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AuthorsC. Codella, B. Lefloch, C. Ceccarelli, J. Cernicharo, E. Caux, A. Lorenzani, S. Viti, P. Hily-Blant, B. Parise, S. Maret, B. Nisini, P. Caselli, S. Cabrit, L. Pagani, M. Benedettini, A. Boogert, F. Gueth, G. Melnick, D. Neufeld, S. Pacheco, M. Salez, K. Schuster, A. Bacmann, A. Baudry, T. Bell, E.A. Bergin, G. Blake, S. Bottinelli, A. Castets, C. Comito, A. Coutens, N. Crimier, C. Dominik, K. Demyk, P. Encrenaz, E. Falgarone, A. Fuente, M. Gerin, P. Goldsmith, F. Helmich, P. Hennebelle, T. Henning, E. Herbst, T. Jacq, C. Kahane, M. Kama, A. Klotz, W. Langer, D. Lis, S. Lord, J. Pearson, T. Phillips, P. Saraceno, P. Schilke, X. Tielens, F. van der Tak, M. van der Wiel, C. Vastel, V. Wakelam, A. Walters, F. Wyrowski, H. Yorke, C. Borys, Y. Delorme, C. Kramer, B. Larsson, I. Mehdi, V. Ossenkopf, J. Stutzki
TitleThe CHESS spectral survey of star forming regions: Peering into the protostellar shock L1157-B1. I. Shock chemical complexity
JournalAstronomy and Astrophysics
Volume518
Year2010
PagesL112-
ISSN00046361
FacultyFaculty of Science
Institute/dept.FNWI: Astronomical Institute Anton Pannekoek (IAP)
AbstractWe present the first results of the unbiased survey of the L1157-B1 bow shock, obtained with HIFI in the framework of the key program Chemical HErschel Survey of Star forming regions (CHESS). The L1157 outflow is driven by a low-mass Class 0 protostar and is considered the prototype of the so-called chemically active outflows. The bright blue-shifted bow shock B1 is the ideal laboratory for studying the link between the hot (similar to 1000-2000 K) component traced by H-2 IR-emission and the cold (similar to 10-20 K) swept-up material. The main aim is to trace the warm gas chemically enriched by the passage of a shock and to infer the excitation conditions in L1157-B1. A total of 27 lines are identified in the 555-636 GHz region, down to an average 3 sigma level of 30 mK. The emission is dominated by CO(5-4) and H2O(1(10)-1(01)) transitions, as discussed by Lefloch et al. in this volume. Here we report on the identification of lines from NH3, H2CO, CH3OH, CS, HCN, and HCO+. The comparison between the profiles produced by molecules released from dust mantles (NH3, H2CO, CH3OH) and that of H2O is consistent with a scenario in which water is also formed in the gas-phase in high-temperature regions where sputtering or grain-grain collisions are not efficient. The high excitation range of the observed tracers allows us to infer, for the first time for these species, the existence of a warm (>= 200 K) gas component coexisting in the B1 bow structure with the cold and hot gas detected from ground.
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