n i s o f t e n n e g l e c t e d . Thus, i s i s i n t e - r e s t i n g t o have a d i r e c t measurement of i n t e r n a l s t r e s s i n o r d e r t o know i t s evolu- t i o n d u r i n g p l a s t i c deformation o r a n n e a l i n g and t o compare w i t h t h e behaviour of t h e Bordoni r e l a x a t i o n . I n p a r t i c u l a r , we have s t u d i e d simultaneously t h e change of i n t e r n a l s t r e s s and t h e non l i n e a r p r o p e r t i e s of t h e Bordoni r e l a x a t i o n , which a r e c o r r e l a t e d w i t h t h e v a l u e of i n t e r n a l s t r e s s .

2. Experimental r e s u l t s i : i n t e r n a l s t r e s s

By d i p t e s t method, i n t e r n a l s t r e s s i s determined on p o l y c r i s t a l l i n e t h i n t u b e s of aluminium 99.999 %. The study i t s e l f i s concerned w i t h t o r s i o n a l c r e e p t e s t s . Maximum s t r e s s g r a d i e n t i s s m a l l e r t h a n 10 % of maximum a p p l i e d s t r e s s . The i n t e r n a l s t r e s s measurements a r e made w i t h a s p e c i a l t e s t machine, s u i t a b l e f o r t h i s t e s t t y p e ( 2 ) . The measurements of t h e c r e e p s t r a i n a r e c a r r i e d o u t w i t h a s p e c i a l s e n s i t i v e c a p t o r , f i x e d on t h e sample i t s e l f . T h i s a p p a r a t u s a l l o w s t o d e t e c t a s t r a i n v a l u e a s low a s 1

o - ~

(2). Samples a r e t h e n submitted t o an a n n e a l l i n g a t 525 K d u r i n g one hour a f t e r a c r o s s s e c t i o n r e d u c t i o n of 7 0 %.

Maximum c r e e p r a t e a r e p l o t t e d v e r s u s s u c c e s s i v e v a l u e s of t h e a p p l i e d s t r e s s i n f i g . 1. T h i s c u r v e p r e s e n t s two r a n g e s : t h e low s t r e s s range i s due t o a n a n e l a s t i c p r o c e s s and t h e high s t r e s s range i s l i n k e d t o a m i c r o p l a s t i c s t r a i n pro- c e s s . S i m i l a r r e s u l t s have been o b t a i n e d on i r o n carbon a l l o y s ( 3 ) . I n t h e high s t r e s s r a n g e , t h e s t r e s s corresponding t o z e r o c r e e p r a t e f o r d i f f e r e n t c r e e p s t r a i n v a l u e s i s determined. As i t w i l l %how below, t h e o b t a i n e d s t r e s s v a l u e s a r e v e r y

c l o s e d t o i n t e r n a l s t r e s s ones. The s t r e s s o b t a i n e d by e x t r a p o l a t i o n a t z e r o t o t a l c r e e p s t r a i n i s t h e i n t e r n a l s t r e s s which i s t y p i c a l of t h e mi.crostructura1 s t a t e of t h e specimen.

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C5-170 JOURNAL DE PHYSIQUE

F i g u r e 2 r e p r e s e n t s t h e e v o l u t i o n of c r e e p r a t e dg a s a f u n c t i o n of a p p l i e d s t r e s s v a l u e s under unloading c o n d i t i o n s .

I n t h i s c a s e , t h e c r e e p s t r a i n , equal t o 3 . ~ 1 O - ~ , i s v e r y lower t h a n t h e p r e p l a s - t i c s h e a r s t r a i n (2.10-'). Assuming t h a t t h e e v o l u t i o n of a n e l a s t i c c r e e p r a t e law i s i d e n t i c a l under l o a d i n g and unloading c o n d i t i o n s , e r r o r v a l u e due t o t h e a n e l a s - t i c p r o c e s s is determined according a n a n a l y s i s method described elsewhere (4). In- t e r n a l s t r e s s +; i s always measured w i t h a p r e c i s i o n b e t t e r t h a n 2 %. I n t e r n a l s t r e s s v a l u e i s c l o s e d t o a p p l i e d s t r e s s one. I t i s i n good agreement with t h e f a c t t h a t thermal s t r e s s component i s v e r y weak i n aluminium a t room temperature. For a p r e p l a s t i c deformation of 2.10-', i n t e r n a l s t r e s s i s p l o t t e d v e r s u s t o t a l c r e e p s t r a i n ( f i g . 3 ) . T y p i c a l i n t e r n a l s t r e s s of t h e m i c r o s t r u c t u r e a s p e c t of specimen i s o b t a i n e d by e x t r a p o l a t i o n a t z e r o t o t a l c r e e p deformation. For s e v e r a l p r e p l a s t i c deformation, e v o l u t i o n of t y p i c a l i n t e r n a l s t r e s s e s i s shown i n f i g . 4. Moreover, f o r a 2 % p r e p l a s t i c s t r a i n , t h e v a r i a t i o n of i n t e r n a l s t r e s s e s with a n n e a l i n g tem- p e r a t u r e i s schown i n f i g . 5. The s t r e s s d e c r e a s e seems t o p r e s e n t two e v o l u t i o n ranges with t h e a n n e a l i n g temperature : one, between room temperature and 340 K, t h e o t h e r above. A t high a n n e a l i n g temperature, i n t e r n a l s t r e s s v a l u e t e n d s towards in- t e r n a l s t r e s s v a l u e o b t a i n e d b e f o r e p r e p l a s t i c deformation.

i.i : i n t e r n a l f r i c t i o n

F i g u r e s 6 and 7 schow t h e e f f e c t of a s t a t i c s t r e s s us on t h e i n t e r n a l f r i c t i o n s p e c t r a measured w i t h a v i b r a t i o n s t r e s s amplitude lower t h a n us. We observe t h a t f o r low p l a s t i c d e f o r m a t i o n t h e s t a t i c s t r e s s i n f l u e n c e i s s t r o n g ( f i g . 6) whereas, f o r important d e f o r m a t i o n , t h e Bordoni r e l a x a t i o n behaviour becomes l i n e a r ( f i g . 7 ) . F i g u r e 8 shows t h e e f f e c t of a n n e a l i n g on t h e non l i n e a r behaviour of t h e Bordoni r e l a x a t i o n . We c a n n o t e t h a t f o r h i g h temperature a n n e a l i n g , t h e Bordoni r e l a x a t i o n becomes v e r y s e n s i t i v e t o t h e amplitude of. t h e a p p l i e d s t r e s s .

3 . Discussion.- I n t e r n a l s t r e s s e s a r e due t o d i s l o c a t i o n s which a r e p r e s e n t i n t h e metal. The r e l a t i o n between i n t e r n a l s t r e s s r i and d i s l o c a t i o n d e n s i t y N i s g e n e r a l - l y given by t h e f o l l o w i n g r e l a t i o n :

r . = a f i (2)

with a a c o n s t a n t parameter. From t h i s r e l a t i o n , t h e i n t e r n a l s t r e s s e v o l u t i o n w i t h p r e p l a s t i c deformation i s given by :

T i

-

+

i 0 = a ( f i -

6)

(3

with T~~ and N o r e s p e c t i v e l y t h e i n i t i a l i n t e r n a l s t r e s s and d i s l o c a t i o n s d e n s i t y v a l u e s . However, t h e d i s l o c a t i o n d e n s i t y can be deduced from t h e a p p l i e d s t r e s s - p l a s t i c deformation c u r v e T, cp by t h e following r e l a t i o n (6) :

with A d a c o n s t a n t v a l u e .

Using a p l a n i m e t e r , t h e e v o l u t i o n of t h e d e n s i t y of d i s l o c a t i o n with p l a s t i c s t r a i n E i s determined from experimental (T

-

e p ) curve according t o r e l a t i o n ( 4 ) . T h i s evoyution c a n b e r e p r e s e n t e d by t h e f o l l o w i n g e x p r e s s i o n :

N

= N O

+

A' Em

d P (5)

w i t h m = 1.16. This r e s u l t i s i n good agreement with t h e ones found by o t h e r s au- t h o r s ( 6 ) and (7)

.

Assuming N >> N o , r e l a t i o n s (3) and (5) can be read a s f o l l o w s : ~ ~ - ~ ~ ~and = aN = A ' c m f i

(4)

n

T .

-

-ciO = K E with K a c o n s t a n t . P

n v a l u e i s equal t o 0.55 which i s near of receding v a l u e (m/2 = 0.58).

F i n a l l y , t h e s e r e s u l t s and t h e good o r d e r of magnitude of d i s l o c a t i o n d e n s i t y deduced from r e l a t i o n ( 2 ) ( e g ~ ~

=

cm-=) i n d i c a t e t h a t experimental r e s u l t s a r e c o h e r e n t .

On t h e o t h e r hand, t h e i n t e r n a l f r i c t i o n experiments show t h a t t h e Pard condi- tion (8) i s not s a t i s f i e d when t h e p l a s t i c deformation i s low ( f i g . 6) o r a f t e r an- nealing ( f i g . 8) because it appears o n l y a badly d e f i n e d peak without s t a t i c s t r e s s . The a p p l i c a t i o n of a b i a s s t r e s s of 5x10-= G r e e s t a b l i s h e d t h e Pard c o n d i t i o n and a

well-defined Bordoni peak appears c l e a r l y ( f i g . 6 and 8 ) .

However, a f t e r a n n e a l i n g , we o b s e r v e a n i n c r e a s e of t h e Bordoni peak a f t e r sup- p r e s s i o n of US : t h u s , t h e a p p l i c a t i o n of us m o d i f i e s t h e i n t e r n a l f r i c t i o n beha- v i o u r

.

For high p l a s t i c deformation, t h e Pard c o n d i t i o n i s always f u l f i l l e d and t h e e f f e c t of a b i a s s t r e s s i s n e g l i g i b l e ( f i g . 7 ) .

By comparison w i t h t h e i n t e r n a l s t r e s s measurements, we can deduce t h a t t h e non l i n e a r behaviour i s observed only when t h e i n t e r n a l s t r e s s e s a r e weak. But from t h e r e l a t i o n (1) and t h e experimental r e s u l t s , t h e Pard c o n d i t i o n i s s a t i s f i e d by s t r e s - s e s lower t h a n t h e i n t e r n a l s t r e s s measured by d i p t e s t ( ~ 5 x 1 0 - s ~ i n s t e a d of ~ 2 x 1 0 - k )

This r e s u l t can b e explained o n l y i f t h e i n t e r n a l s t r e s s e s d i s t r i b u t i o n i s t a - ken i n t o account. Indeed, such d i s t r i b u t i o n s have been observed by " i n s i t u " M.E.T. experiments (9). By d i p t e s t method, we measure t h e mean v a l u e of i n t e r n a l s t r e s s e s which can b e considered a s a "macroscopic" i n t e r n a l s t r e s s (10). On t h e o t h e r hand,

i n t e r n a l f r i c t i o n i s s e n s i t i v e o n l y t o t h e weakest " l o c a l " i n t e r n a l s t r e s s e s . This d i s c u s s i o n a l l o w s u s t o e x p l a i n t h e d i f f e r e n c e between t h e s t r e s s n e c e s s a r y t o f u l - f i l l t h e P a r 6 c o n d i t i o n and t h e i n t e r n a l s t r e s s deduced from t h e d i p t e s t . F u r t h e r - more, t h e f r a c t i o n of d i s l o c a t i o n s submitted t o low i n t e r n a l s t r e s s v a l u e s must de- c r e a s e when t h e p l a s t i c deformation i n c r e a s e s .

I n c o n c l u s i o n , we have observed a q u a l i t a t i v e c o r r e l a t i o n between t h e e v o l u t i o n of t h e i n t e r n a l s t r e s s e s and t h e behaviour of i n t e r n a l f r i c t i o n , e i t h e r a f t e r p l a s - t i c deformation o r a n n e a l i n g . Other experiments must be c a r r i e d o u t t o make more q u a n t i t a t i v e comparison between t h e s e r e s u l t s .

References

. ( I )

G . F a n t o z z i ,

W.

Benoit, C . Esnouf and J . P e r e z , Ann. Phys. F r . , 4 , 7 ( 1 979).

(2) A . Hamel, J. C h i c o i s , R. FougEres and M. T h g o l i e r , J o u r n a l of Physics E , Scien- t i f i c I n s t r u m e n t s , 2 p a r a i t r e .

(3) R. FougSres, A. Hamel and M , T h d o l i e r , Proceedings of ICSMA 5 , Aachen, W. Germany, 1 , 337 (1979).

(4) J. C h i c o i s , A. Hamel, R. FougSres and J. Perez, S c r i p t a Met., sous p r e s s e . (5) I. Kovacs and L. Zsoldos, D i s l o c a t i o n s and p l a s t i c d e f o r m a t i o n s , Pergamon

P r e s s , Oxford, p. 251 (1973).

( 6 ) R. W. Honeycombe, The p l a s t i c deformation of m e t a l s , Edward Arnold (1977).

(7) S. C e r e s a r a , H. Elkholy and T. F e d e r i g h i , Phys. S t a t . S o l . , 8 , 509 (1965). (8)

V.

K. Pard, J. Appl. Phys., 3 , 332 (1961).

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JOURNAL DE PHYSIQUE

Fig. 2 : Evolution of t h e c r e e p r a t e v e r s u s a p p l i e d s t r e s s d u r i n g unloading of t h e sample by succes- s i v e s t e p s .

logi,bth creep rote

preplastic shear strain 2 10-' temperature 290 K

-6--

-7-

+---

inibl phstic strain +creep stram

I I

o

I 000 2000 x d 6

F i g . 3 : Evolution of t h e i n t e r n a l s t r e s s a s a f u n c t i o n of p l a s t i c s t r a i n d u r i n g a c r e e p t e s t .

preplastic shear strain 2 10-' ,+' ,'

4

.

+' test temperature 290 K + / # ,

-

,

.+'

2- 3- ,i + +/ '+

+/c---

---;fl 1-

+'---

+ 0 A & x

lo8

(c')

preplastic shear strain 2 temperalure I -,0.25 ,O ,425 ,o,S 0 -1-

Fig: 1 : Evolution of t h e logarithm of t h e maxlmal c r e e p r a t e a s a f u n c t i o n of t h e l o - -2- garithm of t h e a p p l i e d s t r e s s . P r e p l a s t i c s h e a r deformation b y t o r s i o n equal t o -3- 2 ~ 1 0 - ~ , 5 1 ' 15

,

,

?

,initial +, + , creep stress

,

/ +, * ,,' /

:

/*

.'lanelastic component

+'

;"pccording to the First

,s:%(~~a) A%x104 F i g . 4 : I n t e r n a l s t r e s s and r a t i o

/,:

range of Figure 1

.

I+,/,

I

temperature 290 K

-

of i n t e r n a l s t r e s s and shear modu- l u s v e r s u s p r e p l a s t i c s h e a r s t r a i n by t o r s i o n .

- 5

23

r I preplastit shew strain

0 45

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