Photochemical smog. Rate parameter estimates ... - ACS Publications

Rate Parameter Estimates and Computer Simulations. Alan C. Baldwin,1 John R. Barker,* David M. Golden, and Dale G. Hendry*. Chemistry Laboratory, SRI ...
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Computer Modeling of Photochemical Smog (2) C. W. Gear, ”Numerical Initial Value Problems in (3)

Ordinary Differential Equations”,Prentice Hall, Englewood Cliffs, N.J., 1971, Chapter 11. T. E. Graedel, L. A. Farrow, and T. A. Weber, Atmos. Environ., 10,

1095 (1976). (4) T. E. Graedel, L. A. Farrow, and T. A. Weber, Atmos. Environ., in

press. (5) B. J. Finiayson and J. N. Pitts, Jr., Science, 192, 111 (1976). (6) D. H. Stedman and J. 0. Jackson, Int. J . Chem. Kinet. Symp., 1, 493 (1975). (7) J. G. Calvert, Environ. Sci. Technol., 10, 248 (1976).

Discussion W. H. DUEWER (Lawrence Livermore Laboratory). The stationary state assumption for various free radicals has been tested by other modelers and found to be satisfactory for several. The large discrepancies found by the authors suggest errors either in the formulation of the model or of the steady state expression. Because only a few terms were included in the steady state approximations used, I suspect the latter. If there is no error (e.g., omitted significant terms) then the significant differences between your model and other models that cause your model not to behave

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as a steady state species should be described. In the case of NO/NOz/O, local NO emissions might do this in the evening, but 03 transport is unlikely. The time scales for reaching steady state in that system is =10-100 s. Interbox transport should be very much slower under most circumstances. L. A. FARROW: The more complete discussion in the published paper shows that for HO-the poor agreement at noon can indeed be attributed to the need for inclusion of more terms in the SSA formulation. However, the ability to show this deficiency in terms can only exist because the complete solution, done without any approximations, is available for comparison. In addition once the complete solution is obtained,approximate ones are obviously superfluous. Since the complete solution can be obtained with no sacrifice in computer time, particularly for large systems of equations, and since it gives results without mathematical errors, it should be used for chemical kinetic problems. Upon recalculating the photostationary relationship, I found that taking a mean value for the photodissociative rate for NOzled to an error. When the exact rate corresponding to the time of day is used, the photostationary state is found to hold remarkably well, as is described in the paper submitted for publication.

Photochemical Smog. Rate Parameter Estimates and Computer Simulations Alan C. Baldwin,+ John R. Barker,* David M. Golden, and Dale G. Hendry” Chemistv Laboratory, SRI International, Menlo Park, California 94025 (Received May 12, 1977) Publication costs assisted by the U.S. Environmental Protection Agency

Evaluation of experimental data and estimation techniques have been used to obtain rate coefficients for classes of alkoxyl radical reactions: (1) unimolecular decomposition, (2) reactions with 02,and (3) unimolecular isomerization. The uncertainties in log h (300 K,1 atm air) are estimated to be fO.9, f1.2, and f1.8,respectively, reflecting the current state of knowledge about these reactions. The reaction HOZ + NO2 + M HOzNOz + M is also discussed, and the results of an RRKM calculation are presented; this reaction is shown to be of great potential importance in the urban atmosphere, and experimental data are needed. Using the rate constants obtained in the first portion of this paper, explicit smog mechanisms for n-butane and propene were developed. Several simulations of smog chamber data are presented and the effects of rate constant uncertainties are illustrated. The mechanisms are shown to give good agreement with the experimental data, but several areas of uncertainty remain.

I. Introduction Extensive efforts are underway throughout the world to accurately model atmospheric chemistry. Whether the efforts are directed toward modeling tropospheric or stratospheric phenomena, there is a need to evaluate existing rate constant data and to estimate unknown rate parameters in a way that is consistent with current knowledge for similar reactions. We are developing an explicit reaction mechanism to explain data obtained in smog chambers and we are constantly faced with the fact that too few accurate rate data for elementary reactions are available. Since the kinetic data on particular families of reactions ranges from “excellent and extensive” to “nonexistent”, a variety of methods must be used for evaluation and/or estimation. As a general guiding principle, it has been found that best results are obtained when reactions are treated as “families” rather than as individuals, because only rarely are enough data available on an individual reaction to make a meaningful evaluation. A second guiding principle often overlooked is that an estimate or evaluation is not useful unless accompanied by a fair assessment of its probable accuracy. Since A factor and activation energy combine to give a single rate ‘Postdoctoral Research Associate.

constant, we have adopted the method of propagation of errors to estimate the uncertainty in rate constants, based on the probable uncertainties associated with A factor and activation energy. This estimate of uncertainty is very useful since it is a quantitative measure indicating whether an estimated rate constant can be legitimately varied and over what range. In the next three sections, some reactions of alkoxyl radicals will be discussed. Alkoxy1 radicals are important intermediates in photochemical smog as illustrated by the schematic reaction sequence: OH + RH- H,O t R* R*t 0,-aRO, RO, + N O - RO t NO, RO t 0, HO, + carbonyl compound HO, + NO OH + NO, Three of the possible reactions of alkoxyl radicals in photochemical smog will be discussed in sections 11-IV: decomposition, reaction with oxygen, and isomerization. In section V, estimates for the reactions of HOz with NOz will be presented, and in section VI, several simulations of smog chamber data will be presented for comparison to the experimental data. Our general conclusions are presented in the last section.

-

+

The Journal of Physjcal Chemistry, Vol. 8 1, No. 25, 1977

2484

Baldwin et al. 108

104

107

lo3

1o(

-

102

-

-

10E

10'

10'

100

10:

20

-

35

30

15

'000 T

Flgure 1. t-BuO. 4- M Me 4- acetone 4- M: V, ref 10; 0 , ref 11; A, ref 12; 0, ref 13; dashed line, ref IC; solid line given by log k(s-') = 15.2 - 15.918.

TABLE I: Experimental Values for EO. Decomposition Ratesa ~~~

log

Radical

EtO. i-PrO.

s-BuO. t-BuO,

log

A E A,"' 13.7 22.1 33.4 16.1 20.6 37.8 16.4 18.0 37.7 14.9 15.3 15.1 16.2 4 1 . 2

log A,

log Aest

E'

~

Ref

10-1

-

Figure 2. Et00 4- M Me 4- CH,O 4- M: 0, ref 5; line given by log k(s-') = 13.7 - 21.618. I

I

I

8 . 2 13.7 22.1 5 8 . 2 14.6 17.4 6,7 13.9 a 8,O 14.4 14.2 9 8.0 15.2 16.3 10-13

Units: E in kcal mol-' ; A , in iW1 s-' ; A in s-'

a

11. Alkoxy1 Radical Decomposition Reaction The decomposition reactions of alkoxy1 radicals provide a good example of a family of reactions for which an adequate number of accurate studies have been made. Most of the studies have been made on tert-butoxyl radicals, but several other radicals have been studied as well. All the studies were determinations of relative rate constants and so we returned to the original data and recomputed it on the basis of current values for the reference reaction rate constants. Three different reference reactions have been used: QNO

0" I

R,CR,R, .t NO a R , d R , R ,

ON

0. I

R,CR,R, 0. I

R,CHR,

(1)

+

I

(CI-I,),CH 8

iNO

iI

4

-,R I C E ,

R,CR,R,

+ (CH,),C

+ HNO

(2)

(3)

Values chosen for kl were those obtained by Batt et al.,l which are in good agreement with those obtained by Golden et the value of k2 chosen was that determined by Berces and Trotman-Dicken~on;~ the values chosen for h3 were derived from disproportionation/eombination ratios and values of Other reported data were not used because their reference reaction rates are not sufficiently well known. k1.134

The Journal of Physlcal Chemistry, Vol. 81, No. 25, 1977

-

10001'1

Me 4- MeCHO Figure 3. i-Pro. -I-M given by log k(s-') = 14.6 - 17.8/8.

+ M:

0 . ref 6; 0,ref 7; line

The recalculated data are presented in Figures 1-4, and the corresponding Arrhenius parameters are presented in Table I. The data for t-BuO. are the most extensive

Computer Modeling of Photochemical Smog 108

r-BuO

+

E t + CH,!H

1 0

1

3

2

4

5

6 AH:

7 kcB1 P a l

'

8

9

Flgure 5. Correlation between activation energy reaction 4HRo.

10

E and

11

12

13

enthalpy of

This equation predicts activation energies with an uncertainty of about h0.5 kcal mol-'. It predicts that the reverse reaction has an activation energy given by

E, = E

103

1

I

1 20

-

I

25

30

35

1000IT

+

Et MeCHO Figure 4. s-BuO. 4- M given by log k(s-') = 14.1 - 14.6/6'.

+ M:

0, ref 8; 0 , ref 9; line

(Figure l),covering nearly four orders of magnitude. The individual sets of experimental data taken independently show a rather wide range of Arrhenius parameters and appear to be inconsistent, but taken together, the actual data give a reasonably good straight line with parameters, log k/s-' = 15.1 - 16.210. Given the entropy change of the reaction, ASR" = 41.2 Gibbs mol-l, the A factor for the reverse reaction is A, = 107.9M-ls-l, a value very close to that for the reaction of methyl radicals with isobutene (log A = 8.0).14 This suggests a self-consistent method for evaluating and codifying the limited data available for the other alkoxyl radical reactions: choose an A factor for the reverse reaction and find the corresponding activation energy. Using this unified scheme, the alkoxyl decompositions can be considered together as a class, rather than individually. The decomposition of an alkoxyl radical is the reverse of the addition of an alkyl radical to the carbon atom of a carbonyl group, which is analogous to alkyl radicals adding to the 2 positions of a primary olefin. Since data are only available for alkyl radicals adding to the 1position of primary olefins, the assumption was made that the A factors for addition to both ends of an olefin double bond are the same and only the activation energies differ. Thus, A factors for analogous alkyl radical plus olefin reactions were chosen from the tables of Kerr and Parsonage,14 corrected for any difference in reaction path degeneracy, and applied to the alkoxyl reactions. In Table I, assumed A factors for the reverse reaction, A,, are summarized along with ASR and log Aest. A,,, is calculated from ASR and A,, and using this value, a corresponding activation energy, E', can be calculated from the experimental data. A plot of E' vs. A"," is presented in Figure 5 and gives a good straight line:

E = 12.8 -I- 0.71AH~" =

12.8

AH," > 0 nHR"< 0

(4)

-

AH:

+ R T = 13.6 - 0.29AHr"

(5)

Although these equations apply to -400 K where most of the experiments were carried out, the estimated activation energies will be negligibly different a t -300 K. Estimated decomposition rate constants for a number of alkoxyl radicals at 300 K and atmospheric pressure are presented in Table 11. The A factors were estimated as above, and the activation energies were calculated from eq 4. Fall-off corrections were obtained by use of the Emanuel RRK integral tables.15J6 For the experimental data available, the estimated rates are accurate to about a factor of 2, as demonstrated by comparing estimated and observed rate constants (Figures 1-4). The differences apparent between the estimated and experimental rate constants are due to the f0.5 kcal mol-l uncertainty in estimating the reaction activation energy and round-off errors on the A factors. Estimates made when no experimental data are available can be appraised by using the propagation of errors equation. Since A factor and activation energy are usually estimated independently, the uncertainty in log k can be written

where clogk, clogA, and CQ are standard deviations in log k, log A, and activation energy, respectively, and 0 = 2.303RT. Since log A is probably uncertain by f0.5, and the activation energy is uncertain by about = k l kcal mol-l, the value for clogk = 0.88 a t 300 K, and k is uncertain by about a factor of 8. This represents a relatively favorable case for estimations, since an adequate amount of kinetic data is available, and it is fairly consistent. For the reactions discussed below, very few data are available, and the reliability of the estimates is much lower. 111. Alkoxy Radical Reactions with O x y g e n

The only reliable Arrhenius parameters17known for this class of reactions are: CH,O + 0 , -, CH,O + HO, log k/M-' S-' = 8.5 - 4.Qle

(7)

Rates for other members of this class can only be estimated after making assumptions regarding variations in A factors The Journal of Physical Chemistry, Vol. 8 1, No. 25, 1977

2486

Baldwin et al.

TABLE 11: Estimated RO. Decomuosition Rates

c-co. cc-cos

12.4 9.4

33.4 35.0

8.2 8.0

13.7 13.8

21.6 19.5

0.003 0.6

2.1 x 10-3 1.7 x 10'

7.1 8.9

37.8 36.3

8.2 7.5

14.6 13.6

17.8 19.1

0.5 0.8

1.6 X 10' 2.9 X 10'

2.6

37.7

8.0

14.4

14.6

0.7

2.9 X 10'

4.3

41.2

8.0

15.2

15.9

0.5

1.5x 105

6.8 (3.5)" 8.7

38.0

8.0

14.5

0.8

36.6

7.1

13.3

17.6 (15.3)" 19.0

2.8 x 103 (2.2 x 10S)e 2.1 x l o 2

-9.7

39.2

7.1

13.8

12.8

1

2.1 x

lo6

- 9.6

39.2

6.8

13.5

12.8

1

1.0 x

lo6

(HO),CCC-&OH),

- 30.9

37.7

6.8

13.2

12.8

1

5.2 X 10'

0 (HO),CCC-C( OH),

-24.5

37.7

6.5

12.9

12.8

1

2.6 X 10'

11.4 (8.2)"

37.7

7.5

13.9

-5.1

40.3

7.5

14.5

0 I

c-cc ccc-co. 0 I

cc-cc C

c-co. I

C

0 I

HOC-CC HOCCC-CO.

1

0

HOCCC-&OH

0 ( HO 1,

ccc-)loa 0

C I

HOC-CO,

20.9 (18.6)"

0.9

3.6 X 10' (2.2x 102)"

0.8

8 . 2 X lo6

0 0

ce-cc

?

?

12.8

0

,

Notation: HOC-CC represents HOCH,CHCH, HOCH, + HeCH,, etc. A factor for analogous alkyl. radical + alkene association reaction. E,, = 12.8 t 0.71AH~"(kcalmol-'). Fall-off estimated from RRK Tables for l atm, 300 K. " Based on group additivity," not on experimental AHf" for propane-1,2-di0l.~~ Kate constants for 300 K and 1 atm air.

and activation energies. The concommitant uncertainties in estimating rate constants will be relatively large since little is known about such variations. The A factors for this group of reactions are expected to be similar to that for methoxy radicals, aside from the reaction path degeneracy ( n )factor; therefore, log A can be estimated as follows: log A&/M-' s-'

=

8.0 + log n

Estimates for activation energy variations are rather problematical, especially when E, is low. Two alternative methods can be used: (1) Assume E , is constant for the entire homologous series. (2) Assume that an empirical relationship that holds for other radical reactions applies to this series, as well. A simple empirical relationship18 that gives E, with an uncertainty of about f 3 kcal mol-l for exothermic H, OH, and CHB reactions is given by

Ea = 11.5 + 0 . 2 5 ( A H R )

(9)

where A", is the enthalpy of reaction. For reaction 7 , eq 9 predicts E , = 5 kcal mol-l, about 1 kcal mo1-l too high. The Journal of Physical Chemistty, Vol. 8 I , No. 25, 1977

Equation 9 has two parameters and can be modified in two different ways to give the proper E, for reaction 7: Ea = 10.5 + 0 . 2 5 ( A H R ) (10)

E, = 11.5 + 0 . 2 9 ( A H R )

(11)

Rate constants for a number of alkoxyl radical reactions were estimated by the three methods and are presented in Table 111. Considering the large uncertainty associated with eq 9 and the low activation energies, the estimates in column I11 of the table are highly uncertain and may well be upper limits to the correct rate constants. Similarly, rate constants in column I of the table may be near the lower limits. The overall uncertainties for this family of reactions may be estimated as before. log A is probably uncertain by f0.5 and the activation energy is probably uncertain by an average of f1.5 kcal mol-'. Thus, "log k = 1.2, and the estimated rate constant is uncertain by about a factor of 16. If the activation energy is uncertain by an average of f2.5 kcal mol-', the estimated rate constant is uncertain by a factor of -80.

-

IV. Alkoxy1 Radical Isomerization Reactions The importance of alkoxyl radical isomerization reactions has been inferred from smog chamber data,lg as well

Computer Modeling of Photochemical Smog

TABLE 111: Estimates: RO.

+ 0,

2487

Reactionsa

E;' = 10.6 + 0.25(AH~")

E;'' = 11.5 t 0.29(AH~")

k (min-I)

h (min-I)

h (min-l)

2.0 x 1.3 x 1.3 x 6.7 x 1.3 x 6.7 x

2.0 x 8.2 x 8.2 x 1.5 X 3.5 x 1.1x

2.0 x 1.3 X 1.3 X 3.7 x 5.8 x 2.2 x

E: log ( A)est 8.5 8.3 8.3 8.0 8.3 8.0

Reaction CH,O t 0, E t 0 t 0, n-Pro + 0, i-Pro t 0, n-BuO + 0, S-BuO t 0, a

= 4.0

105 104 105 104

105 105

105 lo6 105

lo6

105

lo6

lo6 lo6 105

lo6

Effective first-order rate constants at 300 K in air (2.1 X l o 5 ppm 0,).

TABLE IV: RO. Isomerization Reactions-Estimation Procedurea Hydrogen abstracted

E(abstraction), kcal mol-'

RCH,-H RCH(0H)-H R, R,CH-H R,R,R,C-H RC(OH),-H

7.2 6.0 4.1 4.1 4.1b

Strain Energy Five-membered ring 5.9 kcal mol-' Six-membered ring 0.5 kcal mol-'

A Factor (per abstractable H ) A =10".* s-' Five-membered ring Six-membered ring A s-' a

105 105

E = E(abstraction) + E(strain).

Estimated.

as from more qualitative considerations.20 The estimation of the isomerization rates is relatively straight forward, but the estimates are somewhat uncertain, as discussed below. A factors for five-membered ring (5R) and six-membered ring (6R) isomerizations were estimated to be and 1010.9s-I (per H atom), respectively. The estimate for the 5R transition state was made by noting that in tying up the methyl and ethyl internal rotations, the change in entropy is about -6.6 Gibbs mol-'; subtracting another 0.3 Gibbs mol-l for the reaction coordinate, we obtain log AjR = 11.7 for three abstractable H atoms. Thus, for each abstractable H atom, log AbR (per H) = 11.2. For the 6R transition state, a model transition state was used. For the decomposition of ethyl vinyl ether (EVE), log A = 11.4 a t 700 K. If log A is about the same a t 300 K and So(EVE) = 82.6 Gibbs then the entropy of the transition state is 74.3 Gibbs mol-l. In comparing the EVE transition state and that of n-butoxyl radical, EVE

has some double bond character, and that of n-butoxyl will be looser by about 0.6 Gibbs mol-l. n-Butoxyl has one more hydrogen atom, worth about 0.2 Gibbs mol-', and has spin, contributing 1.4 Gibbs mol-'. Adding all of these corrections, gives So* = 76.5 and log A = 11.4 for three abstractable H atoms; thus log AGR(perH) = 10.9. The uncertainties in these estimates are probably f 4 Gibbs mol-' and log A is uncertain by fl. Activation energies may be estimated from the activation energies for H abstraction by alkoxyl radicalsz1by adding a "strain" energy of 0.5 kcal mol-l for 6R reactions and 5.9 kcal mol-' for 5R reactions.22 These activation energies are rather uncertain, probably f 2 kcal mol-'. The combination of the two sources of error by the propagation of errors formula gives an estimated uncertainty in log h of h1.8 at room temperature. Thus, the rates are estimated to be uncertain by about a factor of 60. The method for estimating these rates is summarized in Table IV, and estimated rates for several alkoxyl radicals are presented in Table V. All reactions are assumed to be a t the high-pressure limit.

V. Reaction of NOz with HOz These species have long been thought to react via a radical disproportionation to give HONO and 02: HO,

+ NO,

HONO

--f

+ 0,

(12)

Recently, however, Niki and c o - ~ o r k e rhave s ~ ~ studied the reaction and could not detect any HONO. They concluded that the predominant reaction is HO,

+ NO,

M

zHOONO,

(13)

This conclusion is also supported by some of Heicklen's data,24but the reaction was not considered explicitly, and

TABLE V: Estimated RO. Isomerization Reaction Rates

-

Reactiona

log A ( s - ' )

E(kca1 mol-')

h(min-')

11.4

7.7

3.7 x 107

cccc cccc.

11.7

13.1

8.6 X l o 3

H O C C C C ~ HOCCCCOH

11.2

6.5

1.9 x

lo8

11.2

6.5

1.9 x

lo8

(HO),CCCC(OH),

10.9

4.6

2.2 x 109

(~o),cccC( OH),

10.9

4.6

2.2 x 1 0 9

11.4

7.7

3.0

OCCCC

0

-

HOCCCC ?H

+

0

H O ~ C C C O H (HO),CCCCOH +

0 I

(HO),CCCCOH

+

0 I

(HO),CCCC(OH),

OH I

+

OH

CCCCO. -+ CdCCOH

X

10'

OH I

OH OH OH I a Notation: CCCC. + CdCCOH represents CH,CHCH,O* 4 CH,dHCH,CH,OH The Journal of Physical Chemistry, Vol. 8 I, No. 25, 1977

2488

Baldwin et al.

TABLE VII: RRKM Calculated k / k _ for HO,NO, Decomposition

TABLE VI: Frequency Assignment for HO,NO, Frequency in molecules (cm-') 354Oa 1728a 1304a 803a 1396a 633 500 735 125 400 880 200 a

Frequency in transition state (cm-') 3540 1728 1304 803 1396 Reaction coordinate 2 00 435 Free rotor 100 580 150

Collision efficiency Type OH stretch NO3 NO3 NO3 OH bend NO stretch NO, rock NO, wag 0-NO, torsion OOH bend 00 stretch HO-0 torsion

E = 23.1 kcal mol-' log Als-' = 15.9 E = 25.1 kcal mol-' logA/s-' = 15.9 E = 27.1 kcal mol-' log Als-' = 15.9

-

o

0.4

0.5

0.6

0.46

0.50

0.53

0.56

0.60

0.63

0.65

0.68

0.71

l

t

1

From ref 23.

k I 3was not determined. Both H e i ~ k l e nand ~ ~Cox26found that the loss rate due to H o p NO2 is about 2-10 X lo7 M-l s-l. This value is uncertain, however, because they did not consider the effect of HOON02. Calvert and cow o r k e r ~have ~ ~ also observed H02N02and have attempted to obtain some kinetic information from the chemical system, but the system is too complicated to allow unambiguous interpretation. Both Niki and Calvert observed the lifetime of H02N02to be -6-8 min and both ascribed the loss mechanism to wall reactions. Thus, quantitative kinetic information on this reaction is virtually nonexistent. Because H02NOzcan act as a radical reservoir or sink, the kinetics of H 0 2 N 0 2can have far-reaching effects in photochemical smog and in stratospheric chemistry. According to this scheme, H 0 2 and NO2 react to form H02N02, which can "store" the reactive species until it homogeneously decomposes a t its natural unimolecular decomposition rate. At that time, it releases the H 0 2 and NO2 back into the reaction mixture to react further with the other species present. Thus, it is important to estimate the rate constants for association and decomposition. As a starting point for estimating the rate constants, we can use the rates determined by Hendry28for the reaction of peroxyacetylnitrate (PAN):

+

0 II

-

CH,COONO, CH,COO t NO, log k / s L = 16.2 - 26.8Ie

(14)

This reaction is analogous to that for H 0 2 N 0 2and its Arrhenius parameters provide a good starting point. The major uncertainty is whether the [00-N02] bond dissociation energy in PAN is equal to that in H02N02. For most radical association reactions there is no activation energy. Thus the A factor for the association reaction can be derived from that of the decomposition step and ASRO for the reaction. In the case of PAN decomposition, ASRO for the reaction is estimated to be 42 Gibbs mol-', giving log A-14 = 8.8 for the association. This value is not unreasonable for radical association reactions, but may be a little low. A detailed estimate for the entropy of H 0 2 N 0 2was made based on the value of 72.2 eu for MeONOzZgby adjusting for the change of internal rotor from a methyl to an OH and including the corresponding rotational barrier change due to the loss of two hydrogen atoms, and correcting for spin gives Sf0(HO2NO2)= 71.6 eu. The frequency assignment for the molecule is given in Table VI. The first five frequencies listed are those actually observed by Niki et al.;23the remaining frequencies are based on those for FN03, H202,and "OB, with the low frequency torsions adjusted to give Sf"(H02N02) = 71.6 The Journal of Physical Chemisfry, Vol. 8 1, No. 25, 1977

c L

c

t

1 27

25

23 E,

kca -lole)

-

Figure 6. Fall-off calculated by RRKM theory as a function of activation HOz NO2. energy for the reaction HOPNOz

+

eu. The values used are compatible with the known torsion barriers for 0-OH and O-NOz. In the transition state, the N-0 stretch is assumed to become the reaction coordinate, and the NO2 group is assumed to be a free rotor. Other vibrational frequencies were lowered as in Table VI to give an entropy for the transition state that yields the desired high pressure A factor. If E13 = 0 and log A13 = 9.0 (similar to PAN), then log A-13 = 15.9. The results of the calculations are given in Table VI1 for three high-pressure activation energies and three values of y,the collision efficiency. The values of k / k , are near unity at 1 atm and 300 K and are presented as a function of E-13 in Figure 6 for two values of the collision efficiency that are expected to bracket that of N2 or 02.These results show that reactions 13 and -13 may be very important in controlling the concentration of NOz in smog chamber experiments. In the following section, the effects of this reaction will be illustrated by computer simulations. The major question here is whether H 0 2 N 0 2and PAN are expected to have the same activation energy for decomposition. Since this question cannot be answered with any confidence, the activation energy E-13may be used as an adjustable parameter in simulating smog chamber data. Although this procedure is not very satisfactory, it does illustrate the necessity for accurate rate data if this issue is to be resolved. VI. Simulations of Smog Chamber Experiments A major use for an explicit photochemical smog mechanism is to establish U.S. Environmental Protection Agency regulations for controlling pollutant emissions into the troposphere. While it is important to validate a proposed mechanism, it is not possible to use real atmospheric data for this purpose because of the wide variety of organic reactants, the complexity of products, and the presence of capricious transport phenomena. Smog chambers are often employed for carrying out experiments on relatively simple reaction mixtures thought to represent pollutants in the real urban atmosphere; the results ob-

Computer Modeling of Photochemical Smog

tained are useful in testing assumed mechanisms because the effects of transport phenomena are minimized while temperature and light intensity can be controlled. Associated with smog chambers, however, are several troublesome problems. The most obvious problem is that the pollutant concentrations are generally higher in a smog chamber than in the real atmosphere; thus when a reaction mechanism is applied to real atmospheric problems, there is an extrapolation into regimes where the mechanism has not been validated. This extrapolation could tend to magnify errors in the chemical mechanism and thus it is important to devise a mechanism which is as accurate as possible in relation to the smog chamber data. A second and most troublesome problem is that of “chamber effects” in which chemical species interact with the walls of the chamber or even appear to desorb from the walls. This manifests itself in a poor mass balance between reactants and products, and in the sometimes observed necessity for postulating a radical source associated with the chamber. Although every attempt must be made to understand the sources of such problems, there is always the possibility that an effect ascribed to “chamber effects” is really due to a deficiency in the postulated reaction mechanism; conversely, an error in the reaction mechanism might conceal effects better ascribed to the smog chamber. Since the postulated reaction mechanism must be tested against smog chamber data, it is important that the data be of high quality and that care be taken to minimize “chamber effects”. We have been using data reported by Pitts and c o - w o r k e r ~a~t ~the Statewide Air Pollution Research Center located a t the University of California, Riverside, who have taken great care in an effort to minimize chamber effects and to characterize their experimental conditions. The reaction mechanism is complex and partly speculative, and therefore not all elementary reaction steps have been individually measured, yet many important reaction rates are now well known.31 One may hope that the effects of the unknown rate constants will not predominate in the reaction mechanism. Calvert and cow o r k e r ~P, ~ i t~h et al.,33Niki et al.,%and Hecht et al.35have made major strides in elucidating the mechanisms of photochemical smog. Our efforts are built upon their work, with the emphasis placed upon systematically estimating and evaluating families of reactions, as described in the preceding sections. Our guiding philosophy has been to start with a “first guess” mechanism, consisting of wellknown reactions and our own best estimates for other reactions, and then t o make any refinements necessary, within the uncertainties of the experimental data and estimated rate constants. Our work thus far has been primarily concerned with the photooxidation of propene, butane, and propene/ butane mixtures. Although we are continuing to work on the reaction mechanisms for these species, we feel that the postulated mechanisms are substantially complete, and that it is possible to point out the areas of greatest uncertainty. A detailed description and discussion of all the individual steps in the reaction mechanisms will be published in a later paper, along with the results of comparing those mechanisms to experimental data obtained over a range of initial conditions. The results given here are to demonstrate the validity and usefulness of the estimates developed in sections 11-V. Reaction of n-Butane. Since n-butane is thought to be representative of the straight chain alkanes present as pollutants in the urban atmosphere, it is used as a model

2489

compound in smog chamber experiments. 7 !,e experiments are performed on air mixtures containing 3 few ppm of n-butane and somewhat less NO and NO,; ,’Q>is often present, as well. The initial concentrations ad d relative ratios of RH to NO, and NO to NOz have been varied somewhat in different experiments to provide data over a range of initial condition^.^^ The major reaction pathways for carbon-containing species in the n-butane system are depicted in Figure 7. The rate constants shown correspond to 300 K and 1 atm of air and are expressed in units of min-l and ppm-l m i d . For bimolecular reactions involving 02,the concentration of O2 (2.1 X lo5 ppm) has been multiplied by the appropriate bimolecular rate constant (units of ppm-l min-l) to give an effective first-order rate constant (units of min-l). The rate constants shown represent our best estimates or the best experimental data available. The initial attack of OH radical on n-twtane is known to give -86% sec-butyl radical and -1n %O 7;-butyl radi ~ a l These . ~ ~ radicals combine very rapidl. witn O2 to give the corresponding peroxyl radicals. As long as NO is present, the peroxyl radicals oxidize NO to form NO2 and alkoxyl radicals, which can go on to react as described in the preceding sections. sec-Butoxyl radicals can either react with oxygen to give 2-butanone and HOz, or they can decompose to give acetaldehyde and ethoxyl radical; the major fate of ethoxyl is to react with oxygen to give acetaldehyde. Although acetaldehyde and 2-butanone react with OH and photolyze, they disappear only slowly, and the ratio of their yields gives a sensitive measure of the relative rates for loss of sec-butoxyl: decomposition vs. reaction with Oz. Since the sec-butoxyl decomposition rate is known fairly accurately, and its reaction with Oz is rather uncertain, the rate constant for the latter reaction can be adjusted to give the proper relative value, n-Butoxyl radical also can react with O2 or slowly decompose, but it has the additional reaction channel of isomerization. In fact, the estimated isomerization rates are so fast that the other possible reactions hardly compete. Examination of Figure 7 shows that about 98% of the original n-butoxyl radical formed ends up as the polyhydroxylated aldehyde (HO)3CCHzCH0and only a small amount appears as butanal and other products. The fate of (HO)&CH2CH0 is not known, but if it dehydrates, the product HO(CO)CHzCHOmight photolyze quickly to give free radicals that can continue the chain mechanism. Although only 14% of the butane reacts by the n-butoxyl reaction pathways, n-butoxyl accounts for about 36% of the NO oxidized directly by alkoxyl radicals. This is directly attributable to the isomerization reactions. A reaction not included in our mechanism which might dramatically alter the course of reactions is R,HCR, I

0.

+ 0,

--f

R,CR, t HO,

0

If this reaction is fast compared to simple addition of 0, to form peroxyl radical, the isomerization steps would not have an opportunity to take place, and the character of the n-butane reaction would be quite different from that described above. Reliable experimental data are needed in order to assess the importance of reaction 15, but we would not expect it to compete effectively with addition of 02,which has the same A factor and no activation energy. Another area of uncertainty in the mechanism that deserves mention is the photolysis reactions of aldehydes and ketones. Photolysis rate constants and products for The Journal of Physical Chemistry, VoL 8 I, No. 25, 1977

2490

Baldwin et al.

t HO, '

CH,CH,O'

t CH,EH

(tiLI.7)

R

CH,CH

+

HO,

(tin . 7 )

P

9 +

HCOH t HOCH,CH,CH

HO,

(0 .14)

O,,NO

1 .LI x

111" inin-'

many of the carbonyl compounds are not known and must be estimated. Radical photolysis products serve to accelerate the overall reaction and so are very important. In the absence of good data, many of the rates have simply been estimated by analogy with those rates that are known. In the butane simulations presented below, a radical influx from the chamber walls must also be assumed in order to reproduce the observed rate of butane consumption. It is quite possible that the assumed radical influx is merely compensating for an underestimate of the photolysis rates of carbonyl reaction products, or some other reaction sequence that has been overlooked so far. Further experiments are necessary to clear up this point. Two computer simulations of the smog-chamber experiment on the n-butane system are presented in Figures 8 and 9. All the simulations shown were obtained by numerical integration of explicit chemical mechanisms using a program based on Gear's method. The first simulation (Figure 8) represents our "first guess" mechanism, consisting of experimental rate constants, where available, and our best estimates for unknown rate constants. The activation energy for HOzNOz decomposition was assumed to equal that of PAN (26.8 kcal mol-l). Using ppm min-l of HO2 radicals these rates, an influx of is necessary to approximate the correct conversion rate of n-butane. It is noteworthy that HOzNOzacts as a radical reservoir-storing HOz radicals from the early period of the reaction and slowly releasing them in the later stages. Much of the nitrogen is tied up as H02NOz, and relatively less is present as NOz, affecting both the PAN yield and

-

The Journal of Physical Chemistry, Vol. 81, No. 25, 1977

03 production. It may be argued that HOzNOzis expected to contribute to the experimental NOz measurement (as does PAN), and thus the NOp data may represent the sum of contributions from HO2NO2and NOz. This question about the correct interpretation of the experimental NO2 concentration adds an extra element of uncertainty in comparing the simulation to the experiment and must be resolved by laboratory experiments. Another feature of this first simulation is that ozone and PAN production are greatly underestimated as is the consumption of butane. This is due to the quenching effect H 0 2 N 0 2formation has on the reaction mechanism. If the H02NOzdecomposition activation energy is less than 26.8 kcal mol-l, the influence of HOzN02formation becomes less important. If the activation energy for decomposition of HOzNOz is assumed to be -23 kcal mol-l, HOzNOz has little effect, and the simulation is in much better agreement with experiment (see Figure 9). Moreover, an influx of 2 x ppm m i d of radicals need be assumed to match the observed conclusion rate of n-butane. Note that PAN and ozone formation are near the experimental values and HOzNOzconcentrations are too low to be shown in the figure. Our experience with simulations of this nature is that the activation energy for HOzNOzdecomposition probably falls somewhere between 23 and 25 kcal mol-l, but this number is highly tentative, and we must await an experimental determination before this major uncertainty can be resolved. Once the overall mechanism has been brought into good agreement with experiment, various rate constants can be

2491

Computer Modeling of Photochemical Smog I

I

45

90

42

0.3 02 01

1

I

a 1

0 50

I

I

I

45

90

735

I

t -

-

,

- , 0

135

180

1

I

1

225

270

315

C

360

0 50

!

I

!

I

I

b \

4

225

180

315

27C

360

T l U E hllUUTES

Tlhnc h l l h l I l T F S

045

I

Figure 9. Simulation of run EC-41 in ref 30. Radical input is 2 X ppm min-' of HOP. The decomposition of HOzNOzhas an assumed activation energy of 23 kcal mol-'.

-

/0;O ,I:!

HOCH,O'

1 I HO,

HCOH

+

HO,'

0

0

90

45

135

180

225

270

315

I1

360

CH3CH2CH

TIME hlINUTES

Figure 8. (a) Simulation of run EC-41 in ref 30. Initial concentrations as follows: butane, 4.03 ppm; NO2, 0.068 ppm; NO, 0.524 ppm. The points are experimental results; the lines represent the computed concentration profiles for butane and peroxynitric acid. Radical input is 1 X ppm min-' of HOz. The decomposition of HOPNOPhas an assumed activation energy of 26.8 kcal mol-'. (b) Simulation of run EC-41, as in 7(a), showing the concentrations of NOz, NO, and ozone.

CH,