Abstract

In this work (Paper I), we analyse Herschel-PACS spectroscopy for a subsample of 23 O-rich and 3 S-type evolved stars, in different evolutionary stages from the asymptotic giant branch (AGB) to the planetary nebula (PN) phase, from the THROES catalogue. (C-rich targets are separately studied in Paper II). The broad spectral range covered by PACS (∼55–210 μm) includes a large number of high-J CO lines, from J = 14 − 13 to J = 45 − 44 (v = 0), that allow us to study the warm inner layers of the circumstellar envelopes (CSEs) of these objects, at typical distances from the star of ≈1014–1015 cm and ≈1016 cm for AGBs and post-AGB-PNe, respectively. We have generated CO rotational diagrams for each object to derive the rotational temperature, total mass within the CO-emitting region and average mass-loss rate during the ejection of these layers. We present first order estimations of these basic physical parameters using a large number of high-J CO rotational lines, with upper-level energies from Eup ∼ 580 to 5000 K, for a relatively big set of evolved low-to-intermediate mass stars in different AGB-to-PN evolutionary stages. We derive rotational temperatures ranging from Trot ∼ 200 to 700 K, with typical values around 500 K for AGBs and systematically lower, ∼200 K, for objects in more advanced evolutionary stages (post-AGBs and PNe). Our values of Trot are one order or magnitude higher than the temperatures of the outer CSE layers derived from low-J CO line studies. The total mass of the inner CSE regions where the PACS CO lines arise is found to range from MH2 ∼ 10−6 to ≈10−2 M⊙, which is expected to represent a small fraction of the total CSE mass. The mass-loss rates estimated are in the range Ṁ ∼ 10−7 − 10−4 M⊙yr−1, in agreement (within uncertainties) with values found in the literature. We find a clear anticorrelation between MH2 and Ṁ vs. Trot that probably results from a combination of most efficient line cooling and higher line opacities in high mass-loss rate objects. For some strong CO emitters in our sample, a double temperature (hot and warm) component is inferred. The temperatures of the warm and hot components are ∼400–500 K and ∼600–900 K, respectively. The mass of the warm component (∼10−5–8 × 10−2 M⊙) is always larger than that of the hot component, by a factor of between two and ten. The warm-to-hot MH2 and Trot ratios in our sample are correlated and are consistent with an average temperature radial profile of ∝ r−0.5 ± 0.1, that is, slightly shallower than in the outer envelope layers, in agreement with recent studies.

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