The Decomposition of Malic Acid by Sulfuric Acid - Journal of the

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Vol. 56

ROBERTE. DERIGHT [CONTRIBUTION FROM THE CHEMICAL

LABORATORY, UNIVERSITY

O F ROCHESTER]

The Decomposition of Malic Acid by Sulfuric Acid BY ROBERTE. DERIGHT The effect of inhibitors on the decomposition of organic acids by sulfuric acid has been explained on the basis of Taylor’s theory of negative catalysis.’ Wiig2 applied this theory to the decomposition by sulfuric acid of those organic acids for which data were available. Both water and sulfur trioxide have been found to inhibit these decompositions to varying extents. In accordance with this theory, Wiig has found maxima in the rate of decomposition of oxalic and citric acids3 with a change in the concentration of water and sulfur trioxide. Whitford4 found in the case of malic acid that 1% SO3 had no effect, while 12.5% SOs decreased the reaction rate. A study of the decomposition of malic acid by sulfuric acid was undertaken with the purpose of investigating more carefully the velocity of decomposition in the region where a maximum might be expected in order to determine whether the behavior of this acid conformed to the theory. The reaction between malic acid and sulfuric acid has been shown by v. Pechmann5 to take place in two steps COOH I

HCOH Primary

--+

CHz COOH CHO Secondary 2 CHz I I

COOH

+

CO

+ HsO

CHO I

CHz

COOH CH HC”C-COOH

,

+ 2H20

O=C\,CH

0

It is of course the velocity of the primary reaction that is determined. Experimental Part Preparation and Purification of Materials.-Kahlbaum inactive malic acid was used after a preliminary drying in eracuo a t 90’. Three sulfuric acid solutions were employed with compositions corresponding to 95.20, 99.64 and 105.93%. The first solution was the ordinary c. P. reagent, the third consisted of 30% c. P. fuming acid, while the second was Taylor, J. P h y s . Chem., 27,322 (1923). Wiig, THISJOURNAL, 62, 4742 (1930). Wiig, ibid., 62, 4737, 4742 (1930). Whitford, ibid., 47, 953 (1925). (5) V. Pechrnann, B e . , 17, 929, 936 (1884).

(1) (2) (3) (4)

made up of a mixture of the other two. The 95.20 and 105.93% solutions were analyzed by precipitation as barium sulfate, due precautions being taken to prevent absorption of water or loss of sulfiir trioxide. The 99.64yG acid was analyzed by taking a niixed freezing point with the fuming acid, the resulting mixture melting at 10.46”. The concentrations of the acids were further checked by determining the velocity of decomposition of citric acid in mixtures of them. The velocity constants thus obtained were in close agreement with those determined by Wiig.3 The acids were run from glass-stoppered storage bottles through an all-glass siphoning system to the burets, air being admitted, t o replace the acid withdrawn, by aspiration through two bottles containing 100% HZSO~. Apparatus and Method of Procedure.-The velocity of decomposition was determined by observing the volume of carbon monoxide evolved a t various times during the experiment. The apparatus and procedure employed were the same as those used in a previous investigation of formic acid.e The sulfuric acid solutions were made up as before (total volume of 15 cc.). Since concordant results could not be obtained when dry malic acid was used, it was dissolved in 81.63% sulfuric acid (15.99% malic acid; S4.01yo sulfuric acid solution), and this solution measured from a micro-buret into capsules. The water and sulfuric acid thus added were, of course, included in the calculation of the final concentration.

Results Completeness and Order of Reaction.-The reaction between malic and sulfuric acids has been shown by Whitford4 t u be unimolecular and homogeneous, and to be complete in 100% sulfuric acid. Quantitative determinations, in this investigation, showed that yields fell off with increasing amounts of SOs above 3%. This phenomenon is also observed in the decomposition of citric acid.3 Since the reaction is unimolecular, velocity constants may be calculat.ed by the equation k

=

2.303 - log t

a - x

a in most cases being taken as the total amount of carbon monoxide evolved. The Effect of Water and Sulfur Trioxide on the Reaction Rate.-In Tables I, 11, I11 and I V are given the velocity constants corresponding to various percentages of water and sulfur trioxide present. The concentration of inhibitor has been expressed in molality (moles of inhibitor/1000 ( 6 ) DeRight, THISJ O U R N A L , 55, 4761 (1933).

THEDECOMPOSITION OF MALIC ACIDBY SULFURIC ~ C

March, 1934

g. of solvent). Each value corresponds t o the average velocity constant a t 50% decomposition in from three to seven experiments. EFFECT 01' WATERON Water,

%

0 0.04 .07 .l5 .22 .32 .68

TABLE I THE REACTION VELOCITYAT 35" Molality of water

0 0.022 ,039 ,084 .122 .178 ,380

k X 101

87.5 90.3 86.1 75.8 72.1 65.2 45.1

TABLE I1 EFFECTOF SULFUR TRIOXIDE ON THE REACTION VELOCITY Sulfur trioxide, %

0.13 .61 1.32 3.57 7 05

AT 35" Molality of sulfur trioxide

k X 103

0.016 .078 .167 .460 ,950

86.4 35.2 25.1 19.8 18.2

EFFECT OF WATERON Water,

% 0 0.02 .04 .07 .l5

,z2 .32 .G8

619

I D

TABLE I11 THE REACTION VELOCITYAT 45' Molality of water

k X 10s

0 0.011 .022 ,039 ,084 ,122 ,178 .380

328.4 335.0 338.2 337.4 321. :3 280.0 2.54.3 155.3

TABLE IV EFFECT o r SULFUR TRIOXIDE ON THE REACTION VELOCITY AT 45' Sulfur trioxide, %

sulfur trioxide

Molality of

k X 102

0.09 .31 .61 1.51 3.57 7.05

0.011 ,039 ,078 .192 ,460 ,950

305.8 257.9 123.9 93.0 76.9 57.3

meaning unless taken a t the same distance from the maximum. The temperature coefficient 35-45' The data are shown graphically in Fig. 1. for 100% sulfuric acid found in this investigation These curves for the reaction rate a t various con- was 3.75, which is of the same order as those centrations of inhibitor show that after a certain found by the other in~estigators.~" minimum amount of water is present, 2.75 additional amounts of water have a marked inhibitory effect, the relative 2.50 effect diminishing with increasing 2,25 amounts of water. The curves show . a maximum a t molalities of water 5 2.00 0.024 and 0.030 for 35 and 4 5 O , re- X 1.75 spectively. The position of the M maximum and the slope on either 1.50 side is dependent upon the relative 1.25 inhibiting powers of water and sul1.oo fur trioxide. 0.4 0.2 0 0.2 0.4 1.0 0.8 0.6 The Effect of Temperature on Molality of inhibitor. SO3 +I-+ HpO. the Reaction Rate'-The Fig. 1.-Effect of sulfur trioxide and of water on the reaction rate. constants obtained by Whitford4 Discussion and by Dittmar' in 100% sulfuric acid a t 20, 30, 40 and 50" did not agree, but temperature coeffiThe decomposition of malic acid seems to be cients calculated from each set of data were con- best explained by Taylor's theory of negative cordant. The discrepancy was apparently due to catalysis, as is the decomposition of the several a slight error in concentration, as the temperature acids previously studied.2 The decomposition coefficients calculated a t 100% sulfuric acid are occurs through the formation of a malic acid-sulon the steepest part of the curve. The velocity furic acid complex, this disintegrating to give the constants found in this investigation agreed with decomposition products of malic acid and to rethose obtained by Dittmar.7 generate the sulfuric acid. The inhibition by water and by sulfur trioxide Since the maximum of the curve shifts with temperature, temperature coefficients have little appears to be brought about through the formation of a compound between the inhibitor and (7)Dittmar, Tms JOURNAL., 62, 4737 (1930).

3

620

HAROLD G. VESPER

AND

G. K . ROLLEFSON

1701. 56

the sulfuric acid-malic acid complex. The in- same inhibiting power in the decomposition of hibitor thus decreases the concentration of the some compound, the curve for the velocity of decomplex and thereby slows down the reaction. cornposition would be symmetrical and exhibit a The explanation for the maximum appears maximum at lOOyoHzS04. to be the same as for the other acids mentioned:? 'The sharp flattening out of the curve after a concentration of about 2y0 sulfur trioxide has i. e , there exists an equilibrium, H2S04ITSO3 H20. -4s water is removed the velocity of de- been reached is interesting. More than enough composition is accelerated until a point is reached sulfur trioxide is then present to form a molecular where the inhibiting effect of the increased con- compound with all of the malic acid or malic centration of sulfur trioxide more than offsets acid-sulfuric acid complex present ; hence, the the accelerating effect due to the removal of velocity measured from this point on may be that water. The maximum in the velocity of de- of the disintegration of this new complex. composition of malic acid came a t a molality of The author wishes gratefully to express his apwater of 0,024 and 0.030 a t 35 and 4 5 O , respec- preciation to Dr. Edwin 0. W i g , under whose tively, as compared to citric acid which exhibits a direction this work has been done, for his sincere maximum a t molalities of water of 0.10, 0.14, and friendly interest in the completion of it. 0.20 a t lg5, 25 and 35', r e ~ p e c t i r e l y . ~ The posiSummary tion of the maximum and the slope of the curve on either side of the maximum in both cases are The decomposition of malic acid by sulfuric evidence for the correctness of Wiig 's explanation. acid has been found to proceed in the same manner In each case sulfur trioxide is a stronger inhibitor as formic, oxalic and citric acids. -1maximum in the rate of decomposition has than water (as evidenced by the steeper slope of the curve in the sulfur trioxide region); hence, been found, the rate increasing up to a certain the maximum appears a t a small concentration of point as water was removed, then decreasing. water. The relative effect is not so pronounced The location of this maximum, which has been in the case of malic acid as in citric acid, so that overlooked in a previous investigation, brings the maximum falls nearer to zero concentration malic acid into agreement with the theory for of water. One would expect -from this theory. inhibition in the decomposition of these acids. if siilfur trioxide and water should have the ROCHESTER, N Y. RECEIVED NOVEMBER 28, 1933

+

[ C O N T R I B U T I O S FROM THE CHEMICAL

LABORATORY O F THE

The Equilibrium in the Reaction C1,

vNIVERSITY O F CALIFORNIA]

+ Br,

=

2BrC1

BY HAROLD G. VESPER A N D G. K. ROLLEFSON The existence of bromine chloride has been a subject of dispute for many years. Early investigators' recorded the formation of a yellow or red-brown liquid when chlorine was passed into bromine in a freezing mixture, or bromine into liquid chlorine, and assumed the liquid to contain bromine chloride. That this was other than a solution of bromine and chlorine was questioned2 on the basis of the small heat developed in the process, and from studies of the freezing point-. and boiling point-composition curves However, Andrews and Carlton3noted a marked contraction

in volume upon mixing liquid bromine and liquid chlorine, and workers4 in the field of organic chemistry have for some time reported that mixtures of bromine and chlorine in addition reactions give bromochloro products, as if the substance adding were bromine chloride. Physicochemical evidence for the formation of the compound BrC1 on mixing BrI and Clz in carbon tetrachloride solution was furnished by Barratt and Stein5 and by Gillam and Morton.6 I t was found that the absorption of light by the mixtures, in the visible region, was markedly less

(1) (a) Balard, A n n . chim. phys., [Z] 31, 337 (1826): (b) Schonbein, J. prakl. Chem., [ l ]88, 483 (1863); (c) Bornemann, .Inn., 189, 184 (1877): (d) T h o m a s a n d Dupois, C o m p f . rend., 143, 282 (1906). (2) (a) Berthelot, Compt. rend.;94, 1619 (1882); (b) Lebeau, ibid., 143, 589 (1906); (c) Karsten, 2 . anorg. Chem., 63, 365 (1907). (3) Andrews a n d Carlton, THIS J O U R N A L , 19, 688 (1907).

(4) (a) Simpson, Proc. Roy. SOC.(London), A W , 118, 424 (1879); cb) James, J. Chem. SOL.,43, 37 (1883); (c) Delepine and Ville, Compt. rend., 110, 1390 (1920); (d) Hanson and James, J , Chem. Soc., 1955, 2979 (1928). (5) Barratt and Stein, Proc. Roy. SOC. (I,ondoo), 8112, 582 (1929). (6) Gillam and Morton. ibid., Al24, 604 (1929).