2002/09/25 by S. Maret, C. Ceccarelli, E. Caux +2 · 2 citations
Chemistry · Physics and Astronomy · #Astrophysics and Star Formation Studies #Molecular Spectroscopy and Structure #Stellar, planetary, and galactic studies #astro-ph
paper · pdf · doi:10.1051/0004-6361:20021334
published as Astron.Astrophys. 395 (2002) 573-585
arxiv created 2002/09/25 · openalex publication_date 2002/11/01 · arxiv updated 2009/12/01 · openalex created_date 2025/10/10 · openalex updated_date 2026/07/31
We report ISO-LWS far infrared observations of CO, water and oxygen lines towards the protobinary system IRAS 4 in the NGC 1333 cloud. We detected several water, OH, CO rotational lines, and two [OI] and [CII] fine structure lines. Given the relatively poor spectral and spatial resolution of these observations, assessing the origin of the observed emission is not straightforward. In this paper, we focus on the water line emission and explore the hypothesis that it originates in the envelopes that surround the two protostars, IRAS 4 A and B, thanks to an accurate model. The model reproduces quite well the observed water line fluxes, predicting a density profile, mass accretion rate, central mass, and water abundance profile in agreement with previous works. We hence conclude that the emission from the envelopes is a viable explanation for the observed water emission, although we cannot totally rule out the alternative that the observed water emission originates in the outflow. The envelopes are formed by a static envelope where the density follows the r-2 law, at AU, and a collapsing envelope where the density follows the law. The density of the envelopes at 1500 AU from the center is ~ cm-3 and the dust temperature is ~30 K, i.e. about the evaporation temperature of CO-rich ices. This may explain previous observations that claimed a factor of 10 depletion of CO in IRAS 4, as those observations probe the outer ≤ 30 K region of the envelope. The water is ~ less abundant than H2 in the outer and cold envelope, whereas its abundance jumps to ~ in the innermost warm region, at AU where the dust temperature exceeds 100 K, the evaporation temperature of H2O-rich ices. We derive a mass of 0.5 for each protostar, and an accretion rate of , implying an age of about 10000 years, if the accretion rate remains constant. We finally discuss the difference between IRAS 4 and IRAS 16293-2422, where a similar analysis has been carried out. We found that IRAS 4 is probably a younger system than IRAS 16293-2422. This fact, coupled with the larger distance of IRAS 4 from the Sun, fully explains the apparent difference in the molecular emission of these two sources, which is much richer in IRAS 16293-2422.