klike_dcg00#fe7.dat
Resolved Specific Ion Data Collections
- Ion
- Fe7+
- Temperature Range
- 2.757 eV → 276 eV
ADF04
- Filename
- klike_dcg00#fe7.dat
- Full Path
- adf04/klike/klike_dcg00#fe7.dat
Download data
- Spontaneous Emission: Fe+7(i) → Fe+7(j) + hv
- Electron Impact Excitation: Fe+7(i) + e → Fe+7(j) + e
| 3p63d(2d) 2D1.5 | 0.0 cm-1 |
| 3p63d(2d) 2D2.5 | 1836.0 cm-1 |
| 3p53d2(4d) 4D0.5 | 385117.0 cm-1 |
| 3p53d2(4d) 4D1.5 | 386029.0 cm-1 |
| 3p53d2(4d) 4D2.5 | 387571.0 cm-1 |
| 3p53d2(4d) 4D3.5 | 389849.0 cm-1 |
| 3p53d2(4g) 4G5.5 | 408287.0 cm-1 |
| 3p53d2(4g) 4G4.5 | 409895.0 cm-1 |
| 3p53d2(4g) 4G3.5 | 411900.0 cm-1 |
| 3p53d2(4p) 4P2.5 | 412945.0 cm-1 |
| 3p53d2(4g) 4G2.5 | 414070.0 cm-1 |
| 3p53d2(4p) 4P1.5 | 415964.0 cm-1 |
| 3p53d2(4p) 4P0.5 | 418173.0 cm-1 |
| 3p53d2(4f) 4F1.5 | 424038.0 cm-1 |
| 3p53d2(4f) 4F2.5 | 425317.0 cm-1 |
| 3p53d2(4f) 4F4.5 | 425897.0 cm-1 |
| 3p53d2(4f) 4F3.5 | 426733.0 cm-1 |
| 3p53d2(2d) 2D2.5 | 430228.0 cm-1 |
| 3p53d2(2f) 2F2.5 | 431250.0 cm-1 |
| 3p53d2(2d) 2D1.5 | 432013.0 cm-1 |
| 3p64s(2s) 2S0.5 | 433540.0 cm-1 |
| 3p53d2(2f) 2F3.5 | 434555.0 cm-1 |
| 3p53d2(2p) 2P0.5 | 440344.0 cm-1 |
| 3p53d2(2p) 2P1.5 | 445806.0 cm-1 |
| 3p53d2(2h) 2H5.5 | 446481.0 cm-1 |
| 3p53d2(2f) 2F3.5 | 447658.0 cm-1 |
| 3p53d2(2g) 2G3.5 | 451232.0 cm-1 |
| 3p53d2(2g) 2G4.5 | 454098.0 cm-1 |
| 3p53d2(2h) 2H4.5 | 456493.0 cm-1 |
| 3p53d2(2f) 2F2.5 | 459367.0 cm-1 |
| 3p53d2(4d) 4D3.5 | 461691.0 cm-1 |
| 3p53d2(4d) 4D2.5 | 463050.0 cm-1 |
| 3p53d2(4d) 4D1.5 | 464977.0 cm-1 |
| 3p53d2(4d) 4D0.5 | 466839.0 cm-1 |
| 3p53d2(2d) 2D1.5 | 483828.0 cm-1 |
| 3p53d2(2d) 2D2.5 | 487784.0 cm-1 |
| 3p53d2(4s) 4S1.5 | 490366.0 cm-1 |
| 3p53d2(2s) 2S0.5 | 490369.0 cm-1 |
| 3p53d2(2g) 2G4.5 | 493551.0 cm-1 |
| 3p53d2(2g) 2G3.5 | 494249.0 cm-1 |
| 3p53d2(2p) 2P1.5 | 508518.0 cm-1 |
| 3p64p(2p) 2P0.5 | 510277.0 cm-1 |
| 3p64p(2p) 2P1.5 | 515550.0 cm-1 |
| 3p53d2(2p) 2P0.5 | 520822.0 cm-1 |
| 3p53d2(2f) 2F2.5 | 535909.0 cm-1 |
| 3p53d2(2f) 2F3.5 | 541755.0 cm-1 |
| 3p53d2(2p) 2P0.5 | 591964.0 cm-1 |
| 3p53d2(2p) 2P1.5 | 595152.0 cm-1 |
| 3p53d2(2d) 2D2.5 | 596463.0 cm-1 |
| 3p53d2(2d) 2D1.5 | 597065.0 cm-1 |
| 3p64d(2d) 2D1.5 | 667186.0 cm-1 |
| 3p64d(2d) 2D2.5 | 667602.0 cm-1 |
| 3p64f(2f) 2F2.5 | 763703.0 cm-1 |
| 3p64f(2f) 2F3.5 | 763799.0 cm-1 |
| 3p53d4s(4p) 4P0.5 | 826053.0 cm-1 |
| 3p53d4s(4p) 4P1.5 | 828470.0 cm-1 |
| 3p53d4s(4p) 4P2.5 | 833004.0 cm-1 |
| 3p53d4s(2p) 2P0.5 | 837661.0 cm-1 |
| 3p53d4s(2p) 2P1.5 | 842829.0 cm-1 |
| 3p53d4s(4f) 4F4.5 | 844999.0 cm-1 |
| 3p53d4s(4f) 4F3.5 | 847145.0 cm-1 |
| 3p53d4s(4f) 4F2.5 | 849899.0 cm-1 |
| 3p53d4s(4f) 4F1.5 | 852849.0 cm-1 |
| 3p53d4s(2f) 2F3.5 | 855100.0 cm-1 |
| 3p53d4s(2f) 2F2.5 | 860615.0 cm-1 |
| 3p53d4s(4d) 4D3.5 | 874711.0 cm-1 |
| 3p53d4s(4d) 4D2.5 | 876765.0 cm-1 |
| 3p53d4s(4d) 4D1.5 | 877476.0 cm-1 |
| 3p53d4s(4d) 4D0.5 | 878264.0 cm-1 |
| 3p53d4s(2d) 2D2.5 | 879021.0 cm-1 |
| 3p53d4s(2d) 2D1.5 | 881345.0 cm-1 |
| 3p53d4s(2f) 2F2.5 | 884331.0 cm-1 |
| 3p53d4s(2f) 2F3.5 | 887325.0 cm-1 |
| 3p53d4s(2d) 2D1.5 | 889113.0 cm-1 |
| 3p53d4s(2d) 2D2.5 | 890845.0 cm-1 |
| 3p53d4s(2p) 2P1.5 | 1032950.0 cm-1 |
| 3p53d4s(2p) 2P0.5 | 1032950.0 cm-1 |
------------------------------------------------------------------------------- See: Griffin D C, Pindzola M S and Badnell N R, 2000 Astron. Astrophys. Suppl. Ser. 142 217 for a more complete description. From an ICFT R-Matrix close-coupling calculation that included the 33 terms and the 77 levels of the configurations 3p63d, 3p53d2, 3p53d4s, 3p64s, 3p64p, 3p64d, and 3p64f in the close-coupling expansion. The 1s, 2s, 2p, 3s, 3p, and 3d orbitals were generated from a configuration-average Hartree-Fock (CAHF) calculation on 3p53d2, while the 4s orbital was generated from a CAHF calculation on 3p53d4s. Finally the 4p, 4d, and 4f orbitals were generated from CAHF calculations on 3p64p, 3p64d, and 3p64f, respectively. For the J = 0 to 12 even and odd parity JPI partial waves, we performed an R-Matrix calculation with exchange for the LSPI partial waves from L = 0 to L = 14 and then transformed the K-matrices to full intermediate coupling using the ICFT method. For the higher partial waves we performed a no-exchange LS R-Matrix calculation for L = 11 to 50 with the long-range perturbations turned on and with topup to generate JPI partial waves from J = 13 to J = 48. The continuum basis for these calculations was set to 27, the radius of the R-matrix box was 8.02 a.u., and the maximum energy used in the outer region part of the calculation was 600 eV. The level energies employed in the R-matrix calculation were not adjusted from their theoretical values. However, the energies listed above have been adjusted to their experimental values, where known. In addition, in order to keep the relative energies reasonable, we reduced the energies of the 3p53d4s 4P levels and 3p53d4s 4F9/2 level by the average difference between theory and experiment for the 3p53d4s 4F7/2, 3p53d4s 4F5/2, and 3p53d4s 4F3/2 levels. Finally, the highest two 3p53d4s 2P levels were adjusted down by the average energy difference between theory and experiment for all the other doublet terms of 3p53d4s. The majority of the radiative rates were generated from configuration-interaction calculations that included only the 5 even levels and the 72 odd levels that were included in the close-coupling expansion. However, the radiative rates for the strong transitions from the six highest levels of 3p53d2 2F, 2D, and 2F to the 3p63d ground levels and the levels of 3p64f to the ground levels were generated from extended configuration-interaction calculations. They included the five even levels that were in the initial calculation plus the levels of the configuration 3p43d3 that interact strongly with the 3p63d ground levels; and the 72 odd levels that were included in the initial calculation plus those levels of the configuration 3p33d4 that interact strongly with the levels of 3p53d2 2F, 2D, and 2F, and those levels of the configuration 3p43d24f that interact strongly with the levels of 3p64f. Finally, the radiative rates were also corrected for the energy adjustments discussed in the paragraph above. Donald C. Griffin May 18, 2000 ------------------------------------------------------------------------------- --------------------------------------------------------------------------------- ---------------------------------------------------------------------------------