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Table 7:

Predictions of the line fluxes (after subtraction of the continuum) of the water lines observable with the Herschel spectrometer PACS.

PACS range 		  $X_{\rm in}$(H2O) = $2\times 10^{-6}$ $X_{\rm in}$(H2O) = $5\times 10^{-8}$  
Transition Wavelength Flux Flux Flux
  ($\mu $m) (10-12erg s-1 cm-2) (10-12erg s-1 cm-2) (10-12erg s-1 cm-2)
9 $_{3 6} \rightarrow $ 84 5 62.42 0.05 0  
9 $_{1 8} \rightarrow $ 90 9 62.93 0.4 0  
8 $_{1 8} \rightarrow $ 70 7 63.32 1.0 0.1  
6 $_{6 1} \rightarrow $ 65 2 63.91 0.2 0  
7 $_{6 1} \rightarrow $ 75 2 63.96 0.05 0  
6 $_{ 2 5} \rightarrow $ 51 4 65.17 1.7 0.5  
7 $_{1 6} \rightarrow $ 62 5 66.09 1.2 0.2  
3 $_{3 0} \rightarrow $ 22 1 66.44 2.5 1.6  
3 $_{ 3 1} \rightarrow $ 22 0 67.09 0.3 0.3  
3 $_{3 0} \rightarrow $ 30 3 67.27 2.0 0.5  
8 $_{2 7} \rightarrow $ 81 8 70.70 0.6 0  
5 $_{2 4} \rightarrow $ 41 3 71.07 0.03 0.03  
7 $_{0 7} \rightarrow $ 61 6 71.95 1.1 0.2  
7 $_{ 2 5} \rightarrow $ 63 4 74.95 0.6 0  
3 $_{ 2 1} \rightarrow $ 21 2 75.38 2.9 2.4 2.7 $\pm$ 1.0
6 $_{5 2} \rightarrow $ 64 3 75.83 0.3 0  
5 $_{5 0} \rightarrow $ 54 1 75.91 0.5 0  
7 $_{5 2} \rightarrow $ 74 3 77.76 0.2 0  
4 $_{ 2 3} \rightarrow $ 31 2 78.74 2.0 1.5  
9 $_{2 7} \rightarrow $ 91 8 81.41 0.10 0  
6 $_{1 6} \rightarrow $ 50 5 82.03 1.1 0.5  
8 $_{3 6} \rightarrow $ 82 7 82.98 0.2 0  
6 $_{0 6} \rightarrow $ 51 5 83.28 0.04 0.04  
7 $_{1 6} \rightarrow $ 70 7 84.77 0.8 0.1  
8 $_{ 4 5} \rightarrow $ 83 6 85.77 0.06 0  
3 $_{ 2 2} \rightarrow $ 21 1 89.99 0.5 0.5 0.5 $\pm$ 0.5
6 $_{ 4 3} \rightarrow $ 63 4 92.81 0.3 0  
6 $_{ 2 5} \rightarrow $ 61 6 94.64 0.7 0.2  
4 $_{4 1} \rightarrow $ 43 2 94.71 0.6 0.1  
5 $_{1 5} \rightarrow $ 40 4 95.63 0.3 0.3  
5 $_{4 1} \rightarrow $ 53 2 98.49 0.5 0  
5 $_{0 5} \rightarrow $ 41 4 99.49 1.3 1.1  
5 $_{1 4} \rightarrow $ 42 3 100.91 1.1 0.8 1.3 $\pm$ 0.6
2 $_{ 2 0} \rightarrow $ 11 1 100.98 0.8 0.8  
6 $_{ 3 4} \rightarrow $ 62 5 104.09 0.3 0  
2 $_{ 2 1} \rightarrow $ 11 0 108.07 2.2 2.1 1.7 $\pm$ 0.6
7 $_{ 4 3} \rightarrow $ 73 4 112.51 0.07 0  
4 $_{1 4} \rightarrow $ 30 3 113.54 1.5 1.3  
7 $_{ 3 4} \rightarrow $ 64 3 116.78 0.10 0  
4 $_{ 3 2} \rightarrow $ 42 3 121.72 0.4 0.2  
4 $_{0 4} \rightarrow $ 31 3 125.36 0.6 0.6  
3 $_{ 3 1} \rightarrow $ 32 2 126.71 0.1 0.1  
7 $_{ 2 5} \rightarrow $ 71 6 127.88 0.10 0  
4 $_{ 2 3} \rightarrow $ 41 4 132.41 0.7 0.6 0.7 $\pm$ 0.7
8 $_{3 6} \rightarrow $ 74 3 133.55 0.03 0  
5 $_{1 4} \rightarrow $ 50 5 134.94 0.5 0.3  
3 $_{3 0} \rightarrow $ 32 1 136.49 0.6 0.4  
3 $_{ 1 3} \rightarrow $ 20 2 138.53 0.9 0.9 0.9 $\pm$ 0.7
4 $_{ 1 3} \rightarrow $ 32 2 144.52 0.1 0.1  
3 $_{ 2 2} \rightarrow $ 31 3 156.20 0.2 0.2  
5 $_{ 2 3} \rightarrow $ 43 2 156.26 0.3 0.04  
5 $_{ 3 2} \rightarrow $ 52 3 160.51 0.1 0  
7 $_{ 3 4} \rightarrow $ 72 5 166.81 0.05 0  
3 $_{ 0 3} \rightarrow $ 21 2 174.62 1.2 1.2 2.5 $\pm$ 0.6
4 $_{ 3 2} \rightarrow $ 50 5 174.92 0.05 0  
2 $_{ 1 2} \rightarrow $ 10 1 179.53 1.4 1.4 2.9 $\pm$ 0.6
2 $_{ 2 1} \rightarrow $ 21 2 180.49 0.9 0.8 0.9 $\pm$ 0.4
4 $_{ 1 3} \rightarrow $ 40 4 187.11 0.05 0.05  

Notes. The third (fourth) column reports the predictions computed assuming that the inner H2O abundanceis equal to $2\times 10^{-6}$ ( $5\times 10^{-8}$) and the outer H2O abundance is $2.5\times 10^{-7}$, for the Shu-like model best-fit. The fifth column reports the observed ISO fluxes.


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