szd02#li_li0.dat
Electron Impact Ionisation Coefficients
- Ion
- Li0+
- Temperature Range
- 0.150 eV → 1000 eV
- Li0(1s2 2s1 2S) + e → Li+(1s2 1S) + e + e
- Li0(1s2 2s1 2S) + e → Li+(1s1 2s1 3S) + e + e
- Li0(1s2 2p1 2P) + e → Li+(1s2 1S) + e + e
- Li0(1s2 3s1 2S) + e → Li+(1s2 1S) + e + e
- Li0(1s2 3p1 2P) + e → Li+(1s2 1S) + e + e
- Li0(1s2 3d1 2D) + e → Li+(1s2 1S) + e + e
---------------------------------------------------------------------------- ISEL INITIAL MET. DESIG. FINAL MET. DESIG. ION CODE ION CODE ---- ------- ---- ------------------- ------- ---- --------------- 1 Li+ 0 1 1s2 2s1(2S) Li+ 1 1 1s2(1S) 2 Li+ 0 1 1s2 2s1(2S) Li+ 1 2 1s1 2s1(3S) 3 Li+ 0 2 1s2 2p1(2P) Li+ 1 1 1s2(1S) 4 Li+ 0 3 1s2 3s1(2S) Li+ 1 1 1s2(1S) 5 Li+ 0 4 1s2 3p1(2P) Li+ 1 1 1s2(1S) 6 Li+ 0 5 1s2 3d1(2D) Li+ 1 1 1s2(1S) For the ground to ground rate (isel 1) the cross section was scaled to the time-dependent value calculated at Auburn and reported by Colgan et al (Phys. Rev. Lett. 87, 21320 (2001)). The ground to metastable (isel 2) calculated using configuration-average ionization cross sections, with semi-relativistic wavefunctions, using the relaxed-core approximation, the prior form for the scattering potentials, and the natural-phase approximation. They were then multiplied by the appropriate angular coefficients. All other rates from Bray reported by J Schweinzer et al (Atomic Data and Nucl. Data Tab. 72, p239 (1999)). For n=4 transitions use ECIP approximation. Data generated by Stuart Loch on 14-Jul-2002 ---------------------------------------------------------------------------- --------------------------------------------------------------------------------- ---------------------------------------------------------------------------------