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Experiments on collisional energy transfer. ACTA ACUST UNITED AC 2019. [DOI: 10.1016/b978-0-444-64207-3.00001-9] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register]
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2
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Troe J. Refined Representation of Falloff Curves for the Reaction HO + NO2 + N2 → (HONO2, HOONO) + N2. J Phys Chem A 2012; 116:6387-93. [DOI: 10.1021/jp212095n] [Citation(s) in RCA: 11] [Impact Index Per Article: 0.9] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/29/2022]
Affiliation(s)
- Jürgen Troe
- Institut für Physikalische Chemie der Universität and Max-Planck-Institut für Biophysikalische Chemie, Göttingen Tammannstrasse 6, D-37077 Göttingen,
Germany
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3
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Koppenol WH, Bounds PL, Nauser T, Kissner R, Rüegger H. Peroxynitrous acid: controversy and consensus surrounding an enigmatic oxidant. Dalton Trans 2012; 41:13779-87. [DOI: 10.1039/c2dt31526b] [Citation(s) in RCA: 54] [Impact Index Per Article: 4.5] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/21/2022]
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4
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Miller Y, Chaban GM, Finlayson-Pitts BJ, Gerber RB. Photochemical processes induced by vibrational overtone excitations: dynamics simulations for cis-HONO, trans-HONO, HNO3, and HNO3-H2O. J Phys Chem A 2007; 110:5342-54. [PMID: 16623461 DOI: 10.1021/jp0559940] [Citation(s) in RCA: 47] [Impact Index Per Article: 2.8] [Reference Citation Analysis] [Abstract] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 12/24/2022]
Abstract
Photochemical processes in HNO3, HNO3-H2O, and cis- and trans-HONO following overtone excitation of the OH stretching mode are studied by classical trajectory simulations. Initial conditions for the trajectories are sampled according to the initially prepared vibrational wave function. Semiempirical potential energy surfaces are used in "on-the-fly" simulations. Several tests indicate at least semiquantitative validity of the potential surfaces employed. A number of interesting new processes and intermediate species are found. The main results include the following: (1) In excitation of HNO3 to the fifth and sixth OH-stretch overtone, hopping of the H atom between the oxygen atoms is found to take place in nearly all trajectories, and can persist for many picoseconds. H-atom hopping events have a higher yield and a faster time scale than the photodissociation of HNO3 into OH and NO2. (2) A fraction of the trajectories for HNO3 show isomerization into HOONO, which in a few cases dissociates into HOO and NO. (3) For high overtone excitation of HONO, isomerization into the weakly bound species HOON is seen in all trajectories, in part of the events as an intermediate step on the way to dissociation into OH + NO. This process has not been reported previously. Well-established processes for HONO, including cis-trans isomerization and H hopping are also observed. (4) Only low overtone levels of HNO3-H2O have sufficiently long liftimes to be spectrocopically relevant. Excitation of these OH stretching overtones is found to result in the dissociation of the cluster H hopping, or dissociation of HNO3 does not take place. The results demonstrate the richness of processes induced by overtone excitation of HNO(x) species, with evidence for new phenomena. Possible relevance of the results to atmospheric processes is discussed.
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Affiliation(s)
- Y Miller
- Department of Physical Chemistry and Fritz Haber Research Center, The Hebrew University, Jerusalem 91904, Israel
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5
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Williams CF, Pogrebnya SK, Clary DC. Quantum study on the branching ratio of the reaction NO2+OH. J Chem Phys 2007; 126:154321. [PMID: 17461640 DOI: 10.1063/1.2714511] [Citation(s) in RCA: 8] [Impact Index Per Article: 0.5] [Reference Citation Analysis] [Abstract] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/14/2022] Open
Abstract
A reduced dimensionality (RD) approximation is developed for the title reaction which treats the angle of approach of the hydroxyl radical to the nitrogen dioxide molecule and the radial distance between the two species explicitly. All other degrees of freedom are treated adiabatically. Electronic structure calculations at the complete active space self-consistent field level are used to fit a potential energy surface (PES) in these two coordinates. Within this RD model the adiabatic capture centrifugal sudden approximation is used to calculate the high pressure limit rate constant. A correction for reflection from the PES due to rotationally nonadiabatic transitions is applied using the wave packet capture approximation. The branching ratio for the title reaction is calculated for the atmospherically significant temperature range of 200-400 K at 20 Torr without distinguishing between the conformers of HOONO. The result is k(HOONO)k(HNO(3) )=0.051 at 20 Torr and 300 K, which is in good agreement with the measured branching ratio between cis-cis-HOONO and nitric acid. This suggests that most of the different conformers of HOONO were converted to the most stable cis-cis conformer on the time scale of the measurements made.
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Affiliation(s)
- Christopher F Williams
- Physical and Theoretical Chemistry Laboratory, University of Oxford, South Parks Road, Oxford OX1 3QZ, United Kingdom.
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6
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Zhang J, Donahue NM. Constraining the Mechanism and Kinetics of OH + NO2 and HO2 + NO Using the Multiple-Well Master Equation. J Phys Chem A 2006; 110:6898-911. [PMID: 16722705 DOI: 10.1021/jp0556512] [Citation(s) in RCA: 29] [Impact Index Per Article: 1.6] [Reference Citation Analysis] [Abstract] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/30/2022]
Abstract
Several recent experimental studies have provided substantial new constraints for the mechanisms on the HNO3 potential energy surface. These include observations of biexponential OH decay over short time scales from OH + NO2, which constrain key properties of the short-lived HOONO intermediate, observations of both conformers of the HOONO intermediate itself, isotopic scrambling data for 18OH + NO2, and observations of HONO2 production from the HO2 + NO reaction. We combine all of these recent data in a master-equation simulation of the system. This simulation is initialized with computational values for both stable species (wells) and transition states, but parameters are then adjusted to fit the observations. All parameters are kept within limits defined by experimental and theoretical uncertainty, and all converge away from their bounds. The primary fitting is carried out on the OH kinetic data-we first fit the biexponential kinetics, then address the isotopic scrambling. Isotopic scrambling is shown to be rapid but not complete at low pressure, while at least two parameter sets are shown to be consistent with the biexponential data. Of these two parameter sets, one is far more consistent with recent observations of trans-HOONO decay, isotopic scrambling, and HONO2 production from HO2 + NO. This we regard as the most probable potential energy surface for the reaction. On this PES, cis-trans isomerization for HOONO is slow but isomerization of trans-HOONO to HONO2 is rapid. This has significant implications for observed HOONO behavior and also HONO2 formation in the atmosphere from both HO2 + NO and OH + NO2.
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Affiliation(s)
- Jieyuan Zhang
- Department of Chemistry and Chemical Engineering, Carnegie Mellon University, Doherty Hall 1107, 5000 Forbes Avenue, Pittsburgh, Pennsylvania 15213, USA
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7
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Hippler H, Krasteva N, Nasterlack S, Striebel F. Reaction of OH + NO2: High Pressure Experiments and Falloff Analysis. J Phys Chem A 2006; 110:6781-8. [PMID: 16722694 DOI: 10.1021/jp0562734] [Citation(s) in RCA: 18] [Impact Index Per Article: 1.0] [Reference Citation Analysis] [Abstract] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/30/2022]
Abstract
High pressure experiments on the OH + NO2 reaction are presented for 3 different temperatures. At 300 K, experiments in He (p = 2-500 bar) as well as in Ar (p = 2-4 bar) were performed. The rate constants obtained in Ar agree well with values which have been reported earlier by our group (Forster, R.; Frost, M.; Fulle, D.; Hamann, H. F.; Hippler, H.; Schlepegrell, A.; Troe, J. J. Chem. Phys. 1995, 103, 2949. Fulle, D.; Hamann, H. F.; Hippler, H.; Troe, J. J. Chem. Phys. 1998, 108, 5391). In contrast, the rate coefficients determined in He were found to be 15-25% lower than the values given in our earlier publications. Additionally, results for He as bath gas at elevated temperatures (T = 400 K, p = 3-150 bar; T = 600 K, p = 3-150 bar) are reported. The results obtained at elevated pressures are found to be in good agreement with existing literature data. The observed falloff behavior is analyzed in terms of the Troe formalism taking into account two reaction channels: one yielding HNO3 and one yielding HOONO. It is found that the extracted parameters are in agreement with rate constants for vibrational relaxation and isotopic scrambling as well as with experimentally determined branching ratios. Based on our analysis we determine falloff parameters to calculate the rate constant for atmospheric conditions.
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Affiliation(s)
- Horst Hippler
- Lehrstuhl für Molekulare Physikalische Chemie, Universität Karlsruhe, Kaiserstrasse 12, D-76128 Karlsruhe, Germany.
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8
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Butkovskaya NI, Kukui A, Pouvesle N, Le Bras G. Formation of Nitric Acid in the Gas-Phase HO2 + NO Reaction: Effects of Temperature and Water Vapor. J Phys Chem A 2005; 109:6509-20. [PMID: 16833996 DOI: 10.1021/jp051534v] [Citation(s) in RCA: 65] [Impact Index Per Article: 3.4] [Reference Citation Analysis] [Abstract] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/30/2022]
Abstract
A high-pressure turbulent flow reactor coupled with a chemical ionization mass spectrometer was used to investigate the minor channel (1b) producing nitric acid, HNO3, in the HO2 + NO reaction for which only one channel (1a) is known so far: HO2 + NO --> OH + NO2 (1a), HO2 + NO --> HNO3 (1b). The reaction has been investigated in the temperature range 223-298 K at a pressure of 200 Torr of N2 carrier gas. The influence of water vapor has been studied at 298 K. The branching ratio, k1b/k1a, was found to increase from (0.18(+0.04/-0.06))% at 298 K to (0.87(+0.05/-0.08))% at 223 K, corresponding to k1b = (1.6 +/- 0.5) x 10(-14) and (10.4 +/- 1.7) x 10(-14) cm3 molecule(-1) s(-1), respectively at 298 and 223 K. The data could be fitted by the Arrhenius expression k1b = 6.4 x 10(-17) exp((1644 +/- 76)/T) cm3 molecule(-1) s(-1) at T = 223-298 K. The yield of HNO3 was found to increase in the presence of water vapor (by 90% at about 3 Torr of H2O). Implications of the obtained results for atmospheric radicals chemistry and chemical amplifiers used to measure peroxy radicals are discussed. The results show in particular that reaction 1b can be a significant loss process for the HO(x) (OH, HO2) radicals in the upper troposphere.
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Affiliation(s)
- N I Butkovskaya
- CNRS, Laboratoire de Combustion et Systèmes Réactifs, 1C Av. de la Recherche Scientifique, 45071 Orléans Cedex 2, France
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Kinetics and Mechanism of the Oxidation of Alkanes and Alkenes with Peroxynitrous Acid in Aqueous Solution-Gas Phase Systems. KINETICS AND CATALYSIS 2005. [DOI: 10.1007/s10975-005-0083-y] [Citation(s) in RCA: 6] [Impact Index Per Article: 0.3] [Reference Citation Analysis] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 10/25/2022]
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10
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Liu Y, Lohr LL, Barker JR. Quasi-Classical Trajectory Simulations of Intramolecular Vibrational Energy Redistribution in HONO2 and DONO2. J Phys Chem B 2005; 109:8304-9. [PMID: 16851973 DOI: 10.1021/jp047436b] [Citation(s) in RCA: 14] [Impact Index Per Article: 0.7] [Reference Citation Analysis] [Abstract] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/29/2022]
Abstract
By use of an analytic potential energy surface developed in this work for nitric acid, the quasi-classical trajectory method was used to simulate intramolecular vibrational energy redistribution (IVR). A method was developed for monitoring the average vibrational energy in the OH (or OD) mode that uses the mean-square displacement of the bond length calculated during the trajectories. This method is effective for both rotating and nonrotating molecules. The calculated IVR time constant for HONO(2) decreases exponentially with increasing excitation energy, is almost independent of rotational temperature, and is in excellent agreement with the experimental determination (Bingemann, D.; Gorman, M. P.; King, A. M.; Crim, F. F. J. Chem.Phys. 1997, 107, 661). In DONO(2), the IVR time constants show more complicated behavior with increasing excitation energy, apparently due to 2:1 Fermi-resonance coupling with lower frequency modes. This effect should be measurable in experiments.
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Affiliation(s)
- Yong Liu
- Department of Atmospheric, Oceanic, and Space Sciences, University of Michigan, Ann Arbor, Michigan 48109-2143, USA
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11
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D'Ottone L, Bauer D, Campuzano-Jost P, Fardy M, Hynes AJ. Kinetic and mechanistic studies of the recombination of OH with NO2: Vibrational deactivation, isotopic scrambling and product isomer branching ratios. Faraday Discuss 2005; 130:111-23; discussion 125-51, 519-24. [PMID: 16161781 DOI: 10.1039/b417458p] [Citation(s) in RCA: 16] [Impact Index Per Article: 0.8] [Reference Citation Analysis] [Abstract] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/21/2022]
Abstract
The kinetics and mechanism of the three-body recombination of OH with NO2 were studied using a pulsed laser photolysis pulsed laser induced fluorescence technique. The rate coefficients for deactivation of vibrationally excited OH (v = 1-5) by NO2 were found to be independent of vibrational level with a value of (6.4 +/- 0.3) x 10(-11) cm3 molecule s (-1) at 298 K. The rate coefficient for reaction of 18OH with NO2 was measured and found to be much faster than for unlabeled OH with a "zero pressure" rate of 1 x 10(-11) cm3 molecule(-1) s(-1) at 298 K and 273 K. Observation of temporal profiles of 16OH and 18OH suggest that isotopic scrambling in the initially formed [H18ON16O2] complex is complete on the microsecond time scale of our experiments. The rate coefficient for reaction of unlabeled OH with NO2 was measured at 413 K in 400 Torr of He. Biexponential temporal profiles were obtained and are consistent with a 10 +/- 3% yield of the weakly bound HOONO isomer.
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Affiliation(s)
- Luca D'Ottone
- University of Miami, Rosenstiel School of Marine and Atmospheric Science, Division of Marine and Atmospheric Chemistry, 4600 Rickenbacker Causeway, Miami FL 33149, USA
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12
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Fry JL, Nizkorodov SA, Okumura M, Roehl CM, Francisco JS, Wennberg PO. Cis-cis and trans-perp HOONO: Action spectroscopy and isomerization kinetics. J Chem Phys 2004; 121:1432-48. [PMID: 15260688 DOI: 10.1063/1.1760714] [Citation(s) in RCA: 41] [Impact Index Per Article: 2.1] [Reference Citation Analysis] [Abstract] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 01/17/2023] Open
Abstract
The weakly bound HOONO product of the OH+NO2+M reaction is studied using the vibrational predissociation that follows excitation of the first OH overtone (2nu1). We observe formation of both cis-cis and trans-perp conformers of HOONO. The trans-perp HOONO 2nu1 band is observed under thermal (223-238 K) conditions at 6971 cm(-1). We assign the previously published (warmer temperature) HOONO spectrum to the 2nu1 band at 6365 cm(-1) and 2nu1-containing combination bands of the cis-cis conformer of HOONO. The band shape of the trans-perp HOONO spectrum is in excellent agreement with the predicted rotational contour based on previous experimental and theoretical results, but the apparent origin of the cis-cis HOONO spectrum at 6365 cm(-1) is featureless and significantly broader, suggesting more rapid intramolecular vibrational redistribution or predissociation in the latter isomer. The thermally less stable trans-perp HOONO isomerizes rapidly to cis-cis HOONO with an experimentally determined lifetime of 39 ms at 233 K at 13 hPa (in a buffer gas of predominantly Ar). The temperature dependence of the trans-perp HOONO lifetime in the range 223-238 K yields an isomerization barrier of 33+/-12 kJ/mol. New ab initio calculations of the structure and vibrational mode frequencies of the transition state perp-perp HOONO are performed using the coupled cluster singles and doubles with perturbative triples [CCSD(T)] model, using a correlation consistent polarized triple zeta basis set (cc-pVTZ). The energetics of cis-cis, trans-perp, and perp-perp HOONO are also calculated at this level [CCSD(T)/cc-pVTZ] and with a quadruple zeta basis set using the structure determined at the triple zeta basis set [CCSD(T)/cc-pVQZ//CCSD(T)/cc-pVTZ]. These calculations predict that the anti form of perp-perp HOONO has an energy of DeltaE0=42.4 kJ/mol above trans-perp HOONO, corresponding to an activation enthalpy of DeltaH298 (double dagger 0)=41.1 kJ/mol. These results are in good agreement with statistical simulations based on a model developed by Golden, Barker, and Lohr. The simulated isomerization rates match the observed decay rates when modeled with a trans-perp to cis-cis HOONO isomerization barrier of 40.8 kJ/mol and a strong collision model. The quantum yield of cis-cis HOONO dissociation to OH and NO2 is also calculated as a function of photon excitation energy in the range 3500-7500 cm(-1), assuming D0=83 kJ/mol. The quantum yield is predicted to vary from 0.15 to 1 over the observed spectrum at 298 K, leading to band intensities in the action spectrum that are highly temperature dependent; however, the observed relative band strengths in the cis-cis HOONO spectrum do not change substantially with temperature over the range 193-273 K. Semiempirical calculations of the oscillator strengths for 2nu1(cis-cis HOONO) and 2nu1(trans-perp HOONO) are performed using (1) a one-dimensional anharmonic model and (2) a Morse oscillator model for the OH stretch, and ab initio dipole moment functions calculated using Becke, Lee, Yang, and Parr density functional theory (B3LYP), Møller-Plesset pertubation theory truncated at the second and third order (MP2 and MP3), and quadratic configuration interaction theory using single and double excitations (QCISD). The QCISD level calculated ratio of 2nu1 oscillator strengths of trans-perp to cis-cis HOONO is 3.7:1. The observed intensities indicate that the concentration of trans-perp HOONO early in the OH+NO2 reaction is significantly greater than predicted by a Boltzmann distribution, consistent with statistical predictions of high initial yields of trans-perp HOONO from the OH+NO2+M reaction. In the atmosphere, trans-perp HOONO will isomerize nearly instantaneously to cis-cis HOONO. Loss of HOONO via photodissociation in the near-IR limits the lifetime of cis-cis HOONO during daylight to less than 45 h, other loss mechanisms will reduce the lifetime further.
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Affiliation(s)
- Juliane L Fry
- Arthur Amos Noyes Laboratory of Chemical Physics, California Institute of Technology, Pasadena, California 91125, USA.
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13
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Geletii YV, Musaev DG, Khavrutskii L, Hill CL. Peroxynitrite Reactions with Dimethylsulfide and Dimethylselenide: An Experimental Study. J Phys Chem A 2003. [DOI: 10.1021/jp035955t] [Citation(s) in RCA: 11] [Impact Index Per Article: 0.5] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 01/15/2023]
Affiliation(s)
- Yurii V. Geletii
- Department of Chemistry, and Cherry L. Emerson Center for Scientific Computation, Emory University, 1515 Pierce Drive, Atlanta, Georgia 30322
| | - Djamaladdin G. Musaev
- Department of Chemistry, and Cherry L. Emerson Center for Scientific Computation, Emory University, 1515 Pierce Drive, Atlanta, Georgia 30322
| | - Lyuba Khavrutskii
- Department of Chemistry, and Cherry L. Emerson Center for Scientific Computation, Emory University, 1515 Pierce Drive, Atlanta, Georgia 30322
| | - Craig L. Hill
- Department of Chemistry, and Cherry L. Emerson Center for Scientific Computation, Emory University, 1515 Pierce Drive, Atlanta, Georgia 30322
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14
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Zhu RS, Lin MC. Ab initio study of the HO2+NO reaction: Prediction of the total rate constant and product branching ratios for the forward and reverse processes. J Chem Phys 2003. [DOI: 10.1063/1.1619373] [Citation(s) in RCA: 32] [Impact Index Per Article: 1.5] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 01/25/2023] Open
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15
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Cohen RC, Murphy JG. Photochemistry of NO2 in Earth's Stratosphere: Constraints from Observations. Chem Rev 2003; 103:4985-98. [PMID: 14664640 DOI: 10.1021/cr020647x] [Citation(s) in RCA: 18] [Impact Index Per Article: 0.9] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/30/2022]
Affiliation(s)
- Ronald C Cohen
- Department of Chemistry, University of California, Berkeley, CA 94720-1460, USA
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16
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Pollack IB, Konen IM, Li EXJ, Lester MI. Spectroscopic characterization of HOONO and its binding energy via infrared action spectroscopy. J Chem Phys 2003. [DOI: 10.1063/1.1624246] [Citation(s) in RCA: 26] [Impact Index Per Article: 1.2] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/14/2022] Open
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Golden DM, Barker JR, Lohr LL. Master Equation Models for the Pressure- and Temperature-Dependent Reactions HO + NO2 → HONO2 and HO + NO2 → HOONO. J Phys Chem A 2003. [DOI: 10.1021/jp0353183] [Citation(s) in RCA: 57] [Impact Index Per Article: 2.7] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/30/2022]
Affiliation(s)
- David M. Golden
- Department of Mechanical Engineering, Stanford University, Stanford, California 94305, Department of Atmospheric, Oceanic and Space Sciences, University of Michigan, Ann Arbor, Michigan 48109-2143, and Department of Chemistry, University of Michigan, Ann Arbor, Michigan 48109-1055
| | - John R. Barker
- Department of Mechanical Engineering, Stanford University, Stanford, California 94305, Department of Atmospheric, Oceanic and Space Sciences, University of Michigan, Ann Arbor, Michigan 48109-2143, and Department of Chemistry, University of Michigan, Ann Arbor, Michigan 48109-1055
| | - Lawrence L. Lohr
- Department of Mechanical Engineering, Stanford University, Stanford, California 94305, Department of Atmospheric, Oceanic and Space Sciences, University of Michigan, Ann Arbor, Michigan 48109-2143, and Department of Chemistry, University of Michigan, Ann Arbor, Michigan 48109-1055
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Barker JR, Golden DM. Master Equation Analysis of Pressure-Dependent Atmospheric Reactions. Chem Rev 2003; 103:4577-92. [PMID: 14664624 DOI: 10.1021/cr020655d] [Citation(s) in RCA: 87] [Impact Index Per Article: 4.1] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/28/2022]
Affiliation(s)
- John R Barker
- Department of Atmospheric, Oceanic and Space Sciences and Department of Chemistry, University of Michigan, Ann Arbor, MI 48109-2143, USA.
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Affiliation(s)
- Ian W M Smith
- School of Chemical Sciences, The University of Birmingham, Edgbaston, Birmingham B15 2TT, United Kingdom.
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20
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Bean BD, Mollner AK, Nizkorodov SA, Nair G, Okumura M, Sander SP, Peterson KA, Francisco JS. Cavity Ringdown Spectroscopy of cis-cis HOONO and the HOONO/HONO2 Branching Ratio in the Reaction OH + NO2 + M. J Phys Chem A 2003. [DOI: 10.1021/jp034407c] [Citation(s) in RCA: 41] [Impact Index Per Article: 2.0] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/28/2022]
Affiliation(s)
- Brian D. Bean
- Arthur Amos Noyes Laboratory of Chemical Physics, MC 127-72, California Institute of Technology, Pasadena, California 91125
| | - Andrew K. Mollner
- Arthur Amos Noyes Laboratory of Chemical Physics, MC 127-72, California Institute of Technology, Pasadena, California 91125
| | - Sergey A. Nizkorodov
- Arthur Amos Noyes Laboratory of Chemical Physics, MC 127-72, California Institute of Technology, Pasadena, California 91125
| | - Gautham Nair
- Arthur Amos Noyes Laboratory of Chemical Physics, MC 127-72, California Institute of Technology, Pasadena, California 91125
| | - Mitchio Okumura
- Arthur Amos Noyes Laboratory of Chemical Physics, MC 127-72, California Institute of Technology, Pasadena, California 91125
| | - Stanley P. Sander
- NASA Jet Propulsion Laboratory, MC 183-901, California Institute of Technology, Pasadena, California 91109
| | - Kirk A. Peterson
- Department of Chemistry, Washington State University, Pullman, Washington 99164-4630
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22
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D'Ottone L, Campuzano-Jost P, Bauer D, Hynes AJ. A Pulsed Laser Photolysis−Pulsed Laser Induced Fluorescence Study of the Kinetics of the Gas-Phase Reaction of OH with NO2. J Phys Chem A 2001. [DOI: 10.1021/jp012250n] [Citation(s) in RCA: 38] [Impact Index Per Article: 1.7] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/30/2022]
Affiliation(s)
- L. D'Ottone
- Division of Marine and Atmospheric Chemistry, Rosenstiel School of Marine and Atmospheric Science, University of Miami, 4600 Rickenbacker Causeway, Miami, Florida 33149
| | - P. Campuzano-Jost
- Division of Marine and Atmospheric Chemistry, Rosenstiel School of Marine and Atmospheric Science, University of Miami, 4600 Rickenbacker Causeway, Miami, Florida 33149
| | - D. Bauer
- Division of Marine and Atmospheric Chemistry, Rosenstiel School of Marine and Atmospheric Science, University of Miami, 4600 Rickenbacker Causeway, Miami, Florida 33149
| | - A. J. Hynes
- Division of Marine and Atmospheric Chemistry, Rosenstiel School of Marine and Atmospheric Science, University of Miami, 4600 Rickenbacker Causeway, Miami, Florida 33149
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23
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Dransfield TJ, Donahue NM, Anderson JG. High-Pressure Flow Reactor Product Study of the Reactions of HOx+ NO2: The Role of Vibrationally Excited Intermediates†. J Phys Chem A 2001. [DOI: 10.1021/jp002391+] [Citation(s) in RCA: 28] [Impact Index Per Article: 1.2] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/28/2022]
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24
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Perkins KK, Hanisco TF, Cohen RC, Koch LC, Stimpfle RM, Voss PB, Bonne GP, Lanzendorf EJ, Anderson JG, Wennberg PO, Gao RS, Del Negro LA, Salawitch RJ, McElroy CT, Hintsa EJ, Loewenstein M, Bui TP. The NOx−HNO3 System in the Lower Stratosphere: Insights from In Situ Measurements and Implications of the JHNO3−[OH] Relationship. J Phys Chem A 2001. [DOI: 10.1021/jp002519n] [Citation(s) in RCA: 21] [Impact Index Per Article: 0.9] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/29/2022]
Affiliation(s)
- K. K. Perkins
- Department of Chemistry and Chemical Biology, Harvard University, Cambridge, Massachusetts 02138; Departments of Chemistry and of Geology and Geophysics, University of California, Berkeley, California 94720; Divisions of Engineering and of Geological and Planetary Science, California Institute of Technology, Pasadena, California 91125; NOAA Aeronomy Laboratory, Boulder, Colorado 80303; NASA Jet Propulsion Laboratory, California Institute of Technology, Pasadena, California 91109; Meteorological Service
| | - T. F. Hanisco
- Department of Chemistry and Chemical Biology, Harvard University, Cambridge, Massachusetts 02138; Departments of Chemistry and of Geology and Geophysics, University of California, Berkeley, California 94720; Divisions of Engineering and of Geological and Planetary Science, California Institute of Technology, Pasadena, California 91125; NOAA Aeronomy Laboratory, Boulder, Colorado 80303; NASA Jet Propulsion Laboratory, California Institute of Technology, Pasadena, California 91109; Meteorological Service
| | - R. C. Cohen
- Department of Chemistry and Chemical Biology, Harvard University, Cambridge, Massachusetts 02138; Departments of Chemistry and of Geology and Geophysics, University of California, Berkeley, California 94720; Divisions of Engineering and of Geological and Planetary Science, California Institute of Technology, Pasadena, California 91125; NOAA Aeronomy Laboratory, Boulder, Colorado 80303; NASA Jet Propulsion Laboratory, California Institute of Technology, Pasadena, California 91109; Meteorological Service
| | - L. C. Koch
- Department of Chemistry and Chemical Biology, Harvard University, Cambridge, Massachusetts 02138; Departments of Chemistry and of Geology and Geophysics, University of California, Berkeley, California 94720; Divisions of Engineering and of Geological and Planetary Science, California Institute of Technology, Pasadena, California 91125; NOAA Aeronomy Laboratory, Boulder, Colorado 80303; NASA Jet Propulsion Laboratory, California Institute of Technology, Pasadena, California 91109; Meteorological Service
| | - R. M. Stimpfle
- Department of Chemistry and Chemical Biology, Harvard University, Cambridge, Massachusetts 02138; Departments of Chemistry and of Geology and Geophysics, University of California, Berkeley, California 94720; Divisions of Engineering and of Geological and Planetary Science, California Institute of Technology, Pasadena, California 91125; NOAA Aeronomy Laboratory, Boulder, Colorado 80303; NASA Jet Propulsion Laboratory, California Institute of Technology, Pasadena, California 91109; Meteorological Service
| | - P. B. Voss
- Department of Chemistry and Chemical Biology, Harvard University, Cambridge, Massachusetts 02138; Departments of Chemistry and of Geology and Geophysics, University of California, Berkeley, California 94720; Divisions of Engineering and of Geological and Planetary Science, California Institute of Technology, Pasadena, California 91125; NOAA Aeronomy Laboratory, Boulder, Colorado 80303; NASA Jet Propulsion Laboratory, California Institute of Technology, Pasadena, California 91109; Meteorological Service
| | - G. P. Bonne
- Department of Chemistry and Chemical Biology, Harvard University, Cambridge, Massachusetts 02138; Departments of Chemistry and of Geology and Geophysics, University of California, Berkeley, California 94720; Divisions of Engineering and of Geological and Planetary Science, California Institute of Technology, Pasadena, California 91125; NOAA Aeronomy Laboratory, Boulder, Colorado 80303; NASA Jet Propulsion Laboratory, California Institute of Technology, Pasadena, California 91109; Meteorological Service
| | - E. J. Lanzendorf
- Department of Chemistry and Chemical Biology, Harvard University, Cambridge, Massachusetts 02138; Departments of Chemistry and of Geology and Geophysics, University of California, Berkeley, California 94720; Divisions of Engineering and of Geological and Planetary Science, California Institute of Technology, Pasadena, California 91125; NOAA Aeronomy Laboratory, Boulder, Colorado 80303; NASA Jet Propulsion Laboratory, California Institute of Technology, Pasadena, California 91109; Meteorological Service
| | - J. G. Anderson
- Department of Chemistry and Chemical Biology, Harvard University, Cambridge, Massachusetts 02138; Departments of Chemistry and of Geology and Geophysics, University of California, Berkeley, California 94720; Divisions of Engineering and of Geological and Planetary Science, California Institute of Technology, Pasadena, California 91125; NOAA Aeronomy Laboratory, Boulder, Colorado 80303; NASA Jet Propulsion Laboratory, California Institute of Technology, Pasadena, California 91109; Meteorological Service
| | - P. O. Wennberg
- Department of Chemistry and Chemical Biology, Harvard University, Cambridge, Massachusetts 02138; Departments of Chemistry and of Geology and Geophysics, University of California, Berkeley, California 94720; Divisions of Engineering and of Geological and Planetary Science, California Institute of Technology, Pasadena, California 91125; NOAA Aeronomy Laboratory, Boulder, Colorado 80303; NASA Jet Propulsion Laboratory, California Institute of Technology, Pasadena, California 91109; Meteorological Service
| | - R. S. Gao
- Department of Chemistry and Chemical Biology, Harvard University, Cambridge, Massachusetts 02138; Departments of Chemistry and of Geology and Geophysics, University of California, Berkeley, California 94720; Divisions of Engineering and of Geological and Planetary Science, California Institute of Technology, Pasadena, California 91125; NOAA Aeronomy Laboratory, Boulder, Colorado 80303; NASA Jet Propulsion Laboratory, California Institute of Technology, Pasadena, California 91109; Meteorological Service
| | - L. A. Del Negro
- Department of Chemistry and Chemical Biology, Harvard University, Cambridge, Massachusetts 02138; Departments of Chemistry and of Geology and Geophysics, University of California, Berkeley, California 94720; Divisions of Engineering and of Geological and Planetary Science, California Institute of Technology, Pasadena, California 91125; NOAA Aeronomy Laboratory, Boulder, Colorado 80303; NASA Jet Propulsion Laboratory, California Institute of Technology, Pasadena, California 91109; Meteorological Service
| | - R. J. Salawitch
- Department of Chemistry and Chemical Biology, Harvard University, Cambridge, Massachusetts 02138; Departments of Chemistry and of Geology and Geophysics, University of California, Berkeley, California 94720; Divisions of Engineering and of Geological and Planetary Science, California Institute of Technology, Pasadena, California 91125; NOAA Aeronomy Laboratory, Boulder, Colorado 80303; NASA Jet Propulsion Laboratory, California Institute of Technology, Pasadena, California 91109; Meteorological Service
| | - C. T. McElroy
- Department of Chemistry and Chemical Biology, Harvard University, Cambridge, Massachusetts 02138; Departments of Chemistry and of Geology and Geophysics, University of California, Berkeley, California 94720; Divisions of Engineering and of Geological and Planetary Science, California Institute of Technology, Pasadena, California 91125; NOAA Aeronomy Laboratory, Boulder, Colorado 80303; NASA Jet Propulsion Laboratory, California Institute of Technology, Pasadena, California 91109; Meteorological Service
| | - E. J. Hintsa
- Department of Chemistry and Chemical Biology, Harvard University, Cambridge, Massachusetts 02138; Departments of Chemistry and of Geology and Geophysics, University of California, Berkeley, California 94720; Divisions of Engineering and of Geological and Planetary Science, California Institute of Technology, Pasadena, California 91125; NOAA Aeronomy Laboratory, Boulder, Colorado 80303; NASA Jet Propulsion Laboratory, California Institute of Technology, Pasadena, California 91109; Meteorological Service
| | - M. Loewenstein
- Department of Chemistry and Chemical Biology, Harvard University, Cambridge, Massachusetts 02138; Departments of Chemistry and of Geology and Geophysics, University of California, Berkeley, California 94720; Divisions of Engineering and of Geological and Planetary Science, California Institute of Technology, Pasadena, California 91125; NOAA Aeronomy Laboratory, Boulder, Colorado 80303; NASA Jet Propulsion Laboratory, California Institute of Technology, Pasadena, California 91109; Meteorological Service
| | - T. P. Bui
- Department of Chemistry and Chemical Biology, Harvard University, Cambridge, Massachusetts 02138; Departments of Chemistry and of Geology and Geophysics, University of California, Berkeley, California 94720; Divisions of Engineering and of Geological and Planetary Science, California Institute of Technology, Pasadena, California 91125; NOAA Aeronomy Laboratory, Boulder, Colorado 80303; NASA Jet Propulsion Laboratory, California Institute of Technology, Pasadena, California 91109; Meteorological Service
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Troe J. Analysis of the temperature and pressure dependence of the reaction HO + NO2 + M ? HONO2 + M. INT J CHEM KINET 2001. [DOI: 10.1002/kin.10019] [Citation(s) in RCA: 34] [Impact Index Per Article: 1.5] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/09/2022]
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26
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Donahue NM, Mohrschladt R, Dransfield TJ, Anderson JG, Dubey MK. Constraining the Mechanism of OH + NO2 Using Isotopically Labeled Reactants: Experimental Evidence for HOONO Formation. J Phys Chem A 2000. [DOI: 10.1021/jp0035582] [Citation(s) in RCA: 38] [Impact Index Per Article: 1.6] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/28/2022]
Affiliation(s)
- Neil M. Donahue
- Department of Chemistry and Chemical Biology, Harvard University, Cambridge, Massachusetts 02138
| | - Ralf Mohrschladt
- Department of Chemistry and Chemical Biology, Harvard University, Cambridge, Massachusetts 02138
| | - Timothy J. Dransfield
- Department of Chemistry and Chemical Biology, Harvard University, Cambridge, Massachusetts 02138
| | - James G. Anderson
- Department of Chemistry and Chemical Biology, Harvard University, Cambridge, Massachusetts 02138
| | - Manvendra K. Dubey
- Atmospheric and Climate Sciences, Los Alamos National Labortaory, Los Alamos, New Mexico 87545
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