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Astron. Astrophys. 324, 221-236 (1997)

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4. Conclusion

Several projects are planned in the near future to detect rotational lines of O2 using millimeter and submillimeter receivers embarked on satellites or stratospheric balloons: ODIN for the 119 and 487 GHz lines, SWAS for the 487 GHz line, PRONAOS-SMH for the 368 GHz line and PIROG 8 for the 425 GHz line. As a theoretical preparation to these projects, we have used an interstellar cloud model to compute the abundance and rotational populations of O2 in order to predict the intensities of its main rotational lines. The model, which assumes steady-state equilibrium, solves a coupled set of equations: 1) The chemical balance equation for 136 species, mainly the simplest C- and O-bearing compounds and their 13 C and 18 O substitutions, leading to the distribution of their fractional abundances throughout the cloud. 2) The statistical equilibrium equations leading to the rotational population of the molecules H2, CO and O2 and the fine structure population of C, C [FORMULA] and O. 3) The thermal balance equation with gives the gas temperature distribution. 4) The transfer equation for the UV photons giving the photo-destruction rates of the chemical species as a function of depth within the cloud. The cloud model has been adapted from the one developed by Warin et al. (1996) by including the first 24 rotational levels of O2. Their population is computed by using recent calculations of the collisional rates O2 -He from which we estimated O2 -H2 rates; we also computed the spectroscopic parameters (energy levels and line strenghts) necessary to obtain the radiative rates. The main conclusions of this work can be summarized as follow:

  • With the standard C/O abundance ratio of 0.4, the abundance of molecular oxygen increases very sharply with cloud visual extinction, so as to be comparable to that of CO, with O2 /CO ranging for 0.25 to 0.4 as [FORMULA] increases from 10 to 30, whatever the temperature and the hydrogen density. It must be noted that, even in the densest and most opaque clouds computed here, atomic oxygen remains more abundant than O2 and represents between 20 and 30 % of the available gas phase oxygen.
  • With the sensitivities expected for the receivers of the forthcoming missions, the detection of interstellar O2 will be limited to dark clouds, with a possible exception for the ODIN receiver which could observe the 119 GHz line in translucent clouds ([FORMULA]  5) provided the temperature is less than 50 K.
  • Unlike the overall abundance of O2, its rotational population, and consequently the intensity of its rotational lines are fairly sensitive to the temperature. The 368 GHz receiver of PRONAOS and the 487 GHz receivers of ODIN and SWAS are able to detect O2 in opaque clouds ([FORMULA]  10) with temperatures [FORMULA]  25-50 K, somewhat larger than usually expected in dark clouds. Due to larger line intensities, the PIROG 8 receiver could detect the 425 GHz line in less opaque clouds ([FORMULA]  6-7) in the same range of temperatures.
  • Because O2 is rather easily photodissociated, the regions submitted to an intense UV radiation field are very unfavourable to the detection of O2. Typically, if the external UV radiation field is enhanced by a factor 1000 with respect to the local standard value, only the ODIN receiver at 119 GHz is able to detect O2 in dark clouds with [FORMULA]  10, while the three other lines will be observable in more opaque clouds ([FORMULA]  20).
  • The most drastic parameter that controls the abundance of O2 (as well as that of OH and H2 O) and, consequently, the detectability of its rotational lines, is the C/O elemental abundance ratio in the gas phase. The molecule CO is so easily formed in interstellar clouds and so stable that its abundance is very rapidly limited by the available gas phase carbon or oxygen depending to wether C [FORMULA] O or C [FORMULA] O. As the carbon abundance increases and approches that of oxygen, the amount of oxygen available to produce oxygen-bearing molecules other than CO is considerably reduced. For typical dark cloud conditions, as C/O increases from the standard value of 0.4 to 2, O being fixed, the O2 abundance drops by a factor [FORMULA]  4 104 ; at the same time, the H2 O and OH abundances are also decreased, but to a lesser extent, by a factor 2500 and 30, respectively. If C/O [FORMULA] 1, the 119 GHz line of O2 appears accessible to the ODIN receiver only in very opaque clouds ([FORMULA]  20), the three other lines being unobservable as soon as the C/O ratio is larger than 0.7. Because of this strong sensitivity to C/O, the detection of O2 could serve to constrain the carbon and oxygen abundances if parameters like density, temperature, UV field... could be derived by another way; it must be however noted that the amount of O2 is very sensitive to other physical conditions such as the ionization degree, as indicated by alternative model calculations.
  • In regions where the O2 column densities are large enough to be detectable, the rate coefficient of the reaction O+OH [FORMULA] O2 +H, the main route to O2, has little influence on its abundance. It however controls the OH abundance since it is the main destruction process of this molecule. An experimental study of the O+OH [FORMULA] O2 +H reaction at low temperatures would be of great interest for this problem.
  • Our model calculations also predict that radiative de-excitation of O2 could be an important cooling agent of cold molecular gas, to be included in models. Under favourable conditions for the formation of O2, its cooling efficiency is comparable to that of CO mainly because the lower line strenghts of the O2 lines are compensated by their lower opacities.

[TABLE]

Table 8. Analytic fit of the O2 -He collision de-excitation rate (in cm3 s-1): [FORMULA]


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© European Southern Observatory (ESO) 1997

Online publication: May 26, 1998

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