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Untitled - Laboratoire d'Astrophysique de l'Observatoire de Grenoble

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sublimation of water ice trapped either in comets or meteorites or, more in general, in the planetesimals<br />

which formed the Earth. A key parameter in these theories is the HDO/H2O ratio: in oceans it is ten<br />

times larger than the cosmic D/H elemental ratio, close to that of comets, and hundred times smaller than<br />

that observed in solar type protostars (§3.2.2). A big unanswered question is: what is the HDO/H2O in<br />

proto-planetary disks, which contain the material from which planetesimals, meteorites and comets are<br />

formed? Astromol has reported the first <strong>de</strong>tection of HDO in a proto-planetary disk (Fig. 3.7: Ceccarelli<br />

et al. 2005), from which a HDO/H2O ratio (∼ 1%) slightly lower than in protostars has been estimated.<br />

In<strong>de</strong>ed, the big contribution of these observations is that HDO in the measured quantities should have<br />

not been <strong>de</strong>tected, because H2O and HDO are believed to be almost totally frozen onto the grain mantles<br />

(at least in the region probed by the observations)! Since HDO has been observed, something is reinjecting<br />

water molecules from the grain mantles. Soon after the HDO <strong>de</strong>tection, Astromol showed that<br />

grain mantle photo-<strong>de</strong>sorption from the Interstellar UV field can in<strong>de</strong>ed keep the observed water column<br />

<strong>de</strong>nsity in the gas phase (Dominik, Ceccarelli, Hollenbach, Kaufman 2005, ApJL submitted).<br />

• The discovery of a small warm disk in a low mass binary system. By using Adaptive Optics (AO) ai<strong>de</strong>d<br />

2µm observations at Keck, we revealed the presence of a small ( ∼ < 5 AU), warm (∼ 400 K) and <strong>de</strong>nse ( ∼ > 10 7<br />

cm −3 disk surrounding the more massive companion of the binary system forming T Tau S (Duchene et<br />

al. 2005). The observations <strong>de</strong>tected the CO lines (from J=9 to J=20) in absorption against the source<br />

continuum, a technique already used by other authors for studying a (very) few other disk sources. The<br />

originality and importance of our observations is that, thanks to the coupling with the AO, we could study<br />

a close binary system and <strong>de</strong>monstrate that the disk of (at least) one of the two protostars is probably<br />

truncated because of the presence of the other protostar. We plan to carry out similar studies in a larger<br />

sample of sources, with the scope to un<strong>de</strong>rstand how, in<strong>de</strong>ed, the presence of a companion affects the<br />

circumstellar disks of the two composing protostars. More in general, the CO absorption technique is<br />

extremely powerful in characterizing the physical conditions of the gas in the warm layers of the protoplanetary<br />

disks, much more efficient than the mm/submm observations, which only provi<strong>de</strong> one CO J<br />

level at once.<br />

64

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