Solubility of graphite in cobalt and nickel
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		    T a M e I . C a r b u H z a t i o n T r e a t m e m u and Resul~
 
 Temperatu~,~ 1126 1173 1173 1275 1392 1392 1393 1425
 
 0.910 0.823 0.982 0.925 0.984 0.641 0.387 0.136
 
 0.090 0.104 0.116 0.210 0.430 0.290 0.176 0.074
 
 Nickel
 
 1124
 
 0.881
 
 1126 1272 1392 1450 1469 1477
 
 0.910 0.932 0.641 0.503 1.0 1.0
 
 10.093 [0.102 0.126 0.190 0.220 0.200 0.387 0.439
 
 DURINGthe
 
 log ac/Y c = A + B / T + C(1 + lOS/T)yc
 
 *The activityis defined as unity for equilibriumwith graphite.
 
 1200 ' 1
 
 2.5
 
 I
 
 1000
 
 900=C
 
 ' [
 
 '
 
 [1]
 
 w h e r e Yc is the a t o m r a t i o , T i s t h e a b s o l u t e t e m p e r a t u r e and A , B , and C a r e t e m p e r a t u r e and c o m p o s i t i o n independent parameters), Smith's data determine C = 2.5 a n d 5.3 f o r Co(C) a n d Ni(C), r e s p e c t i v e l y . S i n c e the l a s t t e r m in E q . [1] is r e l a t i v e l y s m a l l , its c h o s e n t e m p e r a t u r e d e p e n d e n c e is not i m p o r t a n t f o r the p r e s e n t c o n c l u s i o n s . F i g . 1 d i s p l a y s log ac/Yc - C(1 + 103/T)Yc vs T -x f o r the p r e s e n t d a t a and t h o s e of S m i t h . L e a s t s q u a r e s a n a l y s i s of the p l o t t e d d a t a d e t e r m i n e the f o l l o w i n g equations : log ac/Y c = 4110/7" - 1.34 + 2.5(1 + 103/T)Yc
 
 An~ysis, WtPct C
 
 Cob~t J . C. S W A R T Z c o u r s e of e x p e r i m e n t s 1 on the e l e c t r i c a l r e s i s t i v i t y of c a r b o n d i s s o l v e d in c o b a l t and n i c k e l , s e v e r a l m e a s u r e m e n t s of the s o l u b i l i t y of g r a p h i t e were obtained. This report summarizes these measu r e m e n t s and d i s c u s s e s the s o l u t i o n e n e r g i e s a n d entropies. T h i n s a m p l e s of high p u r i t y c o b a l t and n i c k e l w e r e e q u i l i b r a t e d w i t h c a r b u r i z i n g g a s e s by the u s u a l t e c h n i q u e s . 2 T a b l e I l i s t s the a c t i v i t y of e a c h c a r b u r i z i n g a t m o s p h e r e 3 and the r e s u l t i n g c o m b u s t i o n a n a l y s i s . To c o l l a t e t h e s e data o n e m u s t a s s u m e s o m e b e h a v i o r r e l a t i v e to H e n r y ' s l a w . S m i t h ' s d a t a 4 on Co(C) and Ni(C) at 1000~ show d e v i a t i o n s f r o m H e n r y ' s law w h i c h a r e c o m p a r a b l e to t h o s e of y F e ( C ) . A s s u m i n g t h e s e d e v i a t i o n s v a r y w i t h t e m p e r a t u r e Uke t h o s e of Y F e ( C ) ( i . e . , a s s u m i n g a r e l a t i o n of t h e f o r m : s
 
 Acti~ty Rel. to Graphite*
 
 y
 
 3'0
 
 f ,
 
 =,? -
 
 m
 
 .~ 2.0
 
 -
 
 -
 
 o,i u
 
 o
 
 2.5 %
 
 I
 
 --
 
 %
 
 k5
 
 2.0 o
 
 [2]
 
 f o r c a r b o n in c o b a l t , and 1
 
 logac/Y c = 3070/7 -0.54
 
 + 5.3(1 + 103/T)Yc
 
 [3]
 
 7
 
 I
 
 8 104/T,
 
 f o r c a r b o n in n i c k e l . F i g s . 2 and 3 c o m p a r e t h e g r a p h i t e s o l u b i l i t i e s f r o m E q s . [2] and [3] w i t h o t h e r r e c e n t d e t e r m i n a t i o n s . E q s . I2] and [3] and t h e e q u i v a l e n t e q u a t i o n f o r 7 F e ( C ) d e t e r m i n e the v a l u e s in T		
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