Bibcode
DOI
Cernicharo, José; Goicoechea, Javier R.; Pardo, Juan R.; Asensio-Ramos, Andrés
Bibliographical reference
The Astrophysical Journal, Volume 642, Issue 2, pp. 940-953.
Advertised on:
5
2006
Journal
Citations
43
Refereed citations
38
Description
Several condensations heated externally by nearby hot stars are present
in the Sgr B2 region for which H2O far-IR lines are expected
to probe only an external low-density and high temperature section.
Millimeter-wave lines can penetrate deeper into them (higher densities
and lower Tk). We have conducted a study combining
H2O lines in both spectral regions using the ISO (far-IR
lines) and the IRAM 30 m telescope (183 GHz line). The far-IR
H2O lines, seen in absorption, are optically thick. They form
in the outermost gas in front of the far-IR continuum sources, probing a
maximum visual extinction of ~5-10 mag. IR photons from the dust play a
dominant role in their excitation. We conclude, based on observations of
the CO J=7-6 line at 806.65 GHz, and the lack of emission from the
far-IR CO lines, that the gas density has to be below ~104
cm-3. Using the gas kinetic temperature and density derived
from OH, CO, and other molecular species, we derive a water column
density of (9+/-3)×1016 cm-2 in the
absorbing gas, implying an abundance of ~=(1-2)×10-5 in
this region. The resulting relatively low H2O/OH abundance
ratio, ~=2-4, is a signature of UV photon-dominated surface layers
traced by far-IR observations. As a consequence, the temperature of the
absorbing gas is high, Tk~=300-500 K, which allows very
efficient neutral-neutral reactions producing H2O and OH.
Finally, the 183.31 GHz data allow one to trace the inner, denser
(n(H2)>=105-106 cm-3),
and colder (Tk~40 K) gas. The emission is very strong toward
the cores with an estimated water vapor abundance of a few ×
10-7. There is also moderate extended emission around Sgr B2
main condensations, in agreement with the water vapor abundance derived
from far-IR H2O lines.
Based on observations with ISO, an ESA project with instruments funded
by ESA Member States (especially the PI countries: France, Germany, the
Netherlands, and the United Kingdom) and with participation of ISAS and
NASA.