SPECTRA, EMISSION YIELDS, CROSS SECTIONS, AND KINETIC ENERGY DISTRIBUTIONS OF HYDROGEN ATOMS FROM H2 X 1Σg+- d 3Πu EXCITATION BY ELECTRON IMPACT
被引:5
作者:
Liu, Xianming
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Space Environm Technol, Planetary & Space Sci Div, Pacific Palisades, CA 90272 USASpace Environm Technol, Planetary & Space Sci Div, Pacific Palisades, CA 90272 USA
Liu, Xianming
[1
]
Shemansky, Donald E.
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Space Environm Technol, Planetary & Space Sci Div, Pacific Palisades, CA 90272 USASpace Environm Technol, Planetary & Space Sci Div, Pacific Palisades, CA 90272 USA
Shemansky, Donald E.
[1
]
Yoshii, Jean
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Space Environm Technol, Planetary & Space Sci Div, Pacific Palisades, CA 90272 USASpace Environm Technol, Planetary & Space Sci Div, Pacific Palisades, CA 90272 USA
Yoshii, Jean
[1
]
Johnson, Paul V.
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CALTECH, Jet Prop Lab, 4800 Oak Grove Dr, Pasadena, CA 91109 USASpace Environm Technol, Planetary & Space Sci Div, Pacific Palisades, CA 90272 USA
Johnson, Paul V.
[2
]
Malone, Charles P.
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CALTECH, Jet Prop Lab, 4800 Oak Grove Dr, Pasadena, CA 91109 USASpace Environm Technol, Planetary & Space Sci Div, Pacific Palisades, CA 90272 USA
Malone, Charles P.
[2
]
Ajello, Joseph M.
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Univ Colorado, Lab Atmosphere & Space Phys, Boulder, CO 80303 USASpace Environm Technol, Planetary & Space Sci Div, Pacific Palisades, CA 90272 USA
Ajello, Joseph M.
[3
]
机构:
[1] Space Environm Technol, Planetary & Space Sci Div, Pacific Palisades, CA 90272 USA
[2] CALTECH, Jet Prop Lab, 4800 Oak Grove Dr, Pasadena, CA 91109 USA
[3] Univ Colorado, Lab Atmosphere & Space Phys, Boulder, CO 80303 USA
Electron-impact excitation of H2 triplet states plays an important role in the heating of outer planet upper thermospheres. The d (3)Pi(u) state is the third ungerade triplet state, and the d (3)Pi(u)-a (3)Sigma(+)(g) emission is the largest cascade channel for the a (3)Sigma(+)(g) state. Accurate energies of the d (3)Pi(-)(u)(v, J) levels are calculated from an ab initio potential energy curve. Radiative lifetimes of the d (3)Pi(u)(v, J) levels are obtained by an accurate evaluation of the d (3)Pi(u)-a (3)Sigma(+)(g) transition probabilities. The emission yields are determined from experimental lifetimes and calculated radiative lifetimes and are further verified by comparing experimental and synthetic d (3)Pi(u)-a (3)Sigma(+)(g) spectra at 20 eV impact energy. Spectral analysis revealed that multipolar components beyond the dipolar term are required to model the X (1)Sigma(+)(g)-d (3)Pi(u) excitation, and significant cascade excitation occurs at the d (3)Pi(u)(v = 0,1) levels. Kinetic energy (E-k) distributions of H atoms produced via predissociation of the d (3)Pi(u) state and the d (3)Pi(u)-a (3)Sigma(+)(g)-b (3)Sigma u(+) cascade dissociative emission are obtained. Predissociation of the d (3)Pi(u) state produces H atoms with an average E-k of 2.3 +/- 0.4 eV/atom, while the E-k distribution of the d (3)Pi(u)-a (3)Sigma(+)(g)-b (3)Sigma(+)(u) channel is similar to that of the X (1)Sigma(+)(g)-a (3)Sigma(+)(g)-b (3)Sigma(+)(u) channel and produces H(1s) atoms with an average E-k of 1.15 +/- 0.05 eV/atom. On average, each H-2 excited to the d (3)Pi(u) state in an H-2-dominated atmosphere deposits 3.3 +/- 0.4 eV into the atmosphere, while each H-2 directly excited to the a (3)Sigma(+)(g) state gives 2.2-2.3 eV to the atmosphere. The spectral distribution of the calculated a (3)Sigma(+)(g)-b (3)Sigma(+)(u) continuum emission due to the X (1)Sigma(+)(g)-d (3)Pi(u) excitation is significantly different from that of direct a (3)Sigma(+)(g) excitation.