State-Resolved Dissociation Rates for Extremely Nonequilibrium Atmospheric Entries

10
State-Resolved Dissociation Rates for Extremely Nonequilibrium Atmospheric Entries M. Lino da Silva, V. Guerra, and J. Loureiro Instituto Superior Técnico, 1049-001 Lisboa, Portugal DOI: 10.2514/1.24114 This paper presents the application of the forced harmonic oscillator method to the simulation of state-resolved dissociation processes behind high-temperature shock waves typical of atmospheric reentries. Improvements have been brought to the model, considering a more precise method for the calculation of the different vibrational level energies, therefore increasing the accuracy of the predicted transition probabilities between higher vibrational levels close and above the dissociation limit. The model has been validated against data issued from recent experiments, as well as data issued from semiclassical trajectory calculations for collisions between different species. A good overall agreement is achieved against such other data. A database of reaction rates has been constructed with the purpose of simulating shock-heated nitrogen ows. Dissociation processes behind a shock wave have been simulated for different postshock translational temperatures. At lower temperatures, the well-known ladder-climbing phenomenon is the main dissociation channel behind a shock wave, with dissociation occurring for transitions from the vibrational levels close to the dissociation limit. At higher temperatures, transitions between the different vibrational levels of nitrogen become roughly equiprobable, and the overall range of bound vibrational levels contributes to the dissociation. Nomenclature C k ij = transformation matrix C p = specic heat at constant pressure, J=kg=K C v = specic heat at constant volume, J=kg=K E = level energy, Hz E m = Morse potential well, J h = enthalpy, J=kg J s = Bessel function k B = Boltzmann constant, 1:3806505 10 23 J=K kT = thermal reaction rate, cm 3 =s M = Mach number m = mass, kg ~ m = mass parameter, m AB m C =m AB m C or m AB m CD =m AB m CD P = probability r = internuclear distance, m S VT = vibration-translation steric factor, 4=9 S VV = vibration-vibration steric factor, 1=27 T = macroscopic temperature, K T r = rotational temperature, K T tr = translational temperature, K T tr-r = translational-rotational temperature, K T v = vibrational temperature, K t = time, s Vr = intermolecular potential, J V-T = vibration-translation processes V-V-T = vibration-vibration-translation processes v = vibrational level v = velocity, m=s v = averaged collision velocity, m=s Z = gas-kinetic collisional frequency, Hz = repulsive potential parameter, m 1 = heat capacity ration, C p =C v = mass parameter, m A =m A m B " = two-state rst-order V-T transition probability, P1 ! 0 = mass parameter, m A m B =m A m B = two-state rst-order V-V-T transition probability, 4P1; 0 ! 0; 1 1=2 = generalized two-state rst-order V-V-T transition probability = collision cross section, m 2 ! = vibrational transition frequency, Hz ! e = harmonic oscillator energy, Hz ! e x e = rst-order anharmonic oscillator energy, Hz Subscripts f = nal vibrational quantum number i = initial vibrational quantum number max = maximum vibrational level before dissociation qbound = vibrational level above the dissociation limit tr = translational mode vib = vibrational mode 0 = preshock 1 = postshock I. Introduction S PECIAL focus is currently being brought to high-temperature kinetic phenomena behind high-speed shock-waves. Advances in the qualitative and quantitative understanding of such postshock phenomena [14] are being driven by the denition of interplanetary missions involving the entry (or reentry) of a spacecraft in a planetary atmosphere. Maneuvers such as planetary aerobraking, aerocapture, or direct entry of a spacecraft inbound from another planet follow hyperbolic trajectories where crossing of the planetary atmosphere occurs at velocities well in excess of 10 km=s. For example, a direct entry in Earth atmosphere from planet Mars occurs at 11 km=s (M 44). Comparatively, a Space Shuttle entry from Earths orbit occurs at most at 7 km=s (M 28) [5]. The well-known RankineHugoniot shock relations allow the determination of the postshock translational temperature T 1 according to the equation Received 22 March 2006; revision received 17 May 2006; accepted for publication 18 May 2006. Copyright © 2006 by the American Institute of Aeronautics and Astronautics, Inc. All rights reserved. Copies of this paper may be made for personal or internal use, on condition that the copier pay the $10.00 per-copy fee to the Copyright Clearance Center, Inc., 222 Rosewood Drive, Danvers, MA 01923; include the code $10.00 in correspondence with the CCC. Researcher, Centro de Física dos Plasmas, Av. Rovisco Pais; [email protected]. Member AIAA. Professor, Centro de Física dos Plasmas, Av. Rovisco Pais. JOURNAL OF THERMOPHYSICS AND HEAT TRANSFER Vol. 21, No. 1, JanuaryMarch 2007 40

Transcript of State-Resolved Dissociation Rates for Extremely Nonequilibrium Atmospheric Entries

State-Resolved Dissociation Rates for ExtremelyNonequilibrium Atmospheric Entries

M. Lino da Silva,∗ V. Guerra,† and J. Loureiro†

Instituto Superior Técnico, 1049-001 Lisboa, Portugal

DOI: 10.2514/1.24114

This paper presents the application of the forced harmonic oscillator method to the simulation of state-resolved

dissociation processes behind high-temperature shock waves typical of atmospheric reentries. Improvements have

been brought to the model, considering a more precise method for the calculation of the different vibrational level

energies, therefore increasing the accuracy of the predicted transition probabilities between higher vibrational levels

close and above the dissociation limit. The model has been validated against data issued from recent experiments, as

well as data issued from semiclassical trajectory calculations for collisions between different species. A good overall

agreement is achieved against such other data. A database of reaction rates has been constructed with the purpose of

simulating shock-heated nitrogen flows. Dissociation processes behind a shock wave have been simulated for

different postshock translational temperatures. At lower temperatures, the well-known ladder-climbing

phenomenon is the main dissociation channel behind a shock wave, with dissociation occurring for transitions from

the vibrational levels close to the dissociation limit. At higher temperatures, transitions between the different

vibrational levels of nitrogen become roughly equiprobable, and the overall range of bound vibrational levels

contributes to the dissociation.

Nomenclature

Ckij = transformation matrix

Cp = specific heat at constant pressure, J=kg=KCv = specific heat at constant volume, J=kg=KE = level energy, HzEm = Morse potential well, Jh = enthalpy, J=kgJs = Bessel functionkB = Boltzmann constant, 1:3806505 � 10�23 J=Kk�T� = thermal reaction rate, cm3=sM = Mach numberm = mass, kg~m = mass parameter, mABmC=�mAB �mC� or

mABmCD=�mAB �mCD�P = probabilityr = internuclear distance, mSVT = vibration-translation steric factor, 4=9SVV = vibration-vibration steric factor, 1=27T = macroscopic temperature, KTr = rotational temperature, KTtr = translational temperature, KTtr-r = translational-rotational temperature, KTv = vibrational temperature, Kt = time, sV�r� = intermolecular potential, JV-T = vibration-translation processesV-V-T = vibration-vibration-translation processesv = vibrational levelv = velocity, m=s�v = averaged collision velocity, m=sZ = gas-kinetic collisional frequency, Hz� = repulsive potential parameter, m�1

� = heat capacity ration, Cp=Cv

� = mass parameter, mA=�mA �mB�" = two-state first-order V-T transition probability,

P�1! 0�� = mass parameter, mAmB=�mA �mB�� = two-state first-order V-V-T transition probability,

�4P�1; 0! 0; 1��1=2�� = generalized two-state first-order V-V-T transition

probability� = collision cross section, m2

! = vibrational transition frequency, Hz!e = harmonic oscillator energy, Hz!exe = first-order anharmonic oscillator energy, Hz

Subscripts

f = final vibrational quantum numberi = initial vibrational quantum numbermax = maximum vibrational level before dissociationqbound = vibrational level above the dissociation limittr = translational modevib = vibrational mode0 = preshock1 = postshock

I. Introduction

S PECIAL focus is currently being brought to high-temperaturekinetic phenomena behind high-speed shock-waves. Advances

in the qualitative and quantitative understanding of such postshockphenomena [1–4] are being driven by the definition of interplanetarymissions involving the entry (or reentry) of a spacecraft in a planetaryatmosphere. Maneuvers such as planetary aerobraking, aerocapture,or direct entry of a spacecraft inbound from another planet followhyperbolic trajectories where crossing of the planetary atmosphereoccurs at velocities well in excess of 10 km=s. For example, a directentry in Earth atmosphere from planet Mars occurs at 11 km=s(M� 44). Comparatively, a Space Shuttle entry from Earth’s orbitoccurs at most at 7 km=s (M� 28) [5].

The well-known Rankine–Hugoniot shock relations allow thedetermination of the postshock translational temperature T1

according to the equation

Received 22 March 2006; revision received 17 May 2006; accepted forpublication 18 May 2006. Copyright © 2006 by the American Institute ofAeronautics and Astronautics, Inc. All rights reserved. Copies of this papermay be made for personal or internal use, on condition that the copier pay the$10.00 per-copy fee to the Copyright Clearance Center, Inc., 222 RosewoodDrive, Danvers, MA 01923; include the code $10.00 in correspondence withthe CCC.

∗Researcher, Centro de Física dos Plasmas, Av. Rovisco Pais;[email protected]. Member AIAA.

†Professor, Centro de Física dos Plasmas, Av. Rovisco Pais.

JOURNAL OF THERMOPHYSICS AND HEAT TRANSFERVol. 21, No. 1, January–March 2007

40

T1

T0

� �2�M2 � �� � 1���2� �� � 1�M2�

�� � 1�2M (1)

with T0 denoting the preshock temperature and � � Cp=Cv.In diatomic gases, some relaxation to the rotational and vibrational

modes is immediately established behind the shock wave, loweringthe translational temperature. However, if the shock wave isconsidered as a discontinuity (continuum flow regime), thetranslational temperature obtained immediately behind the shockwave corresponds to the value determined using Eq. (1). In thehypersonic limit, all the translational energy of the flow can beconsidered to be converted to its internal modes: the coherent kineticenergy of the flow particles is firstly transferred to the thermalagitation mode defined by the translational temperature for aMaxwellian velocity distribution function of the particles, andlatterly to the rotational and vibrational modes of the diatomicmolecules, defined by the temperatures Tr and Tv, respectively, for aBoltzmann distribution of such levels populations. In such limitingcase, the calculation of the postshock translational temperatureproceeds very simply:

1

2mv20 �

5

2kB�Ttr�1 � akB�Ttr-r�1 , �Ttr�1 �

mv20�5� 2a�kB

(2)

where a is a constant set to 1 if instantaneous equilibration of therotational temperature �Tr�1 with the translational temperature �Ttr�1is considered, and 0 if the rotational temperature �Tr�1 is consideredto remain at its preshock value �Tr�0 � �Ttr�0.

It is easy to conclude that the understanding of the physical-chemical processes behind hyperbolic shock waves requires thedevelopment of theoretical models valid at very high translationaltemperatures. Applying Eq. (2) (with a� 1) to the aforementionedentry flight speeds, one obtains a postshock translational temperatureof 60,000 K for a direct entry from planet Mars, and a translationaltemperature of 24,000 K for a Shuttle entry from orbit. In brief, thedevelopment of physical-chemicalmodels valid at such temperaturesacquires a particular relevance in the scope of programs such as theESA-sponsored AURORA program for the exploration of the solarsystem.

For all practical purposes, equilibration of the translational androtational modes of the flow molecules can be usually considered asinstantaneous behind a shock wave. Excitation of the molecularvibrational modes (V-T processes) occurs more slowly, and in verystrong nonequilibrium (non-Boltzmann) conditions. Dissociationreactions follow the excitation of the molecular vibrational modes,and are latterly followed by ionization reactions which bring the flowto a plasma state where electron-impact processes become dominant[6].

An adequate description of such excitation processes requires thedefinition of the so-called state-to-state models, where a descriptionof the energy exchanges between the different vibrational levels ofthe flow molecules and their translational energy is developed.

Previous works on this issue have typically resorted to simplerapproaches derived from other fields such as gas discharges [7–9]. Itis not until recently that it has been acknowledged that the specificconditions encountered behind strong shock waves requireddeveloping and usingmore elaborate theoretical approaches [10,11].

This work presents the development of a state-to-state model forthe description of the vibrational excitation and dissociationprocesses behind very high-speed shock waves. A numerical modelhas been developed according to the requirements aforementioned(validity at very high translational temperatures), and has beenvalidated against experimental and othermodels’ data. Care has beenexerted in using the most precise data for the description of thedifferent molecular energy levels and their interactions, whileretaining an affordable computational cost. A database of ratecoefficients has been obtained for the simulation of postshocknitrogen flows (the major species encountered in Earth’s atmosphereentry flows), and is discussed in order to check the validity of themodel and the different assumptions applied in our work. The

different channels through which dissociation proceeds behind ashock wave are also investigated for several limiting cases.

II. Theoretical Models for the Predictionof V-T and V-V-T Rates

Populations of the molecular vibrational levels are controlled byvibration-translation processes in diatom-atom collisions:

AB�i� � C! AB�f� � C (3)

and by vibration-vibration-translation processes in diatom-diatomcollisions:

AB�i1� � CD�i2�! AB�f1� � CD�f2� (4)

where i and f represent the initial and final vibrational quantumnumbers for the AB molecule (index 1) and the CD molecule(index 2).

A. Basic Trends of the Models

The first-order approach for the simulation of such processes is thesemiclassical first-order perturbation theory (FOPT). Namely, acollinear collision model taking into account a repulsiveintermolecular potential is given by the Schwartz, Slawsky, andHerzfeld (SSH) theory [12,13] and its extensions [14–20]. Thistheory is capable to simulate single-jump transition probabilities inconditions where these are much smaller than unity. This is the casefor the simulation of state-to-state processes in gas discharges wherethis theory can be successfully applied [21].

For high-energy flows, where high collision velocities areattained, V-T and V-V-T transition probabilities, includingmultiquantum transitions, become large, preventing them frombeing correctly predicted by FOPT models. Moreover, at highcollision velocities, FOPT models predict unphysical transitionprobabilities larger than unity for the higher vth levels [22,23].

More precise models include exact quantum models [24–27] andsemiclassical models such as the ones developed by Billing [22] andapplied to the simulation of molecular collisions [28–33]. Suchmodels allow the calculation ofmore accurate transition probabilitiesthan FOPTmodels but require a large amount of computer resources(namely for full quantum calculations), making them unpractical forthe systematic calculation of transition probabilities in diatomicgases.

Finally a semiclassical nonperturbative analytic method existswhich allows the calculation of V-T and V-V-T transitionprobabilities for a harmonic oscillator acted upon by an externalexponential force [34–36]. Thismethod is called the forced harmonicoscillator (FHO) and provides a semiclassical nonperturbativeanalytical solution for V-T andV-V-T transition probabilities, whichcompares well with exact quantum methods and the quantum-classical trajectory (QCT) method developed by Billing [22]. Morerecently, Adamovich et al. have successfully applied this method tothe simulation of postshock flows, and extended its scope ofapplication to include 3-D collision trajectories and molecularrotation effects [10,23,37–41].

B. Overline of the FHO Model

This section summarizes the main expressions for the calculationof V-T and V-V-T transition probabilities in collinear atomic-diatomic and diatomic-diatomic collisions.

V-T transition probabilities for collinear atom-diatom nonreactivecollisions are given by Kerner [34] and Treanor [35]

P�i! f; "� � i!f!"i�f exp��"�����Xnr�0

��1�rr!�i � r�!�f � r�!"r

����2 (5)

with n�min�i; f�.V-V-T transition probabilities for collinear diatom-diatom

collisions are given‡ by Zelechow et al. [36]

‡Corrected from typographic errors

DA SILVA, GUERRA, AND LOUREIRO 41

P�i1; i2 ! f1; f2; "; �� �����Xng�1��1��i12�g�1�Ci12

g;i2�1Cf12g;f2�1

� "12�i12�f12�2g�2� exp��"=2�

�����������������������������������������������������������i12 � g� 1�!�f12 � g� 1�!

p� exp��i�f12 � g� 1���

�Xn�gl�0

��1�l�i12 � g� 1 � l�!�f12 � g� 1 � l�!l!"l

����2 (6)

with i12 � i1 � i2, f12 � f1 � f2, and n�min�i1 � i2 � 1; f1�f2 � 1�.

In these equations " and � are related to the two-state FOPTtransition probabilities, with "� PFOPT�1! 0� and �� �4PFOPT

�1; 0! 0; 1��1=2. Finally, Ckij is a transformation matrix calculated

according to the expressionx

Ckij

� 2�n=2k

i � 1

� ��1=2 kj � 1

� �1=2Xj�1

v�0��1�v k � i� 1

j � v � 1

� �i � 1

v

� �(7)

For a purely repulsive intermolecular potential V�r� exp���r�,expressions for " and � are given by Zelechow et al. [36]

"� 8�3!� ~m2=���2

�2hsinh�2

��!

� �v

�(8)

�� 2� ~m2=���2� �v=! (9)

whereas for a Morse intermolecular potential V�r� Em�1 � exp���r��2, the expression for " is given by Cottrell and Ream [19]

"� 8�3!� ~m2=���2

�2h

cosh2f��1� ���!�=� �vgsinh2�2�!=� �v�

�� �2=��tan�1�������������������������2Em= ~m �v2�

p (10)

with an expression for � identical to Eq. (9). Here Em represents thepotential well,! denotes the oscillator frequency, and�, �, and ~m aremass parameters [23,38].

C. Improvements to the FHO Model

To allow a successful application of the FHO model to theprediction of transition probabilities, several improvements need tobe brought to the aforementioned expressions. These havepreviously been discussed by Adamovich et al. [23,38], and theyhave been considered during the development of our model. In short,these include the following:

1) Symmetrization of the collision velocity to enforce detailedbalance (a median collision velocity �v� �vi � vf�=2 is considered).

2) Accounting for the anharmonicity of the oscillator potentialcurve using an average frequency !� j�Ei � Ef�=�i � f�j if i ≠ f,and !� jEi�1 � Eij if i� f.

3) Generalization of the model for nonresonant V-V-T transitionsand V-V-T transitions between different species, by replacing�! ��= sinh���, with �� �2�!1 � !2�=4� �v

4) Generalization of the FHO model to noncollinear collisions(general case) through themultiplication of the parameters " and � bysteric factors such that "� "SVT and �� �

��������SVV

p, using the values

SVT � 4=9 and SVV � 1=27, as proposed by Adamovich et al.[23,38].

An additional improvement to the model is proposed in this paper,concerning the calculation of the energies of vibrational levels whichare usually carried according a polynomial expansion of the type

Ei;f � !e

�v� 1

2

�� !exe

�v� 1

2

�2

(11)

where !e and !exe are spectroscopic constants obtained in theliterature for different molecular electronic levels.

It is well known that this expression cannot be accurately appliedto the calculation of vibrational level energies close and above thedissociation limit. Therefore, a more accurate calculation of thevibrational level energies is carried through the reconstruction ofpotential curves according to the Rydberg–Klynning–Rees (RKR)method, and the resolution of the radial Schrödinger equation for thispotential curve, as described in another work [42]. The predictedmaximum vibrational level of N2 corresponds in this case to vmax �59 instead of vmax � 45 predicted when the polynomial expansion ofEq. (11) is used. Figure 1 depicts the differences between thevibrational levels energies calculated using polynomial expansionsor the RKR method. Differences in the levels’ energies becomeapparent for v > 30. As it will be discussed more in followingsections, the application of this method has a considerable impact onthe prediction of the V-T and V-V-T rates through the FHO model.

D. Scope and Validation of the FHO Model

The FHO model described in this paper, remaining based on asimplified collisionmodel, cannot be straightforwardly applied to thesimulation of any collisonal process. As the model does not accountfor molecular rotational motion, it cannot be directly applied tomolecules with low reduced masses such as hydrogen molecules, inwhich vibration-rotation effects are important. Also, the modelcannot predict reactive collisions or collisions involving non-adiabatic electronic transitions, such as NO-NO collisions. Also,multipole-multipole attractive forces (only important at lowertemperatures) are not considered here, but could be included throughthe collision parameters " and �, calculated according to a Lennard–Jones potential [38].

Experimental measurements of state-to-state rate coefficientsremain scarce and limited to low temperatures and lower quantumnumbers [43–47]. The validation of the FHOmethod has therefore tobe carried against very precise models of molecular collisions.Among these, the results from the QCT method developed byBilling, and applied to the description of N2-N2 [29], N2-N [48,49],N2-O2 [31], and O2-O2 [30] collisions, have been selected here forcomparison and validation of the results provided by the FHOmodel.

Reaction rates have been determined in the usual way, consideringa one-dimensionnal Maxwellian distribution of the particles foraveraging of transition probabilities P� �v� [Eqs. (5) and (6)], andmultiplying them by the gas-kinetic collision frequency:

0 20 40 60 80 1000

1

2

3

4

5

6

7

8

9

10x 10

4

PolynomRKR

Dissociation Limit

Vibrational Level

Ene

rgy

(cm

−1 )

Fig. 1 Calculated vibrational level energies for the ground state of N2.

xAlso corrected from typographic errors

42 DA SILVA, GUERRA, AND LOUREIRO

k�T� � Z

�~m

kBT

�Z �10

P� �v� exp�� ~mv2

2kBT

�v dv; with

Z� �

�����������8kBT

� ~m

r (12)

The compiled data used in the determination of the ratecoefficients for the different collision pairs (collisional cross sectionsand Morse intermolecular potentials) are summarized in Table 1.

The comparisons that were carried against the different QCTreaction rates proposed byBilling reproduced very closely the resultsobtained by Adamovich et al. [23,38]. Here, this comparison isextended by presenting results obtained from the FHO model up to100,000 K, because such high values may be attained in certainconditions immediately behind the shock wave.

Reaction rate coefficients have been calculated for N2-N2 V-Ttransitions up to 100,000 K, and compared with the QCT ratesdetermined byBilling. Also, to illustrate the inability of FOPT theoryfor the calculation of reaction rates at high temperatures, FOPT ratecoefficients have been determined for the N2-N2 V-T transition20! 19. The obtained results are displayed in Fig. 2. The gas-kinetic collision rate was also represented to assert if the differentmodels remain below this limit.

As expected, a good agreement is obtained between the predictedrates according to FHO model and the calculations of Billing [29].This agreement is remarkably good at lower transition quantumnumbers (V-T transition 1! 0). Also, it is verified that reaction ratespredicted by the FHO model remain lower than the gas-kinetic rate,even at very high translational temperatures. This allows having agood confidence in the model’s predictive capabilities, for a largerange of temperatures. It is verified as well that near the high-temperature limit, the reaction rates tend to an asymptotic value. Thisis a trend that occurs for the generality of the predicted FHO rates athigh temperatures. In contrast, although good agreement is verified atlower temperatures, it is verified that the FOPT model predicts ratesthat quickly start diverging from the FHO rates, roughly aboveT � 3000 K. At higher temperatures, a unphysical situation is even

achieved with the FOPT rates becoming larger than the gas-kineticrate. This is a well-known consequence of the failure of FOPT theoryat larger collision velocities [23]. The calculated transition rates alsofollow very closely the ones obtained by Adamovich et al. using apurely repulsive potential [23]. This is not surprising as the Morsepotential used for the calculation of N2-N2 transition probabilitieshas a very shallow potential well. This implies that the calculatedtransition probabilities will follow very closely the transitionsprobabilities obtained using a purely repulsive potential.

Figure 3 presents the comparison between predicted single-quantum, nonresonant V-V rates for different collision pairs. Onceagain, good agreement is reached between the FHO model andBilling’sQCTmodel forN2-N2 collisions, andwith the experimentalresults obtained by Taylor and Bitterman [52] for N2-O2 collisions.Interestingly enough, at sufficiently high temperatures, the reactionrates for a given transition become nearly equivalent, independentlyof the collision partners, if the same intermolecular potential isconsidered. This is of course a consequence of the vicinity of themolecular masses of N and O. This can also be verified in Fig. 3 forthe reaction rates of the V-V transition (1, 0! 0, 1) whenconsidering N2-N2 and N2-O2 collisions.

It has been stated by Adamovich et al. [38] that the FHO modelcannot successfully predict near-resonant V-V rates at lower

Table 1 Data used for the calculation of reaction rates

�, Å�1 Em, K Ref. �, Å2 Ref.

N2-N2 4 200 [38] 44 [50]N2-N 2.7 18,100 [48] 28 a

N2-O2 4 200 [38] 40 b

O2-O2 4 200 [38] 35 [51]

aThis work bAverage of N2-N2 and O2-O2 cross sections

102

103

104

105

10−18

10−17

10−16

10−15

10−14

10−13

10−12

10−11

10−10

10−9

10−8

Rea

ctio

n R

ate

(cm

3 /s)

Translational Temperature (K)

Fig. 2 Single-quantum V-T rates for N2-N2: solid line, FHO model; �,calculations of Billing [29]. V-T transitions 1 ! 0 and 20 ! 19displayedfrom bottom to top. Dashed line, FOPT rate for V-T transition 20 ! 19.Dotted line, gas-kinetic collision rate.

102

103

104

105

10−18

10−17

10−16

10−15

10−14

10−13

10−12

10−11

10−10

10−9

Rea

ctio

n R

ate

(cm

3 /s)

Translational Temperature (K)

N2−N

2 (0,1→1,0)

O2−N

2 (0,1→1,0)

N2−N

2 (1,19→0,20)

Fig. 3 Single-quantum V-V rates for N2-N2 (0, 1 ! 1, 0) and (0,

1 ! 20, 19) transitions and O2-N2 (0, 1 ! 1, 0) transitions. Solid and

dashed lines, FHO model. �, calculations of Billing [29] for N2-N2. �,interpolation of experimental data for N2-O2 (1, 0 ! 0, 1) [52].

11 12 13 14 15 16 17 18 19 20 21 22 23 24 2510

−18

10−17

10−16

10−15

10−14

10−13

10−12

10−11

10−10

Rea

ctio

n R

ate

(cm

3 /s)

vth Vibrational Level

T=1000 K

T=5000 K

T=10000 K

T=100000 K

T=300 K

T=500 K

T=1000 K

Fig. 4 Near-resonant V-V rates for N2-O2 (v� 1,0 ! v-1,1) tran-

sitions. Solid line, FHOmodel; dashed line with�, calculations of Billing[31].

DA SILVA, GUERRA, AND LOUREIRO 43

temperatures, due to the fact that this model considers any transitionas a succession of V-T transitions. These act as a bottleneck,compared to the direct resonance transition. This is indeed verifiedwhen the predictions of the FHO model are compared with thepredictions of Billing’s QCT calculations [31] for near-resonant N2-O2 V-V transitions. Figure 4 displays the reaction rates predicted byBilling and the ones predicted by the FHO model (the FHO modelreaction rates at 300 and 500 K, being several orders of magnitudelower, are not displayed here). It is verified that at highertemperatures (>5000 K), V-T processes become more efficient,eliminating this bottleneck, and the predicted FHO reaction ratesbecome much higher than the lower temperature rates predicted byBilling’s model.

Finally a comparison of the FHO model with QCT calculationsobtained byBilling [30] is carried out for the prediction ofO2-O2V-Trates. This comparison is presented in Fig. 5.

A good agreement is achieved between the two models except atlower temperatures where the reaction rates predicted by the FHOmodel are slightly lower than those predicted by Billing. This islikely due to the fact that Billing has accounted for quadrupole-quadrupole attractive interactions in the definition of its internuclearpotential. These interactions need to be accounted for at lowercollision velocities (lower temperatures), which would explain theobserved differences in the predicted rates, at temperatures below1000 K. This is not accounted for in our FHOmodel, which relies ona simpler Morse intermolecular potential.

III. Application to the Simulation of Postshock Flows

The suitability of the FHO model for the calculation of V-T andV-V-T transition probabilities has been inferred, and a database ofrate equations has been developed. It has been chosen to calculatereaction rates at translational temperatures from 100 to 100,000 Kthrough increments of 100 K. The upper limit of 100,000 K has beenjudged as sufficient to cope with the most extreme atmospheric entryflows. However, these rates can be easily extrapolated to highertemperature values, because they asymptotically tend to a uniquevalue lower than the gas-kinetic collision rate, roughly somewherefrom 50,000 to 100,000 K.

A. Challenges and Possible Simplifications for the Application

of the FHO Model

For the application of the FHO method to shock-heated flows, adatabase of reaction rates needs firstly to be built.

An initial issue arises when one has to consider multiquantumtransitions. As it will be verified more ahead in this paper, at hightranslational temperatures typical of a postshock flow (above

10,000 K), reaction rates for multiquantum transitions become ofequivalent magnitudes, and transitions between the overall system ofquantum states need to be taken into account. Taking only intoaccount the 60 vibrational bound levels of nitrogen, the simulation ofall the multiquantum V-T and V-V reaction rates [Eqs. (3) and (4)]results in 602 and 604 different transitions, respectively. Namely, fortheV-Vprocesses,more than 107 reaction rates need to be calculated.In practice, the need to calculate such a high number of reaction ratesprevents the full simulation of the overall V-T and V-V processesbehind a shock wave, to the exception of simpler 1-D geometries.Nevertheless, such simplified geometries still need large computingresources and the application of simplified expressions for thecalculation of reaction rates is needed [10].

An additional issue arises for the calculation of transitionsbetween higher vibrational levels. Equations (5) and (6) are poorlyconditioned, and the factorial terms cannot be exactly calculated forthese higher level transitions. Moreover, it can be easily seen thatoverflow and underflow situations to the usedmachine precision willeventually be reached for such transitions. Different approaches maybe devised for levelling this issue.

These two issues are discussed in detail in the next sections.

1. Asymptotic Transition Probabilities

Expressions of Eqs. (5) and (6) are rather cumbersome.Calculation of the V-T and V-V-T transition probabilities includes asummation of terms whichmay achieve a broad range of magnitudesnear the computational system underflow limit. Indeed, it is easy torecognize that the calculation of V-T transition probabilities betweentwo higher vibrational levels will result in a summation of steadilyincreasing values from near the underflow limit of the computersystem (calculation of the exp��"�jPr��1�r�r!�i � r�!�f � r�!"r��1j2 term).Moreover, this term is to bemultiplied to a termnear theoverflow limit of the computer system (calculation of the i!f!"i�f

term). Therefore, overflow and underflow exceptions are difficult toavoid, and even so, the multiplication of very large and very smallnumerical values will result in very poor precision for the obtainedresults (moreover, the factorial expressions can no longer becalculated exactly for higher numbers). For the expression of V-V-Trates [Eq. (6)], the same comments apply.

Preliminary calculations carried in MATLAB, which provides a64 bit calculation precision (equivalent to 2:23 � 10�308–1:80 �10308 numeric range), showed that for transitions between vibrationalquantum numbers typically larger than v� 20–40 (depending on theinteraction potential), accurate transition probabilities could nolonger be calculated (numerical noise, probabilities higher than 1,underflow, and overflow exceptions). Therefore, it is concluded thatnot even the increased precision ofMATLAB (64 bit digits instead ofthe usual 32–64 bits of languages such as C and FORTRAN) sufficesfor allowing accurate calculations to be carried out for highervibrational levels.

Nikitin andOsipov [53] have suggested asymptotical formulas forEqs. (5) and (6). For such approximations V-T and V-V-T transitionprobabilities may be rewritten asymptotically as

P�i! f; "� � J2s �2�������ns"p � (13)

for i, f s� ji � fj, and ns � �max�i; f�!min�i; f�!��s, andP�i1; i2 ! f1; f2; "; �� � J2s �2�n�1�s n�2�s �2�=4�1=2� (14)

for i1 � i2 � f1 � f2 and i1 � i2 � f1 � f2 s� ji1 � f1j.In Eqs. (13) and (14) Js stands for the Bessel function of the first

species and sth order.These expressions prove to be very useful in avoiding underflow

and overflow errors in the calculation of V-T and V-V-T transitionprobabilities, in addition to allowing faster calculation times.However, these asymptotic expressions are unable to fit the initialexpressions of Eqs. (5) and (6) at higher collision velocities [53]. Acomparison of Eq. (5) and (13) has been carried out for thedetermination of the V-T transition probability 5! 4 in a N2-N2

collision. Typical Maxwellian energy distribution functions (EDF)

102

103

104

105

10−18

10−17

10−16

10−15

10−14

10−13

10−12

10−11

10−10

10−9

10−8

Rea

ctio

n R

ate

(cm

3 /s)

Temperature (K)

Fig. 5 Single-quantum V-T rates for O2-O2. 1 ! 0 and 2 ! 1transitions displayed from bottom to top. Solid line, FHO model; �,calculations of Billing [30].

44 DA SILVA, GUERRA, AND LOUREIRO

ofN2 atTtr � 10; 000 and 100,000Khave also been determined. Theobtained results are presented in Fig. 6 against the colliding velocity.

It can be observed that for higher collision velocities (typicallyv > 10 km=s), the asymptotic expression proposed by Nikitin andOsipov is no longer valid. Interestingly enough, it is verified that theintegration of both expressions with maxwellian EDF’s give verysimilar predicted reaction rates, independently of the temperaturerange. For lower translational temperatures (� 10; 000 K), the EDFmainly overlaps the part where both models allow very close values.Although not valid at higher collision velocities, the transitionprobability predicted by Nikitin and Osipov’s expression has anequivalent area to the exact expression, and this results in similarpredicted rates. Therefore, for practical purposes, Nikitin andOsipov’s expressions can be usedwithout a sensible loss of accuracy.

Additional simplifications for Nikitin and Osipov’s transitionprobabilities have been proposed by Adamovich et al. [23,38]

J2s �2�������ns"p � � �ns�s

�s!�2 "s exp

��2ns"

s� 1

�(15)

J2s

h2�n�1�s n�2�s �2�=4

�1=2i�hn�1�s n�2�s

is

�s!�2 �2�4

!s

exp

�n�1�s n�2�s

s� 1

�2�4

!

(16)

These approximations work well for transitions involving smallquanta exchange. However, for larger quantum number transitions,

such expressions become unreliable, and the predicted transitionprobabilitiesmay even exceed unity, with important consequences inthe calculation of reaction rates at higher temperatures. An exampleis presented in Fig. 7 for a 15! 30 N2-N2 V-T collision.

In short, the motivations of our work being related to thesimulation of postshock flows at hyperbolic velocities, suchasymptotic expressions cannot be applied, as they would result indifferent predicted rate coefficients for the temperature range10,000–100,000 K. Instead, a greater accuracy is retained here whenusing Eqs. (5) and (6) for the calculation of V-T and V-V-Tprobabilities.

For this work, it has been chosen to devise a method allowing thenumerical implementation of the exact transition probabilities[Eqs. (5) and (6)]. The problem has been solved by using thesymbolic math toolbox included in MATLAB for an exactcalculation of the factorial factors in Eqs. (5) and (6), and thecalculation of the other parameters of the equations using variableprecision arithmetics. An accuracy of 32–64 digits has allowed oneto obtain rate coefficients for transitions between any vibrationallevel up to v� 100. This solution comes at a cost of largercalculation times (typically 30 min on a Pentium 4 at 3 GHz fortransitions between the higher vibrational levels). Owing to theextremely larger computational overhead, transition probabilitieswhere calculated using standard MATLAB with 64 bit numericalprecision for transitions between lower vibrational levels, andcompleted with variable precision arithmetics for transitions where64 bit arithmetics fail in providing accurate results.

2. Reduction of the Number of Calculated Rates

At very high translational energies with Etr Evib, such asbehind a strong shockwave, it has been verified thatV-V-Tprocessesoccur as two independent V-T processes such that the correspondingprobability is given by [37,38]

P�i1; i2 ! f1; f2; "; �� � P�i1 ! f1; "�P�i2 ! f2; "� (17)

Purely V-V exchange processes can therefore be neglected in thiscase and summing over all of the possible vibrational states of theCDmolecule can be performed. This hypothesis holds approximately forT 10; 000 K [23]. The FHO transition probability scaling is thenequivalent to the expression of Eq. (5) for molecule atom collisions

P�i1; all! f1; all; "; �� � P�i1 ! f1; "� (18)

B. Modeling of Dissociation Processes

State-specific dissociation rates according to the process

AB�i� �M! A� B�M (19)

may be determined using the FHO method, according to theapproach proposed and discussed byMacheret and Adamovich [40].The probability for dissociation can be calculated as the product ofthe transition probability to a quasi-boundk state such that v > n, withn� 59 denoting the last bound vibrational level, times theprobability of the subsequent decay of the energetic complex

P�i!; "� � P�i! vqbound; "�Pdecay (20)

with Pdecay 1. This assumption is not entirely justified when v ismuch higher than n, the formation of an intermediary quasi-boundstate being unlikely . However, for dissociation processes behind ashock wave with Etr Evib, occurring directly from the lowervibrational levels, this assumption provides a realistic approximationto the gas dissociation rates.

10−5

10−4

10−3

10−2

10−1

100

Pro

babi

lity

0 5 10 15 20 25 30

0.5

1

1.5

2

2.5x 10

−4

v (km/s)

10,000 K

100,000 K

Fig. 6 Exact (bold) and asymptotic probability (light) for a 5 ! 4 N2-

N2 V-T collision (upper figure) and Maxwellian velocity distribution

functions at 10,000 and 100,000 K (lower figure).

0 5 10 15 20 25 3010

−5

10−4

10−3

10−2

10−1

100

Pro

babi

lity

v (km/s)

103

104

105

10−20

10−19

10−18

10−17

10−16

10−15

10−14

Rea

ctio

n R

ate

(cm

3 /s)

Translational Temperature (K)

Fig. 7 Nikitin (light) and Adamovich (bold) asymptotic transitionprobabilities for a 15 ! 30 N2-N2 V-T collision as a function of the

colliding velocity (upper figure) and corresponding reaction rates

against the translational temperature (lower figure).

kThe concept of a quasi-bound state must be understood here as avibrational level above the dissociation limit, solely bound by the repulsivepart of the intramolecular potential.

DA SILVA, GUERRA, AND LOUREIRO 45

IV. Simulation of Dissociation Processesin High-Energy Nitrogen Shock Waves

The FHO model has been applied to the simplified simulation ofN2 dissociation processes behind high-energy shock waves.Nitrogen is the major constituent of Earth’s atmosphere, andtherefore the analysis of such dissociation processes has a clearrelevance for the prediction of high-speed hyperbolic entry flows inEarth.

A. Development of a Complete Database of Nitrogen V-T

and Dissociation Rates up to 100,000 K

A database of reaction rates has therefore been previouslydeveloped for V-T and V-V-T transitions in N2 molecules. It is now

necessary to determine how many quasi-bound states need to beconsidered for the simulation of high-temperature postshock flows.The more restrictive case obviously happens for the maximaltemperature of 100,000 K considered in our study. Here, a largeamount of translational energy is available, which allows thattransitions with large quantum jumps may occur. A preliminaryanalysis of the different predicted reaction rates at 100,000 K hasshowed that a maximum vibrational level v� 100 needs to beconsidered. Selecting a lesser number of vibrational levels wouldhave a nonnegligible impact on the overall dissociation processesbehind the shock wave, as transitions which may still considerablypopulate such higher levels would be neglected. On the other hand,reaction rates populating vibrational levels with v > 100 decreaseexponentially, even in the high-temperature limit, and therefore suchlevels can be safely disregarded in our model.

According to Sec. II, a full set of V-T rates has been determinedusing Eq. (18) for 100 levels ofN2. This results in a 61 � 101matrixin a 100–100,000 K temperature range (transitions between quasi-bound levels v� 59–100 are disregarded as dissociation of themolecule is considered to occur after a transition to a quasi-boundlevel). The predicted rates at 1000, 10,000, and 100,000 K arepresented in Fig. 8.

An analysis of thematrix of rate coefficients at lower temperatures(1000 K) shows a sharp decrease for multiquantum transitions,especially in the case of transitions from lower to upper levels. This awell-known trend, because at lower temperatures multiquantumtransitions may be safely disregarded in a state-to-state model.However, for rate coefficients at higher temperatures, outside thedomain of application of usual state-to-state models (>10; 000 K), itis verified that multiquantum transition rates become increasinglyimportant, and at the high-temperature limit for this study(100,000 K), a plateau is reached because transitions between anyvibrational level of N2 become equiprobable.

This last point has a major relevance for the simulation ofatmospheric entry flows, implying that the full matrix set of reactionrates between any level ofN2 needs to be taken into account, insteadof considering solely single-quantum transitions as it is usual inaerospace applications [54]. Unfortunately, this implies consideringamuch larger reaction rate set in the simulation of entry flows, whichmay be computationally unfeasible at the time.

Finally, an abrupt decrease of the reaction rates populating thevibrational levels v > 90 is observed, which validates ourassumption of considering a maximum quasibound level v equal to100 in our FHO model. Interestingly enough, the use of polynomialexpansions [Eq. (11)] for the calculation of vibrational level energies,instead of themore accurate RKRmethod, would have prevented thecalculation of level energies for v > 81, as the application of Eq. (11)using the usual spectroscopic constants of N2 results in an artificialplateau at v� 81. Furthermore, Eq. (11) also provides erroneousvalues for the level energies from sensibly v� 40 [42]. Thisrestriction has prevented higher quasi-bound levels to be consideredin other works using the FHOmodel [40]. Moreover, the accuracy ofthe calculated reaction rates for energy levels above v� 40 becomesquestionable, as it depends on poorly predicted energies.

B. Simulation of State-Resolved Dissociation Processes Behinda Strong Shock Wave

To evaluate the dissociation channels behind a shock wave, thedeveloped reaction rates sets have been applied to the simulation ofsimplified shock geometries. Here, a gas at an initial equilibriumtemperature of T � 195 K and at a density corresponding to analtitude of 76 km (conditions typical of an atmospheric entry [55]) isheated by a shock wave to a translational temperature of 1000,10,000, and 100,000K.Relaxation of the translational temperature isdisregarded behind the shock, which means that the translationalmode of the nitrogen molecules acts as an infinite energy reservoir,with different energy transfer rates (which depend on thetranslational temperature). This limiting case is useful for evaluatingthe behavior of the different V-T processes at different temperaturesretaining temperature specific reaction rates (see Fig. 8). Also, to

0 20 40 60 80 1000

20

40

60

−150

−100

−50

0

vi

vf

log(

Rea

ctio

n R

ate

(cm

3 /s))

0 20 40 60 80 1000

20

40

60

−60

−50

−40

−30

−20

−10

0

vi

vf

log(

Rea

ctio

n R

ate

(cm

3 /s))

0 20 40 60 80 1000

20

40

60

−40

−30

−20

−10

0

vi

vf

log(

Rea

ctio

n R

ate

(cm

3 /s))

Fig. 8 V-T reaction rates at 1000, 10,000, and 100,000 K, from top to

bottom.

46 DA SILVA, GUERRA, AND LOUREIRO

limit the scope of the study to the analysis of the dissociationchannels behind a shock wave, recombination processes aredisregarded. We note that these will only be important at lowertemperatures. State-resolved vibrational kinetics are simulated here,according to the usual system of master equations [10], and using theaforementioned rate coefficient database.

The obtained time-dependent vibrational distribution functions(VDF) are presented in Fig. 9 for three translational temperatures(once more 1000, 10,000, and 100,000 K). The populations of thequasi-bound levels (v� 59–100) are also presented to evaluate theirimportance in the overall dissociation rate (here we are consideringthat the population of such levels corresponds in practice to the

dissociation of the molecule). At 1000 K, the translationaltemperature is too low to induce noticeable dissociation of the flowmolecules, and the VDF tends to an equilibrium Boltzmanndistribution. At 10,000 K, the temperature is sufficiently high toallow the establishment of dissociation reactions. The higher levelsare progressively populated (without the occurrence of a plateau inthe population of the intermediary levels) until dissociation isprogressively established, ultimately leading to the depopulation ofthe overall bound levels (for t > 10�2 s). It is verified thatdissociation occurs primarily from the first quasi-bound levels closeto the dissociation limit, with a sharp decrease of dissociationprocesses from quasi-bound levels with v > 90. In the most severedissociation case at 100,000 K, population of the overall vibrationallevels occurs equiprobably, as expected according to theexamination of the reaction rates presented in Fig. 8. A plateau inthe population of the different vibrational levels is observed up tov� 90 where the population of the upper levels also abruptlydecreases, similarly to the case where T � 10; 000 K. Dissociationof the overall molecules proceeds very quickly in this limiting case(the flow is completely dissociated at t� 10�5 s).

Finally, the time evolution of the fractional molecular dissociationis displayed in Fig. 10, for different shock temperatures.

At higher translational temperatures (T > 50; 000 K), the timeincrease of the dissociated fraction of the flow exhibits a constantslope, which confirms that dissociation occurs equiprobably fromany vibrational level of the N2 molecule. At lower temperatures(T < 25; 000 K), a sharp increase in the dissociated fractions isobserved, which indicates the existence of a ladder-climbingphenomenon only noticeable at lower temperatures. This is typicallythe phenomenon that contributes for dissociation in other lower-temperature applications such as gas discharges [21], where onlysingle-quantum transitions are considered. Also the determinantinfluence of the shock temperature on the delay after which the flowis completely dissociated is clearly seen. At 100,000 K the flow iscompletely dissociated after roughly 1 �s, at 10,000 K the flow iscompletely dissociated after 1 s, and at shock temperatures roughlybelow 7000 K larger times are required to achieve completedissociation.

C. Thermal Dissociation Rates Predicted by the FHO Model

A further validation of the FHOmodel has been carried through acomparison with thermal dissociation rates proposed by differentauthors. In previousworks, Adamovich andMacheret have extendedthe FHO model to include three-dimensional and rotation effects foratom-diatom V-T processes [39], and for diatom-diatom V-T and V-V processes at moderate collision velocities [41]. Thermaldissociation rates have been obtained by the authors [40] andcompared to a good agreement with experimentally-determineddissociation rates for N2-N2 collisions. Here, we have further

0 20 40 60 80 10010

−120

10−100

10−80

10−60

10−40

10−20

100

1020

Vibrational Level

Num

ber

Den

sity

t=0

t=10−6t=1

t=5

t=106

0 20 40 60 80 10010

−15

10−10

10−5

100

105

1010

1015

Vibrational Level

Num

ber

Den

sity

t=0

t=10−15

t=10−10

t=10−6

t=10−4

t=10−2

t=1

0 20 40 60 80 10010

−15

10−10

10−5

100

105

1010

1015

Vibrational Level

Num

ber

Den

sity

t=0

t=10−15

t=10−10

t=10−5

t=1.5×10−4

t=10−3

25 of 32

Fig. 9 Time evolution of postshock N2 VDFs (Ttr � 1000, 10,000, and100,000 K from top to the bottom).

10−15

10−10

10−5

100

105

10−20

10−15

10−10

10−5

100

100 kK

50 kK

25 kK

10 kK

7.5 kK 5 kK 2.5 kK

Time (s)

Fra

ctio

n of

Dis

soci

ated

Mol

ecul

es

Fig. 10 Time evolution of N2 dissociation at different shock

temperatures.

DA SILVA, GUERRA, AND LOUREIRO 47

compared the thermal dissociation rates predicted by our FHOmodelwith such previously determined rates, as well as with experimentaldissociation rates proposed by Shatalov [56]. Such dissociation ratesare compared in Fig. 11.

Overall, it is verified that a good agreement is found between thedissociation rates predicted by the different models using the FHOapproach. The agreement with the experimentally determineddissociation rate is also adequate, although the rates predicted by theFHO models fall below this dissociation rate by 1–2 orders ofmagnitude. Comparing the rates predicted by the authors’ 1-D FHOmodel with the rates predicted by the 3-D model of Adamovich andMacheret, explicitly accounting for 3-D and rotational effects, resultsin about an order of magnitude increase of the predicted rates.However, at higher temperatures, the dissociation rates predicted bythe 1-D model increase more sharply than the dissociation ratespredicted by the 3-Dmodel. This is likely to result from the improvedRKR calculation of the vibrational levels energies, as applied in ourmodel. Accounting for 60 instead of 46 bound vibrational levels, aswell as considering a maximum vibrational level vmax � 100 insteadof vmax � 81 has been verified to increase the dissociation rates by atleast 1 order of magnitude.

V. Concluding Remarks

The forced harmonic oscillator theory has been shown to beadequate for the description of shock-induced dissociation processesduring an atmospheric entry. Once the practical difficultiesassociated with the numerical calculation of transition probabilitiesare copedwith using appropriate methods, the method can be used toyield an adequate and complete set of rate coefficients valid up tovery high temperatures. The agreement between the state-resolvedrates predicted by our model and other state-resolved rates isexcellent. The dissociation rates predicted by our model achieve anadequate agreement with experimentally determined rates althoughthe former fall 1–2 orders of magnitude lower.

One improvement that can be considered as having been broughtby the application of the forced harmonic oscillator theory for thesimulation of atmospheric entry shock waves is the availability ofreaction rates up to very high temperatures. Obviously, the obtainedrates can only be considered as tentative as the considered high-temperature range is beyond the common limits of experimentalvalidations and other dynamic calculations. However, the adequateagreement of the predicted rates at lower temperatures, as well as thephysical adequacy of the reaction rates at high temperatures (whichremain well below the kinetic collision rate), allows havingconfidence of the adequacy of this model for a tentative prediction ofvery high-temperature state-resolved reaction rates.

Furthermore it has been shown that at such higher temperatures,the collisional processes differ greatly from those seldomencountered at lower temperatures. It has been verified thatmultiquantum transitions become preponderant, and need to be takeninto account if one is to accurately simulate high-temperaturedissociation processes. Also, it has been verified that uncertainties onthe determination of the higher-lying vibrational levels energiessensibly affect the quality of the predicted reaction rates. TheRydberg–Klein–Reesmethod, which has been used in this work, canbe considered as a first improvement towards the determination ofthe higher vibrational levels close to the dissociation limit. Usingother accurate approaches could also bring some further insights onthis question.

In brief, the approach presented in this paper is a first step towardsthe development of a full collisional-radiative model for thesimulation of high-speed atmospheric entries. The state-resolvedrates presented in this work can be considered as a tentative but solidbasis where more elaborate descriptions can be developed, forexample, explicitly taking into account rotational effects, orinteractions between different molecular electronic levels.

Acknowledgments

The authors would like to thank I. V. Adamovich for fruitfuldiscussions about the FHO model, and for sending the source codesof his own FHO model, which were used for comparison purposes.

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104

105

10−22

10−20

10−18

10−16

10−14

10−12

10−10

10−8

10−6

Temperature (K)

Dis

soci

atio

n R

ate

(cm

3 /s)

Fig. 11 Thermal dissociation rates of nitrogen from N2-N2 collisions.Solid line, FHO model (this work); dashed line with +, 3-D FHO model,

impulsive approach [40]; dashed line with �, 3-D FHO model, free-

rotation approach [40]; dashed line with �; experimental rate [56].

48 DA SILVA, GUERRA, AND LOUREIRO

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