9 Mechanism of Ozonation Reactions
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V . Feist's Ester RONALD
E. ERICKSON
and GARY D.
MERCER
University of Montana, Missoula, Mont. 59801
The
ozonation
of Feist's
ester yields
three
dicarbomethoxytetrahydrofuran-4-one thoxy-5-hydroxy-2-oxa-2,3-dihydropyran
NMR,
primarily
and infrared
is probably
through
and trapping
studies).
4,5-diwere
evidence
(mass,
compounds
product
A mechanism is
and
Structures
The last of these
ozonation
the initial step is formation stage, the breakdown
spectroscopic
spectra).
not a direct
(V).
2,3-
3,4-dicarbome-
(IV),
carbomethoxy-1-oxaspiro[2.2]pentane assigned
products:
(III),
(stoichiometry
is proposed
in
ozonide.
From
of a primary
which that
abnormal.
>Tphe structure of Feist's a c i d , l a , w a s d e t e r m i n e d w i t h c e r t a i n t y some 60 years after its p r e p a r a t i o n (1-6).
M o r e r e c e n t l y , the p r o p o s a l
that the o z o n a t i o n p r o d u c t of F e i s t ' s ester ( l b ) s h o w n to b e i n c o r r e c t ( 7 ) .
h a d s t r u c t u r e I I was
O u r i n i t i a l r e p o r t not o n l y s h o w e d t h a t no I I
w a s present i n a n y o z o n a t i o n of Feist's ester b u t offered c h e m i c a l a n d spectroscopic p r o o f for I I I as a m a j o r o z o n a t i o n p r o d u c t . RO—C^ Ο II RO-C
Η —
Ο II R O - C —
Ο CH
2
Ο
Ο
RO—C—C—C—C—CH
.
Ο.
HC \ HC-
I
I
COOR
I
Η la, R = H Ib, R = C H
Η
\
II
CH
2
/ -C Ο
RO
Ο
III
3
114 In Ozone Reactions with Organic Compounds; Bailey, P.; Advances in Chemistry; American Chemical Society: Washington, DC, 1972.
9.
ERICKSON A N D M E R C E R
Ozonation
115
Reactions
T h i s p a p e r is c o n c e r n e d w i t h t h e s t r u c t u r e p r o o f of e a c h of t h e major p r o d u c t s of the o z o n a t i o n of t h e m e t h y l ester of Feist's a c i d . O t h e r d a t a p e r t a i n i n g to t h e m e c h a n i s m of this u n u s u a l o z o n a t i o n are p r e s e n t e d , and
a m e c h a n i s m is h y p o t h e s i z e d .
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Experimental Materials. Solvents w e r e t h e best c o m m e r c i a l grades a v a i l a b l e a n d w e r e n o t p u r i f i e d f u r t h e r . F e i s t s a c i d w a s p r e p a r e d b y t h e m e t h o d of Goss et al. ( 2 ) . T h e m e t h y l ester w a s p r e p a r e d i n t h e n o r m a l F i s h e r m a n n e r w i t h m e t h a n o l a n d s u l f u r i c a c i d . A d d i t i o n of w a t e r , ether ex t r a c t i o n , r e m o v a l of ether, a n d d i s t i l l a t i o n y i e l d e d a colorless l i q u i d ( b p 7 8 ° - 8 0 ° C at 1.5 m m H g ) w h i c h c r y s t a l l i z e d u p o n s t a n d i n g , m p 30 ° C (lit. v a l u e 3 0 ° C ) ( 8 ) . 2,3-DiCARBOMETHOXYMETHYLENECYCLOPROPANE-2,3d2.
The
methyl
ester of Feist's a c i d w a s specifically d e u t e r a t e d b y d i s s o l v i n g 5.0 grams of t h e ester i n 25 m l of d e u t e r o m e t h a n o l c o n t a i n i n g 0.5 g r a m s o d i u m m e t h o x i d e a n d a l l o w i n g t h e m i x t u r e to s t a n d f o r o n e d a y . A f t e r a d d i n g 40 m l of d i l u t e s u l f u r i c a c i d a n d e x t r a c t i n g w i t h t w o 2 0 - m l p o r t i o n s of m e t h y l e n e c h l o r i d e , a d i s t i l l a t i o n y i e l d e d 3.5 grams of t h e d i d e u t e r o c o m p o u n d . Its N M R s p e c t r u m s h o w e d o n l y t h e m e t h o x y protons ( singlet at δ = 3.63) a n d m e t h y l e n e protons ( s i n g l e t at δ = 5.53). Ozonations. T h e ozonations w e r e c a r r i e d o u t u s i n g a W e l s b a c h T - 2 3 ozonator at — 78 ° C i n m e t h a n o l , m e t h y l e n e c h l o r i d e , F r e o n 11, or acetone. N o changes i n p r o d u c t ratios o r o z o n e s t o i c h i o m e t r y w e r e n o t e d w h e n n i t r o g e n w a s u s e d as the o z o n e c a r r i e r . Isolation of Products. P r o d u c t i s o l a t i o n p r o v e d to b e e x t r e m e l y difficult. A t y p i c a l p r o c e d u r e i n v o l v e d t h e o z o n a t i o n of t h e ester (2.0 g r a m s ) i n 30 m l m e t h a n o l at — 7 8 ° C u n t i l t h e s o l u t i o n b e c a m e b l u e a n d a precipitate h a d formed. After flushing w i t h nitrogen, a n d a l l o w i n g the m i x t u r e to s t a n d o v e r n i g h t at —78°C., w e c o l l e c t e d 1.0 g r a m of p r e c i p i tate. T h i s w a s r e c r y s t a l l i z e d three times f r o m 15 m l of a n h y d r o u s ether to y i e l d I I I , m p 6 7 ° - 7 1 ° C ( l i t . 6 8 ° C ) . E v a p o r a t i o n of t h e first ether r e c r y s t a l l i z a t i o n r e s i d u e a n d s l o w c r y s t a l l i z a t i o n f r o m 1.5 m l of a n h y d r o u s ether y i e l d e d c o m p o u n d I V , m p 9 6 ° - 1 0 2 ° C [ c a l c u l a t e d f o r C H i O : C — 44.04, Η = 4.58, Ο — 51.8; f o u n d : C = 44.67, Η — 4.66]. C o m p o u n d V w a s i s o l a t e d b y o z o n a t i o n of t h e ester i n F r e o n 11 at — 78 ° C a n d a l l o w i n g t h e p r e c i p i t a t e w h i c h f o r m e d to s t a n d i n s o l u t i o n o v e r n i g h t . A f t e r the p r e c i p i t a t e w a s c o l l e c t e d i n a c o l d B u c h n e r f u n n e l ( t h e p r e c i p i t a t e melts b e l o w 0 ° C a n d w a s s h o w n to b e a m i x t u r e of I I I a n d I V b y N M R ) , t h e filtrate w a s e v a p o r a t e d a n d t h e l i q u i d r e s i d u e w a s d i s t i l l e d to y i e l d ( b p 9 5 ° - 1 0 0 ° C . , 1 m m ) a m i x t u r e r i c h i n V ( > 9 0 % a c c o r d i n g to N M R ) [ c a l c u l a t e d f o r C H O r > : C = 51.63, Η =* 5.34, Ο = 43.03; f o u n d : C = 50.24, 50.53, Η = 5.27, 5.29]. 8
8
0
7
1 0
Product Analysis. Q u a n t i t a t i v e analysis f o r e a c h of t h e p r o d u c t s of t h e o z o n a t i o n of F e i s t ' s ester w a s c a r r i e d o u t b y a n N M R m e t h o d ( V a r i a n H A 6 0 ) . T h e solvent f o r t h e o z o n a t i o n w a s e v a p o r a t e d in vacuo, a s u i t a b l e i n t e r n a l s t a n d a r d ( u s u a l l y tert-butyl benzoate), was added a n d t h e spectra w e r e d e t e r m i n e d a n d i n t e g r a t e d i n c h l o r o f o r m - d . A l l analyses w e r e r e p r o d u c i b l e to ± 1 0 % .
In Ozone Reactions with Organic Compounds; Bailey, P.; Advances in Chemistry; American Chemical Society: Washington, DC, 1972.
116
OZONE REACTIONS W I T H ORGANIC COMPOUNDS
Table I.
Important Ions in the Mass Spectra of III and I l i a ///
ΙΠα m / e (%
Assignment Ρ P-H 0 P-OCH P-CH3OH 2
3
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P-C2H3O2
and P-C H and P-C H 2
2
{OCH CO}H 0 , CH 0, {C H 0 CHO}H 0 , CH OH
202 184 171 170 143
(2) (3) (9) (53) (73)
2
3
2
2
2
3
2
3
Assignment Ρ P-HDO P-OCH P-CH OD 3
3
P-C2H3O2
P-{OCH CO}D P-C2H3O2, C H 0 P-{C H 0 CDO}H P - C H 0 , CH2OD 2
113 (100)
2
3
m / e (% rel. abundance)
rel.
abundance)
2
2
111
(53)
2
3
3
2
2
204 (1) 185 (3) 173 (4) 171 (60) 145 (21) 144 (75) 115 (33) 114(100) 112 (63)
Results T h e structure of I I I was reasonably w e l l established i n l i m i n a r y c o m m u n i c a t i o n of this w o r k . A c o m p a r i s o n of its mass ( T a b l e I ) w i t h that of its d i d e u t e r o a n a l o g I l i a confirms its a n d p r o v i d e s a mass s p e c t r a l m o d e l for c o m p a r i s o n w i t h compounds I V and V . D H s C O O C - C ^ 1 H3COOC-C D
our pre spectrum structure unknown
,0, X
C H I C
2
0
III a T h e h i g h mass peaks i n T a b l e I c a n b e r a t i o n a l i z e d q u i t e easily. H o w e v e r , the ions of highest a b u n d a n c e at 143 a n d 113 i n I I I w h i c h at first glance c a n be assigned to f r a g m e n t a t i o n of a c a r b o m e t h o x y g r o u p are, f r o m i n s p e c t i o n of the d a t a f r o m I l i a , of m o r e c o m p l e x o r i g i n . C o m p o u n d I l i a h a d a p e a k at 145 as expected for loss of c a r b o m e t h o x y , b u t it also shows a n intense p e a k at 144 w h i c h m u s t c o m e f r o m the loss of { — O C H C = 0 } D . T h e d e u t e r i u m t h e o r e t i c a l l y c o u l d be transferred f r o m either t h e a or β carbons to either the keto or ether functions. N o n e of these rearrangements are p a r t i c u l a r l y f a c i l e a c c o r d i n g to the l i t e r a ture. T h e base peaks i n the spectra of I I I a n d I l i a ( 113 a n d 114 respec t i v e l y ) are also of interest. L o s s of c a r b o m e t h o x y a n d C H 0 , w h i c h appears to b e a l i k e l y f r a g m e n t a t i o n p a t t e r n , does not seem to o c c u r to a m a j o r extent for I l i a w h e r e the c o r r e s p o n d i n g 115 p e a k is present i n 2
2
In Ozone Reactions with Organic Compounds; Bailey, P.; Advances in Chemistry; American Chemical Society: Washington, DC, 1972.
9.
Ozonation
ERICKSON A N D M E R C E R
only 3 3 %
relative abundance.
117
Reactions
T h u s , a n o t h e r h y d r o g e n transfer, this
t i m e f r o m the m e t h y l e n e g r o u p to one of the o x y g e n atoms, m u s t t a k e place. T h e i n f r a r e d s p e c t r u m of I V i n d i c a t e s a n e n o l (3200 a n d 1650 c m " ) , 1
a n α,β u n s a t u r a t e d ester (1675 c m " ) , a n d a n o r m a l c a r b o m e t h o x y c a r 1
b o n y l g r o u p (1725 c m " ) .
T h e N M R s p e c t r u m substantiates t h e e n o l i c
1
character of the m o l e c u l e w i t h a singlet (δ •= 11.3 p p m ) . t w o d o u b l e t s ( ^ 4 . 4 0 a n d 4.84 p p m , / =
It also shows
16.5 c p s ) w h i c h c a n b e assigned
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to t w o m e t h y l e n e protons ( s i m i l a r c h e m i c a l shift to analogous
protons
i n I I I ) , a n d singlets at 3.78 p p m a n d 5.16 p p m . T h e r a t i o of protons w a s s h o w n to be 1 : 1 : 1 : 6 : 1 i n the o r d e r g i v e n . S u c h a s p e c t r u m is consistent w i t h either the e n o l f o r m of I I I ( I l l b s h o w n b e l o w ) or w i t h s t r u c t u r e I V .
H cooc-cif ° o
Hscooc^
N
3
?
H COOC— Cs.
P*
H
1 2
I
I
/C =
C
H COOC
2
^cr
I
OH
3
. C H
3
0
Illb
H
IV
C o m p o u n d I V gave a p o s i t i v e p e r o x i d e test w i t h p o t a s s i u m i o d i d e i n m e t h a n o l a n d a n a l y z e d r e a s o n a b l y w e l l for t h e s t r u c t u r e s h o w n .
How
ever, i t w a s difficult to p u r i f y a n d d e c o m p o s e d u p o n s t a n d i n g , a n d w e b e l i e v e d that mass s p e c t r a l e v i d e n c e w a s necessary for its final s t r u c t u r e proof.
W e e x p e r i e n c e d some difficulty i n o b t a i n i n g p u r e d i d e u t e r o I V
b u t w e r e a b l e to o b t a i n a satisfactory m o n o d e u t e r o
compound by
ex
c h a n g e of the e n o l i c p a t t e r n w i t h methanol-ci. T a b l e I I c o m p a r e s
the
mass s p e c t r u m of I V w i t h that of the m o n o d e u t e r o d e r i v a t i v e . H C O O C 8
^(V
N
CH
Ο
I
H C O O C ^
I
3
I OD
Although
IVa the p a r e n t , p a r e n t - O H ( D ) , a n d p a r e n t - H 0 2
(HDO)
peaks g i v e strong c o r r o b o r a t i v e e v i d e n c e for I V a n d I V a as the correct
In Ozone Reactions with Organic Compounds; Bailey, P.; Advances in Chemistry; American Chemical Society: Washington, DC, 1972.
118
OZONE REACTIONS W I T H
Table II.
Important Ions in the Mass Spectra of IV and IVa IV
Ρ P-OH P-H 0 P-OCH3 P-COOCH P-C H 0 or C H 0
218 (4) 201 (1) 200 (3) 187 (1) 159 (100)
2
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3
7
IVa
3
2
m / e (% rel. abundance)
m / e (% rel. Assignment abundance)
Assignment
3
ORGANIC C O M P O U N D S
3
127
4
(44)
Ρ P-OD P-HDO P-OCH P-COOCH P-C H 0 P-C H 0 P-C H D0 or C H D 0
219 (4) 201 (2) 200 (3) 188 (1) 160 (100)
3
3
3
7
3
2
3
4
3
6
128
(17)
127
(25)
3
2
2
4
s t r u c t u r e for the h i g h m e l t i n g c o m p o u n d , i n t e r p r e t a t i o n of the c o m p l e t e mass s p e c t r u m is not s t r a i g h t f o r w a r d . F o r e x a m p l e , t h e base p e a k for b o t h I V a n d I V a is a c c o u n t e d for r e a d i l y b y a loss of c a r b o m e t h o x y , b u t t h e s e c o n d most intense m/e, pathways
127, m u s t arise f r o m at least t w o different
( n e i t h e r of w h i c h is o b v i o u s ) .
The accumulated
evidence
leaves l i t t l e d o u b t b u t t h a t I V is the correct s t r u c t u r e of the h i g h m e l t i n g product. T h e t h i r d c o m p o u n d to b e i s o l a t e d f r o m ozonations of Feist's ester w a s V . Its N M R s p e c t r u m w a s of p r i m e i m p o r t a n c e i n e s t a b l i s h i n g its structure. O t h e r t h a n t h e m e t h o x y s i g n a l at 3.67 p p m , the o u t s t a n d i n g feature of the s p e c t r u m w a s t h e presence of t w o sets of A B d o u b l e t s w i t h c h e m i c a l shifts f o r the f o u r protons at 3.33, 3.23, 2.90, a n d 2.72 p p m . T h e r a t i o of p e a k intensities w a s 6 : 1 : 1 : 1 : 1 for the five types of protons. I n t h e s p e c t r u m of the d i d e u t e r o d e r i v a t i v e , the A B p a t t e r n at h i g h field w a s n o t present, s h o w i n g t h a t these h i g h field protons w e r e those a to the c a r b o m e t h o x y Table III.
groups. Important Ions in the Mass Spectra of V and V a V m / e (% rel. abundance)
Assignment Ρ P-CH 0 P-OCH3 P-CH3OH P-C H 0 P-C H 0 , C H 2
2
3
2
3
2
2
Va
2
186 (0) 156 (2) 155 (11) 154 (12) 127 (100) 113 (40)
m / e (% rel. abundance)
Assignment Ρ P-CH 0 P-OCH3 P-CH OD 2
3
P-C2H3O2
P-C H 0 , C H 2
3
2
2
188 (0) 158 (2) 157 (12) 155 (13) 129 (100) 115 (44)
T h e m a j o r features of the mass s p e c t r a of V a n d its d i d e u t e r o d e r i v a t i v e are p r e s e n t e d i n T a b l e I I I . A l t h o u g h w e w e r e u n a b l e to detect t h e p a r e n t p e a k for V , t h e r e a s o n a b l e assignments i n T a b l e I I , the s i m p l i c i t y
In Ozone Reactions with Organic Compounds; Bailey, P.; Advances in Chemistry; American Chemical Society: Washington, DC, 1972.
9.
ERiCKsoN AND M E R C E R
Ozonation
119
Reactions
of the N M R s p e c t r u m , a c o m p a r i s o n w i t h n o r m a l e p o x i d e c h e m i c a l shifts ( m e t h y l e n e signals at l o w e r field t h a n m e t h o x y s i g n a l s ) , a n d the a n a lytical
data
compound
argue
for
4 , 5 - d i c a r b o m e t h o x y - l - o x a s p i r o [2.2] p e n t a n e
as
V. Ο
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II
T a b l e I V s u m m a r i z e s s o m e of the s p e c t r a l d a t a for the assignment of s t r u c t u r e to c o m p o u n d s I I I , I V , a n d V . T a b l e V shows the r e l a t i v e amounts of I I I , I V , a n d V f o u n d i n differ ent solvents u n d e r v a r i a b l e e x p e r i m e n t a l c o n d i t i o n s . K n o w l e d g e of the m a j o r p r o d u c t s of the o z o n a t i o n of F e i s t ' s ester does not l e a d i m m e d i a t e l y to a k n o w l e d g e of t h e m e c h a n i s m of the r e a c t i o n a l t h o u g h the n a t u r e of t h e p r o d u c t s m a k e s i t o b v i o u s
t h a t the
m e c h a n i s m is different f r o m t h a t of most ozonations. H o w e v e r , i n s p e c t i o n of T a b l e I V , i n w h i c h p r o d u c t ratios change w i t h changes i n c o n d i t i o n s a n d other types of e x p e r i m e n t s , a l l o w s us to r a t i o n a l i z e a reasonable m e c h a n i s t i c sequence. T h e m o s t i m p o r t a n t p o i n t s to n o t e a r e : ( 1 ) T h e e p o x i d e is not a p r i m a r y p r o d u c t ; b o t h the s t o i c h i o m e t r y a n d the t e t r a c y a n o e t h y l e n e experiments i n d i c a t e that i t is f o r m e d f r o m a t t a c k of a n i n t e r m e d i a t e o n u n r e a c t e d F e i s t ' s ester. F o r e x a m p l e , less t h a n 1 m o l e of o z o n e p e r m o l e of Feist's ester is r e q u i r e d for a l l o z o n a t i o n s — w i t h the less r e a c t i v e solvents, s u c h as m e t h y l e n e c h l o r i d e a n d F r e o n 11, the d e f i c i e n c y i n o z o n e r e q u i r e d is a p p r o x i m a t e l y e q u a l to the a m o u n t of e p o x i d e f o r m e d . A d d i t i o n of t e t r a c y a n o e t h y l e n e b e f o r e o z o n a t i o n results i n a n o z o n a t i o n of n o r m a l s t o i c h i o m e t r y w i t h n o e p o x i d e being formed. ( 2 ) I f the r e a c t i o n is s t o p p e d b e f o r e c o m p l e t i o n , t h e r e l a t i v e a m o u n t s of I V f o r m e d are g r e a t l y decreased. T h i s suggests to us t h a t the i n i t i a l o z o n a t i o n p r o d u c t has s e v e r a l m o d e s of d e c o m p o s i t i o n a v a i l a b l e , a n d that r e a c t i o n w i t h F e i s t ' s ester ( o r t e t r a c y a n o e t h y l e n e ) is m o r e r a p i d than unimolecular decomposition. ( 3 ) W e w e r e u n a b l e to mary ozonide ( 9 ) ] b y l o w a b o v e - m e n t i o n e d results a n d ester s t r o n g l y suggest t h a t a
detect a n i n t e r m e d i a t e [e.g., Criegee's p r i t e m p e r a t u r e N M R (to — 1 3 0 ° C ) ; y e t t h e t h e f a c t t h a t I V does n o t r e a c t w i t h F e i s t ' s h i g h l y r e a c t i v e i n t e r m e d i a t e does exist.
In Ozone Reactions with Organic Compounds; Bailey, P.; Advances in Chemistry; American Chemical Society: Washington, DC, 1972.
120
O Z O N E R E A C T I O N S W I T H ORGANIC
COMPOUNDS
Table I V .
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Compound
C-H
Mp,
Spectral MW
°C
III
ΟδΗχοΟβ
67-71
202
IV
ΟδΗχοΟγ
96-102
218
V
CSHIOOÔ
liquid
186
° As reported i n Ref.
7.
W e h y p o t h e s i z e t h e f o l l o w i n g g e n e r a l r e a c t i o n scheme: H
C O O C .
3
C H
2
+
0
3
H3COOC la
N C
C N
P a t h a i n v o l v e s u n i m o l e c u l a r d e c o m p o s i t i o n of a n i n i t i a l (VI).
I t is i m p o r t a n t to n o t e that since o t h e r
ozonide
methylenecyclopropane
d e r i v a t i v e s , s u c h as 2 , 3 - d i m e t h y l m e t h y l e n e c y c l o p r o p a n e , d o not u n d e r g o r i n g o p e n i n g o f t h e c y c l o p r o p a n e r i n g , b o t h r i n g strain a n d t h e presence of t h e c a r b o m e t h o x y g r o u p s m u s t be necessary for s u c h a n u n u s u a l d e c o m p o s i t i o n of a n i n i t i a l o z o n i d e .
T h e f o l l o w i n g sequence r a t i o n a l i z e s
In Ozone Reactions with Organic Compounds; Bailey, P.; Advances in Chemistry; American Chemical Society: Washington, DC, 1972.
9.
ERICKSON AND
MERCER
Ozonation
121
Reactions
Data for III, I V , and V
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Infrared,
NMR σ mult. (rel. intensity)
cm~i
1778, 1740, 1675, 1636
5.1d(l), 4.25d(l), 3.8e(6), 3.7d(l)
3200, 1725, 1675, 1600
1 1 . 3 8 ( 1 ) , 5.16e(l), 4 . 8 4 d ( l ) , 4 . 5 5 d ( l ) , 3.78s(6)
3080, 3030, 1720, 890, 865, 833
3.67sC6), 3 . 3 3 d ( l ) , 2.90d(l), 2.72d(l)
4.12d(l),
e
3.23d(l),
s u c h a n o c c u r r e n c e b y suggesting that a p a r t i a l n e g a t i v e charge is sta b i l i z e d b y the c a r b o m e t h o x y groups.
Just as the c o n v e r s i o n of V I to I V m a y b e a c o n c e r t e d r e a c t i o n w i t h o u t the i n t e r m e d i a r y a c t i o n of V I I , so p a t h w a y b m i g h t r e a s o n a b l y i n v o l v e either V I or V I I . C r i e g e e a n d G u n t h e r h a v e s h o w n that t e t r a c y a n o e t h y l e n e c a n c h a n g e the n o r m a l course of t h e o z o n a t i o n of alkenes b y r e a c t i o n w i t h e i t h e r a z w i t t e r i o n or t h e " p r i m a r y " o z o n i d e p r o d u c e d i n s u c h reactions (10).
W e h a v e no p r o o f as to w h e t h e r t e t r a c y a n o e t h y l e n e
reacts w i t h V I or V I I , a n d e i t h e r r e a c t i o n c a n b e e n v i s a g e d t o p r o d u c e I I I as i n p a t h w a y c.
W e are left w i t h t h e d i f f i c u l t y of e x p l a i n i n g t h e
r e l a t i v e l y h i g h y i e l d s of I I I i n some solvents l i s t e d i n T a b l e I V .
When
I I I , a t w o - o x y g e n p r o d u c t is f o r m e d , e i t h e r o x y g e n or some o t h e r o x i d i z e d
In Ozone Reactions with Organic Compounds; Bailey, P.; Advances in Chemistry; American Chemical Society: Washington, DC, 1972.
122
OZONE REACTIONS W I T H
Table V .
CH2CI2 CH3OH CH OH« F r e o n 11 Freon 1 1 Acetone Acetone-CH Cl Acetone-CH Cl ' b
2
2
2
2
c
d
Relative III 40 64 57 35 62 38 33 71
0.67 0.76 0.86 0.74 0.71 0.75 0.65 1.03
3
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Relative Yields
Stoichiometry, moles Oz/moles I
Solvent
ORGANIC C O M P O U N D S
Yields,
%
IV
V
21 23 13 33 0 30 32 29
39 13 30 30 37 32 35 0
Reaction stopped after 60% of I had reacted. Reaction stopped after 34% of I had reacted. 75% C H 2 C I 2 by volume. Tetracyanoethylene (equimolar with I) added before reaction began.
a 6 c d
product must be produced.
W i t h o x i d i z a b l e solvents, s u c h as m e t h a n o l
or acetone, t h e most reasonable a s s u m p t i o n m i g h t b e that V I o r V I I reacts w i t h solvent to y i e l d I I I ( p a t h d ) , b u t w e h a v e n o d i r e c t p r o o f for such a n assumption. S t o r y et al. h a v e suggested that V I I I m i g h t b e t h e i m p o r t a n t i n t e r m e d i a t e i n t h e o z o n a t i o n o f Feist's ester ( I I ) .
VIII
I f this is the i n t e r m e d i a t e , other m e t h y l e n e c y c l o p r o p a n e s s h o u l d g i v e o z o n a t i o n p r o d u c t s s i m i l a r t o those f o u n d i n t h e o z o n a t i o n o f Feist's ester.
Since they do not a n d because o u r evidence indicates that t h e
e p o x i d e is n o t a p r i m a r y p r o d u c t , t h e m e c h a n i s m o f Story et al. does n o t seem t o a p p l y t o this r e a c t i o n .
Literature Cited 1. Feist, F., Chem. Ber. (1893) 26, 747. 2. Goss, F. R., Ingold, C. T., Thorpe, J. F., J. Chem. Soc. (1923) 123, 327.
In Ozone Reactions with Organic Compounds; Bailey, P.; Advances in Chemistry; American Chemical Society: Washington, DC, 1972.
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Ozonation Reactions
123
9.
ERICKSON AND M E R C E R
3. 4. 5. 6. 7. 8. 9. 10. 11.
Ettlinger, M . G . , J. Amer. Chem. Soc. (1952) 74, 5805. Ettlinger, M . G . , Kennedy, F . , Chim. Ind. (1956) 166. Kende, A. S., Chim. Ind. (1956) 437. Bottini, A. T., Roberts, J. D . , J. Org. Chem. (1956) 2 1 , 1169. Erickson, R. E., Tetrahedron Letters (1966) 1753. Schwan, U . , Ph.D. thesis, Technische Hochschule, Karlsruhe (1958). Criegee, R., Rec. Chem. Progr. (1957) 18, 111. Criegee, R., Günther, P., Chem. Ber. (1963) 96, 1564. Story, P. R., Alford, J. Α., Ray, W . L., Burgess, J. R., Preprints, Div. Petro leum Chemistry, ACS (1971) 16, A13.
R E C E I V E D May 20, 1971. Supported by the Petroleum Research Fund, admin istered by the American Chemical Society.
In Ozone Reactions with Organic Compounds; Bailey, P.; Advances in Chemistry; American Chemical Society: Washington, DC, 1972.
COMPOUNDS
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O Z O N E R E A C T I O N S W I T H ORGANIC
In Ozone Reactions with Organic Compounds; Bailey, P.; Advances in Chemistry; American Chemical Society: Washington, DC, 1972.