Table A.1
Rest frequenciesa (MHz) of para- and ortho-H2O+ ground state transitions from different sources.
Quantab | ALMAc | CDMS newc | CDMS oldd | Mürtz et al. (1998) e | ||||
|
||||||||
para-H2O+, 110−101, J = | ||||||||
|
||||||||
1.5−0.5 | 604 684 | .10 (76) | 604 682 | .66 (38) | 604 678 | .6 (25) | 604 758 | .7 |
1.5−1.5 | 607 225 | .79 (17) | 607 225 | .80 (17) | 607 227 | .3 (19) | 607 223 | .9 |
0.5−0.5 | 631 725 | .08 (42) | 631 724 | .98 (39) | 631 724 | .1 (37) | 631 773 | .0 |
0.5−1.5 | 634 266 | .44 (78) | 634 268 | .11 (39) | 634 272 | .9 (24) | 634 238 | .2 |
ortho-H2O+, 111−000, J = 1.5−0.5, F = | ||||||||
|
||||||||
1.5−0.5 | 1 115 155 | .98 (76) | 1 115 150 | .75 (85) | 1 115 150 | .3 | ||
0.5−0.5 | 1 115 191 | .40 (72) | 1 115 186 | .18 (81) | 1 115 186 | .0 | ||
2.5−1.5 | 1 115 209 | .33 (73) | 1 115 204 | .15 (82) | 1 115 204 | .0 | ||
1.5−1.5 | 1 115 268 | .08 (75) | 1 115 262 | .90 (82) | 1 115 263 | .0 | ||
0.5−1.5 | 1 115 303 | .50 (82) | 1 115 298 | .33 (87) | 1 115 298 | .7 | ||
ortho-H2O+, 111−000, J = 0.5−0.5, F = | ||||||||
|
||||||||
0.5−0.5 | 1 139 536 | .62 (96)f | 1 139 541 | .5 (10) | 1 139 541 | .1 | ||
1.5−0.5 | 1 139 555 | .79 (84)f | 1 139 560 | .6 (9) | 1 139 560 | .6 | ||
0.5−1.5 | 1 139 648 | .73 (85)f | 1 139 653 | .7 (9) | 1 139 653 | .5 | ||
1.5−1.5 | 1 139 667 | .89 (91)f | 1 139 672 | .7 (10) | 1 139 673 | .3 | ||
para-H2O+, 212−101, J = | ||||||||
|
||||||||
2.5−1.5 | 1 626 333 | .5 (13) | 1 626 324 | .6 (23) | 1 626 315 | .0 | ||
1.5−0.5 | 1 638 944 | .9 (12) | 1 638 934 | .8 (20) | 1 638 972 | .0 | ||
1.5−1.5 | 1 641 488 | .1 (12) | 1 641 483 | .6 (24) | 1 641 437 | .2 |
Notes.
Numbers in parentheses after the values refer to the uncertainties in units of the least significant figures.
Version 1, available, e.g., at http://www.astro.uni-koeln.de/site/vorhersagen/catalog/archive/H2O+/vers.1/.
Estimated uncertainties are about 1.8 MHz throughout (Mürtz et al. 1998).
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