Table 5
Line kinematic properties along lines of sight.
| Pointing | CO | [C II] | H I | [Ne III] | Hα | |||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| MAGMA | ALMA; 45′′ | ALMA; 14.4′′ | ||||||||||||
| v(a) | Δv(b) | v | Δv | v | Δv | v | Δv | v | Δv | v | Δv | v | Δv | |
| #1 | − 1.1 | 7.7 | ... | ... | ... | ... | − 0.6 | 10.1 | (0.9) | (27.9) | 2.3 | 22.9 | ... | ... |
| #2 | 5.3 | 6.6 | 4.7 | 5.0 | 5.2 | 5.2 | 5.4 | 6.6 | (− 5.2) | (37.3) | (11.1) | (34.8) | 6.0 | 39.4 |
| #3 | − 0.7 | 8.5 | 2.0 | 2.8 | 2.5 | 2.8 | (2.8) | (5.2) | (− 5.8) | (39.8) | 9.6 | 25.1 | 5.1 | 33.4 |
| #4 | − 0.5 | 7.0 | − 0.1 | 4.9 | − 0.4 | 5.1 | 1.1 | 6.9 | 0.6 | 38.9 | (7.4) | (37.4) | 3.3 | 42.0 |
| #5 | ... | ... | ... | ... | ... | ... | − 10.6 | 4.0 | − 11.3 | 15.9 | − 3.4 | 7.4 | − 9.7 | 12.4 |
| ... | ... | ... | ... | ... | ... | 5.7 | 7.0 | ... | ... | 17.1 | 7.4 | 11.6 | 30.6 | |
| #6 | 0.8 | 5.0 | ... | ... | ... | ... | 0.5 | 8.1 | (− 6.3) | (28.5) | 4.9 | 22.1 | − 0.1 | 32.5 |
| #7 | 0.8 | 5.0 | ... | ... | ... | ... | − 0.5 | 6.2 | (− 6.3) | (28.5) | 4.9 | 22.1 | − 0.1 | 32.5 |
| #8 | − 0.1 | 3.2 | ... | ... | ... | ... | − 1.1 | 8.6 | (− 3.6) | (22.7) | 6.6 | 23.1 | 1.1 | 32.6 |
| #9 | 0.1 | 4.3 | ... | ... | ... | ... | − 0.2 | 7.0 | − 4.1 | 20.2 | 6.6 | 23.1 | 1.1 | 32.6 |
| #10 | − 3.9 | 4.5 | ... | ... | ... | ... | − 4.2 | 4.6 | 1.4 | 23.7 | ... | ... | − 2.0 | 33.8 |
| #11 | − 1.9 | 7.5 | ... | ... | ... | ... | − 0.4 | 5.1 | − 1.0 | 21.4 | ... | ... | − 1.0 | 30.1 |
| #12 | − 1.1 | 6.1 | ... | ... | ... | ... | 0.0 | 5.4 | (0.8) | (20.1) | ... | ... | ... | ... |
Notes. All values are in km s−1. Values between parentheses indicate that the profile is not Gaussian (i.e., either asymmetric and/or multiple components). Only distinct components are considered. The larger FWHM observed for CO with MAGMA as compared to ALMA (45′′) is due to the low S/N of the former (Fig. 4). (a)Radial velocities in km s−1 offset from 280 km s−1. (b) Line FWHM in km s−1.
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