Bibcode
DOI
Cernicharo, José; Goicoechea, Javier R.; Pardo, Juan R.; Asensio-Ramos, Andrés
Referencia bibliográfica
The Astrophysical Journal, Volume 642, Issue 2, pp. 940-953.
Fecha de publicación:
5
2006
Revista
Número de citas
43
Número de citas referidas
38
Descripción
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.