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Table 3
Radial zones in which the water lines form.
Wavelength | Desig. | E up | A ij | R 15% | R 85% | ||
[μm] | [K] | [s-1] | [AU] | [AU] | |||
|
|||||||
o-H2O | |||||||
538.28 | 110−101 | 60.96 | 3.458(−3) | 35 | 160 | ||
180.49 | 221−212 | 194.1 | 3.058(−2) | 4 | 11 | ||
179.53 | 212−101 | 114.4 | 5.593(−2) | 5 | 110 | ||
78.74 | 423−312 | 432.2 | 4.838(−1) | 4 | 4.5 | ||
71.95 | 707−616 | 843.5 | 1.157 | 4 | 4.5 | ||
63.32 | 818−707 | 1071. | 1.751 | 4 | 4.5 | ||
|
|||||||
p-H2O | |||||||
269.27 | 111−000 | 53.43 | 1.842(−2) | 22 | 150 | ||
158.31 | 331−404 | 410.4 | 1.630(−4) | 4 | 4.5 | ||
144.52 | 413−322 | 396.4 | 3.316(−2) | 4 | 4.5 | ||
89.99 | 322−211 | 296.8 | 3.524(−1) | 4 | 5.5 | ||
78.93 | 615−524 | 781.1 | 4.526(−1) | 4 | 4.5 | ||
63.46 | 808−717 | 1070.6 | 1.742 | 4 | 4.5 |
Notes. Listed are the radii within which 15 and 85% of the line flux have built up (note that these values are calculated from the vertical escape probability approach).
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