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Table 5

IR luminosity, H2O line luminosity and global dust temperature of the entire sample.

Source H2O Transition LIR LH2O(211–202) LH2O(202–111) LH2O(321–312)
(1012L) (107L) (107L) (107L)

G09v1.97 211–202 , 321–312 22.1 ± 5.9 10.7 ± 1.4 15.0 ± 1.9
G12v2.43 202–111 , 321–312 83.2 ± 16.6 /μ 88.4 ± 10.7 /μ 143.2 ± 11.5 /μ
NCv1.143 211–202 , 321–312 11.4 ± 3.1 9.0 ± 1.4 18.9 ± 3.3
NAv1.195 202–111 , 321–312 18.0 ± 4.6 16.4 ± 3.0 < 12.3
NAv1.177 202–111 , 321–312 55.0 ± 11.0 /μ 82.0 ± 12.8 /μ 129.1 ± 10.8 /μ
NBv1.78 202–111 , 321–312 8.2 ± 2.2 9.4 ± 2.1 11.0 ± 1.5

G09v1.124-W 211–202 33.1 ± 3.2 < 12.9
G09v1.124-T 211–202 14.5 ± 1.8 < 6.9
G09v1.40 211–202 4.2 ± 1.3 3.7 ± 0.9
SDP11 202–111 5.7 ± 1.6 5.8 ± 1.4
NCv1.268 211–202 8.6 ± 2.3 11.5 ± 1.5
NAv1.56 211–202 9.7 ± 2.6 10.3 ± 1.2

SDP81 202–111 6.1 3.3
NAv1.144 211–202 11 9.7
SDP9 211–202 5.2 7.0
G12v2.30 202–111 16 13
SDP17b 202–111 16 20
G15v2.779 211–202 21 26.6

Notes.LIR is the intrinsic total infrared luminosity (8–1000 μm) taken from B13. The intrinsic H2O luminosities are inferred from μLH2O using μ in B13. The first group of the sources are the ones with both J = 2 and J = 3 H2O lines observed, the next group are the sources with only J = 2 H2O observed, and the last group are the previous published sources in O13.

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