AIAA 2009-4257 41st AIAA Thermophysics Conference 22 - 25 June 2009, San Antonio, Texas Transport Properties of High-Temperature Jupiter-Atmosphere Components A. Laricchiuta, D. Bruno, C. Catalfamo, M. Capitelli, G. Colonna, O. De Pascale, P. Diomede, C. Gorse, S. Longo, F. Pirani and D. Giordano CNR-IMIP Bari, via Amendola 122/D 70125 Bari, Italy Dept Chemistry, University of Bari, via Orabona 4 70125 Bari, Italy Dept Chemistry, University of Perugia, via Elce di Sotto 8 06123 Perugia, Italy ESA-ESTEC, Aerothermodynamics Section, Noordwijk, the Netherlands The designing phase of components for vehicles used in the planetary exploration is assisted by the numerical simulation of critical entry conditions. In this framework reliable and consistent data sets are needed for transport coefficients of the atmospheric components and also of the species formed in the dissociation/ionization regime, during the vehicle impact. Jupiter atmosphere has been considered in this paper, moving to higher approximations of the Chapman-Enskog theory for the calculation of single-component and gas-mixture transport coefficients, considering equilibrium and non-equilibrium composition. To this aim existing transport cross section database for relevant interactions has been updated and extended to exotic species, proposing a phenomenological approach for the derivation of the corresponding elastic collision integrals in neutral-neutral and neutral-ion interactions. Inelastic collision integrals terms, due to resonant charge-exchange channels, have been also considered. I. Introduction uture missions for the exploration of the planet Jupiter will certainly presuppose hypersonic entries into F the atmosphere of that planet. The design of thermal protection systems (TPS) is assisted by the accurate knowledge of the high-temperature transport properties of the various components that constitute the gas mixture. A vehicle flying hypersonically through the atmosphere has a drastic impact on the composition, in fact main component (He/H2 ) undergo a number of processes (dissociation, ionization) leading to the appearance of new chemical species. The derivation of transport coefficients for such a complex gas-mixture + (He, He+ , He++ , H, H+ , H− , H2 , H+ 2 , H3 and electrons), in the frame of Chapman-Enskog theory, relies on the accurate description of the microscopic dynamics of binary collisions, in an appropriately extended temperature range. Different models of the Jovian atmosphere have been proposed1, 2 and attempt can be found in literature of creating a reliable database of transport cross sections.3, 4 The completion of an high-order (up to (`, s)=(4,4)) collision-integral database for Jupiter-components’ relevant interactions in an wide temperature range [50 to 50 000 K] is still a challenging issue. The study of the dynamics on a multi-potential surfaces, for many interactions, is hindered by the lack of electronic-structure information for the corresponding molecular states. In the present work a phenomenological approach, already validated in the case of Earth and Mars atmospheres,5 has been adopted. Effective odd-order collision integrals, resulting from both elastic and inelastic processes, have been estimated. In particular the resonant charge transfer process in atom-parent ion collision could be experimentally measured or derived in the framework of the asymptotic theory, considering also multiply charged ions. Transport coefficients for equilibrium and non-equilibrium compositions have been derived in the ChapmanEnskog third-order approximation (2nd-order for viscosity). The following values for the parameters that control the state of the plasma have been considered: 1 of 13 American Institute Aeronautics Copyright © 2009 by the American Institute of Aeronautics and Astronautics, Inc. All of rights reserved. and Astronautics • fixed 1 atm pressure • temperature varying in the range 50-50 000 K • parametric study with composition (the equilibrium plasma composition is fixed while the temperature is varied, allowing the analysis of strong non-equilibrium conditions). II. Collision integrals The collision integrals for the interaction between two colliding species (i,j) can be defined as follows6 (`,s) p (`,s) Ω̂i,j 2πν/KB T Ωi,j i h ` 1/2(s + 1)! 1 − 12 1+(−1) 1+` = (`,s)? πσRS Ωi,j = 4(` + 1) (s + 1)![2` + 1 − (−1)` ] = Z ∞ 2 (`) e−γ γ 2s+3 Qi,j dγ (1) 0 where γ 2 = µg 2 /2KB T , σRS is rigid sphere cross-section, Q(`) is the transport cross-section Z (`) ∞ Qi,j = 2π (1 − cos` (χ))b db = 2π 0 Z π (1 − cos` (χ))σ(g, χ) sin χ dχ (2) 0 σ is the elastic collision differential cross-section and χ is the deflection angle. II.A. Heavy particle interactions Collision integrals for neutral-neutral and ion-neutral interactions involving atomic and polyatomic species and multiply charged ions have been calculated by integration of the classical equation of motion,6 using a novel algorithm, recently implemented, that can handle any potential function regardless the number of extrema.7 The interaction potentials have been fitted with different analytical forms: • the Hulburt-Hirschfelder potential8 ϕ(r) = » „ «– » „ «– r r ϕ0 exp −2αHH −1 − 2 exp −αHH −1 re re „ «3 » „ «– » „ «–ff r r r +βHH −1 1 + γHH − 1 exp −2αHH −1 re re re (3) • the modified Morse potential9 ϕ(r) = ϕ0 [1 + exp (−βMM (r − re ))]2 − ϕ0 (4) βMM = β0 [1 + β1 (r − re ) + β2 (r − re )2 ] (5) ϕ(r) = ϕ0 exp (−ar − br2 − cr3 ) (6) • the modified repulsive potential10 • the inverse power potential11 ϕ(r) = d rδ 2 of 13 American Institute of Aeronautics and Astronautics (7) or modeled with the phenomenological potential12, 13 " ϕ = ϕ0 m n(x) − m „ «n(x) „ «m # n(x) 1 1 − x n(x) − m x (8) where x = r/re and n(x) = β + 4x2 . The phenomenological potential simulating the average interaction, allows the direct evaluation of collision integrals for unknown collisional systems. Potential features, such as the well depth, ϕ0 , and well position, re , can be derived, in the framework of a phenomenological approach, by correlation formulas given in terms of fundamental physical properties of involved interacting partners (polarizability α, charge, number of electrons effective in polarization).14–18 The validity of this approach was demonstrated in a paper19 by comparing, for some benchmark systems relevant to Earth atmosphere, results obtained using the model potential with those calculated with more accurate methods20–23 and applied to the Mars atmosphere.5 The m parameter depends on the interaction type (4 for ion-neutral and 6 for neutral-neutral interactions, respectively), while a simple empirical formula, based on polarizability of colliders, has been proposed19 for the estimation of β parameter, whose values range from 6 to 10 depending on the hardness of interacting electronic distribution densities. Reduced collision integrals Ω(`,s)? , calculated over a wide range of reduced temperatures, have been fitted as a function of β 24 through the expression ln Ω(`,s)? = [a1 (β) + a2 (β)x] +a5 (β) exp [(x − a3 (β))/a4 (β)] exp [(x − a3 (β))/a4 (β)] + exp [(a3 (β) − x)/a4 (β)] exp [(x − a6 (β))/a7 (β)] exp [(x − a6 (β))/a7 (β)] + exp [(a6 (β) − x)/a7 (β)] (9) where x = ln T ? = ln kT /ϕ0 and parameters ai are polynomial functions of β ai (β) = 2 X cj β j (10) j=0 Parameters entering eq. (10) are presented in Refs.5, 24 for neutral-ion (m=4) and neutral-neutral (m=6) interaction. H-H, H-H2 , H2 -H2 For these systems accurate collision integral calculations have been performed by Stallcop et al.25, 26 based on ab-initio potential energy surfaces, considering an angular averaged potential for anisotropic atomdiatom and diatom-diatom collisions. For H-H2 and H2 -H2 data have been tabulated up to T =20 000 K, therefore in the high-temperature region, dominated by the short-range interaction, collision integrals has been calculated by integration of a repulsive potential used in Ref.27 and based on experimental data. A full-range fitting expression (Eq. (11)), merging the low- and high-temperature data sets, has been used. The sigmoidal form is the same already used for the phenomenological case, though in this case the dimensional σ 2 Ω(`,s)? is obtained directly as a function of x = ln (T ). σ 2 Ω(`,s)? = [a1 (β) + a2 (β)x] +a5 (β) exp [(x − a3 (β))/a4 (β)] exp [(x − a3 (β))/a4 (β)] + exp [(a3 (β) − x)/a4 (β)] exp [(x − a6 (β))/a7 (β)] exp [(x − a6 (β))/a7 (β)] + exp [(a6 (β) − x)/a7 (β)] (11) Fitting coefficients ai are reported in Table 1. H-He, H- -He, H-He+ , He-He+ The existence of weakly bound states of H- -He molecular ion where the H-He neutral molecule itself is either unbound or barely bound has been theoretically investigated.28, 29 The interaction potentials, merging short-range repulsive and long-range weakly attractive ab-initio results by different authors,28–30 have been fitted with Hulburt-Hirschfleder functions. Optimized potential parameters are (ϕ0 = 6.14 10−4 eV, re = 3.524 Å, αHH = 6.2613, βHH = 3.6046, γHH = 0.8732) for the H-He system and (ϕ0 = 6.22 10−4 eV, re = 6.15 Å, αHH = 3.8, βHH = 7.9166, γHH = 3.2832) for H- -He. For the H-He+ interaction the Hulburt-Hirschfelder fitting of the accurate ab-initio potential by Aubreton4 has been considered (ϕ0 = 2.040 eV, re = 0.7743 Å, αHH = 2.1243, βHH = -0.3528, γHH = -1.7676) and collision integrals derived by integration. The accurate ab-initio potential energy curves for the gerade and ungerade electronic terms, arising in the He-He+ interaction, have been fitted by Hulburt-Hirschfelder potential in Eq. (3) (ϕ0 = 2.4730 eV, re = 1.081 Å, αHH = 3 of 13 American Institute of Aeronautics and Astronautics 2.23, βHH = 0.2205, γHH = 4.3890) and modified repulsive potential in Eq. (6) (ϕ0 = 359.0 eV, a = 4.184 Å−1 , b = -0.649 Å−2 , c = 0.08528 Å−3 ) in Ref.10 The effective collision integrals results from the usual averaging procedure σ 2 Ω(`,s)? = P n (`,s)? wn σ 2 Ωn P n wn (12) being wn the statistical weight of each electronic term. In Table 1 the fitting coefficients, ai , entering Eq. (11) are reported. Table 1. Fitting coefficients, entering eq. (11), for σ 2 Ω(`,s)? in heavy-particle interactions. (`, s) a1 a2 H-H26 (1,1) (1,2) (1,3) (1,4) (1,5) (2,2) (2,3) (2,4) (3,3) 15.09506044 14.14566908 13.39722075 12.97073246 12.69248000 22.08948804 17.94703897 18.78590499 13.82986524 -1.25710008 -1.17057105 -1.09886403 -1.06479185 -1.04857945 -1.85066626 -1.42488999 -1.59291967 -1.01454290 9.57839369 9.02830724 8.50097335 8.18885522 7.97861283 8.50932055 7.66669340 7.97734302 7.48970759 a3 -3.80371463 -3.00779776 -2.86025395 -2.78105132 -2.73621289 -7.66943974 -4.76239721 -5.66814860 -3.27628187 a4 0.98646613 0.74653903 0.85345727 0.89401865 0.90816787 0.77454531 1.26783524 1.01816360 2.08225623 a5 9.25705877 9.10299040 8.90666490 8.73403138 8.57840253 9.69545318 9.53716768 9.32328437 9.21388055 -0.93611707 -0.68184353 -0.67571329 -0.65658782 -0.63732002 -0.62104466 -0.73914215 -0.60882006 -1.32086596 H-H2 25 (1,1) (1,2) (1,3) (1,4) (1,5) (2,2) (2,3) (2,4) (3,3) 12.49063970 12.02124035 11.69204285 11.45792771 11.00483923 7.45048892 10.84507417 11.55088396 -15.25288758 -1.14704753 -1.19514025 -1.24240232 -1.29677120 -1.27212994 -1.43326160 -1.42859529 -1.41480945 -1.39293852 8.76515503 8.76515503 8.76515503 8.76515503 8.76515503 9.59201391 9.20889644 8.98739895 9.59147724 -3.52921496 -3.45192920 -3.49608019 -3.64478512 -3.51537463 -1.35066206 -1.29890434 -1.39880703 -1.62599901 0.32874932 0.45922882 0.63354264 0.85298582 0.85298582 7.15859874 3.37747184 2.32276221 28.71128123 12.77040465 12.77040465 12.77040465 12.77040465 12.77040465 9.88881724 9.83307970 9.89142509 9.68396961 -3.04802967 -2.29080329 -2.29080329 -2.29080329 -2.29080329 -1.39484886 -1.30321649 -1.26804718 -1.63186985 H2 -H2 26 (1,1) (1,2) (1,3) (1,4) (1,5) (2,2) (2,3) (2,4) (3,3) 24.00841090 23.02146328 21.17218602 20.05416161 19.06639058 27.54387526 26.22527642 24.59185702 24.57128293 -1.61027553 -1.70509850 -1.57714612 -1.51326919 -1.45577823 -1.98253166 -1.94538819 -1.83729737 -1.80855250 3.88885724 3.88885724 3.88885724 3.88885724 3.88885724 3.88885724 3.88885724 3.88885724 3.88885724 -8.89043396 -10.46929121 -9.72209606 -9.38278743 -9.14716131 -12.91940775 -13.40557645 -12.78050876 -11.86035430 0.44260972 0.36330166 0.59112956 0.70004430 0.81250655 0.34707960 0.40398208 0.62739891 0.36590658 8.88408687 8.26405726 8.15580488 8.00952510 7.85268967 8.72131306 8.42662474 8.27557505 8.38682707 -1.05402226 -1.02331842 -1.46063978 -1.57063623 -1.66995743 -0.88296275 -0.96878644 -1.33071440 -1.00746362 He-H28, 29 (1,1) (1,2) (1,3) (1,4) (1,5) (2,2) (2,3) (2,4) (3,3) 10.06955597 7.19869772 6.55743323 6.35904452 6.25347577 11.79267184 9.11713279 8.55265897 8.45675669 -0.78208832 -0.68092029 -0.71505725 -0.73482728 -0.74253418 -0.91854409 -0.82598144 -0.88142795 -0.74217526 8.90551185 9.54561159 9.75769768 9.66498209 9.51511012 9.46049069 10.00526403 10.32649048 9.61034137 -4.17119119 -3.73700195 -3.90437553 -4.00054192 -4.02417882 -4.15691291 -3.68708893 -3.83898513 -3.82155303 76.18192207 76.18192207 76.18192207 76.18192207 76.18192207 76.18192207 76.18192207 76.18192207 76.18192207 -2.53113293 -8.84268703 -11.7792635 -13.1043859 -13.6296726 -2.52045886 -10.9038647 -15.7314905 -8.95019085 -2.89309888 -7.48001507 -9.63359232 -10.4621344 -10.6948126 -2.67556855 -8.42960742 -11.8299368 -7.14064928 He-H- 28, 29 (1,1) (1,2) (1,3) (1,4) (1,5) (2,2) (2,3) (2,4) (3,3) 16.83383128 11.26280636 8.49517155 6.92882973 5.99889967 18.96022395 14.24553114 11.68946064 13.37723617 -1.40086033 -1.02780542 -0.88101058 -0.78943626 -0.73327723 -1.59117471 -1.27240767 -1.13472411 -1.18163311 9.03792344 9.48063008 9.91582728 10.13073161 10.17888281 9.72963354 9.96040497 10.21270634 9.67449296 -3.76712840 -2.93672204 -2.56415853 -2.45943130 -2.44506151 -3.60520521 -2.85245325 -2.43973469 -3.11159621 76.18192207 50.16628602 45.66368787 43.96165902 42.80471500 72.97489590 56.52153525 52.00801821 53.82204847 0.0128648 0.0128648 0.0128648 0.0128648 0.0128648 0.0128648 0.0128648 0.0128648 0.0128648 -2.87368310 -4.15375249 -4.89901464 -5.28289363 -5.47961017 -3.19508067 -4.18966597 -4.81326828 -4.03136340 4 of 13 American Institute of Aeronautics and Astronautics a5 a7 (`, s) a1 a2 a3 a4 a5 a5 a7 H-He+ 4 (1,1) (1,2) (1,3) (1,4) (1,5) (2,2) (2,3) (2,4) (3,3) 7.26019648 5.31621068 4.17730650 3.17455995 1.68374817 4.47457332 3.75792422 2.98401159 11.80660156 -0.45830355 -0.25198722 -0.13011997 -0.00742372 0.19151490 -0.22703750 -0.14961184 -0.06111433 -1.03306109 8.75289388 8.39297559 8.12931880 7.90685901 7.70176676 9.11487604 8.85486132 8.63912765 8.70928231 -1.05196080 -0.93572327 -0.85589802 -0.80603726 -0.76610507 -0.84002241 -0.77896426 -0.74591089 -1.32152742 7.88022406 8.72583156 9.22623392 9.70796087 10.49889283 13.68381322 13.27800873 13.14184555 7.24503625 5.84488923 5.65613996 5.50181035 5.34685366 5.20973048 4.46462878 4.46462878 4.46462878 4.46462878 -2.83633436 -2.63420758 -2.54217036 -2.47598237 -2.40196402 -3.36880863 -3.22466335 -3.11327610 -3.57325027 He-He+ 10 (1,1) (1,2) (1,3) (1,4) (1,5) (2,2) (2,3) (2,4) (3,3) 23.80276836 22.57798208 21.77686866 21.11384220 20.64796097 30.01038539 29.62345576 29.31400621 25.03330307 -1.53417198 -1.37458298 -1.29515584 -1.22362410 -1.18639584 -1.71614435 -1.80193239 -1.84347108 -1.29500767 7.14997977 6.71823986 6.44908263 6.23671845 6.07978682 5.80735212 5.65162107 5.48758712 6.24002334 -3.74339421 -3.53660052 -3.42650635 -3.33679994 -3.28123742 -4.49537445 -4.53517495 -4.55520888 -3.72851310 2.24179600 2.18797641 2.18797641 2.18797641 2.18797641 2.18797641 2.18797641 2.18797641 2.18797641 8.83793442 8.56245919 8.32964088 8.14201577 7.98030797 9.31326960 9.07520846 8.87814997 8.65029782 -0.99003900 -0.88202165 -0.88202165 -0.88202165 -0.88202165 -0.88202165 -0.88202165 -0.88202165 -0.88202165 He2+ -He, He2+ -H, He2+ -H2 Collision integrals for interactions involving the He2+ dication has been derived in the framework of a polarization model. The potential function ze2 αpol (13) 8πε0 r4 the polarizability of neutral collider, can be considered as a special case for the general ϕ(r) = − being z the ion charge and αpol σ 2 Ω(`,s)? ze2 αpol . 8πε0 In this case collision integrals assume a closed form11 r „ « 4(` + 1) dδ 2 (`) = A (δ) Γ s + 2 − (14) (s + 1)![2` + 1 − (−1)` ] kT δ inverse power potential in Eq. (7) with δ=4 and d = − where Γ is the Gamma function and A(`) is a temperature-free coefficient correlated to the transport cross section. The A` (4) values have been estimated by Smith31 for `=1, 2 and 3 in the 3 attractive case (A1 (4)=0.5523, A2 (4)=0.3846, A3 (4)=0.6377), leading to simple Table 2. Polarizability values [Å ] for Jupiter atmosphere species. relations r αpol 2 (1,1)? He 0.205 σ Ω = 424.443z T H2 0.81 H He+ HH+ 2 H+ 3 0.6668 0.03 27.0 0.424 0.4663 σ 2 Ω(1,2)? = 0.833 σ 2 Ω(1,1)? σ 2 Ω(2,2)? = 0.870 σ 2 Ω(1,1)? (1,3)? = 2 (1,1)? 0.729 σ Ω σ 2 Ω(2,3)? = 0.761 σ 2 Ω(1,1)? σ 2 Ω(1,4)? = 0.656 σ 2 Ω(1,1)? σ 2 Ω(2,4)? = 0.685 σ 2 Ω(1,1)? = 2 2 σ Ω 2 σ Ω (1,5)? (1,1)? 0.602 σ Ω σ 2 Ω(3,3)? = 0.842 σ 2 Ω(1,1)? (15) Polarizability values are reported in Table 2. H+ -H, H+ -H2 , H+ -He Accurate potential energy curves are available for the two electronic terms, 2 Σg and 2 Σu , 32 of the H+ correlating with H(2 S)-H+ , allowing the rigorous multi-potential procedure. The gerade term 2 system has been fitted with the Hulburt-Hirschfelder potential (Eq. (3) with parameters ϕ0 = 2.791 eV, re = 1.060 Å, αHH = 1.28, βHH = -0.5, γHH = -2.0) while the modified Morse potential proposed in Ref.33 (Eq. (4) with parameters ϕ0 = 3.018 eV, re = 1.058 Å, β0 = 1.3870 Å−1 , β1 = 0.0135, β2 = 0.0117) has been adopted for the ungerade state. The H+ -H2 and H+ -He systems have been studied by Krstic34, 35 within the frame of a quantum approach, obtaining accurate diffusive and viscosity transport cross–sections in the energy range [0.1-20 eV] and [0.1-100 eV], respectively. The derivation of collision integrals is straightforward by integration in Eq. (1), however the lower energy limit does not allow the σ 2 Ω(`,s)? estimation at low-temperatures. In order to estimate the transport cross sections, Q(`) , for E ≤0.1 eV the long-range potential for the H+ -He + has been described by a polarization model (Eq. (13)), while the potential surface for H+ 3 in the limit of H -H2 36 dissociation has been fitted with a Hulburt-Hirschfelder potential (ϕ0 = 4.78 eV, re = 0.73291 Å, αHH = 1.3767, βHH = -0.590, γHH = -1.653). The σ 2 Ω(3,3)? values, required by the adopted approximation in the Chapman-Enskog method, for H+ -H2 has been calculated by the Hulburt-Hirschfelder potential and in the case of H+ -He interaction has been set equal to σ 2 Ω(1,1)? . Collision integrals have been fitted by using the expression in Eq. (11) and ai coefficients given in Table 3. 5 of 13 American Institute of Aeronautics and Astronautics Table 3. Fitting coefficients, entering eq. (11), for σ 2 Ω(`,s)? in H+ -neutral interactions. (`, s) a1 a2 a4 a5 a5 a7 H+ -H (1,1) (1,2) (1,3) (1,4) (1,5) (2,2) (2,3) (2,4) (3,3) 46.68783791 46.68783791 46.68783791 46.68783791 46.68783791 46.68783791 46.68783791 46.68783791 46.68783791 -0.33303803 -0.33303803 -0.33303803 -0.33303803 -0.33303803 -0.33303803 -0.33303803 -0.33303803 -0.33303803 4.25686770 3.92217635 3.65740159 3.43102576 3.23079831 4.10212490 3.89701552 3.73496748 3.95678840 a3 -2.03851201 -2.00886829 -2.01434735 -2.04002032 -2.07543755 -1.85454858 -1.76267951 -1.69596577 -2.00381603 14.98170958 14.98170958 14.98170958 14.98170958 14.98170958 14.98170958 14.98170958 14.98170958 15.72150840 8.59618369 8.24501842 7.97534885 7.76086951 7.58613195 8.86285119 8.61913831 8.41234103 8.30656354 -1.65616736 -1.65616736 -1.65616736 -1.65616736 -1.65616736 -1.65616736 -1.65616736 -1.65616736 -1.79347178 H+ -H2 35 (1,1) (1,2) (1,3) (1,4) (1,5) (2,2) (2,3) (2,4) (3,3) 21.26444082 22.04614090 22.20902097 22.03893787 21.58227738 16.29263601 15.17470368 14.08165081 11.21674909 -1.66425043 -1.82881022 -1.90013155 -1.91163206 -1.87980396 -1.32780746 -1.24428548 -1.15372544 -0.56122635 9.43954208 9.15603332 8.91515513 8.70196666 8.51589918 10.00998032 9.70964984 9.48976675 9.08694827 -1.18521519 -1.09802478 -1.04865323 -1.02144928 -1.00037698 -0.70566506 -0.61129207 -0.58297710 -1.28700668 17.72506447 16.51669691 15.76252584 15.03274560 14.35787253 17.72506447 17.72506447 17.72506447 25.96742671 5.16010621 4.84818012 4.62340367 4.48334473 4.41475379 5.16010621 4.99747949 4.89671501 4.83728681 -2.45568134 -2.34842201 -2.26445563 -2.16080985 -2.05912196 -2.45568134 -2.45568134 -2.45568134 -2.37965195 H+ -He34 (1,1) (1,2) (1,3) (1,4) (1,5) (2,2) (2,3) (2,4) (3,3) 2.71952379 0.90687201 -1.51856588 -4.74037779 -7.26104273 -3.94194326 -5.23082562 -6.28592988 2.71952379 -0.04746783 0.18953042 0.53435861 1.00045484 1.37303488 0.73466954 0.92841556 1.09364996 -0.04746783 8.74213997 8.34680329 7.99486464 7.68664217 7.46364505 8.79837656 8.50739551 8.27457168 8.74213997 -0.88498112 -0.81094456 -0.78866372 -0.76331244 -0.72571710 -0.85969721 -0.83699163 -0.81943409 -0.88498112 91.77715465 67.45506771 53.68311327 45.61529587 41.33193035 76.18192207 63.85598616 56.74233232 91.77715465 2.49590845 2.84282065 3.16719614 3.46378279 3.63435585 2.86197842 3.05252604 3.16129013 2.49590845 -2.82208634 -2.68838648 -2.55404045 -2.42943739 -2.34213326 -2.85970495 -2.75743238 -2.68295935 -2.82208634 phenomenological interactions The phenome- Table 4. Parameters of phenomenological potential for nological approach has been adopted for the other interac- interactions relevant to Jupiter atmosphere. tions relevant to Jupiter atmosphere. Polarizability values β ϕ0 [meV] re [Å] m for jupiter species, taken from literature37–40 or estimated He-He 8.0 0.947 2.974 6 through an empirical formula41 as for H- , have been reHe-H2 9.29 1.865 3.189 6 ported in Table 2 and potential parameters for different He-H+ 9.73 30.664 2.574 4 2 interactions, needed for the used of bi-dimensional fit, pre9.66 29.471 2.606 4 He-H+ 3 sented in Table 4. H-H7.05 15.151 4.975 4 A special note is required in the case of He-He interH-H+ 8.00 73.104 2.769 4 2 action. The adopted parameter values, describing the po7.98 70.982 2.797 4 H-H+ 3 sition and the depth of the potential well and reported in H2 -H7.27 18.896 4.962 4 Table 4, have been taken from accurate theoretical results H2 -He+ 9.22 177.500 2.223 4 H2 -H+ 8.97 83.283 2.809 4 in literature.42, 43 A special comment is required for the 2 H2 -H+ 8.93 80.981 2.838 4 value assigned to the parameter β, in fact, in the general 3 approach, for hard interactions involving atoms of noble gases β is usually set approximately 9 or 10, but in the He-He case the phenomenological potential predicts a short-range interaction too repulsive and, by comparison with different potentials,44, 45 β = 8 has been chosen, giving accurate description of both short and long-range part of the interaction potential. II.B. Charge Transfer The contributions to odd-` terms of collision integrals coming from inelastic channels, i.e. the resonant charge transfer cross–section in atom-parent ion and molecule-molecular ion interactions has been also estimated and, following ref.,46 the actual collision integral for relevant interactions has been estimated through the relation q (`,s)? 2 (`,s)? ) + (Ωch-ex )2 ` = odd (16) Ω(`,s)? = (Ωel (`,s)? Ωch-ex , in this paper, have been evaluated by means of a closed formula, suggested by Devoto,47 for a linear dependency of the square root of charge transfer cross–section on collision velocity and then fitted with the following formula 6 of 13 American Institute of Aeronautics and Astronautics σ 2 Ω(`,s)? = d1 + d2 x + d3 x2 (17) where x = ln (T ). Table 5 reports fitting parameters for different systems, together with the references in literature for resonant charge exchange cross–sections. For atom-parent ion interactions experimental results have been considered.48, 49 The cross-section for the double charge transfer in He-He2+ collisions has been theoretically derived in Ref.50 In the case of H–H+ accurate charge-transfer cross sections have been obtained by Krstic34 by quantum 51 approach. H2 –H+ obtained by 2 interaction has been included, using resonant cross–sections by Yevseyev et al., extending the asymptotic theory to diatoms. For H-H interaction the experimental cross–sections by Huels49 have been used, that compares well with theoretical results obtained in the framework of the asymptotic theory52 and with a perturbed-stationary-states approach.53 (`,s)? Table 5. Fitting coefficients, entering eq. (17), for σ 2 Ωch−ex in neutral-ion interactions. (`, s) II.C. d3 (`, s) d1 d2 d3 He-He+ 48 (1,1) (1,2) (1,3) (1,4) (1,5) 38.6185 37.5764 36.8042 36.1948 35.6877 d1 -3.1289 -3.0869 -3.0551 -3.0302 -3.0085 d2 6.3410(-2) 6.3429(-2) 6.3424(-2) 6.3459(-2) 6.3422(-2) He-He2+ 50 (1,1) (1,2) (1,3) (1,4) (1,5) 12.1147 11.7937 11.5550 11.3658 11.2103 -0.9650 -0.9524 -0.9426 -0.9347 -0.9283 1.9236(-2) 1.9245(-2) 1.9229(-2) 1.9223(-2) 1.9218(-2) H-H- 49 (1,1) (1,2) (1,3) (1,4) (1,5) 363.2187 349.9484 340.1784 332.4694 326.1197 -39.8121 -39.0841 -38.5383 -38.1009 -37.7370 1.0922 1.0922 1.0922 1.0922 1.0922 51 H2 -H+ 2 (1,1) (1,2) (1,3) (1,4) (1,5) 38.2368 36.9454 35.9923 35.2418 34.6202 -3.8755 -3.8101 -3.7608 -3.7220 -3.6888 9.8299(-2) 9.8307(-2) 9.8299(-2) 9.8329(-2) 9.8306(-2) H-H+ 34 (1,1) (1,2) (1,3) (1,4) (1,5) 63.5437 61.8730 60.6364 59.6591 58.8493 -5.0093 -4.9431 -4.8936 -4.8544 -4.8213 9.8797(-2) 9.8766(-2) 9.8767(-2) 9.8785(-2) 9.8776(-2) Electron-molecule interactions Collision integrals for electron-neutral species interactions have been calculated by straightforward integration based on the corresponding transport cross–sections, Q` (E) as functions of electron energy. Electronic scattering from hydrogen atoms has been deeply investigated theoretically54, 55 finding an excellent agreement with absolute crossed-beam measurements.56, 57 The diffusion-type collision integral has been calculated here by integration of the momentum transfer cross section by Ref.,27 whereas the corrections Q(2) /Q(1) and Q(3) /Q(1) have been obtained by integrating the elastic differential cross sections by Ref.54 for the low energy range [0.582-30 eV] and by Ref.55 for energies above 50 eV. The momentum transfer cross section Q(1) for e-H2 interaction by Ref.58 has been integrated, including low (E < 0.01 eV) and high-energy (E > 25 eV) data by Biagi.59 The corrections to higher momentum transport cross sections, Q(2) /Q(1) and Q(3) /Q(1) , have been obtained by integrating the elastic differential cross sections by Refs.58, 60 For e-He interaction the momentum transfer and elastic cross sections were taken from Biagi59 and the Q2 /Q1 and Q3 /Q1 ratios were deduced from the known Q1 /Q0 by assuming a model angular dependence of the differential cross–section: 1 (1 − h(E) cos θ)2 (18) where h is here an adjustable parameter that depends on the electron energy, obtained from the Q1 /Q0 ratio. Electron-neutral interaction collision integrals have been fitted, as a function of x = ln (T ), using the following formula " „ «2 # g3 xg5 exp [(x − g1 )/g2 ] x − g7 σ 2 Ω(`,s)? = + g6 exp − + g4 (19) exp [(x − g1 )/g2 ] + exp [−(x − g1 )/g2 ] g8 Fitting coefficients gj , entering Eq. (19), are presented in Table 6, for relevant interaction in the Jupiter atmosphere. Concerning interactions between charged particles, corresponding collision integrals have been obtained assuming a screened Coulomb potential.61 7 of 13 American Institute of Aeronautics and Astronautics Table 6. Fitting coefficients, entering eq. (19), for σ 2 Ω(`,s)? in electron-neutral interactions. (`, s) g1 g2 e-He59 (1,1) (1,2) (1,3) (1,4) (1,5) (2,2) (2,3) (2,4) (3,3) 10.59136372(+00) 10.38275022(+00) 10.21366567(+00) 10.06183007(+00) 9.92613479(+00) 11.02594479(+00) 10.95544093(+00) 10.68567439(+00) 10.27636518(+00) -1.52697125(+00) -1.47464657(+00) -1.44621765(+00) -1.41920632(+00) -1.39377540(+00) -2.75226422(+00) -2.24065670(+00) -2.03462360(+00) -1.60869251(+00) 2.18892432(-02) 6.90741396(-02) 0.15768321(+00) 0.26516138(+00) 0.37258117(+00) 0.25837224(+00) 1.42500349(+00) 1.47732284(+00) 0.18373753(+00) -17.3791485(+00) -3.37723956(+00) -0.40718547(+00) -0.15710196(+00) -8.83214413(-02) -1.80065315(+00) -0.65562457(+00) -0.44873292(+00) -0.44953771(+00) e-H54, 55 (1,1) (1,2) (1,3) (1,4) (1,5) (2,2) (2,3) (2,4) (3,3) 10.35291134(+00) 10.09959930(+00) 9.84443341(+00) 9.65959253(+00) 9.50113220(+00) 10.33445440(+00) 10.08612484(+00) 9.89312188(+00) 9.99023294(+00) -1.58301162(+00) -1.50068352(+00) -1.42568830(+00) -1.38293428(+00) -1.36043711(+00) -1.44880911(+00) -1.39070408(+00) -1.34820033(+00) -1.41457896(+00) 12.45844036(+00) 12.54524872(+00) 12.97194554(+00) 13.18865311(+00) 13.23885240(+00) 12.08534341(+00) 12.39823810(+00) 12.63138071(+00) 12.53875975(+00) -0.23285190(+00) -7.29529868(-02) -9.24067489(-02) -6.34310879(-02) -4.44172748(-02) -1.86163984(-02) -3.26532858(-02) -1.96030794(-02) -2.82169003(-02) e-H2 58, 60 (1,1) (1,2) (1,3) (1,4) (1,5) (2,2) (2,3) (2,4) (3,3) 7.61552567(+00) 7.82045948(+00) 7.91713411(+00) 7.86089850(+00) 7.76607601(+00) 8.44904482(+00) 8.28235333(+00) 8.14899029(+00) 8.09697330(+00) -1.31152238(+00) -1.28509145(+00) -1.18533267(+00) -1.10926763(+00) -1.06076517(+00) -0.85941165(+00) -0.77764787(+00) -0.71893844(+00) -1.08367568(+00) 1.08767030(+00) 0.84661899(+00) 0.77902584(+00) 0.77235681(+00) 0.78630351(+00) 0.45608703(+00) 0.39162611(+00) 0.33943549(+00) 0.67651715(+00) -8.58478684(-02) 7.30252753(-03) 4.56053378(-02) 5.98096935(-02) 6.51985996(-02) -3.28370076(-02) 3.15214680(-02) 8.34297336(-02) 5.92335717(-02) (`, s) g6 g3 g4 g7 g8 g9 e-He59 (1,1) (1,2) (1,3) (1,4) (1,5) (2,2) (2,3) (2,4) (3,3) 1.99019765(+00) 1.54430366(+00) 1.22119154(+00) 1.01178482(+00) 0.87073597(+00) 1.11428478(+00) 0.31741278(+00) 0.25766199(+00) 1.13659747(+00) 19.13183426(+00) 36.06175647(+00) 36.06175647(+00) 36.06175647(+00) 36.06175647(+00) 36.06175647(+00) 36.06175647(+00) 36.06175647(+00) 36.06175647(+00) -3.87345716(+00) -115.629356(+00) -41.6895622(+00) -27.9895600(+00) -21.8337945(+00) -41.1176569(+00) -9.11869898(+00) -3.57516627(+00) -42.9018487(+00) 52.39042000(+00) 82.85050640(+00) 24.95446099(+00) 16.41208651(+00) 12.72530780(+00) 27.16469738(+00) 5.60148399(+00) 2.96346809(+00) 25.63994176(+00) e-H54, 55 (1,1) (1,2) (1,3) (1,4) (1,5) (2,2) (2,3) (2,4) (3,3) 5.36628573(-02) 4.37301268(-02) 2.32754987(-02) 1.11968653(-02) 7.88864536(-03) 3.30723152(-02) 1.75287406(-02) 4.55766915(-03) 2.70547916(-02) -5.34372929(+00) -5.73166847(+00) -5.71948057(+00) -5.77977010(+00) -5.83593794(+00) -6.45649277(+00) -6.48186913(+00) -6.50687636(+00) -6.11376507(+00) 9.35561752(+00) 9.09798179(+00) 8.83259870(+00) 8.64525855(+00) 8.49000000(+00) 9.15932646(+00) 8.90783546(+00) 8.71405704(+00) 8.89657156(+00) -2.15463427(+00) -2.13265127(+00) -2.05797013(+00) -2.02715634(+00) -2.01418763(+00) -2.13494419(+00) -2.08119318(+00) -2.04690115(+00) -2.09400530(+00) e-H2 58, 60 (1,1) (1,2) (1,3) (1,4) (1,5) (2,2) (2,3) (2,4) (3,3) 0.60307406(+00) 0.77338688(+00) 0.84160605(+00) 0.86441504(+00) 0.86956793(+00) 0.88418654(+00) 0.98366646(+00) 1.07846844(+00) 0.86030007(+00) 5.01125522(+00) 4.59038620(+00) 4.29393447(+00) 4.18795370(+00) 4.14851371(+00) 3.62672485(+00) 3.59756557(+00) 3.56463327(+00) 4.05861889(+00) 9.07403916(+00) 8.92912750(+00) 8.81056581(+00) 8.67601998(+00) 8.54553153(+00) 9.45483919(+00) 9.25577830(+00) 9.10019221(+00) 9.00694175(+00) 1.92416429(+00) 1.72315372(+00) 1.59949292(+00) 1.53347205(+00) 1.49396365(+00) 1.67160237(+00) 1.57423504(+00) 1.49404727(+00) 1.62336471(+00) 8 of 13 American Institute of Aeronautics and Astronautics III. Transport properties The collision integrals discussed in the previous section have been used to calculate the transport properties of Jupiter atmosphere. The calculation of the relevant coefficients entails the solution of systems of integro-differential equations. The coefficients are then expanded in a series of orthogonal Sonine polynomials and the series truncated at the desired order of approximation. The calculation thus reduces to the solution of systems of linear algebraic equations.62 The third Chapman-Enskog approximation has been used throughout in order to provide accurate results also in the ionization regime. Calculated transport coefficients include multicomponent diffusion coefficients (Dij ), thermal diffusion coefficients (DiT ), translational thermal conductivity (λ), viscosity (η) and electrical conductivity (λe ) coefficients.63 III.A. Single component and equilibrium H2 -He mixture transport coefficients VISCOSITY [104 kg m-1 s-1] 10.0 1.0 pure He 0.1 pure H2 pure H 0.0 102 103 104 105 TEMPERATURE [K] Figure 1. Viscosity for pure species (lines) compared with results by Biolsi1 (open markers) and by Hansen2 (closed markers). The mixture equilibrium compositions have been taken from.62 Pure gas transport coefficients are calculated for each of the three neutral species considered. These data provide reference values for those who wish to use approximate mixture rules in their CFD calculations. Singlecomponent viscosities are reported in figure 1 as a function of temperature and compared in different temperature ranges with two series of data in literature.1, 2 An excellent agreement is found with the only exception of the high-temperature coefficient for helium, attributable to differences in the adopted values of collision integrals for He-He interaction. In figures 2 and 3 the comparison is shown of viscosity and translational thermal conductivity for equilibrium Jupiter atmosphere at 1 atm pressure with results in refs.1, 2 Despite the good agreement in the low-temperature region, dominated by neutral interactions, increasing the temperature (T >10 000 K) differences are found where ionized species appear. This seems to give an indication of the relevance of the adopted Jupiter-atmosphere model with respect to the simplified 5-species-model adopted by Biolsi1 and to the calculations by Hansen,2 based on mixing rules. 100.0 TRANSLATIONAL THERMAL CONDUCTIVITY [W m-1 K-1] -1 -1 VISCOSITY [10 kg m s ] 10.0 4 1.0 0.1 0.0 101 10 2 3 10 4 10 10.0 1.0 0.1 0.0 101 5 102 10 103 104 105 TEMPERATURE [K] TEMPERATURE [K] Figure 2. Viscosity of equilibrium Jupiter atmosphere at 1 atm pressure compared with results by Biolsi1 (open circles) and by Hansen2 (open diamonds). Figure 3. Translational thermal conductivity (including electrons) of equilibrium Jupiter atmosphere at 1 atm pressure compared with results by Biolsi1 (open circles). 9 of 13 American Institute of Aeronautics and Astronautics III.B. Non-Equilibrium H2 -He mixture trans- port coefficients VISCOSITY [104 kg m-1 s-1] The investigation of non-equilibrium Table 7. Non-equilibrium compositions, cases ci conditions has been performed considering a frozen composition system ci species c1 c2 c3 c4 c5 and studying the temperature depenHe 2.0000(-01) 1.6094(-01) 9.4874(-02) 2.1026(-03) 7.6259(-05) dence of transport coefficients. The H2 8.0000(-01) 4.4846(-01) 8.8133(-06) 1.2473(-12) 1.1946(-15) chosen compositions, reported in taH 3.7016(-36) 3.9060(-01) 6.0956(-01) 6.3193(-03) 2.5981(-03) ble 7, correspond to equilibrium valHe+ 2.8943(-25) 5.0593(-06) 5.4128(-02) 2.4971(-02) He2+ 1.9669(-22) 4.2152(-06) 2.9125(-02) ues at fixed temperature, miming strong H+ 4.0107(-11) 4.7042(-06) 1.8852(-09) 3.7565(-11) non-equilibrium conditions and allowing 2 H+ 8.2049(-10) 1.2914(-11) 2.2508(-19) 1.5231(-23) an insight on the relative role of different 3 H+ 1.2420(-09) 1.4943(-01) 4.4356(-01) 4.3079(-01) species. Five different cases are considH1.0450(-11) 7.0068(-06) 2.6139(-09) 2.3248(-11) ered exploring extreme conditions from e2.0921(-09) 1.4944(-01) 4.9770(-01) 5.1401(-01) the c1 mixture, containing only neutral components H2 (80%) and He (20%) and corresponding to equilibrium composition at T =300 K, to the c5 illustrating the behavior of the completely ionized gas (T =50 000 K), passing through c2 , c3 , c4 intermediate cases, representing the equilibrium composition at T =3 500 K, 13 000 K, 30 000 K, respectively. Viscosity is controlled by the collisions between heavy particles. Therefore a decrease is expected with ionisation 101 degree because the electrons do not contribute and bec2 c1 cause the Coulomb cross-sections are larger, as shown in figure 4. In figure 5 the translational thermal conductivity c3 is shown as a function of temperature for different compo0 10 sitions. It is seen that the thermal conductivity increases equilibrium composition with the dissociation degree, while decreasing with the ionization degree. Also, the temperature dependence is much -1 stronger for the Coulomb interactions than for collisions c 10 4 involving neutral species. The electrical conductivity, in c5 figure 6, is essentially due to electron diffusion. Therefore, non negligible values are attained only if the electron component is present. The equilibrium case is reported in 10-2 0 100 1 104 2 104 3 104 4 104 5 104 each figure to emphasize the large discrepancies arising in TEMPERATURE [K] comparing the results obtained in this assumption. Figure 4. Viscosity as a function of temperature for strongly non-equilibrium conditions of Jupiter atmosphere, at 1 atm pressure, compared with equilibrium case (see table 7 for fixed ci compositions). ELECTRICAL CONDUCTIVITY [S m-1] TRANSLATIONAL THERMAL CONDUCTIVITY [W m-1 K-1] 35.0 30.0 c3 25.0 c5 c4 20.0 equilibrium composition 15.0 c2 10.0 5.0 0 100 c1 1 104 2 104 3 104 4 104 5 104 3.5 104 c4 3.0 104 c5 2.5 104 equilibrium composition 2.0 104 1.5 10 c3 4 1.0 104 5.0 103 0.0 100 1 104 TEMPERATURE [K] 2 104 3 104 4 104 5 104 TEMPERATURE [K] Figure 5. Translational thermal conductivity as a function of temperature for strongly non-equilibrium conditions of Jupiter atmosphere, at 1 atm pressure, compared with equilibrium case. Figure 6. Electrical conductivity as a function of temperature for strongly non-equilibrium conditions of Jupiter atmosphere, at 1 atm pressure, compared with equilibrium case. 10 of 13 American Institute of Aeronautics and Astronautics IV. Conclusion In this paper a considerable effort has been devoted to the construction of a reliable database of transport cross sections for interactions relevant to Jupiter atmosphere components. High-order collision integrals have been derived for neutral-neutral, neutral-ion and electron-neutral interactions in a wide temperature range [50-50,000 K]. Moreover suitable fitting formulas have been provided that could be easily implemented in existing numerical transport codes. Based on a new thermodynamic model, transport coefficients have been derived for pure neutral species (H2 , He and H), equilibrium and non-equilibrium Jupiter atmosphere compositions, emphasizing the relevance of the adopted model and extending the range of validity to very high temperatures. Acknowledgemets The present work has been partially supported by ESA (Project 17283/03/NL/PA) and by MIUR PRIN 2007 (2007H9S8SW 003). 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