Chapter 26
Group Isolation of Nickel and Vanadyl Porphyrins from Crude Oil Using Macroporous Silica Gel 1
1
2,3
2
David H. Freeman , Rosalie M. Angeles , Katherine H. Freeman , Thomas C. Hoering , Joseph S. Flynn , Tracie A. Lango1, and C. T. Homonay-Preyer 1,4
1
1
Department of Chemistry and Biochemistry, University of Maryland, College Park, MD 20742 Geophysical Laboratory, Carnegie Institution of Washington, 2801 Upton Street, Washington, DC 20008 Department of Geology, Wellesley College, Wellesley, MA 02181 U.S. Naval Academy, Annapolis, MD 21412
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3
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An efficient, ten-fold concentration of combined nickel and vanadyl porphyrins in crude o i l is obtained by liquid column chromatography with disposable, macroporous silica gel. The concentrate contains the biomarker metalloporphyrins based on chromatographic and spectral comparisons with etioporphyrin-I standard compounds. The concentrate is free of asphaltene materials that would otherwise cause major chromatographic interference. The procedure, in brief, begins with one gram of crude oil sorbed on top of a column containing 5 grams of 5 0 0 Åpore size s i l i c a gel. The initial elution is with petroleum ether:methylene chloride (97v:3v) to remove saturated and aromatic hydrocarbons. The metalloporphyrins are eluted next with methyl acetate while the remaining asphaltene components are immobilized. In a second step, 100Å silica gel is used to further separate the metalloporphyrins. The method is rapid, simple and reproducible. It is applicable to processing large numbers of samples and i t is economical in its use of solvent and adsorbent. Details on the considerable effort expended on this method development are given. 0097-6156/87/0344-0402$06.25/0 © 1987 American Chemical Society
In Metal Complexes in Fossil Fuels; Filby, R., et al.; ACS Symposium Series; American Chemical Society: Washington, DC, 1987.
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26.
FREEMAN ET AL.
Group Isolation of Nickel and Vanadyl Porphyrins
403
M u l t i - s t e p s e p a r a t i o n and p u r i f i c a t i o n p r o c e d u r e s a r e needed t o i s o l a t e m e t a l l o p o r p h y r i n pigments from g e o l o g i c a l samples. The many r e p o r t e d p r o c e d u r e s v a r y f r o m m i n i m a l m e t h o d o l o g y p r e c e d i n g mass s p e c t r o m e t r y (1) t o l e n g t h y i s o l a t i o n s o f i n d i v i d u a l compounds f o r X - r a y c r y s t a l l o g r a p h y (2.) , c o m b i n e d m a s s s p e c t r o m e t r i c a n d NMR a n a l y s i s Q ) a n d h i g h r e s o l u t i o n HPLC a n d mass spectrometry (4.) . The g o a l o f t h e p r e s e n t s t u d y i s t o d e v e l o p a r u g g e d and r o b u s t method f o r g r o u p s e p a r a t i o n o f t r a c e s of metalloporphyrins. This includes r e l i a b i l i t y and m i n i m a l m o d i f i c a t i o n when a p p l i e d t o a w i d e r a n g e o f samples. I s o l a t i o n from a g e o l o g i c a l matrix i n v o l v e s d e a l i n g w i t h u n c e r t a i n numbers o f p o r p h y r i n homologues and i s o m e r s , and unbounded numbers o f o t h e r compounds that are a l s o present. Trace enrichment with high r e c o v e r y and m i n i m a l i n t e r f e r e n c e i s needed t o a s s u r e q u a l i t a t i v e and q u a n t i t a t i v e a c c u r a c y (5-7). O p t i m i z a t i o n o f a m u l t i - s t e p s e p a r a t i o n s scheme r e q u i r e s an e x p e r i m e n t a l a p p r o a c h , b u t n o t e x c l u s i v e l y . A proper choice of l i q u i d chromatographic v a r i a b l e s i s e s s e n t i a l , a t l e a s t i n a p r a c t i c a l sense (&). Many s i n g l e step o p t i m i z a t i o n c r i t e r i a are a v a i l a b l e Q ) a l t h o u g h m i x t u r e s c o n t a i n i n g unbounded numbers o f compounds a r e t h e most d i f f i c u l t . Solvent and a d s o r p t i v e r o u t e s t o c h e m i c a l s e l e c t i v i t y have become more a c c e s s i b l e and f a s t e r ( 1 0 ) . In d e a l i n g w i t h h i g h l y c o m p l e x m i x t u r e s , t h e f i r s t s t e p may b e t h e m o s t d i f f i c u l t t o work o u t , and t h e most i m p o r t a n t . E x t e n s i v e e x p e r i m e n t a t i o n was n e e d e d t o a c h i e v e t h e present g o a l , d e t a i l s of which are given below. First, i t was d e m o n s t r a t e d t h a t a m u l t i m o d a l liquid c h r o m a t o g r a p h i c procedure, u s i n g s i l i c a g e l , Sephadex L H - 2 0 a n d C-18 b o n d e d p h a s e a s s u b s t r a t e s c o u l d make t h e desired separation. Thin l a y e r chromatography proved to be a v a l i d m e t h o d f o r r a p i d m e t a l l o p o r p h y r i n s c o u t i n g . Many s o l v e n t s y s t e m s w e r e t r i e d b e f o r e a b a s i s f o r i m p r o v e d e l u a n t c o m p o s i t i o n was f o u n d . Column t e s t i n g s h o w e d t h a t c r u d e o i l f r a c t i o n a t i o n on n a r r o w p o r e s i l i c a gel i s not a p p r o p r i a t e i n the f i r s t step. An o p t i m u m e l u e n t s e q u e n c e was f o u n d o n t h e b a s i s o f t w o d i m e n s i o n a l TLC s c o u t i n g e x p e r i m e n t s . The b r e a k t h r o u g h came w h e n i t was o b s e r v e d t h a t c o n v e n t i o n a l s i l i c a g e l d i d not p r o v i d e the needed r e t e n t i v e c a p a c i t y for the dark asphaltene f r a c t i o n that s e r i o u s l y i n t e r f e r e s w i t h c h r o m a t o g r a p h i c s e p a r a t i o n and a n a l y s i s . A c r i t i c a l t e s t i n g of s i l i c a g e l p o r o s i t y lead to the use o f macroporous s i l i c a g e l . A d u a l o p t i m i z a t i o n o f s o l v e n t a n d a d s o r b e n t was t h u s o b t a i n e d a n d t h e s e p a r a t i o n g o a l was reached. r
Experimental
T e s t o f M u l t i - M o d a l LPLC. The u s e o f n o n - r e d u n d a n t s o r p t i v e modes i s known t o be t h e o r e t i c a l l y w e l l - s u i t e d
In Metal Complexes in Fossil Fuels; Filby, R., et al.; ACS Symposium Series; American Chemical Society: Washington, DC, 1987.
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f o r i s o l a t i n g compounds f r o m e x t r e m e l y c o m p l e x m i x t u r e s (10) s u c h a s c r u d e o i l s . A f e a s i b i l i t y s t u d y w a s made u s i n g l o w p r e s s u r e l i q u i d c h r o m a t o g r a p h y (LPLC) t o concentrate themetalloporphyrins, s p e c i f i c a l l y the predominant n i c k e l p o r p h y r i n (NiP)group i n t h e Messel S h a l e o f Germany ( J J J . F r e s h l y p u l v e r i z e d s a m p l e s o f t h e s h a l e were e x t r a c t e d w i t h benzene a n d m e t h a n o l (1:1 volume/volume) s o l u t i o n . One g r a m o f t h e o r g a n i c e x t r a c t remained a f t e r r o t a r y evaporation. The e x t r a c t was (A) e l u t e d s u c c e s s i v e l y w i t h h e x a n e a n d b e n z e n e f r o m a 60cm b y 5 cm p r e p a r a t i v e c h r o m a t o g r a p h i c c o l u m n o f s i l i c a g e l (Grade 62, D a v i s o n C h e m i c a l Co., B a l t i m o r e , MD). C o l l e c t i o n o f t h e r e d p o r p h y r i n band i n t h e b e n z e n e e l u a t e was e s t i m a t e d v i s u a l l y . T h e n , (B) s i m i l a r p r e p a r a t i v e c h r o m a t o g r a p h y w i t h S e p h a d e x LH-20 gel i n 1:1 b e n z e n e a n d m e t h a n o l s o l u t i o n w a s c a r r i e d o u t on t h e c o n c e n t r a t e f r o m s t e p ( A ) . T h e s e t w o s t e p s a r e b a s e d o n p r o c e d u r e s d e s c r i b e d b y B a k e r (12.) · H P L C a p p a r a t u s w a s t h e n u s e d w i t h (C) C-18 b o n d e d phase, Sep-Pak c a r t r i d g e s used as s h o r t , d i s p o s a b l e c h r o m a t o g r a p h i c columns (Waters A s s o c i a t e s , Framingham, MA). A l i n e a r g r a d i e n t was u s e d f r o m 1:1 a c e t o n i t r i l e (MeCN) a n d w a t e r t o p u r e MeCN. The m e t a l l o p o r p h y r i n c o n c e n t r a t e w a s c h r o m a t o g r a p h e d i n a s i m i l a r w a y (D) o n Sep-Pak s i l i c a g e l u s i n g a l i n e a r g r a d i e n t o f hexane t o benzene. The c a r t r i d g e s u s e d i n C a n d D were c o n f i n e d to a t i g h t - f i t t i n g metal holder and t h e i n s e r t i o n o f machined e n d f i t t i n g s reduced t h e dead volume. I n d e p e n d e n t t e s t s showed a t 1 ml/min f l o w r a t e t h a t c o l u m n e f f i c i e n c i e s o f c a . 40 t h e o r e t i c a l p l a t e s c o u l d be a c h i e v e d . The Sep-Pak columns b u r s t o c c a s i o n a l l y , p e r h a p s due t o m i g r a t e d p a r t i c l e s t h a t p l u g g e d t h e e n d frit . E n r i c h m e n t o f t h e N i P g r o u p was m o n i t o r e d b y v i s i b l e absorption spectrophorometry a f t e r each step and i s d e m o n s t r a t e d i n F i g u r e 1 w h e r e i n t h e S o r e t B-band a t 408 nm e m e r g e s f r o m t h e UV a b s o r b i n g b a c k g r o u n d . D e f i n i t i v e , s i n g l e peak i s o l a t i o n o f t h e m e t a l l o p o r p h y r i n s , s h o w n i n F i g u r e 2, w e r e o b t a i n e d b y m o n i t o r i n g t h e e f f l u e n t a t 550nm i n a f l o w spectrophotometer. It i sconcluded that t h euse o f short disposable column c h r o m a t o g r a p h y i n s t e p s C a n d D (See F i g u r e s 1 a n d 2) i s i n d e e d a p p l i c a b l e t o t h e p r o b l e m , g i v e n t h a t the b u l k o f t h e sample m a t r i x , t h e non-analyte group, h a s b e e n p r e v i o u s l y r e m o v e d b y s t e p s A a n d B. T h e A a n d Β s t e p s were c o s t l y i n terms o f t i m e , s o r b e n t a n d carrier liquid. This experiment defined t h e o v e r a l l goal: t o streamline t h e i n i t i a l clean-up procedure and produce a metalloporphyrin concentrate that i s s u i t a b l e for high r e s o l u t i o n chromatographic separation. P r e l i m i n a r y Test o f LP-LSC. S i l i c a g e l i sa versatile and i n e x p e n s i v e a d s o r b e n t t h a t i s a t t r a c t i v e f o r p o t e n t i a l use i n t h e clean-up procedure sought i n t h i s
In Metal Complexes in Fossil Fuels; Filby, R., et al.; ACS Symposium Series; American Chemical Society: Washington, DC, 1987.
Group Isolation of Nickel and Vanadyl Porphyrins
405
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26. FREEMAN ET AL.
350
650 Wavelength
(nm)
F i g u r e 1. Nickel petroporphyrins (NiP) e x t r a c t e d from the M e s s e l s h a l e a r e m o n i t o r e d by s p e c t r o p h o t o m e t r y as they are c o n c e n t r a t e d i n f o u r - s t e p p r e p a r a t i v e column chromatography: e l u t i o n w i t h (A) b e n z e n e o n s i l i c a , a n d (B) b e n z e n e - m e t h a n o l o n L H - 2 0 , (C) w a t e r - M e C N gradient o n S e p - P a k C - 1 8 , a n d (D) h e x a n e - b e n z e n e g r a d i e n t o n S e p Pak s i l i c a .
In Metal Complexes in Fossil Fuels; Filby, R., et al.; ACS Symposium Series; American Chemical Society: Washington, DC, 1987.
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Elution Time (Min)
F i g u r e 2. The C-18 Sep-Pak column, s t e p C o f F i g u r e 1, i s shown w i t h a l i n e a r g r a d i e n t a t l m l / m i n f r o m 1:1 MeCN-water t o p u r e MeCN (10 min) w i t h N i P e l u t i o n a t 20 min. S i m i l a r l y , i n s t e p D a s i l i c a Sep-Pak column, e l u t i o n g r a d i e n t from p u r e hexane t o 1:2 hexane:benzene (9 m i n ) , i s shown. The N i P peak e l u t e s a t 13 min. The f e a s i b i l i t y o f s h o r t column c l e a n - u p p r o c e d u r e s i s demonstrated.
In Metal Complexes in Fossil Fuels; Filby, R., et al.; ACS Symposium Series; American Chemical Society: Washington, DC, 1987.
Downloaded by UNIV OF PITTSBURGH on May 3, 2015 | http://pubs.acs.org Publication Date: July 6, 1987 | doi: 10.1021/bk-1987-0344.ch026
26. FREEMAN ET AL.
Group Isolation of Nickel and Vanadyl Porphyrins
work. P r e l i m i n a r y column t e s t s were p e r f o r m e d w i t h s i l i c a g e l i n an attempt t o d e f i n e p r o p e r chromatographic conditions. An g l a s s c o l u m n w i t h a n a d j u s t a b l e b e d o f t h e M i c h e l - M i l l e r d e s i g n (Ace G l a s s Co., V i n e l a n d , N . J . ) was p a c k e d w i t h 1 0 0 g o f W o e l m s i l i c a g e l , 32-63μπι p a r t i c l e s i z e . A carrier gradient was r u n f r o m c y c l o h e x a n e t o d i c h l o r o m e t h a n e w h e r e i n t h e s o l v e n t s t r e n g t h was v a r i e d b y 0.04 p e r c o l u m n v o l u m e (13). N i a n d v a n a d y l p o r p h y r i n c o m p l e x e s , N i P a n d VOP, of e t i o p o r p h y r i n - I (Mid-Century Chemicals, Posen, IL) were u s e d t o m o n i t o r t h e s e p a r a t i o n s . Resolution of the N i P a n d VOP s t a n d a r d s b y t h e m s e l v e s was d e m o n s t r a t e d a s s h o w n i n t h e u p p e r c h r o m a t o g r a m o f F i g u r e 3. A similar t e s t w i t h a 1% l o a d o f N o r t h B e l r i d g e c r u d e o i l ( U n i o n O i l Company, B r e a , C A ) , t h a t h a d b e e n s p i k e d w i t h e q u i v a l e n t amount o f s t a n d a r d s , g a v e much w o r s e r e s u l t s a s s h o w n i n t h e l o w e r c h r o m a t o g r a m o f F i g u r e 3. Here, t h e N i P a n d VOP s e p a r a t i o n s w e r e i n c o m p l e t e a n d irreproducible. The h i g h l y p o l a r a n d d a r k l y p i g m e n t e d asphaltene m a t e r i a l s , sorbed i n i t i a l l y a t t h e head o f the column, b l e d o f f and coated t h e adsorbent, thus changing column c o n d i t i o n s as t h e s e p a r a t i o n proceded. An a d d i t i o n a l c o m p l i c a t i o n was a n t i c i p a t e d b e c a u s e vanadyl m e t a l l o p o r p h y r i n s form strong complexes w i t h L e w i s b a s e s (14) t h a t a r e p o s s i b l e c o m p o n e n t s o f c r u d e oil. Such complex f o r m a t i o n w i l l change t h e i r chromatographic behavior ( l u ) . Therefore, the present work i s n o t c o n f i n e d t o t h e i s o l a t i o n o f a d e f i n i t e c l a s s o f m e t a l l o p o r p h y r i n s , b u t t o a c l a s s t h a t may change i t s c o m p o s i t i o n d u r i n g t h e a n a l y s i s . A p r e l i m i n a r y s t r a t e g y was f o r m u l a t e d f r o m t h e s e experiments. An i n e x p e n s i v e s o r b e n t w i t h p r a c t i c a l mass l o a d i n g f o r adsorbed asphaltenes i s needed. A more d e t a i l e d knowledge o f s o l v e n t s e l e c t i v i t y e f f e c t s i s needed. An u n n e c e s s a r y c o m p l i c a t i o n w o u l d be a v o i d e d b y f i n d i n g conditions that minimize separation behavior of t h e N i P a n d VOP c o m p o n e n t s . Effect of S i l i c a Gel Porosity. I t i s known t h a t m a c r o p o r o s i t y tends t o boost t h e macromolecular sample l o a d c a p a c i t y o f s i l i c a g e l and i t s bonded phase derivatives. The p r e p a r a t i v e s e p a r a t i o n o f p r o t e i n s a n d o t h e r m a c r o m o l e c u l e s c a n be i m p r o v e d on t h i s b a s i s . Because asphaltene c o n t a i n s macromolecular components, t h e e f f e c t o f s i l i c a g e l p o r e s i z e was s t u d i e d u s i n g a s e r i e s o f Matrex s i l i c a g e l samples p r o v i d e d by t h e A m i c o n C o r p o r a t i o n ( D a n v e r s , MA). A t e s t s o l u t i o n was p r e p a r e d c o n s i s t i n g o f 1.00g o f B o s c a n o i l ( P h i l l i p s P e t r o l e u m C o m p a n y , B a r t l e s v i l l e , OK) d i s s o l v e d i n 4 0 m l of petroleum ether and methylene c h l o r i d e s o l u t i o n ( 5 0 : 1 ) . T h e l a t t e r was a d d e d t o r e t a r d d e a s p h a l t e n i n g . The c h r o m a t o g r a p h i c c o l u m n s u s e d i n t h i s w o r k w e r e g l a s s Flex-Columns (Kontes, V i n e l a n d , N J ) . The t e s t s o l u t i o n t u r n e d t h e s i l i c a g e l b l a c k a t the i n l e t end o f t h e column as t h e pigmented components
In Metal Complexes in Fossil Fuels; Filby, R., et al.; ACS Symposium Series; American Chemical Society: Washington, DC, 1987.
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408
METAL COMPLEXES IN FOSSIL FUELS
were a d s o r b e d . The b l a c k zone was f o u n d t o be c o r r e l a t e d i n s i z e w i t h t h e mass o f o i l sample. The sample l o a d c a p a c i t y , mass o f o i l p e r u n i t mass o f s i l i c a g e l bed t h a t had become d a r k , was t h e r e b y ascertained. P r e l i m i n a r y e x p e r i m e n t s were c a r r i e d out w i t h s i l i c a g e l samples o f 20-45μιη and 35-70μπι p a r t i c l e s i z e s , w i t h 60, 100, 250, 500 and 1000Â a v e r a g e p o r e sizes. The l o a d c a p a c i t y was h i g h e s t f o r t h e 500Â p o r e s i z e and 20-45μπ\ p a r t i c l e s i z e range, and t e n - f o l d h i g h e r t h a n t h a t o b t a i n e d w i t h 60Â and 35-70μπι. With s p e c i f i c regard t o the r e t e n t i o n of the a s p h a l t e n e - l i k e group, t h e e x p e r i m e n t s showed t h a t column l e n g t h can be s h o r t e n e d by p r o p o r t i o n t o l o a d c a p a c i t y f o r t h i s s i m p l e group s e p a r a t i o n . While the p r e s e n t r e s u l t s are s p e c i f i c f o r t h e Boscan r e f e r e n c e o i l , t h e h i g h sample l o a d c a p a c i t y o f t h e 250Â and 500Â m a t e r i a l s f o r t h e a s p h a l t e n e component have been v e r i f i e d i n t h e i n i t i a l a d s o r p t i o n s t e p w i t h s e v e r a l dozen c r u d e o i l s a m p l e s . A more d e t a i l e d i n v e s t i g a t i o n o f t h e e f f e c t o f p o r e s i z e i s b e i n g made ( 1 6 ) . T h i n l a y e r chromatography. 5μg samples o f NiP a n d / o r VOP s t a n d a r d s were s p o t t e d on aluminum b a c k e d s i l i c a g e l s h e e t (Eastman Kodak), 5cmX5cm s q u a r e s , and d e v e l o p e d i n the p r e s e n c e o f s o l v e n t v a p o r . 700μg o f s p i k e d c r u d e o i l ( d i s s o l v e d i n m e t h y l e n e c h l o r i d e ) was s p o t t e d o v e r 5μg s p o t s o f e a c h o f t h e s t a n d a r d s . P h o t o d e g r a d a t i o n was o b s e r v e d a f t e r NiP and VOP s p o t s were e x p o s e d f o r 16 h o u r s t o a 60 watt i n c a n d e s c e n t o r 16 watt f l u o r e s c e n t l i g h t (6 i n c h d i s t a n c e from l i g h t t o s a m p l e ) . A f t e r t h e e x p o s u r e , TLC development showed a new, more d e e p l y c o l o r e d and more h i g h l y r e t a i n e d band. NiP and VOP s t a n d a r d s , f o l l o w i n g TLC development, were a l s o f o u n d t o d a r k e n on s i l i c a a f t e r two weeks o f s t o r a g e a t room t e m p e r a t u r e i n t h e dark. The r e s u l t s showed c e r t a i n l i m i t a t i o n s b u t TLC a p p e a r s t o be v a l i d f o r m e t a l l o p o r p h y r i n s c o u t i n g under r e s t r i c t e d e x p o s u r e t o l i g h t , a i r and c o n t a c t w i t h t h e TLC a d s o r b e n t (17,18). The TLC e l u t i o n window f o r m e t a l l o p o r p h y r i n s has a wide s o l v e n t a c t i v i t y range ( 1 9 ) . Over one h u n d r e d TLC s c o u t i n g t e s t s were c a r r i e d out on t h e s p i k e d c r u d e o i l . S i n g l e and b i n a r y s o l v e n t s o l u t i o n s were u s e d f o r development i n t h e s o l v e n t a c t i v i t y range shown i n F i g u r e 4. The q u a l i t y o f t h e r e s u l t s was u n s a t i s f a c t o r y and m u l t i p l e p r o b l e m s were a p p a r e n t . P r a c t i c a l l y a l l of the i n d i v i d u a l s o l v e n t s a p p e a r e d t o be i n a p p r o p r i a t e . In t o l u e n e , f o r example, NiP and VOP m i g r a t i o n was s a t i s f a c t o r y b u t t h e d a r k a s p h a l t e n e s showed marked forward s t r e a k i n g , or f r o n t i n g . Metalloporphyrin t a i l i n g o c c u r r e d i n a c e t o n i t r i l e (MeCN), l i g h t e r a l c o h o l s and m e t h y l a c e t a t e (MeOAc). In p o l a r s o l v e n t s s u c h a s , MeCN, some o f t h e i n i t i a l sample s p o t o c c a s i o n a l l y f a i l e d t o d i s s o l v e and r e m a i n e d a t t h e origin. In h a l o g e n a t e d h y d r o c a r b o n s o l v e n t , s u c h as
In Metal Complexes in Fossil Fuels; Filby, R., et al.; ACS Symposium Series; American Chemical Society: Washington, DC, 1987.
26.
Group Isolation of Nickel and Vanadyl Porphyrins
FREEMAN ET AL.
NiP
409
κ Λ" VOP
Porphyrin
Boscan Oil
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1g., Spiked
llhlllllllls 1 2 3 4 5 6 7 8 9 10111213141516
718192021 22 2324 25 262728 2930
No. of Bed Volumes
0
10
F i g u r e 3. L i q u i d c h r o m a t o g r a p h y o f N i P a n d VOP s t a n d a r d s , a l o n e a n d i n c r u d e o i l i s s h o w n f o r a 60Â s i l i c a g e l column; s o l v e n t g r a d i e n t from c y c l o h e x a n e t o methylene c h l o r i d e . C h r o m a t o g r a p h y o f 10μg o f i n j e c t e d s t a n d a r d s , m o n i t o r e d a t 405nm, g a v e s a t i s f a c t o r y N i P / V O P separation. This s e l e c t i v i t y i s l o s t i n t h e lower c h r o m a t o g r a m w h e r e 1.Og o f B o s c a n c r u d e o i l , c o n t a i n i n g 0 . 1 % o f e a c h o f N i P a n d VOP s t a n d a r d s , w a s i n j e c t e d .
Rf
0.0
0.1
0.2
0.3
0.4 0.5
Solvent Strength
F i g u r e 4. O v e r o n e h u n d r e d d i f f e r e n t i n d i v i d u a l a n d b i n a r y s o l v e n t c o m p o s i t i o n s were mapped i n T L C experiments. T y p i c a l R f v a l u e s a r e shown i n t h e a b o v e (see r e f 18, p . 2 3 0 ) . The p r e s e n c e o f crude o i l ( n o t shown) c o n s i s t e n t l y i n t e r f e r e d w i t h t h e q u a l i t y o f t h e results.
In Metal Complexes in Fossil Fuels; Filby, R., et al.; ACS Symposium Series; American Chemical Society: Washington, DC, 1987.
410
METAL COMPLEXES IN FOSSIL FUELS
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methylene c h l o r i d e , t h e d a r k l y colored a s p h a l t e n e - l i k e components m i g r a t e d a l o n g w i t h t h e m e t a l l o p o r p h y r i n s . S o l v e n t b l e n d i n g was t r i e d . Improved band s h a r p n e s s was o b s e r v e d i n t h e p r e s e n c e o f t h e m o r e v o l a t i l e s o l v e n t s , e s p e c i a l l y m e t h y l e n e c h l o r i d e , MC, and p e t r o l e u m e t h e r , PE, (Baker C h e m i c a l Co., 35-60°C). Two d i m e n s i o n a l T L C s c o u t i n g . This approach gives a c l o s e r p a r a l l e l t o t h e d e s i r e d sequence i n which s a t u r a t e d a n d a t l e a s t some a r o m a t i c h y d r o c a r b o n s a r e e l u t e d before desorbing t h e m e t a l l o p o r p h y r i n group w i t h a stronger solvent. The i n i t i a l TLC d e v e l o p m e n t was d o n e w i t h 3:97 MC:PE. A o n e - m i n u t e p a u s e was made f o r solvent evaporation. T h e T L C p l a t e was t h e n r o t a t e d f o r p e r p e n d i c u l a r development. The s o l v e n t s a r e l i s t e d i n Table I . S i l i c a G e l TLC S c o u t i n g f o r Optimum E l u e n t C o m p o s i t i o n . The r e t e n t i o n a n d s e l e c t i v i t y o f t h e t w o metalloporphyrins s t a n d a r d s , N i P a n d VOP, w e r e a p t t o vary markedly with solvent composition. This i s i l l u s t r a t e d b y t h e T L C x e r o g r a p h s s h o w n i n F i g u r e 5. The c a p a c i t y f a c t o r s , k ( N i P ) a n d k ' ( V O P ) , a n d c o r r e s p o n d i n g VOP/NiP s e l e c t i v i t i e s were c a l c u l a t e d from t h e R f v a l u e s o b t a i n e d i n t h e TLC e x p e r i m e n t s u s i n g t h e w e l l - k n o w n r e l a t i o n s h i p , k' = (1 - R f ) / R f . The s e l e c t i v i t y , alpha, i s d e f i n e d as t h e r a t i o o f two d e s i g n a t e d k' v a l u e s — l a r g e r o v e r s m a l l e r . The o b s e r v e d s e l e c t i v i t y maxima f o r two b i n a r y s o l v e n t s y s t e m s a r e shown i n F i g u r e 6. Selectivity v a r i a t i o n s p r e s e n t two o p t i o n s , species s e p a r a t i o n under c o n d i t i o n s o f h i g h s e l e c t i v i t y and group s e p a r a t i o n s under c o n d i t i o n s o f low s e l e c t i v i t y . In t h e f i r s t stage o f a multi-step s e p a r a t i o n , group s e p a r a t i o n i snormally p r e f e r r e d . The c h a r a c t e r i s t i c s o f t h e N i P a n d VOP s t a n d a r d s were s t u d i e d a l o n e a n d a s s p i k e s added t o a sample o f a Boscan crude o i l ( P h i l l i p s Petroleum Co.), an a s p h a l t e n e - r i c h and m e t a l l o p o r p h y r i n - r i c h o i l used f o r reference purposes. The e f f e c t s o f s o l v e n t composition on t h e m e t a l l o p o r p h y r i n a n d t h e a s p h a l t e n e - l i k e g r o u p s were s t u d i e d . T h r e e o f t h e more h i g h l y d i f f e r e n t i a t e d TLC r e s u l t s are i l l u s t r a t e d i n Figure 7 ( a - c ) . I n F i g u r e 7(a) with toluene-cyclohexane (1:1) i n t e r m e d i a t e r e t e n t i o n o c c u r s but t h e N i P band i sb a d l y t a i l e d . The s t r o n g l y r e t a i n e d , d a r k l y c o l o r e d , a s p h a l t e n e - l i k e m a t r i x shows pronounced forward s t r e a k i n g , o r f r o n t i n g . In Figure 7 ( b ) w i t h T H F - c y c l o h e x a n e (7:3) t h e m e t a l l o p o r p h y r i n s t a n d a r d s a n d t h e dark m a t r i x components appear t o e x h i b i t f r a c t i o n a t i o n o f t h e a s p h a l t e n e - l i k e group which i s not s t r o n g l y r e t a i n e d and which brackets t h e metalloporphyrins. T h i s may b e d u e t o e x c e s s i v e s t r e n g t h o f t h e THF c o m p o n e n t . I n F i g u r e 7(c) with M e C N - m e t h y l e n e c h l o r i d e s o l v e n t s (1:1) t h e a s p h a l t e n e l i k e b a n d was r e t a i n e d w i t h o u t p r e d o m i n a n t f r o n t i n g . 1
In Metal Complexes in Fossil Fuels; Filby, R., et al.; ACS Symposium Series; American Chemical Society: Washington, DC, 1987.
26.
FREEMAN ET AL.
Table
I.
Group Isolation of Nickel and Vanadyl Porphyrins
Results
of
ID
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2D
ε
SOLVENT Pet. Ether (PE) Toluene Methylene Chloride Ethylene Chloride MeCN-MC-PE 1:1:4 1:2:3 1:3:2 1:4:1 2:3:1 2:1:0
and
(Fig. (0) (3) (6) (3) (6) (6)
Scouting
0
0.0 0.29 0.42 0.49 If)
Ν GN GN
R Ν GN G
R Ν GN GN
GN G GN GN G G
GN G GN GN G GR
GN GN GNR GN GNR GNR
GR R GNR GR
GNR GR GNR GR
GR R R GNR
GR R R GNR
0.5
G
A c e t o n i t r i l e (MeCN) Methanol Acetic Anhydride * Dimethylformamide *
0.65 0.95 1 1
G
G
GN
strength parameter values, ε
0
, are
S n y d e r ( H ) . A b o v e , ID a n d 2D, r e f e r t o TLC c r u d e o i l s p i k e d w i t h N i P a n d VOP standards G Ν R *
= = = =
TLC
2D
0.60 0.62 0.63 0.64
solvent
by
in
STPS-,
Methyl Acetate (MeOAc) Dimethylsulfoxide * Morpholine * Nitromethane
The
Tests
411
mainly
:
of Boscan O t h e r not
N i P and VOP G r o u p I s o l a t i o n ( R f > 0. 7) . N o n - t a i l i n g of metalloporphyrins A s p h a l t e n e s t r o n g l y r e t a i n e d (Rf < 0.2). S l o w TLC d e v e l o p m e n t .
In Metal Complexes in Fossil Fuels; Filby, R., et al.; ACS Symposium Series; American Chemical Society: Washington, DC, 1987.
412
METAL COMPLEXES IN FOSSIL FUELS
α = 9.4
α = 1.8
V
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• NiP
m Q
c
m
«
oa
i oa
NiP
VOP
. VOP
F i g u r e 5. S i l i c a T L C x e r o g r a p h y s h o w s how t h e a d s o r p t i o n s e l e c t i v i t y f o r N i P a n d VOP s t a n d a r d s v a r i e s f i v e - f o l d a s t h e c y c l o h e x a n e t o m e t h y l e n e c h l o r i d e (MC) s y s t e m i s c h a n g e d f r o m 1:1 ( l e f t ) t o p u r e MC ( r i g h t ) .
10H
10
20
40
30
50
%MC 1.0
MC, Cyclohexane System
• «—
1
MC, MeCN System
7—^^-w,
0.9
0.8
0.2 0.0
0.6 80
• •
0.7
Q VOP • NiP 100
1
1
10
1
1
1
20
Γ
1
30
VOP NiP 1
«
40
%MC
F i g u r e 6. N i P a n d VOP s t a n d a r d s o n s i l i c a g e l T L C g i v e v a r i e d R f a n d s e l e c t i v i t y (a) v a l u e s . While high metal speciation i s obtainable, the minimal metal species s e l e c t i v i t y needed f o r p o r p h y r i n group s e p a r a t i o n i s o b t a i n e d a t l o w a , p r e f e r a b l y on t h eMC-rich s i d e w i t h cyclohexane.
In Metal Complexes in Fossil Fuels; Filby, R., et al.; ACS Symposium Series; American Chemical Society: Washington, DC, 1987.
50
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26.
FREEMAN ET AL.
Group Isolation of Nickel and Vanadyl Porphyrins
•iNIP
Tol:CH (1:1)
1 Oil
VOP
THF:CH (7:3)
413
f NiP
Oil
VOP
MeCN:MC (1:1)
Figure 7. X e r o g r a p h e d s i l i c a TLC s c o u t i n g r e s u l t s a r e s h o w n f o r N i P a n d VOP s p i k e d B o s c a n o i l a t t h e c e n t e r o f e a c h TLC. At l e f t : a s p h a l t e n e components m i g r a t e w i t h marked forward s t r e a k i n g which i s t y p i c a l o f aromatic s o l v e n t systems. Middle: metalloporphyrins migrate together with asphaltenes. Right: t h i s was t h e f i r s t indication of asphaltenes being retained while metalloporphyrins migrate.
In Metal Complexes in Fossil Fuels; Filby, R., et al.; ACS Symposium Series; American Chemical Society: Washington, DC, 1987.
414
METAL COMPLEXES IN FOSSIL FUELS
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M e t a l l o p o r p h y r i n m i g r a t i o n w a s o b t a i n e d a t t h e same time. The p o t e n t i a l f o r s e p a r a t i n g t h e m e t a l l o p o r p h y r i n s f r o m t h e a s p h a l t e n e - l i k e g r o u p was i n d i c a t e d f o rt h e f i r s t time by t h i s r e s u l t . The c o l l e c t e d T L C r e s u l t s p r o v i d e d a k e y e v i d e n c e for t h e use o f s i l i c a g e lt o separate metalloporphyrins from t h e asphaltene group i n t e r f e r e n c e s . F u r t h e r , i n F i g u r e 7 (c) i t i s s e e n t h a t N i P a n d VOP a p p r o a c h c o e l u t i o n due t o t h e i r h i g h R f v a l u e s . Other problems were a p p a r e n t i n c l u d i n g m e t a l l o p o r p h y r i n t a i l i n g a n d less than complete r e t e n t i o n o f t h e a s p h a l t e n e - l i k e components. Y e l l o w p i g m e n t e d components were o b s e r v e d with diverse a f f i n i t i e s f o rs i l i c a g e l although t h i s i s not apparent i n t h e x e r o g r a p h i c records. O p t i m i z a t i o n o f TLC S o l v e n t T r i a d . Binary solvent s o l u t i o n s s h o w e d q u a l i f i e d a d v a n t a g e s , n o t a b l y MeCN o r methylene c h l o r i d e combined w i t h a s a t u r a t e d alkane d i l u e n t s u c h a s c y c l o h e x a n e (CH) o r p e t r o l e u m e t h e r (PE). A ternary mixture offered t h ep o t e n t i a l that t h e d i f f e r e n t advantages o f b i n a r y blends might be combined. An o p t i m i z a t i o n s t u d y i s u s u a l l y b a s e d o n t h e r e s o l u t i o n o f a l i m i t e d number o f compounds ( 2 0 ) . We a d a p t e d t h i s t y p e o f a p p r o a c h t o s t u d y t h e TLC o f t h e h i g h l y c o m p l e x m i x t u r e o f N i P a n d VOP s p i k e d c r u d e o i l w i t h t h e MeCNMC-PE s o l v e n t t r i a d . This extends t h e data i n Figure 6 beyond t h e two sets o f b i n a r y mixtures which a r e p a r t o f this triad. These TLC e x p e r i m e n t s g e n e r a t e d o v e r one h u n d r e d qualitative observations. The r e s u l t s were i n f o r m a t i v e , i n g e n e r a l terms f a i r t o good o v e r a l l , b u t no one s o l v e n t b l e n d seemed t o be e x c e l l e n t . A q u a n t i t a t i v e d e s c r i p t i o n o f t h e r e s u l t s w a s made i n o r d e r t o o b t a i n a more p r e c i s e c o m p o s i t e d e s c r i p t i o n o f e a c h TLC r e s u l t . The o b s e r v a t i o n s e t was r e f i n e d b y assigning numerical values t o previously q u a l i t a t i v e criteria. The f o l l o w i n g e v a l u a t i o n c r i t e r i a were d e f i n e d : (a) m i s c i b i l i t y o f s o l v e n t b l e n d s , (b) n o n t a i l i n g o f t h e m e t a l l o p o r p h y r i n s p i k e s , (c) s i m i l a r h i g h Rf v a l u e s f o r t h e m e t a l l o p o r p h y r i n s p i k e s — s i n c e t h a t c o n v e r g e s t o w a r d s u p p r e s e d V O P / N i P s e l e c t i v i t y , (d) n o n f r o n t i n g o f t h e N S O - a s p h a l t e n e b a n d , a n d (e) l a c k o f y e l l o w s u b s t a n c e s t h a t were a p t t o c o - e l u t e w i t h t h e metalloporphyrins. These performance c r i t e r i a d e s i g n a t e d ρ(a) t h r o u g h p ( e ) , w e r e m e a s u r e d o n t w o s c a l e s , 0-1 f o r t h e f i r s t , s o l v e n t m i s c i b i l i t y , a n d 0-3 for t h e others. The s c a l e s a r e b o t h p o s i t i v e ; z e r o i s bad a n d h i g h v a l u e s a r e good. To i l l u s t r a t e , i f t h e porphyrin e x h i b i t e d pronounced t a i l i n g then that r e s u l t was g r a d e d z e r o , p ( c ) = 0 f o r t h a t p a r t i c u l a r s o l v e n t composition. O r , s t r o n g a s p h a l t e n e r e t e n t i o n w i t h no d i s c e r n a b l e f r o n t i n g w o u l d s c o r e t h r e e , ρ ( d ) = 3. T h e s c a l e s have worst case zero v a l u e s , so zero l e v e l performance i n any c r i t e r i o n a t any composition forces a corresponding zero value i n t h e composite product value.
In Metal Complexes in Fossil Fuels; Filby, R., et al.; ACS Symposium Series; American Chemical Society: Washington, DC, 1987.
26.
Group Isolation of Nickel and Vanadyl Porphyrins
FREEMAN ET AL.
The n u m e r i c a l s c o r e s f o r e a c h o f t h e c r i t e r i a a r e shown i n F i g u r e 8 ( a - e ) f o r e a c h p e r f o r m a n c e c r i t e r i o n and c o m p o s i t i o n c o o r d i n a t e s as d e s i g n a t e d w i t h i n t h e triangular plots. A c o m p o s i t e p e r f o r m a n c e i n d e x , P, was obtained by m u l t i p l y i n g t h e i n d i v i d u a l performance values together a t each solvent composition.
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Ρ
=
p(a)p(b)p(c)p(d)p(e)
The c o m p o s i t e p e r f o r m a n c e i n d i c e s r e a c h e d t o 3 6 o u t o f 81 a s a p o s s i b l e maximum. Conveniently, the results g a v e s i n g l e d i g i t i n t e g e r v a l u e s a f t e r d i v i s i o n b y 6. The r e s u l t s a r e s h o w n i n F i g u r e 8 ( f ) . F i g u r e 8 ( f ) s h o w s t h e n u m e r i c a l l y h i g h e s t c o m p o s i t e i n d i c e s (P = 6) t h a t d e n o t e t h e o p t i m a l c a r r i e r c o m p o s i t i o n s b a s e d upon t h e s e one d i m e n s i o n a l TLC e x p e r i m e n t s . These s c o u t i n g e x p e r i m e n t s were c a r r i e d f u r t h e r by testing several intermediate l i q u i d compositions a d j a c e n t t o a l i n e c o n n e c t i n g t h e TLC p e r f o r m a n c e maxima a t Ρ = 6. No i m p r o v e m e n t was o b s e r v e d . B i d i m e n s i o n a l TLC a s a S o l v e n t S c r e e n . I t was r e c o g n i z e d t h a t t h e o n e d i m e n s i o n a l ID TLC e x p e r i m e n t s were n o t s t r i c t l y a n a l o g o u s t o t h e p l a n n e d t w o - s t e p i s o l a t i o n o f t h e m e t a l l o p o r p h y r i n group. A TLC s c o u t i n g s t u d y was c a r r i e d o u t s o a s t o b e m o r e a n a l o g o u s t o a n i n i t i a l d e v e l o p m e n t t o remove t h e s a t u r a t e s g r o u p . A second dimension, o b t a i n e d by p e r p e n d i c u l a r development, was d o n e w i t h v a r i o u s s o l v e n t s b e l i e v e d c a p a b l e o f p r o p e r l y desorbing t h e sought m e t a l l o p o r p h y r i n s . An e s s e n t i a l g o a l was t h a t t h e a s p h a l t e n e - l i k e g r o u p r e m a i n adsorbed. The 2D T L C r e s u l t s s u m m a r i z e d i n T a b l e I c o n f i r m t h e I D T L C f i n d i n g s g i v e n i n F i g u r e 8. The t h r e e o p t i m a l s o l v e n t b l e n d s n o t e d i n t h e MeCN-MC-PE s y s t e m , a s w e l l a s t h r e e new s y s t e m s , g a v e g o o d g r o u p s e p a r a t i o n o f t h e c o m b i n e d N i P a n d VOP s p i k e s f r o m c r u d e o i l . The 2D T L C e x p e r i m e n t s g a v e r e s u l t s t h a t d i f f e r e d s i g n i f i c a n t l y f r o m t h e ID TLC. I n f o u r i n s t a n c e s , a s shown i n T a b l e I , t h e p r e l i m i n a r y r e m o v a l o f t h e s a t u r a t e s g r o u p i m p r o v e d t h e q u a l i t y o f t h e s e c o n d TLC development. T h i s i s apparent from t h e improvement t r e n d i m p l i e d by t h e o v e r a l l r e s u l t s i n Table I . An i m p o r t a n t e x a m p l e o f t h i s o c c u r s w i t h MeOAc ( m e t h y l a c e t a t e ) w h i c h g a v e g r o s s t a i l i n g d u r i n g 1D-TLC o f t h e m e t a l l o p o r p h y r i n standards, alone and i n t h e spiked Boscan. I n 2D-TLC t h i s t a i l i n g e f f e c t d i s a p p e a r e d a n d MeOAc j o i n e d t h e s o l v e n t s d e s i g n a t e d w i t h s u p e r i o r performance. Among t h e s o l v e n t s t e s t e d , t h e l o w b o i l i n g p o i n t a n d l o w v i s c o s i t y o f MeOAc a r e m a r k e d a d v a n t a g e s . It i s concluded that t h e presence o f thesaturated and aromatic hydrocarbons, soon t o be c a l l e d t h e A l f r a c t i o n , i s able t o i n t e r f e r e w i t h t h e subsequent removal of t h e metalloporphyrins. A s t h e s o l v e n t s t r e n g t h (21.) was i n c r e a s e d f u r t h e r ,
In Metal Complexes in Fossil Fuels; Filby, R., et al.; ACS Symposium Series; American Chemical Society: Washington, DC, 1987.
415
416
METAL COMPLEXES IN FOSSIL FUELS
MC 1
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1
3 1
1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 0 0 0 0 0
3
1
(a) Miscibility
MeCN
3 3 3 2 3 3 3 2 0 3 3 2 0 0 0 2 2 2 0 0 0 0 0 0 3
3
PE
(b) NiP, VOP Tailing
2 0
0 3
2 3 3 2 2 3 3 0 3 3 2 3 0 3 3 3 3 2 0 2 3 3 2 3 0 0
(c) NiP, VOP Co-Elution
0 1
2
2 1 3 2 2 1 3 3 2 2 0 3 3 2 1 1 2 3 3 2 3 0 1 3
(d) Asphaltene Retention
1
0 0 1 1 1 2 2 1 2 3 1 1 0 2 3 2 2 0 2 3 3 3 3 3 1 3
(e) Yellow Pigment Isolation
0
2:3:1
0
0
1:3:2
\ 0
3 2 ^ 2 6 6 0 2:1:0—6 0 2 3 0 0 0 0 2 0 0 0 0 0 0 0 0 0
(f) Overall Performance
F i g u r e 8. A 2 8 - p o i n t TLC o p t i m i z a t i o n i s c a l c u l a t e d from e s t i m a t e d q u a l i t y o f s e p a r a t i o n b r o k e n down by category. Ο i s bad, 1 i s m i n i m a l and 3 i s maximal, as described i n the text. In (a) MC p r e v e n t s MeCN/PE i m m i s c i b i l i t y w h i l e i n (b) MC c o u n t e r s m e t a l l o p o r p h y r i n tailing. In (c) MeCN b o o s t s N i P and VOP c o - e l u t i o n w h i l e i n (d) i t promotes a s p h a l t e n e r e t e n t i o n . In (e) h i g h l e v e l s o f y e l l o w pigmented contamination, appearing immediately f o l l o w i n g the m e t a l l o p o r p h y r i n spikes, i s seen a t ρ = 0 o r 1 i n o n l y t h r e e l i q u i d c o m p o s i t i o n s . The " b e s t " o v e r a l l p e r f o r m a n c e c o m p o s i t i o n s a r e shown i n ( f ) ; see a l s o t a b l e I .
In Metal Complexes in Fossil Fuels; Filby, R., et al.; ACS Symposium Series; American Chemical Society: Washington, DC, 1987.
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26.
FREEMAN ET AL.
Group Isolation of Nickel and Vanadyl Porphyrins
t h e 2D TLC p e r f o r m a n c e improved and t h e n d e t e r i o r a t e d . One h i g h p o l a r i t y s o l v e n t , d i m e t h y l f o r m a m i d e , q u a l i f i e d as a s u p e r i o r m e t a l l o p o r p h y r i n d e s o r b a n t . (Less b e n e f i c i a l : i t e x h i b i t e d slow TLC development and i t has a high b o i l i n g point.) I t s d i s t i n c t i v e r o l e i n vanadyl p o r p h y r i n e x t r a c t i o n was r e p o r t e d i n t h e work o f S p e n c e r et a l ( 2 2 ) . I t i s l i k e l y t h a t o t h e r a t t r a c t i v e s o l v e n t systems c a n be f o u n d t o s a t i s f y t h e p e r f o r m a n c e c r i t e r i a named so f a r . The 2D TLC r e s u l t s f o r t h e b e s t s o l v e n t s i n T a b l e I show t h a t t h e i s o l a t i o n o f t h e N i P and VOP b i o m a r k e r g r o u p was e v a l u a t e d w i t h r e g a r d t o t h r e e key p r o p e r t i e s : i t was weakly r e t a i n e d , Rf v a l u e s o f 0.7 o r h i g h e r ( c l a s s "G" i n T a b l e I ) , w i t h o u t a p p a r e n t t a i l i n g ( c l a s s "N" i n T a b l e I) and w i t h s t r o n g r e t e n t i o n o f t h e a s p h a l t e n e - l i k e group ( c l a s s " R " ) . B a s e d on TLC, column e l u t i o n o f t h e m e t a l l o p o r p h y r i n g r o u p by t h e b e s t s o l v e n t s a r e d e s i g n a t e d by t h e t r i o o f s a t i s f a c t o r y c r i t e r i a , "GNR" i n T a b l e I . The G a l o n e means t h a t t h e combined b i o m a r k e r s a r e e x p e c t e d t o be c o m p l e t e l y e l u t e d w i t h i n one column volume a f t e r t h e f r o n t o f t h e m e t a l l o p o r p h y r i n band. W i t h f o u r s o l v e n t systems, d e s i g n a t e d w i t h an a s t e r i s k i n T a b l e I, t h e TLC m i g r a t i o n was c o n s p i c u o u s l y s l o w e r . These systems were not c o n s i d e r e d a c c e p t a b l e f o r column a p p l i c a t i o n b a s e d upon p o o r dynamic b e h a v i o r . Desorption of Metalloporphyrins. T e s t s were made o f t h e d e s o r p t i o n o f a d s o r b e d m e t a l l o p o r p h y r i n s from a m a c r o p o r o u s s i l i c a g e l column u s i n g t h e u n s p i k e d B o s c a n reference o i l . I n i t i a l l y t h e o i l was a d s o r b e d from c y c l o h e x a n e w i t h 3% MC as d e s c r i b e d i n t h e e x p e r i m e n t a l section. Then, 1:3:2 MeCN:MC:PE was added as t h e s e c o n d solvent t o desorb the metalloporphyrins. This solvent b l e n d r a n k e d among t h e b e s t b a s e d on t h e TLC t r i a d o p t i m i z a t i o n (see F i g u r e 8) and i t had t h e l e a s t amount of t h e h i g h e r b o i l i n g MeCN s o l v e n t . However, t h e c o l l e c t e d f r a c t i o n s showed t a i l i n g t h a t spanned o v e r e i g h t column volumes. T h i s was measured a t 20% sample l o a d (Boscan r e f e r e n c e o i l ) as shown i n F i g u r e 9. This d e s o r p t i o n c h a r a c t e r i s t i c was c o n s i s t e n t l y p o o r even a t s u b s t a n t i a l l y s m a l l e r sample l o a d s . This f a i l u r e i n r e t r o s p e c t s h o u l d n o t be c o n s i d e r e d t o o s u r p r i s i n g b e c a u s e t h e TLC t e s t s d i d n o t a c t u a l l y t e s t f o r desorption. Comparison was made, a g a i n a t 20% sample l o a d , w i t h MeOAc s o l v e n t f o r m e t a l l o p o r p h y r i n d e s o r p t i o n . These r e s u l t s a r e a l s o shown i n F i g u r e 9. The m e t a l l o p o r p h y r i n d e s o r p t i o n was 95% c o m p l e t e w i t h i n two column v o l u m e s . A l t h o u g h 20% sample mass l o a d i n g may seem u n u s u a l l y h i g h , we have so f a r o n l y r a r e l y o b s e r v e d evidence f o r overload during the i n i t i a l adsorption step. Thus, t h e i n i t i a l m e t a l l o p o r p h y r i n g r o u p i s o l a t i o n i s achieved: strong r e t e n t i o n of the a s p h a l t e n e - l i k e group w h i l e t h e s a t u r a t e s f r a c t i o n i s
In Metal Complexes in Fossil Fuels; Filby, R., et al.; ACS Symposium Series; American Chemical Society: Washington, DC, 1987.
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METAL COMPLEXES IN FOSSIL FUELS
418
removed, a n d h i g h r e c o v e r y o f t h e desorbed metalloporphyrins while t h e remainder o f t h e asphaltenel i k e group i sn o t desorbed.
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Final
Results
and Conclusions
P e t r o p o r p h y r i n s i n Boscan Crude O i l . As t h e r e s u l t o f the e x p e r i m e n t s on macroporpous s i l i c a g e l , a n d two d i m e n s i o n a l TLC a s g i v e n a b o v e , a g r o u p s e p a r a t i o n o f p o r p h y r i n c l a s s e s was d e v i s e d . The f i n a l scheme t h a t was a d o p t e d i s p r e s e n t e d i n F i g u r e 1 0 . T h r e e m a j o r p o r p h y r i n f r a c t i o n s i n t h e Boscan crude o i l and i n other petroleums subsequently studied a r e defined by t h e i r r e l a t i v e b e h a v i o r i n t h i s scheme: B - l t h e l o w p o l a r i t y N i P a n d VOP b i o m a r k e r m o l e c u l e s ; B-2 t h e p o l a r p o r p h y r i n s a n d A-3, a s p h a l t e n e - b o u n d m a t e r i a l . Details o f t h e e x p e r i m e n t a l method c o m p r i s i n g t h i s scheme a r e a s follows. A f i v e g r a m b e d o f M a t r e x s i l i c a g e l (500Â p o r e s , 20-45μπ\ p a r t i c l e s i z e ) was p a c k e d i n a 2.5cm i . d . b y 10 cm F l e x c o l u m n ( K o n t e s , V i n e l a n d , NJ) w i t h a r e s u l t i n g b e d h e i g h t o f a b o u t 3.5 cm. T h e s i l i c a g e l h a d b e e n d r i e d o v e r n i g h t a t 105°C. T h e b e d was e q u i l i b r a t e d w i t h m e t h y l e n e c h l o r i d e a n d t h e n washed w i t h f i v e column volumes o f a h y d r o c a r b o n s o l v e n t ; hexane o r p e t r o l e u m e t h e r gave s i m i l a r r e s u l t s . A one gram sample o f B o s c a n c r u d e o i l w a s a p p l i e d i n 4 0 m l o f c y c l o h e x a n e w i t h 3% added m e t h y l e n e c h l o r i d e . The m e t h y l e n e c h l o r i d e r e t a r d s asphaltene p r e c i p i t a t i o n and promotes e l u t i o n o f yellow non-porphyrins that interfere with spectrophotometry. T h e c o l u m n was t h e n e l u t e d w i t h 5 0 m l of hexane and methylene c h l o r i d e (97:3). M e t a l l o p o r p h y r i n s a r e s i g n i f i c a n t l y more s o l u b l e i n c y c l o h e x a n e t h a n i n p e t r o l e u m e t h e r and, d e p e n d i n g on the c o n d i t i o n o f t h e s i l i c a and t h e asphaltene content, some N i P may b e e l u t e d w i t h t h i s s o l v e n t . I t i s important t o t e s t t h e i n i t i a l hydrocarbon-rich eluant for losses of porphyrins. The s o l v e n t was c h a n g e d t o m e t h y l a c e t a t e t o d e s o r b the metalloporphyrins. A sharply defined asphaltene band remained s t r o n g l y r e t a i n e d w h i l e t h e deeply c o l o r e d m e t a l l o p o r p h y r i n g r o u p s m o v e d t o g e t h e r down t h e w h i t e column. E t h y l a c e t a t e was s u b s e q u e n t l y found t o behave a b o u t t h e same. R e t e n t i o n o f t h e A s p h a l t e n e - l i k e Group. The chromatographic retention o f the asphaltene-like i n t e r f e r e n c e s i s t h e k e y t o t h e s e p a r a t i o n scheme. The adsorption/desorption steps a r ea t least i n part c o n t r o l l e d by s o l u b i l i t y r e l a t e d processes. The A 1 / A 2 / A 3 s o l v e n t s t e p g r a d i e n t ( F i g u r e 10) e x e r t s control t o a s i g n i f i c a n t extent by providing low s o l u b i l i t y o f t h e a s p h a l t e n e - l i k e group i n t h e two i n i t i a l s o l v e n t s where t h e p r e d o m i n a n t a l k a n e a n d t h e n m e t h y l a c e t a t e h a v e t h e common c h a r a c t e r i s t i c t h a t
In Metal Complexes in Fossil Fuels; Filby, R., et al.; ACS Symposium Series; American Chemical Society: Washington, DC, 1987.
Group Isolation of Nickel and Vanadyl Porphyrins
FREEMAN ET AL.
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2
3
4
5
6
7
8
1
No. of Column Bed Volumes
2
3
4
5
6
419
7
8
No. of Column Bed Volumes
F i g u r e 9. T h e b i o m a r k e r f r a c t i o n f r o m t h e B o s c a n i s separated from t h e r e t a i n e d asphaltene f r a c t i o n a t high sample l o a d l g o i l / 5 g s i l i c a g e l . The m e t a l l o p o r p h y r i n e l u t i o n i n MeCN-MC-PE i s b a d l y t a i l e d . However, 95% o f the biomarker metalloporphyrins e l u t e d i n methyl acetate s o l v e n t w i t h i n two column volumes. (At l a s t ! )
Boscan Oil - 1.OOg Silica Gel (500A)-5.0g
MC:PE 600mg* (O.Omg)** I Sats, Aromatics
'Mass
"(Mass)
* Whole fraction ** Metalloporphyrin
MeOAc
Toluene:MC:MeOH
200mg (1.6mg) Silica Gel (100A)
40mg (0.2mg)
MC I 100mg (1.2mg) NiP and VOP Biomarkers
|
Asphaltenes
MeOAc 30mg (0.1 mg) Polar Metalloporphyrins
F i g u r e 10. S h o r t column c h r o m a t o g r a p h y w i t h m a c r o p o r o u s s i l i c a provides three i n i t i a l fractions of specified m a s s , w i t h t h e d e s i g n a t e d m e t a l l o p o r p h y r i n m a s s () b a s e d on S o r e t b a n d s p e c t r o p h o t o m e t r y . Various second stage options are available. I n t h e above, s i l i c a g e l separates t h e biomarker metalloporphyrins concentrated t e n - f o l d f o l l o w e d b y a more p o l a r m e t a l l o p o r p h y r i n fraction.
In Metal Complexes in Fossil Fuels; Filby, R., et al.; ACS Symposium Series; American Chemical Society: Washington, DC, 1987.
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METAL COMPLEXES IN FOSSIL FUELS
asphaltene group i s s t r o n g l y r e t a i n e d and b u t s p a r i n g l y soluble. The a s p h a l t e n e - l i k e g r o u p i s r e t a i n e d d u r i n g t h e i n i t i a l d e s o r p t i o n c o n d i t i o n s : (1) t h e e l u t i o n o f t h e s a t u r a t e d h y d r o c a r b o n s w i t h some a r o m a t i c c o m p o u n d s i n f r a c t i o n A l , a n d (2) d u r i n g t h e d e s o r p t i o n o f t h e m e t a l l o p o r p h y r i n A2 f r a c t i o n . N o t e t h a t t h e A2 f r a c t i o n contains metalloporphyrins concentrated f i v e - f o l d , but A2 i s s t i l l o v e r 9 9 % n o n - p o r p h y r i n i c a s s t a t e d i n F i g u r e 10. The f i n a l d e s o r p t i o n o f t h e A3 a s p h a l t e n e group depends upon a s p h a l t e n e s o l u b i l i t y i n t h e MeOH:Toluene:MC b l e n d . The " a s p h a l t e n e - l i k e " g r o u p A 3 i s d e f i n e d o p e r a t i o n a l l y by t h epresent chromatographic procedure. This appears t o overlap t h e o r i g i n a l Boussingault d e f i n i t i o n made i n 1 8 3 7 ( 2 3 ) i n w h i c h asphaltene s o l u b i l i t y i n turpentine and i n s o l u b i l i t y i n methanol are both s p e c i f i e d . This i sdiscussed i ngreater d e t a i l by B o c k r a t h a n d S c h w e i g h a r d t ( 2 4 ) . The a s p h a l t e n e - l i k e m a t e r i a l , as d e f i n e d by t h e present chromatographic p r o c e d u r e , appears t o be u n l i k e t h e s i m p l e r o p e r a t i o n a l d e f i n i t i o n based on i n s o l u b i l i t y i n a s p e c i f i e d lower a l k a n e s o l v e n t (2ϋ). Alkane p r e c i p i t a t e d asphaltenes normally contain metalloporphyrins while the " a s p h a l t e n e - l i k e " components d e f i n e d h e r e do n o t , e x c e p t p o s s i b l y t o a minor extent. I t i squite possible that the l a t t e r metalloporphyrins a r e chemically d i s t i n c t f r o m t h o s e o b t a i n e d b y e l u t i o n w i t h MeOAc. The e f f e c t o f t h i s o p t i m i z e d s e p a r a t i o n i s a much f a s t e r chromatographic basis f o r s u b - d i v i d i n g t h e crude o i l into a fraction that contains the metalloporphyrin groups which e l u t e e a s i l y , and t h e asphaltene i n t e r f e r e n c e s that a r e s t r o n g l y adsorbed. The m e a s u r e d 1 0 - f o l d r a n g e i n t h e s o r p t i o n c a p a c i t y of s i l i c a g e l , depending upon p o r e s i z e a n d p a r t i c l e s i z e , shows i t s e l f i n t h e f i n d i n g t h a t column h e i g h t s o f o n l y a f e w (3.5) c e n t i m e t e r s w e r e n e e d e d t o c a r r y o u t the present group s e p a r a t i o n s . The o p t i m i z e d asphaltene group s o r p t i o n c a p a c i t y provided by macroporous s i l i c a g e l means t h a t c o r r e s p o n d i n g l y l e s s s i l i c a g e l i s required. Correspondingly smaller quantities of elution solvent and o f e l u t i o n time a r et h e r e s u l t . I t i s n o t e d i n F i g u r e 10 t h a t t h e r e t a i n e d c o l u m n l o a d i s 2 0 0 mg o f A2 a n d 40mg f o r A 3 f r a c t i o n s . This s u g g e s t s t h a t t h e e f f e c t i v e l o a d s h o u l d be r e s t r i c t e d t o t h e a d s o r b e d c o m p o n e n t s : t h i s c o r r e s p o n d s t o 5% b a s e d o n a d s o r b e d mass o f t h e B o s c a n sample p e r mass o f t h e macroporous s i l i c a . This view i s l e s s i n f l a t e d than t h e 20% o f c o l u m n l o a d , s t a t e d e a r l i e r . The l a t t e r i n c l u d e s components t h a t do n o t a d s o r b and, p e r h a p s , s h o u l d n o t be c o u n t e d . The B o s c a n B l m e t a l l o p o r p h y r i n f r a c t i o n i s concentrated approximately t e n - f o l d as i n d i c a t e d i n F i g u r e 10. I n t h e t e s t i n g done s o f a r , m i n o r amounts o f t h e m o r e p o l a r B2 m e t a l l o p o r p h y r i n s h a v e b e e n o b s e r v e d in other crude o i l samples. I n sum, t h e s c h e m e
In Metal Complexes in Fossil Fuels; Filby, R., et al.; ACS Symposium Series; American Chemical Society: Washington, DC, 1987.
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g e n e r a t e s t h e A2 f r a c t i o n a n d t h e B l a n d B2 s u b f r a c t i o n s which appear t o be m e t h o d o l o g i c a l l y r o b u s t . The B l a n d B2 c l a s s i f i c a t i o n s a r e e a s i l y m o d i f i e d t o s e p a r a t e t h e N i P a n d VOP c o m p o n e n t s b y v a r y i n g t h e eluant r a t i o o f methylene c h l o r i d e and alkane diluent. The k e y t o t h i s f l e x i b i l i t y i s t h e p r i o r r e m o v a l o f t h e major i n t e r f e r e n c e s i nt h ei n i t i a l step. This enables more d e f i n i t i v e s u b s e q u e n t i s o l a t i o n s i n s u c c e e d i n g steps. These f a c i l e group s e p a r a t i o n s a r e o b t a i n e d because o f t h e i n t e r f e r e n c e s t h a t have been removed. The m e t h o d d e v e l o p m e n t c o n c l u d e s w i t h t h e finding that i t i s t h e f i r s t separation step that i so f primary importance. I n the present case, m e t a l l o p o r p h y r i n i s o l a t i o n i ss i m p l i f i e d by the i n i t i a l removal o f t h e major i n t e r f e r e n c e . I t i s because o f t h i s t h a t t h e d e f i n e d N i P a n d VOP b i o m a r k e r s c a n b e s e p a r a t e d f r o m e i t h e r t h e A2 o r B l g r o u p s . Acknowledgments
T h i s r e s e a r c h was f u n d e d i n p a r t b y a g r a n t f r o m t h e U.S. D e p a r t m e n t o f E n e r g y . C l i f f o r d Walters and P a t r i c k L. G r i z z l e w i t h t h e Sun E x p l o r a t i o n a n d P r o d u c t i o n Co. p r o v i d e d h e l p f u l g u i d a n c e a n d s u p p o r t . T e c h n i c a l d i s c u s s i o n s a n d s i l i c a g e l samples were h e l p f u l l y p r o v i d e d by the Chromatography Marketing Department o f Amicon C o r p o r a t i o n . Literature Cited 1.
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R E C E I V E D January 2, 1987
In Metal Complexes in Fossil Fuels; Filby, R., et al.; ACS Symposium Series; American Chemical Society: Washington, DC, 1987.