pourbaix diagram of cadmium

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Chemical Geology, 54 (1986) 271--278 271 Elsevier Science Publishers B.V., Am sterdam -- Printed in The Netherlands [3] GEOCHEMICAL BEHAVIOR OF ANTIMONY ARSENIC CADMIUM AND THALLIUM: Eh-pH DIAGRAMS FOR 25°C 1-BAR PRESSURE DOUGLAS G. BROOKINS Department of Geology, University of New Mexico, Albuquerque, NM 87131 U.S.A.) (Received September 5, 1985; accepted for publication October 1, 1985) Abstract Brookins, D.G., 1986. Geochemical behavior of antimony, arsenic, cadmium and thallium: Eh--pH diagrams for 25°C, 1-bar pressure. Chem. Geol., 54: 271--278. New Eh--pH diagrams have been derived for Sb, As, Cd and T1. These diagrams are useful in discussing the common association of several or all of these elements around epithermal Au deposits. Slight differen- ces in pH, Eh or both pH--Eh are sufficient to account for partitioning of these elements from deposit to deposit. In addition, chloride concentration--pH diagrams for Au, Hg and T1 are useful to further discuss the role of chloride (and possibly chloride complexes) in the migration of some of these elements under low T,P conditions. 1. ntroduction Many elements have been proposed as pathfinder elements for telethermal--xeno- thermal--epithermal ore deposits of gold. These include Sb, As, Cd, T1, Mn, Hg and Ag, among others. Thallium, in particular, has attracted much interest as a gold pathfinder (Ikramuddin et al., 1983). Lesser but none- theless important traces of Sb, As and Cd (and others) are also common around these low-pressure gold deposits. This note will present new Eh--pH diagrams for the elements Sb, As, Cd and T1; as well as published Cl--pH diagrams for T1--Hg--Au (Baes and Mesmer, 1976) and attempt to ex- plain why certain elements such as T1 are useful pathfinders for Au and other metals. This note does not pretend to cover the background geochemistry of the elements Sb, As, Cd and T1, and the reader is referred to general geochemical literature for such information. Some key references will be identified as they pertain to this work, how- ever. 2. Previous work The use of Eh--pH diagrams for assistance in dealing with geochemical problems has been described, for example, by Garrels and Christ (1965), Krauskopf (1979), Verink (1979) and Brookins (1984). Previous Eh--pH diagrams for Sb and Cd have been given by Brookins (1978), and for As by Brookins (1979) and Longmire (1983). The data used

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  • 5/24/2018 Pourbaix Diagram of Cadmium

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    C hemi ca l Geo l ogy , 5 4 ( 1 9 8 6 ) 2 7 1 - - 2 7 8 2 7 1El s ev ie r S c i ence P ub l i she r s B .V . , Am s t e rd am - - P r i n t ed i n The N e t he r l ands[3 ]

    G E O C H E M IC A L B EH A V IO R O F A N T IM O N Y A R S E N ICC A D M IU M A N D T H A L LIU M :E h -p H D I A G R A M S F O R 2 5C 1 -B A R P R E S S U R E

    D O U G L A S G . B R O O K I N SD e p a r t m e n t o f G e o l o g y, U n i v e r s it y o f N e w M e x i c o , A l b u q u e r q u e , N M 8 7 1 3 1 U . S .A . )

    ( R e c e i v e d S e p t e m b e r 5 , 1 9 8 5 ; a c c e p t e d f o r p u b l i c a ti o n O c t o b e r 1 , 1 9 8 5 )

    A b s t r a c tB r o o k i n s, D . G . , 1 9 8 6 . G e o c h e m i c a l b e h a v i o r o f a n t i m o n y , a r s en i c, c a d m i u m a n d t h a l li u m : E h - - p H d i a g r a m sfo r 25 C , 1 -ba r p res s u re . C hem . Geo l . , 54 : 271 - -278 .

    New Eh - -pH d i ag ram s have b een de r i ved fo r S b , As , C d and T1. Thes e d i ag ram s a re u s e fu l i n d i scus s ingt he com m on as s oc i a t i on o f s eve ra l o r a l l o f t hes e e l em en t s a round ep i t he rm al Au depos i t s . S l i gh t d i f f e ren -c e s in p H , E h o r b o t h p H - - E h a r e s u f f ic i e n t t o a c c o u n t f o r p a r t it i o n in g o f t h e s e e l e m e n t s f r o m d e p o s it todepos i t . I n add i t i on , ch l o r i de co nce n t r a t i on - -pH d i ag ram s fo r Au , Hg and T1 a re u s e fu l t o fu r t h e r d i s cus st h e r o l e o f c h l o r id e ( a n d p o s s i b ly c h lo r i d e c o m p l e x e s ) in t h e m i g r a t i o n o f s o m e o f t h e s e e l e m e n t s u n d e rl o w T ,P cond i t i ons .

    1 . n t r o d u c t i o nM a n y e l e m e n t s h a v e b e e n p r o p o s e d a s

    p a t h f i n d e r e l e m e n t s f o r t e l e t h e r m a l - - x e n o -t h e r m a l - - e p i t h e r m a l o r e d e p o s i t s o f g o l d .T h e s e i n c l u d e S b , A s , C d , T 1 , M n , H g a n d A g ,a m o n g o t h e r s . T h a l l i u m , i n p a r t i c u l a r , h a sa t t r a c t e d m u c h i n t e r e s t a s a g o l d p a t h f i n d e r( I k r a m u d d i n e t al . , 1 9 8 3 ) . L e s s e r b u t n o n e -t h e l e s s i m p o r t a n t t r a c e s o f S b , A s a n d C d( a n d o t h e r s ) a r e a ls o c o m m o n a r o u n d t h e s el o w - p r e s s u r e g o l d d e p o s i t s .

    T h i s n o t e w i ll p r e s e n t n e w E h - - p H d i a g r a m sf o r t h e e l e m e n t s S b , A s , C d a n d T 1; a s w e l la s p u b l i s h e d C l - - p H d i a g ra m s f o r T 1 - - H g - - A u( B a es a n d M e s m e r , 1 9 7 6 ) a n d a t t e m p t t o ex -p l a i n w h y c e r t a i n e l e m e n t s s u c h a s T1 a r eu s e fu l p a t h f i n d e r s f o r A u a n d o t h e r m e t a l s .

    T h i s n o t e d o e s n o t p r e t e n d t o c o v e r t h eb a c k g r o u n d g e o c h e m i s t r y o f t h e e l e m e n t sS b , A s , C d a n d T 1 , a n d t h e r e a d e r i s r e f e r r e dt o g e n e r a l g e o c h e m i c a l l i t e r a t u r e f o r s u c hi n f o r m a t i o n . S o m e k e y r e f e r e n c e s w il l b ei d e n t i f i e d a s t h e y p e r t a i n t o th i s w o r k , h o w -e v e r .2 . P r e v i o u s w o r k

    T h e u s e o f E h - - p H d i a g r a m s f o r a s s i s t a n c ein d e a l in g w i t h g e o c h e m i c a l p r o b l e m s h a sb e e n d e s c r i b e d , f o r e x a m p l e , b y G a r re l s a n dC h r is t ( 1 9 6 5 ) , K r a u s k o p f ( 1 9 7 9 ) , V e r i n k( 1 9 7 9 ) a n d B r o o k i n s ( 1 9 8 4 ) . P r e v i o u s E h - - p Hd i a g r a m s f o r S b a n d C d h a v e b e e n g i v e n b yB r o o k i n s ( 1 9 7 8 ) , a n d f o r A s b y B r o o k i n s( 1 9 7 9 ) a n d L o n g m i r e ( 1 9 8 3 ) . T h e d a t a u s e d

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    272in these earlier works were subject to fairlylarge errors, however, and these three di-agrams have been recalculated here. No prev-ious diagram, using modern data, has beenatte mpt ed for T1, however.

    The role of total dissolved C1 in affectingthe geochemical behavior of the elementsSb, As, Cd and T1 is not well known, butBaes and Mesmer (1976) have calculated thetota l Cl--pH diagrams for the stability fieldsof Hg, Au and T1. Some of their work, withpermission, are presented herein to helpinterpret the Eh--pH diagrams. The authorassumes, however, responsibility for all dis-cussion and conclusio ns drawn involving theirwork.3. Ther modyn amic data

    In order to be as consistent as possible, Ihave restr ic ted my choice of thermodynamicdata to that presented by Wagman et al.(1982). The data are presented in Table I.All Gibbs free energies of f orm ati on (A G}) forthe species of interest have been recalculatedto kilocalories per mole (kcal. mo1-1) andonly 298.15 K, and 1-bar pressure data havebeen employed. Further, since I am mostinterested in trace amounts of the elementsSb, As, Cd and T1 in waters, activities fordissolved amounts of these elements aretak en at 10 -8 and 10 -6 . Th ese values arechosen in accord with the approaches of theearlier workers (i.e. Garrels and Christ, 1965;Brookins , 1978 , 1984) and, since the di-agrams are for generic purposes only, theseactivities are assumed to be equal to concen-tration (molalit ies) and unaffected by ionicstrength. While an over-simplification, thiswill not drastically change the Eh--pH di-agrams presented. Finally, the errors for thethermodynamic data are discussed in detailby Wagman et al. (1982) and the readeris referred to this source for detail . The readeris also reminded that not shown fo r theEh--pH diagrams are stability fields for mostsulfide complexes, etc., due to a lack oftherm odynam ic data .

    TABLE IGibbs free energies of formation for speciesSpecies AG~(kcal. mol -~ )

    A r s e n i c :AsS --16.80As:S 3 --40.30As203 --137.66H3AsO4 --183.08H~AsO~ --180.01HAsO:~ --170.69AsO~- --154.97

    C a d m i u m :Cd 2 --18.55CdS --37.40CdO --54.59CdO~- --67.97CdOH+ --62.40HCdO --86.88Cd(OH)2 --113.19CdCO: --159.99

    A n t i m o n y :SbO --42.33SbO~ --81.31Sb2S ~ --41.49S b 2 S ~ - - 2 3 . 7 8H S b O : - - 9 7 . 3 9S b O H ) 3 - - 1 6 3 . 7 7S b 2 0 4 - - 1 9 0 . 1 8Sb:O~ --198.18

    T h a l l i u m :Tl --7.74TI(OH)~ --58.48TIOH~ --3.80T ~O --35.20T120 ~ --74.50T120 --82.98TI(OH)~ --121.18TI2S --22.39

    O t h e r s :H2S --6.65HS- +2.89SOt --177.95H20 --56.69H:CO~ --148.94HCO3 --140.26C O ~ - - - 1 2 6 . 1 7All data from Wagman et al. (1982).

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    273

    4 . E h - - p H d i a gr a m sT h e E h - - p H d i a g r a m s , c a l c u l a t e d f o l l o w i n g

    t h e m e t h o d s d e s c r i b e d i n B r o o k i n s ( 1 9 8 4 ) ,a r e s h o w n f o r S b , A s , C d a n d T 1 a s F i g . 1 A ,B , C a n d D , r e s p e c t i v e l y . T h e s e a r e d i s c u s s e di n t u r n .T r a n s p o r t o f S b i n h y d r o t h e r m a l w a t e r sm a y b e a s ac i d ic o r b a s i c o x y i o n s , S b O o rS b O ~ , r e s p e c t i v e l y , u n d e r m i l d l y o x i d i z i n gc o n d i t i o n s ( i. e. j u s t a b o v e t h e s u l f i d e - - s u l f a t ef e n c e ) a s s h o w n i n F i g. 1A . U n d e r re d u c i n g ,n e a r - n e u t r a l t o m o r e a lk a l in e c o n d i t i o n s ,t r a n s p o r t a s a s u lf i d e c o m p l e x s u c h a s S b : S ~ -i s p o s s i b l e ( n o t e : a c t i v i t y o f t o t a l d i ss o l v e dS = 1 0 -3 a s s u m e d ) . B y f a r th e b u l k o f t h es t a b i l i t y f i e ld o f w a t e r i s c o v e r e d b y s o l idS b s p e c i e s ( S b 2 S 3 , S b ( O H ) 3 , S b 2 0 4 , S b 2 0 5 ) ,t h u s s u g g e st in g t h a t S b t r a n s p o r t m u s t t a k ep l a c e a t m o d e r a t e l y l o w E h - v a lu e s . N o d a t aa r e a v a i l a b l e f o r c h l o r i d e c o m p l e x e s o f S b .T r a n s p o r t o f S b s p e c i e s a s a c h l o r i d e c o m -p l e x is d i f fi c u l t t o a s se ss . B o y l e a n d J o n a s s o n( 1 9 8 4 ) s u g g e s t t h a t s p e c i e s s u c h a s S bC136 ,S bC 13 , Sb O C 1 , e t c . , m a y b e l o c a l l y i m p o r t a n ti n c h l o r i d e - r i c h a c i d i c h o t s p r i n g w a t e r s . N od a t a a r e a v a i la b l e f o r t h e a q u e o u s s p ec i e s,h o w e v e r .T h e E h - - p H d i a g r a m f o r A s is s h o w n a sF i g. l B . O n l y o n e a c t i v i t y ( 1 0 -6 ) h as b e e na s s u m e d f o r d i s s o lv e d A s s p e c i es f o r c o n -v e n i e n c e . W i d e t r a n s p o r t b y A s ( V ) s p e c ie sa b o v e t h e s u l f i d e - - s u l f a t e f e n c e i s i n d i c a t e d( H 3 A s O 4 , H 2 A s O ~ , H A s O2 4 , A s O ~ - ) . A s m a l lf i e l d o f A s 2 0 3 m a y s e r v e a s a p a r t i a l b a r r i e rt o d i s s o l v e d A s m i g r a t i o n u n d e r a c i di c m i l d -l y - o x i d i z i n g c o n d i t i o n s . U n d e r s u l f i d e - s t a b l ec o n d i t i o n s , A s m o b i l i t y s h o u l d b e f ai r lyl i m i t e d ( i gn o r i ng s u l f id e c o m p l e x e s ) . A g a i n,A s -- C 1 c o m p l e x e s a r e n o t w e l l d e f i n e d a n dn o t h e r m o d y n a m i c d a t a a re a v a il ab l e f o rs u c h s p e c ie s . B o y l e a n d J o n a s s o n ( 1 9 8 4 )p o i n t o u t t h a t S b is a g o o d p a t h f i n d e r e le -m e n t f o r a w i d e v a r i e t y o f m i n e r a l d e p o s i t s ,i n c l u d in g A u . F u r t h e r , s o m e s i m i la r b e h a v i o ro f S b w i t h A s i s a l so n o t e d , p o s s i b l y d u e t oz o n e o f f o r m a t i o n o f S b ( O H ) 3 a n d A s :O 3 .T h e C d E h - - p H d i a g r a m i s s h o w n a s F i g.

    1 C . W h i l e a l a r g e s t a b i l i t y f i e l d f o r C d S i sp r e s e n t u n d e r s u l f id e - s t a b le E h - - p H , a b o v et h e s u l f i d e - - s u l f a te f e n c e C d s h o u l d b e v e r ym o b i l e a t n e a r -n e u t r a l a n d a c i d p H - v a l u e . T h isi s c o n s i s t e n t , f o r e x a m p l e , w i t h o b s e r v e dC d m o b i l i t y a t t h e O k l o n a t u r a l r e a c t o r ,G a b o n ( B r o o k i n s , 1 9 7 8 , 1 9 8 4 ) , a s o n l y s m a l lf i e l d s o f C d C O 3 a n d C d ( O H ) 2 , a n d a t h i g hp H , a r e p r e s e n t u n d e r o x i d i z i n g c o n d i t i o n s .M o b i l i t y a s C d 2 ( a s s u m e d t o b e m o r e a b u n -d a n t t h a n C d O H ) a n d / o r C d O ~ u n d e r o x i d iz -i n g c o n d i t i o n s i s a s s u m e d . H o w e v e r , i n t h ep H r a n ge o f 8 - -1 0 , C d C O 3 - - C d ( O H ) 3 m a yp r e v e n t C d m o b i l i t y .

    T h e E h - - p H d i a g r a m f o r T 1 i s s h o w n i nF i g. 1 D . W h i le m o s t o f t h e E h - - p H f i e ld isc o v e r e d b y s o l i d s p e c i e s , f r o m m i l d l y t os t r o n g l y o x i d i z i n g c o n d i t i o n s , T 1 2 0 , T 1 2 0 3 ,T1 2 0 4, t h e r e i s a s i g n i f i c a n t l y l a r g e f i e l d f o rT 1 t h a t e x i s t s f r o m a c i d i c t o s l i g h t ly a l k a l i n ep H u n d e r r e d u c i n g c o n d i t i o n s t o , a s a f u n c -t i o n o f d e c r e a s in g p H , s o m e w h a t o x id i z i n g,a c i di c c o n d i t i o n s . T h i s is i m p o r t a n t f o r s e v e ra lr e a s o n s ( d i s c u s s e d b e l o w ) . S o m e T 1 - - C l - - p Hd a t a h a v e b e e n d e t e r m i n e d o r c a l c u l a t e d ( B a e sa n d M e s m e r , 1 9 7 6 ) , t h e i m p o r t a n c e o f w h i c hi s d i s c u s s e d l a t e r i n th i s p a p e r .5 . D i s c u s s i o n

    T h e r o l e o f s p e c ie s o t h e r t h a n S o n t h em e t a l - - w a t e r s y s t e m E h - - p H d i ag r a m s f o r S b ,A s , C d a n d T 1 is n o t w e l l k n o w n . Y e t i n t h ec a se o f T 1, B a e s a n d M e s m e r ( 1 9 7 6 ) h a v ec a l c u l a t e d t h e C l - - p H d i a g r a m f o r T 1 s p e c ie s .T h i s i s s h o w n a s F i g. 2 A . I n a d d i t i o n , a l s of r o m t h e i r w o r k , F i g. 2 B a n d C s h o w s t h eC l - - p H d i a g r a m s f o r H g a n d A u s p e ci e s. T h e s ew i ll b e d i s c u s s e d b e l o w .I t i s a p p a r e n t f r o m i n s p e c t i o n o f F ig . 1t h a t t h e r e a r e s i g n i f i c a n t d i f f e r e n c e s in t h eE h - - p H d i ag r a m s f o r t h e f o u r e l e m e n t s inq u e s t i o n . A l t h o u g h a ll c a n b e t r a n s p o r t e di n s o l u t i o n t o g e t h e r u n d e r v e r y a c i d i c m i l d l y -o x i d i z i n g c o n d i t i o n s , a t o t h e r E h - - p H c o n d i -t i o n s t h e y e x h i b i t q u i t e d i f f e r e n t b e h a v i o r .A t i n t e r m e d i a t e - p H m i l d l y - o x i d i z i n g c o n d i -t i o n s , T 1 - - C d - -A s c a n s t i ll b e t r a n s p o r t e d

  • 5/24/2018 Pourbaix Diagram of Cadmium

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  • 5/24/2018 Pourbaix Diagram of Cadmium

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    t o g e t h e r , b u t n o t S b . U n d e r h ig h e r- p H c o n -d i t i o n s C d - - A s c a n s t il l b e m o b i l e , b u t n o tT 1 - -S b . F r o m t h e E h - - p H d i a g r a m s a l o n e ,o n e w o u l d h a v e t o a r g u e f o r a c i d ic o x i d i z in g( E h = 0 . 4 5 V o r s o ) f o r t h e t r a n s p o r t o f t h eg r o u p S b - - A s - - C d - -T 1 . A n y s h i f t in e i t h e r p Ho r E h w i ll r e m o v e o n e o r m o r e s p e c ie s f r o ms o l u t i o n . I n a c t u a l i t y , t h i s m a y a c c o u n t f o rh a l o e s o f , f r o m A u o r e o u t w a r d , o f A s, t h e nS b , t h e n T 1 w i t h C d f ix e d i n f a r t h e s t r e m o v e ds e c o n d a r y s u l fi d e s ( n o t e : t h i s k i n d o f z o n a -t i o n i s f o r a g e n e r i c c a s e o n l y ) .

    T h e E h - - p H d i a g r a m f o r T1 ( F ig . 1 D )is a l so u s e f u l t o e x p l a i n t h e c o m m o n f i xa -t i o n o f T1 i n K - b e a r i n g m i n e r a l s f o u n d i na l t e ra t i o n h a l o e s a r o u n d s o m e o r e d e p o s i ts .T h e i o n i c r a d i u s o f T1 i s 1 . 4 9 A , w h i c h i sv e r y c l o s e t o t h a t o f K o f 1 . 3 3 A ( S h a w ,1 9 5 2 ) , a n d s u b s t i t u t i o n o f T1 f o r K is b o t hp r o b a b l e a n d o b s e r v e d ( s e e a l so V o s k r e s e n s -k a y a , 1 9 5 9 ) . I n ca s e s w h e r e T 1 - -K d i a d o c h yi s p o s s i b l e , t h i s w i l l a l l o w i t t o b e s e g r e g a t e df r o m t h e r e m a i n i ng S b - - A s - -C d . A n y o x y -h y d r o x i d e p h a s e s w i ll p r e s u m a b l y r e m o v e S ba n d A s in t h e s a m e r o c k s w h e r e T 1 - - K f i xa -t i o n h a s o c c u r r e d . O n l y C d w o u l d b e t r an s -p o r t e d f u r t h e r i n t h i s c as e .T h e C l - - p H d i a g r a m s ( F ig . 2 ) f o r T 1 - - H g - -A u a r e u s e f u l i n t h a t t h e r e la t i v e i m p o r t a n c eo f c h l o r i d e c o m p l e x e s o f t h e s e m e t a l s c a nb e e x a m i n e d . W h i le E h c o n d i t i o n s a re n o tg i v en i n B a e s a n d M e s m e r ( 1 9 7 6 ) , t h e E hm u s t b e a s s u m e d t o b e q u i t e h i g h , i .e . h i ghe n o u g h t h a t t h e s p e c i e s T l ( I I I) , H g ( I I ) a n dA u ( I I I ) p r e d o m i n a t e . F r o m t h e E h - - p H di -a g r a m f o r T 1 ( F ig . 1 D ) , i t w o u l d a p p e a r t h a tT l ( I V ) s h o u l d b e t h e s p e c i e s c o e x i s t i n g w i t hH g ( I I ) a n d A u ( I I I ) , b u t d a t a a r e n o t a v a il -a b l e .B a e s a n d M e s m e r ( 1 9 7 6 ) p o i n t t o t h e im -p o r t a n c e o f c h lo r i d e - -h y d r o x i d e c o m p l e x e sf o r t h e m e t a l s T 1 - - H g - - A u . I n d e e d , t h e s p e c i e sT 1O H C1 + i s c o n s i d e r e d b y B a e s a n d M e s m e r( 1 9 7 6 ) t o b e i m p o r t a n t , a s a r e H g O H C 1 a n dA u O H ( C 1 ) : -- A u ( O H ) 2 C 1 . W h a t t h ei r w o r ki n d i c a t e s i s t h a t a ll t h r e e m e t a l s , T 1 - - H g - - A um a y b e t r a n s p o r t e d a s c h l o r i d e - - h y d r o x i d ec o m p l e x e s f o r t h e c o n d i t i o n s g i v e n . I n n a t u r a l

    277s e t ti n g s , s i m i l ar c o m p l e x e s m a y b e a s i m p o r -t a n t i f n o t m o r e s o . T h e p r o b l e m o f A us p e c i e s is c o m p l i c a t e d b y t h e f a c t t h a t w h i l eA u ( I ) is k n o w n , t h e r e a r e v er y f e w t h e r m o -d y n a m i c d a t a f o r A u ( I ) s p e c i es . T h e l i m i t e dd a t a ( W a g m a n e t al ., 1 9 8 2 ) d o , h o w e v e r , s ug -g e s t t h a t A u ( 0 ) w i ll o x i d i z e t o A u ( I ) inA u C l~ a t a n E h o f r o u g h l y 1 . 2 5 V , a p p r o x i -m a t e l y r i g h t a t t h e u p p e r s t a b i l i t y l i m i t o fw a t e r u n d e r p H = 0. T h e E h f o r A u ( I ) t oA u ( I I I ) i s h i g h e r t h a n t h i s f o r a ll s p e c i e s.F u r t h e r , w h i l e t h e b o u n d a r i e s f o r A u ( 0 ) - -A u ( I I I ) s p e c i e s s u c h a s H 2 A u O ~ a n d H A u O ~ -f a ll a b o v e t h e w a t e r s t a b i l i t y fi e ld , in t h e o r yt h e A u ( I ) s p e c i e s s h o u l d f a l l b e l o w t h e m .T h i s c o u l d b r i n g s o m e a q u e o u s A u ( I ) s p ec i e si n t o t h e s t a b i l i t y fi e ld f o r w a t e r . T h e r e v i se dE h - - p H d i ag r am f o r A u - - C I - - S - - H - O b y t h ew r i t e r w i ll b e p u b l i s h e d s e p a r a t e l y ( D . G .B r o o k i n s , i n p r e p . ) .6 . C o n c l u s i o n s

    T h e c o n c l u s i o n s f r o m t h is w o r k a r e a sf o l l o w s :

    ( 1 ) T h e g r o u p T 1 - - C d - - A s - - S b c a n b e t r an s -p o r t e d t o g e t h e r u n d e r a c i d i c o x i d i z i n g c o n d i -t i o n s .( 2 ) U n d e r h i gh p H b u t s t il l o x i d i z i n g c o n -d i t io n s , A s - - C d m a y r e m a i n m o b i l e , b u tT 1 - -S b m a y b e i n c o r p o r a t e d i n t o s o li d s.

    ( 3 ) U n d e r i n t e r m e d i a t e - p H m o d e r a t e - E hc o n d i t i o n s , T 1 - - C d - -A s c a n b e t r a n s p o r t e dt o g e t h e r , b u t n o t S b .

    ( 4 ) H a l o e s o f t h e e l e m e n t s S b - - T 1 - - C d - - A sa b o u t e p i t h e r m a l A u d e p o s i ts ar e c o m m o n ;t h e E h - - p H d i ag r a m s h e l p e x p l a in s o m e , b u tc e r t a i n l y n o t a ll , o f t h e h a l o e s n o t e d .

    ( 5 ) T h e r o l e o f c h l o r i d e c o m p l e x e s i s n o tw e l l u n d e r s t o o d , y e t t h e C l - - p H d i ag r a m sf o r H g - - A u - - T 1 s p e c i e s ( f r o m B a e s a n dM e s m e r , 1 9 7 6 ) s t r o n g l y s u g g e s t t h a t s u c hc o m p l e x e s a r e v e r y i m p o r t a n t f o r t r a n s p o r t o fn o t o n l y H g - -A u - -T 1 , b u t f o r o t h e r e l e m e n t sa s w e l l .cknowledgementsT h a n k s a r e d u e t o D r . C h a r l e s B a e s , a n d

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    J o h n W i l e y S o n s , P u b l i s h e rs , f o r p e r m i s s i o nf o r u s e o f t h e d i a g r a m s s h o w n a s F i g. 2 .B . K a l m a n a s s i s t e d i n t h e c a l c u l a t i o n s , a n dE . S t e w a r t d i d t h e d r a f t i n g o f F i g . 1 .

    e f e r e n c e sBaes, C.F. and Mesmer, R.E., 1976. The Hydrolysisof Cations. Wiley--In terscienc e, New York, N.Y.,325 pp.Boyle, R.W. and Jonasson, I.R., 1984. The geo-chemistry of antimony and its use as an indicatorelement in geochemical prospecting. J. GeochemExplor., 20: 223--302.Brookins, D.G., 1978. Eh--pH diagrams for elementsfrom Z = 40 to Z = 52: applicatio n to the Oklonatural reactor, Gabon. Chem. Geol., 23: 324--243.Brookins, D.G., 1979. Uran ium deposits of theGrants, New Mexico mineral belt (II). U.S. Dep.Energy, Washington, D.C., Rep. BFEC-GJO-76-

    029E, 422 pp.Brookins, D.G., 1984. Geochemical Aspects of Radio-active Waste Disposal. Springer, New York, N.Y.,345 pp.Garrels, R.M. and Christ, C.L., 1965. Solutions,Minerals and Equilibria. Harper & Row, NewYork, N.Y., 450 pp.

    Ikramuddin, M., Asmeron, Y., Nordstrom, P.M.,Kinart, K.P., Martin, W.M., Digby, S.J.M., Elden,D.N., Nijak, W.F. and Afemari, A.A., 1983.Thallium -- a potential guide to mineral deposits.J. Geochem. Explor., 19: 465--490.Krauskopf, K.B., 1979. Intro duct ion to Geochemis-try. McGraw-Hill, New York, N.Y., 2nd ed.,617 pp.Longmire, P.A., 1983. Geoche mistry, diagenesis andcontaminant transport of uranium tailings, GrantsMineral Belt, New Mexico. M.S. Thesis, Universityof New Mexico, Albuquerque (unpublished).Shaw, D.M., 1952. The geochemistry of thallium.Geochim. Cosmochim. Acta, 2: 118--130.Verink, E.D., 1979. Simplified procedure for con-structing Pourbaix diagrams. J. Educ. ModulesMat. Sci. Eng., 1: 535--560.Voskresenskaya, N.T., 1959. Geoch emistr y of thal-lium and rubidium in igneous rocks. Geochem.Int., 4: 559--565.Wagman, D.D., Evans, W.H., Parker, V.B., Schumm,R.H., Halow, I., Bailey, S.M., Churney, K.L. andNuttall, R.L., 1982. The NBS tables of chemicalthermodynamic properties: selected values for in-organic and C, a nd C2 organic substa nces in SIunits. J. Phys. Chem. Ref. Data, Vol. 11, Suppl. 2,390 pp.