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1. • z CO NBS TECHNICAL NOTE 866 \ * 'VaT of

U.S. DEPARTMENT OF COMMERCE/ National Bureau of Standards NATIONAL BUREAU OF STANDARDS

established by an act of Congress March 3, 1901. The National Bureau of Standards' was advance the Nation's science and technology The Bureau's overall goal is to strengthen and for public benefit. To this end, the Bureau conducts and facilitate their effective application Nation's physical measurement system, scientific research and provides: (1) a basis for the (2) technical basis for equity in trade, and technological services for industry and government, (3) a public safety. The Bureau consists of the Institute for and (4) technical services to promote Research, the Institute for Applied Technology, Basic Standards, the Institute for Materials Technology, and the Office for Information Programs. the Institute for Computer Sciences and THE INSTITUTE FOR BASIC STANDARDS provides the central basis within the United physical measurement; coordinates that system States of a complete and consistent system of with measurement systems of other nations; and furnishes essential services leading to accurate and uniform physical measurements throughout the Nation's scientific community, industry, and commerce. The Institute consists of a Center for Radiation Research, an Office of Meas- urement Services and the following divisions: Applied Mathematics — Electricity — Mechanics — Heat — Optical Physics — Nuclear 1 3 Sciences" Applied Radiation " — Quantum Electronics — Electromagnetics — Time and Frequency " — Laboratory Astrophysics " — Cryogenics ".

THE INSTITUTE FOR MATERIALS RESEARCH conducts materials research leading to improved methods of measurement, standards, and data on the properties of well-characterized materials needed by industry, commerce, educational institutions, and Government; provides advisory and research services to other Government agencies; and develops, produces, and distributes standard reference materials. The Institute consists of the Office of Standard Reference Materials and the following divisions: Analytical — Polymers — — Inorganic Materials — Reactor Radiation — .

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THE OFFICE FOR INFORMATION PROGRAMS promotes optimum dissemination and accessibility of scientific information generated within NBS and other agencies of the Federal Government; promotes the development of the National Standard Reference Data System and a system of information analysis centers dealing with the broader aspects of the National Measurement System; provides appropriate services to ensure that the NBS staff has optimum accessibility to the scientific information of the world. The Office consists of the following organizational units:

Office of Standard Reference Data — Office of Information Activities — Office of Technical Publications — Library — Office of International Relations.

1 Headquarters and Laboratories at Gaithersburg, Maryland, unless otherwise noted; mailing address Washington, D.C. 20234. 8 Part of the Center for Radiation Research. > Located at Boulder, Colorado 80302. » Part nf thp Center for RtiilHino Tprhnr.lr.ov "* STAKTDABD3 LIBRARY

2 8 JUL Chem.cal Kinetic and

Photochemical Data for C 100 1515_ Modelling

Edited by

Robert F. Hampson, Jr., and David Garvin

Physical Chemistry Division Institute for Materials Research National Bureau of Standards Washington, D.C. 20234

This work was supported by

The Department of Transportation Climatic Impact Assessment Program, and the Office of Standard Reference Data, N.B.S.

*< "*

U.S. DEPARTMENT OF COMMERCE, Rogers C. B. Morton, Secretary

NATIONAL BUREAU OF STANDARDS, Richard W. Roberts, Director

Issued June 1975 Library of Congress Catalog Card Number: 75-600025

National Bureau of Standards Technical Note 866

Nat. Bur. Stand. (U.S.), Tech. Note 866, 118 pages (June 1975) CODEN: NBTNAE

Supersedes NBSIR 74-430

U.S. GOVERNMENT PRINTING OFFICE WASHINGTON: 1975

For sale by the Superintendent of Documents, U.S. Government Printing Office, Washington, D.C. 20402 (Order by SD Catalog No. C 13.46:866). Price $1.85 (Add 25 percent additional for other than U.S. mailing) FORWARD

The National Standard Reference Data System was established in 1963 for the purpose of promoting the critical evaluation and dis- semination of numerical data of the physical sciences. The program is coordinated by the Office of Standard Reference Data of the National Bureau of Standards, but involves the efforts of many groups in uni- versities, government laboratories, and private industry. The primary aim of the program is to provide compilations of critically evaluated numerical data. These tables are published in the Journal of Physical

and Chemical Reference Data , the NSRDS-NBS Publication Series of the National Bureau of Standards, and through other appropriate channels.

The present report consists of tables of data assembled for use in modelling the chemistry of the stratosphere. It represents contri- butions from the Chemical Kinetics Information Center, other NSRDS data centers, and a number of individual experts. Support for the preparation of those tables has been provided by the Department of Transportation, under the Climatic Impact Assessment Program, and by the Office of Standard Reference Data.

David R. Lide, Jr. Chief, Office of Standard Reference Data

111 TABLE OF CONTENTS

Abstract 1

1. Introduction 1

1.1 Content and History 1 1.2 Related Data Evaluations 3 1.3 Guide to the Tables 4

2. Matrix 9

3. Table. Data for chemical reactions and of neutral species 10

4. Supplemental Table. Rate constant for the reaction

HO + N0 (+ N ) -» HN0 (+ N ) as a function of 2 2 3 2 and total 72

5. Reference List and Notes 74

Appendices :

1. Chemical Thermodynamic Properties of Selected Molecular Species 91

2. Addenda and Errata 105

3. Conversion Tables 110

IV .

Chemical Kinetic and Photochemical Data

for Modelling Atmospheric Chemistry

R. F. Hampson, D. Garvin, Editors

A table of data for gas chemical reactions and photochemistry of neutral species is presented. Specifically, it gives preferred values for constants, photoabsorption cross sections, and quantum yields of primary photochemical processes and also cites recent experimental work. It is intended to provide the basic physical chemical data needed as input data for calculations modelling atmospheric chemistry. An auxiliary table of thermo chemical data for the pertinent chemical species is given in the appendix.

Key words: Atmospheric chemistry; chemical kinetics; data evaluation; gas phase; photoabsorption cross section; photochemistry; quantum yield; rate constant.

1 . Introduction

1.1. Content and History

This technical note consists of a table of data on the kinetics of chemical reactions and the photochemistry of neutral species. This is supplemented by a table of thermochemical d ata for the species involved. It is designed for use in modelling the chemistry of the stratosphere

The table is an extract from the chapter "Chemistry of the

Stratosphere" by H . S. Johnston, P. J. Crutzen, R. J. Cvetanovic, M. L. Corrin. D. D. Davis, E. S. Domalski, E. E. Ferguson, D. Garvin, R. F. Hampson, R. D. Hudson. L. J. Kieffer, H. I. Schiff, R. L. Taylor, D. D. Wagman. and R. T. Watson in "The Natural Stratosphere of 1974", E. Reiter, editor, Climatic Impact Assessment Program Monograph 1, U. S. Department of Transportation. The present table will also appear in the

This work was supported by the Climatic Impact Assessment Program, Office of the Secretary, Department of Transportation and by the Office of Standard Reference Data, N.B.S. .

final version of the monograph to be published in the Fall of 1975.

The table includes contributions of rate evaluations by other scientists. These contributors represented in the present edition are D. L. Baulch, D. D. Drysdale and D. G. Home, University of Leeds; J. Heicklen, Pennsylvania State University; A. C. Lloyd, University of California, Riverside; T. G. Slanger, Stanford Research Institute; J. Troe and K. Glanzer, Ecole Poly technique Federale de Lausanne; K. H. Welge, York University; W. H. Breckenridge, University of Utah, and E. S. Domalski and D. D. Wagman of the NBS Physical Chemistry Divi sion

Several preliminary versions of the main table in this Note have been distributed. The history is explained below. The date of preparation of each version is given in the upper left hand corner of each page. The present version, dated November 22, 1974 supersedes all earlier tables. Addenda and errata, which may be found as Appendix 2, update the main table to March 1975.

The first version of this table of data on the chemical reactions and photochemistry of neutral species was prepared by the Chemistry Panel on the Natural Stratosphere in December, 1972 at the Fort Lauderdale, Florida meeting and received limited distribution in the first preliminary draft of CIAP Monograph No. 1. A revised and expanded version was distributed in NBSIR 73-203 in May, 1973. Another revised and expanded version was distributed in NBSIR 74-430 in January. 1974.

The present table updates these. In particular, it incorporates pertinent new data presented at the Symposium on Chemical Kinetics Data for the Lower and Upper Atmosphere, Airlie House, Warrenton. Virginia, September 1974.

The two NBS reports referred to above also contained separate tables of rate data on vibrational energy transfer processes (R. Taylor), high temperature air reactions (R. Taylor), and - reactions

(E . E. Ferguson). The high temperature air reactions have been incorporated in the present table. The other two have been published independently as indicated below.

a. Vibrational energy transfer processes - R. Taylor, "Energy Transfer Processes in the Stratosph re," Can. J. Chem. 52, 1436 (1974).

b. Ion-molecule reactions - E. E. Ferguson. "Rate Constants of Binary Ion-Molecule Reactions of Aeronomic Interest." in Atomic Data and Nuclear Data Tables 12, 159 (1973). The present tables (and earlier versions) include recommended values for reactions of O(-'-D) . The evaluation of these data is explained in the CIAP Monograph 1 and has been published separately as R. J. Cvetanovic, " Chemistry in the Stratosphere," Can. J. Chem. _52, 1452 (1974).

1.2. Related Data Evalutions

This table relies heavily upon other modern data evaluation work. Some pertinent sources are summarized here.

Contributors to this data survey were mentioned in section 1.1. Their evaluations are given in more detail in NBS Report 73-206 (May 1973).

Evaluations by a team of at NBS have been published in J. Phys. Chem. Ref. Data 2_, 267 (1973). Earlier versions of these evaluations had been distributed as NBS Report 10692 (January 1972) and NBS Report 10828 (April 1972). Additional evaluations have been published in NBSIR 73-207 (August 1973).

Evaluations by a group at the University of Leeds under the direction of D. L. Baulch have been published in "Evaluated Kinetic Data for High Temperature Reactions, 1, Homogeneous gas phase the -0 reactions of H 2 ? system" D. L. Baulch, D. D. Drysdale, D. G. Home and A. C. Lloyd, (Butterworths, London, 1972) and volume 1, "Homogeneous gas phase reactions of the H2~N^-02 system" D. L. Baulch

D. D. Drysdale and D. G. Home, (Butterworths , London, 1973). Earlier evaluations by the same group have appeared in five reports from the Department of Physical Chemistry, University of Leeds, entitled "High Temperature Reaction Rate Data".

Data on reactions occurring in photochemical smog have been evaluated in "The Mechanism of Photochemical Smog Formation" by K. L. Demerjian, J. A. Kerr and J. G. Calvert (Advances in Environmental Science and Technology, J. N. Pitts. Jr. and R. L. Metcalf, editors, Wiley-Interscience, volume 4, 1974).

Kinetic data for reactions of the hydroperoxyl have been evaluated in "Evaluated and Estimated Kinetic Data for Gas Phase Reactions of the Hydroperoxyl Radical" A. C. Lloyd, Intern. J. Chem. Kinet. 6_.

169-228 (1974) .

Kinetic data for reactions of chlorine atoms and chlorine oxides have been evaluated by R. T. Watson in "Chemical Kinetics Data Survey VIII. Rate Constants of C10 x of Atmospheric Interest" NBSIR 74-516 (distributed by Chemical Kinetics Information Center, National Bureau of Standard^, Washington. D. C. 20234.) .

1.3. Guide to the Table

1.3.1. General

This table provides current (November 1974) information on reaction rate constants, quantum yields and absorption cross sections. For many reactions, preferred values are given. The reactions included in the table are summarized on a "reaction grid" described in section 1.3.4., Arrangement of the Table. That grid also shows processes for which data (or data evaluations) are needed.

Most of the more important stratospheric reactions are in the tables. A number of the less important ones and some related systems are included, often simply for comparison.

The following remarks summarize the content of the table. It lists 271 reactions and gives a preferred value of the rate constant for 160 reactions, 136 based on recent reviews and 24 based on recent (1972-1974) experimental work. New data entries (1972-1974) are given for 121 reactions.

Several principles have been used in the selection and presentation of data.

(a) Where a preferred value is given for a rate constant or photochemical quantity, it is so indicated by an asterisk placed ahead of the reference column.

(b) Where there is a recent published evaluation of the data and tbere are no newer data, the evaluation is adopted and usually, but not always, marked with an asterisk. The original data covered by the evaluation are not listed

separately .

(c) Where there is an evaluation but there are new data, both are listed and a preferred value is indicated (marked by an asterisk)

(d) Where desirable, the available recent data sets are listed, and a selection is made or a preferred value is synthesized from them.

(e) The uncertainty in a preferred value given in the table is the evaluator's estimate of that value's reliability. This is a subjective judgment that, to a high degree of probability, the true value of the quantity lies within the bounds indicated. . .

Uncertainties are indicated in several ways:

A < k < B means k lies in the range between A and B. k < B means B is an upper limit. k ~ B means that Bis only a rough guide to the value of k. k = A ± B means that a reasonably reliable estimate of the likely error can be stated. This is an estimate by the evaluator of the absolute accuracy of the preferred value. It is a subjective judgment derived from intercomparison of data sets, consideration of related reactions studied with the same technique, estimates of how well the parameters could have been controlled, and comparison with theory. It means that in the evaluators judgment, the true value will lie within the indicated limits to a high level of confidence (90 to 95 percent)

Sometimes it is more appropriate to give logiQk = C ± D, "k uncertain to E percent" or "k uncertain to a factor of F", all three of which are equivalent statements of multiplicative

limits . The statement that k has the value k^ and is uncertain to a factor of F means k /F < k < kF.

The identity of the contributor who selected a particular preferred value has been retained wherever possible. This is shown by initials after the appropriate entry in the Reaction/Reference column. The editors take responsibility for any unidentified selections and for inadvertant ommission of identification of selectors.

1.3.2. Conventions Concerning Rate Constants

a. General Convention . Almost all of the reactions in the table are elementary processes. For them the rate expression is derivable from a statement of the reaction, e.g.

A + 2B -» AB

2 -d[A]/dt = -(1/2) d[B]/dt = d[AB J/dt = k[A][B] 2

Note that the stoichiometric coefficient for B, i.e. 2, appears in the denominator before B's rate of change (which is equal to 2k[A][B] ) and as a power on the right hand side.

Wherever there may be any doubt an explicit rate expression is given b. Dissociation and Combination Reactions . Some reactions of these types are not of integral kinetic order over the stratospheric pressure and temperature range. That is, although they require an energy transfer agent, "M, " they are in the "pressure fall-off region". For many such reactions we tabulate rate constants that include the effect of the energy transfer agent and give rates for various altitudes. The reactions are written to deemphasize "M, " e.g.,

N0 + N0„ (+M) -> NO (+M) 2

M HNO -» HO + N0„

The rate expressions to be used do not have the concentration of M in

them, e.g., Rate = k[N0 [NO3] and k[HN0 ] respectively. The units 2 l 3 _J given for the k's. s - for first order, and cm" molecule s for second order, are consistent with this convention.

The altitude, temperature and number density regime used in these cases is

-3

altitude/km temp . /K log[M] /molecule cm

15 220 18.60 20 217 18.27 25 222 17.93 30 227 17.58 35 235 17.26 40 250 16.92 45 260 16.60

Expect for the temperature at 15 km this table follows the U. S. standard atmosphere, 1962.

c. Forward and Reverse Reactions . In some cases there are no data on a reaction of interest but there are data on the "reverse" reaction. Occasionally, for

A -t B (f)

B -» A (r) an evaluation will use the data on the "reverse" reaction together with an equilibrium constant to obtain the other rate constant. Obviously this is an approximation but it often is a useful method of estimating non-measured physical properties. .

The table contains notations to warn the reader when this procedure has been used, such as "based on reverse reaction," or when = " = both reactions _f and _r are listed together "kf k rKeq or k r kf/Keq These expressions, which are those used in the analyses, are based on equating the two rates at equilibrium.

f r

k [A] = k [B] f r

K = [B]/[A] = k /k . f r

1.3.3. Convention Concerning Optical Absorption Coefficients

These are reported in the table as "absorption cross sections per molecule, base e" . They are defined by the equations

I/I = exp(-cr[N]J&) Q

a = (l/([N]A))ln (I /I) o where I and I are the intensities of incident and transmitted light, 0" is the absorption molecule" [N] is the cross section, cm^ , concentration of absorbers, cm, and i is the path length, cm. Other definitions and units are frequently used. The terms "absorption coefficient" and "extinction coefficient" are common. It is always necessary to know what concentration units path length units and type of logarithim (base e or base 10) are used in the definition. To convert "cross-sections" to absorption coefficients in (atm at 1 1 19 273 K)" cm" , base e, multiply by 2.69 x 10 .

1.3.4. Arrangement of the Tables

a. Reaction Grid . The contents of the data table and the location of a reaction in it are shown on the "reaction grid," that follows this discussion.

This grid shows the molecules of interest for stratospheric chemistry along the top and left edges. The symbol "K" in the inter- section for two reactants means that data for the reaction are in the table- Combination reactions, A + B + M-*AB+M are above the main diagonal. Bimolecular reactions, typically A + B -» C + D, are below the diagonal .

The first four columns in the reaction grid indicate whether the table contains the following data for a particular species listed along

the left edge of the grid: 1. (ABS . J) , ultraviolet or visible photoabsorption cross section; 2. (Q.Y.), quantum yields for primary- photochemical processes; 3. (E.TR.), rate coefficients for processes involving energy transfer from excited species; and 4. (DISS.) rate data for its thermal dissociation.

b. Sequence of Reactions . The order in which reactions are listed follows the grid. All reactions of atoms, the first species, shown in its row and column are listed first, then those of the second

species, 0( D) , with all species other than atoms, and so on. Thus a particular reaction is placed with the reactant highest (or to the left) on the grid, Bimolecuiar and combination reactions with the same reactants appear together in the table.

The algorithm used to assign reaction locations is to construct an ordered ascending sequence of number pairs (or triplets), one for each reaction according to the following rules:

(1) Assign numbers to each reactant in an equation. Use the numbers at the left side of the grid

(2) Arrange this set of numbers in ascending order, e.g. 1, 3 not 3, 1; 4, 10, 11 not 10, 11, 4.

(3) Order the sets in ascending order, giving priority to the lower number in the corresponding position of two sets being compared, e.g. 1,4; 1,7; 4,10,10; 4.10.11; 18, 24 etc. This completes the assignment of reaction sequence.

If a reaction is not filed according to this scheme, a cross reference appears at the proper spot. Exceptions are made principally to put forward and reverse reactions together.

c. Status of the Data . The reaction grid also shows what data are available and what are needed. A "dash" (-) means that the reaction may be ignored for stratospheric chemistry. An "0" means that data are needed or existing data should be evaluated. Often this means the reaction is important, but at times it means that data are required so that the importance of the reaction can be assessed. A blank inter- section merely means that no decision can be made at present. Finally, data are included in the table for some reactions that are unimportant. They are presented for comparison. 2.m Chemical Reaction Matrix K = Data in table, = Data selection or new data needed, - = Unimportant for stratospheric chemistry, E = Data else- where in the chapter, (Blank) = Role of process not assessed

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71 .

4. Rate constant for the reaction HO + N0 (+ N ) -» HNO„ (+ N ? )

as a function of temperature and total gas concentration.

W. Tsang

National Bureau of Standards

May, 1974

Rate constants for this reaction are provided here in tabular form covering the temperature range 190-350 K and the total

concentration range 10 - 3 x 10 molecule cm . They are recommended for use in modelling of the atmosphere.

These numbers were obtained using the correlation developed

by W. Tsang, Int. J. Chem. Kinetics _5, 947, (1973), and also presented in R. F. Hampson, editor, "Chemical Kinetics Data Survey. VI",

NBSIR 73-207 (Aug. 1973). The calculations have been made with the same parameters as used for the graphs and tables presented earlier.

This correlation is rated as good to a factor of 2 in k on an absolute scale throughout the range tabulated. It is, however, fitted to the room temperature data and is presumably better in this region than the rating stated above. Relative values throughout the table may be good to 25% in k. Thus the second decimal place in log k should be considered a guard digit. Linear interpolation should be used

The correlation passes through the low pressure data of Anderson,

Margitan, and Kaufman, J. Chem. Phys. 60, 3310-3317 (1974) but has a smaller pressure dependence than they found.

72 1\ 1 I1 '', 1 1 11 —1 i '> i I

e o o • u vO M-l i—l

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I 1 4-1 1 1 1 i i i i Tl

ctj . R "- i—l i—i C n vO r-l CU a i i 1 1 1 1 o cu —I i-i CJ 1 J-l 1 J= o CO 4-1 CU 4-1 c CM 4-t I— CO o CTi i—l . 1 S-i a i—i c 0) o CM CM 00 o CM on 3 CM 1—1 o I— M-4 o> O i—i CN cn cn cn cn s cu i—l /molecu] fj 1 1-1 3 •N 17.5 J= ' i—l CM 4J u o — CM CM CM CM CM CM CM CM o II i—l i—l i— r-l i—l r-l 1—1 i—i i—i i—l CW cd 0) CNI — i— I— o ] 1 1 1 1 i IW 0) o 53 S-i o r*

1 CO !~i 1 6 ' i—l S-l 00 00 O cn 1— 3 o o O R o CN cn CM ON m 00 o m O o r-l 1—1 vO r-v f-v, CJ cc o o CM cn in in vO 00 cu "--^ 1—1 1—1 . 4-1 I J CU c ^ oo r-. CM CM CM CM CM CM CM CM CN CN o rC 00 r-l i—l i—i i-H i—i i—i i—i 1—1 —I i—l rH 4-1 • 03 v_^ X O 4J o rJ 1 i 1 i i i 1 1 1 £ a) 1—1 Q) 4-1 CO II C 00 4-1 CJ •s, O o 4J CO fi o r-l Tj CU U g in CT> 00 vO cn VO ON m o rC 4-1 3

1 CT> i—i 4-> t— cu CD — in vO 00 o O o CM rQ 4J S-i cn 3 o vO CM CM CM CM CM cn cn cn cn on S-l cn CJ cO cfl o i—i i—i r-l i—l i—l i—l i—i i—i i—i i-H i—i o S-i . S3 i i 14-1 CO rC i 1 1 i i •\ CO i—l 4-1 c o — o G T3 1 •r4 iH rVS cn 4J -o CM c vO i—i i O cu CM vO 00 00 CM oo •H I—l CM CO U o CT> O cn in m vO o CU I—l i— S-l 01 cc! ctf i—i vO CM cn cn cn cn cn cn cn on cn 3 0) 3 i— r-l r-l i—i i—i i—i i—i i—i r—i i—i i—i c o hQ i 1-1 rO 1 1 i i cu R nj CO I—l 3 4-1 4-1 o C rO R cu o rC rC o o o o o o o o o o vO CJ ON H on r-l cn m o r-i on m O R cO CM CM CM CM CM cn m on on H a a)

73 5. Reference List

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" Simonaitis, R. , and Heicklen, J., "The Reaction of HO ? w ith NO and NO? J. Phys. Chem. 78, 653-657 (1974)

" Simonaitis, R., and Heicklen, J., "Reactions of CH-o? with NO and NO- J. Phys. Chem. 78, 2417-2421 (1974)

I. R., Pruss, F. J., Jr., and Gutman, D., the Steady Slagle, "Kinetics into n State. I. Study of the Reaction of Oxygen Atoms with Methyl Radicals," Intern. J. Chem. ivinet. 6, 111-123 (1974)

Slanger, T. G., and Black, G., "Reaction Rate Measurements of 0( 3P) Atoms by 3 3 Resonance Fluorescence. I. 0( P) + Q + m -> 0„ + M and 0( P) + NO + M ->

N0 + M," J. Chem. Phys. 53., 3717-3721 (1970) 2

Slanger, T. G., Wood, B. J., and 21ack, G., "investigation of the Rate Coefficient

for 0(3p) + NO -> o + NO," Intern. J. Chem. Kinet. 5. 615-620 (1973) g 2

Slanger, T. G., and Welge, K. H., "Rate Constants for Reactions of 0( 1 S)," in Chemical Kinetics Data Survey V. Sixty-six Contributed Rate and Photo- chemical Data Evaluations on Ninety-four Reactions, NBSIR 73-206, D. Garvin, Ed., National Bureau of Standards, Washington, D.C., (1973) pages 22-32 i

09

Smith, I. W c M. t and Zellner, R. , Rate Measurements of Reactions of OH b^ ' Resonance Absorption Part 2. Reactions of OH with Co, C h . and C H_ 4 d J. Chem. Soc e Faraday Trans. II 69, 1617-1627 (1973)

Smith, I, W. M a , and Zellner, R., "Rate Measurements of Reactions of OH by Resonance Absorption, Part 3. Reactions of OH with H_ £u hydrogen and Deuterium Halides," J. Chem. Soc. Faraday Trans. II 70, 1045-1056 (1974a)

Smith, I. W, M., and Zellner, R. , "Rate Measurements of Reactions of OH by Resonance Absorption. Part 4. - Reactions of OH with NH, and HNO-*," Presented at Symposium on Chemical Kinetics Data for the Lower and Upper Atmosphere, Airlie House, Warrenton Virginia, September 1974. Proceedings to be published Intern. J. Chem. Kinet.

Sperling, H. P., and Toby, S., "The Photochemical Decomposition of Caseous Formaldehyde/' Can. J. Chem. 51, 471-475 (1973)

Stedman, D. H.„ and Niki, H«^ 'Kinetics and Mechanism for the Photolysis of Nitrogen Dioxide in Air, J. Phys. Chem. 77, 2604-2609 (1973)

Stedman, D« H., Wu, C. K. , and Niki, H«, "Kinetics of Cas-Phase Reactions of Ozone with Some Olefins," J. Phys. Chem. 77, 2511-2514 (1973)

Stuhl, F, "Absolute Rate Constant for the Reaction OH + NH„ 0," s _> nh2 + H2 J. Chem. Phys. 5g, 535-537 (1973a)

Stuhl* Fe , Rate Constant for the Reaction of OH with n-C Naturforsch. 4h1Un * g a Pt A 28, 1383-1384 (1973b)

Stuhl, F. , Determination of Rate Constants for the Reactions of OH with Propylene and Ethylene by a Pulsed Photolysis-Resonance Fluorescence Method," Ber 9 Bunsenges. Physik. Chem. 2Z, 674-677 (1973c).

Stuhl, F„, "Determination of the Rate Constant for the Reaction OH + H 2 s by a Pulsed Photolysis - Resonance Fluorescence Method, Ber. Bunsenges.

Physik. Chem 9 78, 230-232 (1974)

3 Stuhl, F. , and Niki, H., "Detection of Oxygen ( P) Atoms in Pulsed Vacuum UV Photolysis of NO and Its Application to Atom Reactions,' Chem. Phys. Lett. 2. 197-200 (1970)

Stuhl, F., and Niki, H., "Measurements of Rate Constants for Terraolecular Reactions of 0( 3P) with NO, Vacuum-uv 2f CO, N2 , and COg Using a Pulsed Photo lysis-Che mi luminescent Method," J. Chem. Phys. 55, 3943-3953 (1971)

Stuhl, F , and Niki, H., "Pulsed Vacuum-uv Photochemical Study of Reactions of OH with R^ Detection Method," j^ t and' CO Using a Resonance-Fluorescent J. Chem. Phys. 52, 3671-3677 (1972) Takacs, G. A., and Glass, G. P., Reactions of Hydroxy! Radicals with Some Hydrogen Halides," J. Phys. Chem. 77, 194S-1951 (1973)

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89 Washlda, N., and Bayes, K. D., The Rate of Reaction of Methyl Radicals with Atomic Oxygen," Chem. Phys. Letts. 23, 373-375 (1973)

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Zahniser, M. S., Kaufman, F., and Anderson, J. G., "Kinetics of the Reaction of OH with HC1," Chem. Phys. Lett. 27, 507-510 (1974)

Zellner, R., and Smith, I. W. M., "Rate Constants for the Reactions of OH with NH d HNO^/' Phys. Lett. ?6, 72-74 (1974) 3 an Chem. 90 APPENDIX 1.

Chemical Thermodynamic Properties of Selected Molecular Species

E. S. Domalski, D. Garvin, and D. D. Wagman

Two tables are provided showing chemical thermodynamic properties of selected molecular species of interest in stratospheric chemistry. In these tables there are sufficient data for the usual calculations of heats of reaction and equilibria.

The first table lists enthalpy and Gibbs energy of formation, and heat capacity data. The information was extracted from "Selected Values of Chemical Thermodynamic Properties" (D. D. Wagman, et. al., NBS

Technical Note 270-3, January 1968) except as indicated in the Notes.

The thermodynamic properties tabulated are:

1. enthalpy of formation at OK and 298. 15K,

2. Gibbs energy of formation at 298. 15K,

3. enthalpy increment between OK and 298. 15K,

4. entropy at 298. 15K,

5. heat capacity at constant pressure at 298. 15K.

The values given for the heats of formation are based on experimental thermodynamic and spectroscopic measurements except where otherwise indicated;

o the values of S , C and H° -Hn for the gaseous species were calculated p ZyO U by standard statistical-mechanical equations, using corrections for vibra- tional anharmonicities, rotational stretching, and rotation-vibration inter- actions where these data were available.

91 The second table presents bond dissociation energies or bond strengths. These usually are the enthalpies of simple bond scission reactions. However, there are some cases in which there is a substantial contribution from rearrangement of electronic structure in the products (reducing the bond energy).

The values given here for some molecules will differ slightly from values adopted by the CODATA Task Group on Key Values for

Thermodynamics (see CODATA Bulletin 10, published by the International

Council of Scientific Unions Committee on Data for Science and

Technology, December 1973). These differences will have no significant effect on the enthalpies or free energies of reaction calculated from the tables.

92 I 1 V*1

ON r-. vO r~ OS cn m oo tH cn ,_, en i-l r»« vo 00

T3 i^ en i-i 00 O CM r^ 1^ p n) vo O 00 OS o OS 00 s CM - CT\ ocm if) •— 8 • i-. 33 00 a C^ IM n) as i-l •d- cn u 00 00 00 en •* 00 cn vo © 00 M-l en o m r-l vo CM 00 vO CM r^ a\ en 4-» O • • o • • o • O • • • • CO 3 m os 00 00 - (4 en m vO OS u m 00 st rH OS i-l OS 00 r^ r^ cn t-l o> ft. .-1 1^ 8 JH J* m r~- s m in o cn m OS m os © VO tH o 51 • In "J OS VO CM 1^ st CM os m r^ CM CM t-l r^ r^ OS CM w m c3 in CM en en m m en i-l CM tH t-l C h r-l i i i-l W a

rt OS r^ tH O > in m m tH tH i-i r^- i-i CM 1^ en 00 «d-

in aj

H rt 60 60 60 60 60 60 60 60 60 60 60 60 60 60 60 60 60 60 60 60 W

§ c ri a>> X to eg v-^ i-l J3 V U 01 u X 3 •\ CO o CO 0) o W l-l I-H •H tH ai 13 l-l CD o i-l 4J T3 X 3 TJ !-) ^-1 o o CJ o t-i X CD C 4-1 O B 9) l-l O CD •H u o i-l I-H CD H tH o (- 6 >s eo 43 4J 4-1 1-1 1-1 •H •O fr •-s y- fr <] W N t^ >^ ^ £1 S 4-1 •H 1-1 c G G 2 Q oo O i-l i-l e J= fl 43 CM 1-1 (3 c »* I-H h v-^ v*-* CM c CM en © c >.• v-^ o O o CM CM CM en CM 33 O CM CM CM o O © CM CM c o o O O O O o 33 3= s 33 P3 3B B Z B z B5 55 53 M

!"

93 I

CM 00 O CO u Q

c

in r-- cm o o> CM o m o r- 3 O O co m oo co m C ro vO

o 00 r~ CO CM m vt i-l r~ r-l CO T vO r^ oo oo o in i-l m o\ CO CM M O CO CO CO \o vO oo o m o m

nj a. CTi i-l 00 o CO 00 o> CO CM CO o\ r-- 2 3 ? i-l 00 CO

C a! i£> vO sj- oo >• co ON Oi c W a o

o \0 O

vo \o cm in vf oo CM CM CM m m «3- o c3 J- CO CO CO CM CO CM CM CM CM .-H VD O \D VO VD S .5? o O O O O O O rH O I- Hi o > oo in vo r^ CO CM CM co 00 CO 00 ct\ a> oo co hi

J3 ,Q 60 00 60 •rH 60&060606060b06060

a «/5

c nl a>-

C W 3 rr 01 y X) X U 0) O •u CO V4 D 4J CD •H 3 a /-N •fl O CO 4-1

94 CM i-l

o in m

00 CM ^D 00

t-H «£> °° CT\ 00 VO

! SP 00 CO 0> CO ^ "^

CO CI CO

CO CT\ CO

co m co

Ol o> CO «-*

o^ vo cr>

o> N o in in m c*v m co oo ^d o o CM CO CO CO cS a

oOoOcJJcJJbOtxOOOOOOOOObOW) 00

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95 * i 1 1i t 1 ii1 1 1 I I 1 1 i 1 1 1

o u-i CM CO o i-l 00 r~ I-. ON

4) XI r-- "^ vO ui vO ITl u-i o i— CM CM vO 00 o '- vO oo 00 u-i , CO in vO ^1- ITl m u-i VO VD O

•pp ITl rv] ON ON ON o *'' CM ITl vO r-~ CM in vO CO r^- l-H i— ON r^ 00 1 on CM u-i CO r— ^ CM u-i -* tNI u-i CO u-i oo CM UO VO CM oo o 00 X 1—1 CM CM CM CM CO CO -tf - etM in >r4 PS — o CO a 0- Cvl CM o 00 vO O i-l r^ i-i 1—1 00 vO 00 o on ON vO CO CM VO 00 4j O CM O vO O oo O O 53 (4 rH !— u-i 00 o vO CM r-- u-l in CO * CO o CO V 1 1—4 1 u-i CM CM u-l i-l CO i i-H i 1 CO CM _ 1 1 XI E <4 ^ > ni CM 1^- 00 a o ON O-i oo CM CO r-^ CM r~ r^ u-l J< I-l r-- 3 oo O o O -* 00 O O d- o s^

00 rt li*t CO r~ CM CO vw «

rt vO vO 00 CM CM r-~ i-l vO vO oo oo VO vO * CO CM i— > oo H £ .2? o O o o o o 4) Ih 0) -* 00 in r-l r^ vO oo ON o CM -d- oo oo CM CO c >

xi 01 XI 00 00 OO 00 00 00 00 00 00 00 00 00 oo (4 60 00 6 w W X) C «!

>- > a (4 Q .c c w c H w V 'J C .& (4 t-l 4-» u 6 (0 u >> XI w 4) w 3 a)

XI •i-i 0) c i-i X X <0 > 4J -r-l u i— i-l >N t4 3 o a) In 14 V4 o X> in 4-> 0) o 2 1 4) u n] o 4) x: a x; o •H 1— o 4J 4J 4J u u c X CO i-l o J3 2 O l-H X, o u (4 a) 41 4J p. a. o C o o o O PS O -C u I-l o CM XI CM u g g g g o o

I

96 1 i i I< t i —

CT\ en \D 00 00 O 00 VO in o> en 14D CT\ o a\ 00 VO p» r-l CJ T-( *o 00 o CM 00 o E CM

oi -d \D 00 .—

10 °pP in r\i ^o o *J3 m cn vO en CN CM CM CM CM CM CM OCM lD en cn en en —i o 00 w ed o W cvj fl) r~ en o en m CM \o 00 H 14-4 r^ 1— r~ r^ en a\ CM ai ^J (-3 O CM o> 00 a) <5 in o in in in cn en i 1 W CD CM o CM CM CM CM i a i o X T3 E C ^~ (X rt "5 > CM o CM in o o> a u vO \D •2 • M en O en o en ctn r-~ o> CM 2 • ;-. CM vo V43 CM < r^ CM CN en o CM 1 1 i— c CM en CM i i i z 1 !* Q c O O 2 CO CM o-\ CM i— CM K n tf r-^ o 00 CM o in CM C o ^-j CM CM e^ W § £> oo CM ^ CN CM f—' i— CM ^o <£> CM o CM 1 1

H 1 1 Ui 1 -5

< rt ,_, 00 CM O -* m ^ vO CO £> CM O > "3 X o O-i 00 \D m en o> o> c^ o> cn 00 2 o -tf o 1- •* w C en ^O CM o CO

XI QJ X 00 60 00 00 00 oo 00 60 60 60 60 o Ri 60 60 00 w 6 W w c ed > > a cd Q -C c W g w 4) CJ u a, c U c CJ CO 01 W ni S* c c o CO ed CJ en en CJ CJ X •a C 4J X W J3 01 CJ 4-J B u CJ erj 'A 3 3 T) CJ o CJ u u T3 i-i to C • H e u B o CJ o CJ ed •H VJ o o o XI ^-l CD -o CJ •H a CJ X o Vj 3 ^4 x c •o •r4 -a O •H -o 3 o X 3 o o (j •H ed Vj efl •H X •H o c O 3 M-l 3 <0 L X 6 u o U CJ o U m -4 u ed o CO T-l CJ C H o O 6 ecj U-J 13 4-J "3 •H JJ 3 X D. ^t •H o o CJ CJ IS T3 4J X. o o J= S 4J ^. 1-1 u 4J Vj CJ o o c CJ 4-J o o a E CJ CJ O •H C o c *H a c a >, eu M •H u X ^ o 2 1 H •H CJ X U) C o >J C o (J -D k Vj ^J 00 o O & •H r- O o H •H 14 o ^ 4J -C t-H 2 O O o U ^ X 13 n ed u a u H o o X Vj CJ 4-1 CJ 3 •H •H 2 X X! >, c o eej CM CJ (J u >, X C X a U en f=K c X. o 33 PS B s CJ CJ CJ

97 i — t t t 1

1

i

en NO en o

TJ ~"~- on r^ en en CN on ON ^3 m nO en in on _ O NO . OCN m ON CN 3 i-H i-H l-H CN • nl a u ON en NO I^- NO i-4 o 3 X m oo NO -* ON 00 o >H ON CN

en en cn n) r-t l-H i-H -* CN 00 en 00 NO O en oo o bJi 3 £ P^ r-. 00 en o oo m «3f Ih £ .2? -* o> en o cn i-H 0) Ih ID m cn o ON ON oo no cn cn C l-H £ m 3 NO i-H <—1 •— w i-H l-H

.fl o Xi a 00 oo 00 00 00 do oo oo •a c n) > Q.

Ri x c c 0) W u i-H c .2* CD l-H CO tt Ih T3 CO o •H u t4 01 y iH <0 CO u •o c N "-1 01 T3 o l-H x >n c •v •i-l •l-l >N 4-> X CO ^V c u •O >N X 0) 4J X CO o X 4-1 o u 4-> e C i-H oi 4J a Ih O 01 o c id x c e 01 6 O U o <4H o 01 o 6 -H O u o 3 i-H MH O Ih X l-H o u v. 1— >N O Ih O o x: i-H ft £ >N X U O l-H ea o X i-4 f* 43 4J O 3 X U tH u X 2 •u 01 l-H O 4-1 Ih t4 CJ h 01 e X ItH IH OJ 4J u g o •H u 4J en 4-1 l-H 2 CN u 4-1 cn i-H 1 ^N i-H i-H en 4-1 ^ l-H o i-H X 4J 4) o u i-H en ^H o o «, 1 en CN O en i-H o EC cn i-H 01 c 3 Ph c_> CN CN fB V s g B O u o O l-H H

98 Notes

1. Hampson, R. F. et al, J. Phys. Chem. Ref . Data 2, 267-312 (1973)

[Data sheet on + hv (u.v.) p. 303.

2. Contributions of the higher electronic states of molecular oxygen

to the enthalpy, entropy, and heat capacity at 298 K are

insignificant.

3. Stull, D. R. and Prophet, H. "JANAF Thermochemical Tables" 2nd.

ed. NSRDS-NBS 37 (1971).

4. Tsang, W. Estimated from kinetic data on the decomposition of

N H, . Chapter 12, NBS Report 10904, 1 July 1972.

5. NB." Report 10904, l ju ly 1972, pp. 239-307.

6. R. A. Fletcher and G. Pilcher, Trans. Faraday Soc. 66_, 794-799

(1970) provide more recent data for £Hf°, 298.15 K.

7. Data obtained from Benson and O'Neal ("Kinetic Data on Gas

Phase Unimolecular Reactions", NSRDS-NBS -21, Feb. 1970, page 55).

8. We estimated the AHf °[CH~0 ] by assuming that: (a) the breaking 9 (g)

of the 0-0 bond in CH 0„ was equivalent to the 0-0 bond scission

(37 kcal mol"'~) in CH OOCH and (b) the breaking of the 0-H bond

in CH H was equivalent to the 0-H bond scission (104 kcal mol )

in CH OH.

° o o 9. Values for AHf , S , and Cp at 298.15 K were calculated using

the group additivity method described by Benson and O'Neal

("Kinetic Data on Gas Phase Unimolecular Reactions", NSRDS-NBS -

21, Feb. 1970, ppg. 40-42).

99 o -1 10. The value for AHf [CH 0N0(g)] = -16.5 kcal mol " was derived 3

from the combustion data of Geiseler and Thierfelder (Z. physik,

Chem., N.'T., 29, 248-257 (1961)), and the equilibrium data of

Leermakers and Ramsperger (J. Am. Chem. Soc. 54, 1837-1845

(1932)) for: CH 0H(g) +-N0C^(g) = CH 0N0(g) +HCX(g). 3 3

derived The value for £Hf° (CH 0N0 (g)) = -29.8 kcal mol"' was 11. 3 2

from the work of Ray and Ogg (J. Phys. Chem. 63, 1522-1523

with CHgONO. (1959)) on the enthalpy of reaction of N^

based upon have chosen S° [CH ON(> (g)] = 76.1 cal mol" K~ 12. We 3 2 Chem. Soc. low temperature thermal data of Gray and Smith (J.

studies by 1953 2380-2385). Calculations from microwave

give S° = Dixon and Wilson (J. Chem. Phys. 35, 191-198 (1961)) -1 -1 72.15 cal mol K .

13. Davies, J. V., and Pritchard, H. 0., J. Chem.

o 4, 23-29 (1972) provide more recent AHf data.

14. Data on AHf S°, C obtained from S. W. Benson and H. E. , p

O'Neal ("Kinetic Data on Gas Phase Unimolecular Reactions",

NSRDS-NBS-21, Feb. 1970, page 567).

15. Rossini, F. D., Pitzer, K. S., Arnett, R. L., Braun, R. M.

and Pimentel, G. C, "Selected Values of Physical and Thermo-

dynamic Properties of Hydrocarbons and Related Compounds",

API Research Project 44, Carnegie Press, Pittsburgh, 1953.

100 16. £Rf° data from Pittam and Pilcher (J. Chem. Soc, Faraday

Trans. I, 68, 2224-2229 (1972).

17. AHf° data from R. L. Nut tall, A. H. Laufer and M. V. Kilday.,

J. Chem. Thermodynamics 3, 167-174 (1971).

18. Devore, J. A., and O'Neal, H. E., J. Phys. Chem. 73_, 2644-

2648 (1969).

19. Data on S° and C were obtained from Note (14), page 589;

data on ZXHf° came from Note (18).

20. Spectroscopic studies of N. Basco and R. D. Morse, J. Molec.

Spectros. 4_5, 35 (1973); R. A. Durie and D. A. Ramsay, Can.

J. Phys. 36, 35 (1958); P. A. G. O'Hare and A. C. Wahl, J.

Chem. Phys. 54, 3770 (1971); L. Andrews and J. I. Raymond,

J. Chem. Phys. 55, 3087 (1971); D. R. Johnson and F. X. Powell,

Bull. Am. Phys. Soc. 13, 594 (1968); A. Carrington, P. N. Dyer,

and D. H. Levy, J. Chem. Phys. 47 , 1756 (1967) were examined

and used to calculate the thermodynamic properties.

21. Arkell, A., and Schwager, I., J. Am. Chem. Soc. 89, 5999

(1967); Johnston, H., Morris, E. D., and Vanden Bogaerde, J.,

J. Am. Chem. Soc. 91, 7712 (1969), Clyne, M. A. A. and White,

I. F., Trans. Faraday Soc. 67, 2068 (1971).

22. Studies by D. J. Gardiner, J. Mol. Spectroscopy 38, 476 (1971)

and G. E. Herberich, R. H. Jackson, and D. J. Miller, J. Chem.

Soc. (A) 1966 , 336 were examined and the data used to calculate

the thecmodynamic properties.

101 .

23. The spectroscopic data of K. 0. Christe, C. J. Schack and

E. C. Curtis, Inorg. Chem. 10, 1589 (1971) were used.

24. Thermal Constants of Substances (Termichesky Konstanty

Veshchestv), Vol. IV, V. P. Glushko, Editor, Moscow (1970).

25. The combustion data of A. T. Hu and G. C. Sinke, J. Chem.

Thermodynamics 1_, 507-513 (1969) were used to derive ^Hf°

298.15 K values for CC1,, CHCl and CH C1 in the liquid state 2

26. The vaporization data of D. L. Hildenbrand and R. A. McDonald,

J. Phys. Chem. 63_, 1521-1522 (1959) were used.

27. The combustion data of R. A. Fletcher and G. Pilcher, Trans.

Faraday Soc. 67, 3191-3201 (1971) were used to calculate

AHf° [CH Cl(g)]. 3

28. J. Chao, A. S. Rodgers, R. C. Wilhoit, and B. J. Zwolinski,

J. Phys. & Chem. Ref. Data 3, 141-162 (1974) provide a recent

evaluation of the thermodynamic properties of CH„CC1„

10^ (

o Bond Dissociation Energies, D at K •

Reaction kj/mol kcal/mol Note (1)

- 20 493.59±0.4 1L7.97±0.1 2

o - o + 101.4±2.1 24.24±0.5 (2) 2

H -» 2H 432.00±0.04 103.25±0.01 2 HO - H + 423.8±2.1 101.3±0.5

HO - HO + 264.4±4 63.2±1

- H + 192+13 46±3 2 H - HO + H 493.7±0.8 118.0±0.2 2 H - 2H0 207.1±2.1 49.5±0o5 2 2

H - H'+ H0 370o3±8 o 4 88.5±2.0 2 2 2

N - N + N 941.69±0.04 225o07±0o01

NO -* N + 627.9 150.1 (2)

N0„ - NO + 300.5 71.83 (2)

NO - N0 + 205±21 49±5 (2) N-0 2

NO - N + NO 474o9±4 113. 5±1

- N + 38.58 (2) 2 161.3 NO - NO + NO 35.1±0.8 8.4±0.2 N-0

N o0. - NO„ + N0 o 53.2 12.7 (2)N-N 2 4 2. I

N„0 C - N0 o + NO. 89.5 21.4 (2) N-0 2 5 2 j

HNO - H + NO 203 48,6 (2)

- NH + 475 113.5

trans-HN0 - 2 HO + NO 209. 49.07 (2) N-0

HNO - HO + NO 200 47.8 (2) N-0

NH - H + N 356±8 85±2

NH - H + HN 360 86 (2,3)

103 Bond Dissociation Energies, D at K o

Reaction kJ/mo 1 kcal/mol Note (1)

NH -» NH. + H 453 108 (2,3)

CO -» C + 1071.94 + 0.4 256.2 ± 0.,1

CO -» CO + 525.9 + 0.,4 125.7 ± 0,,1

CHO -» CH + 859 205 (2)

-» CO +H 119.7 28.6

CH -» CHO + H 314 75

CH -» CH + 378 90.4 (2,3) 3

-» H + H C = 88.2 21.1 (2,3)

+ 41.5 CH 3°2 ~* ^S 173. (2,3)

HCH3+ C*2 53.6 12.8 (2,3)

CH -» CH + H 469.9 + 0.,4 112.3 ± 0,,1 3 2

CH. - CH„ + H 425.1 + 8,.4 101.6 ± 2.,0 4 3

CH OOH -> CH + HO 184. 44.0 (2,3)

-» CH + H0 295. 70.6 (2,3) 3 2

CH ONO -» CH + N0 248 59.2 (2,3) 3 2

CH N0 -* CH + N0 254 60.6 (2,3) 3 2 3 2

CH ON0 -» CHO + N0 174 41.6 (2,3) 3 2 2

-» CH + N0 341 81.6 (2,3) 3

SO -» S + 517.1 + 8 123.6 + 2 so -> SO + 547.3 + 8 130.8 ± 2,,0 2 + S0„ -» S0 o + 342.7 4 81.9 i L

Notes

1. Unless another source is indicated , the values are those recommended by Darwent, B. deB., "Bond Dissociation Energies in Simple Molecules," Natl. Stand. Ref. Data Series - Natl. Bur. Standards 31 (January 1970).

2. Calculated from heats of formation in the accompanying table "Chemical Thermodynamic Properties of Selected Molecular Species". Sources of data are indicated in notes to that table. 3. Calculated for 298 K, values at OK not being available.

104 8 »

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112 Announcement of New Publications on

Chemical Kinetics Data

Director, Chemical Kinetics Information Center Chemistry Building A158 National Bureau of Standards Washington, DC 20234

Dear Sir:

Please add my name to the announcement list for new publications on chemical kinetics and photochemical data from the Chemical Kinetics Information Center.

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4. II I !.!: ANI1 SUBTITLE 5. Publ icat ion Date

Chemical Kinetic and Photochemical Data for June 1975 Modelling Atmospheric Chemistry 6. Performing Organization ( o<

7. author(S) 8. Performing Organ. Report No.

R. F. Hampson, Jr. , and David Garvin; Editors 9. PERFORMING ORGANIZATION NAME AND ADDRESS 10. Project /Task/Work Unit Ni NATIONAL BUREAU OF STANDARDS DEPARTMENT OF COMMERCE 11. Contract/Grant No. WASHINGTON, D.C. 20234 3165409

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16. ABSTRACT (A 200-word or less (actual summary ol most significant information. If document includes a significant

bibliography or literature survey, mention it here.)

A table of data for gas phase chemical reactions and photochemistry of neutral species is presented. Specifically, it gives preferred values for reaction rate constants, photoabsorption cross sections, and quantum yields of primary photochemical processes and also cites recent experimental work. It is intended to provide the basic physical chemical data needed as input data for calculations modelling atmospheric chemistry. An auxiliary table of thermochemical data for the pertinent chemical species is given in the append ix.

17. KEY WORDS (six to twelve entries; alphabetical order; capitalize only the first letter of the first key word unless a proper name; separated by semicolons) Atmospheric chemistry; chemical kinetics; data evaluation; gas phase; photoabsorption cross section; photochemistry; quantum yield; rate constant

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