Water In Star-forming regions with Herschel  A 429 hr GT key-program with Herschel to study the physical and chemical structure of star forming regions.

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Water In Star-forming regions with Herschel  A 429 hr GT key-program with Herschel to study the physical and chemical structure of star forming regions focussing on H 2 O and its related species  Program covers ~90 sources ranging from pre- stellar cores, low- to high-mass protostars in different evolutionary stages as well as protoplanetary disks  Both HIFI and PACS-spectroscopy are used  Includes small maps up to ~2’x2’  Collaboration of ~70+ scientists from 30 different institutes See

Follow water trail during star and planet formation D. Lommen Dark pre-stellar cores  Low-mass YSOs  Disks Intermediate mass YSOs High-mass YSOs Infrared dark clouds

Why water?  H 2 O abundance shows large variations in SF regions: <10 -8 (cold) – (warm)  unique probe of different physical regimes  Natural filter of warm gas  Main reservoir of oxygen  affects chemistry of all other species  Traces basic processes of freeze-out onto grains and evaporation, which characterize different stages of evolution  Astrobiology: water associated with life on Earth  characterize water ‘trail’ from clouds to planets, including origin of water on Earth pre-stellar cores  YSO’s  disks  comets

Origin of hot CO and H 2 O? Hot core: Compact (~200 AU) region where H 2 O ice evaporates Outflows Extended emission along outflow; H 2 O enhanced in shock 0.05 pc ~ 1’ ISO-LWS: Nisini et al Ceccarelli et al. 1999

Red: HIFI Blue: PACS H 2 O lines: HIFI vs PACS Observe mix of low- and high-excitation lines to probe cold and hot environments

SDP Data  Received:  L1157: Low-mass Class 0 YSO  outflow map 179  m H 2 O line  HH 46: Low-mass Class I YSO  NGC 7129: Intermediate mass YSO  Still pending:  Complete PACS spectral scans of  Class 0 low-mass YSO  High mass YSO  All HIFI SDP/PSP data

WISH-team  E.F. van Dishoeck, Y. Aikawa, R. Bachiller, A. Baudry, M. Benedettini, A. Benz, E. Bergin, P. Bjerkeli, G. Blake, S. Bontemps, J. Braine, A. Brandeker, S. Bruderer, P. Caselli, J. Cernicharo, L. Chavarria, C. Codella, F. Daniel, C. Dedes, P. Encrenaz, A.M. di Giorgio, C. Dominik, S. Doty, H. Feuchtgruber, M. Fich, W. Frieswijk, A. Fuente, T. Giannini, J.R. Goicoechea, Th. De Graauw, F. Helmich, F. Herpin, G. Herczeg, M. Hogerheijde, T. Jacq, J. Jørgensen, D. Johnstone, A. Karska, M. Kaufman, E. Keto, L. Kristensen, B. Larsson, B. Lefloch, D. Lis, R. Liseau, M. Marseille, C. McCoey, G. Melnick, D. Neufeld, B. Nisini, M. Olberg, G. Olofsson, L. Pagani, O. Panić, J. Pearson, R. Plume, C. Risacher, D. Salter, N. Sakai, J. Santiago, P. Saraceno, R. Shipman, M. Tafalla, F. van der Tak, T. van Kempen, R. Visser, S. Viti, S. Wampfler, M. Walmsley, F. Wyrowski, S. Yamamoto, U. Yildiz (blue indicates subteam leader)

Those who did the work to make this presentation possible….  E.F. van Dishoeck, Y. Aikawa, R. Bachiller, A. Baudry, M. Benedettini, A. Benz, E. Bergin, P. Bjerkeli, G. Blake, S. Bontemps, J. Braine, A. Brandeker, S. Bruderer, P. Caselli, J. Cernicharo, L. Chavarria, C. Codella, F. Daniel, C. Dedes, P. Encrenaz, A.M. di Giorgio, C. Dominik, S. Doty, H. Feuchtgruber, M. Fich, W. Frieswijk, A. Fuente, T. Giannini, J.R. Goicoechea, Th. De Graauw, F. Helmich, F. Herpin, G. Herczeg, M. Hogerheijde, T. Jacq, J. Jørgensen, D. Johnstone, A. Karska, M. Kaufman, E. Keto, L. Kristensen, B. Larsson, B. Lefloch, D. Lis, R. Liseau, M. Marseille, C. McCoey, G. Melnick, D. Neufeld, B. Nisini, M. Olberg, G. Olofsson, L. Pagani, O. Panić, J. Pearson, R. Plume, C. Risacher, D. Salter, N. Sakai, J. Santiago, P. Saraceno, R. Shipman, M. Tafalla, F. van der Tak, T. van Kempen, R. Visser, S. Viti, S. Wampfler, M. Walmsley, F. Wyrowski, S. Yamamoto, U. Yildiz

Nisini, Liseau, Tafalla, Benedettini et al. 3’ Water traces ‘hot spots’ where shocks dump energy into cloud L1157-mm outflow D = 440 pc, L bol = 11 L o

L1157 mm Spitzer IRAC Herschel PACS H 2 O 179  m 10 4 AU - Strong water emission from the embedded protostar Water traces interaction more directly than Spitzer Looney et al. 2008

Comparison with other gas main coolants Bachiller et al CO 2-1 H S(1) 17  m Neufeld et al Correlation between H 2 O and H 2 warm gas at T ~ 300 K - All coolants observed  can determine total energy budget

Shock enhanced molecular abundances B2 B1 B0 R0 R R2 H2OH2O H2OH2O CH 3 OHSiO NH 3 Water and other molecule abundances increase in shocks due to desorption from grain mantles and shock induced chemical reactions  relative intensities between peaks change with tracer  H 2 O, SiO and NH 3 trace the regions at higher density  Only H 2 O traces all the hot spots Pérez-Gutiérrez 1997 Bachiller et al. 2001

HH 46 low-mass YSO: velocity resolved [O I] [O I] also present in high velocity (~200 km/s) jet! van Kempen, Kristensen, Herczeg, et al. Spitzer Image: Noriega- Crespo et al ISO-LWS PACS L bol ~12 L o D =450 pc

HH 46 [O I] Most of [O I] along outflow is in high-velocity jet

Many lines detected on source CO OH H2OH2O O I CO O I CO OH Van Kempen, Kristensen, Herczeg, Wampfler, Bruderer, Benz et al. Binned spectra Warning: fluxes uncertain by 50% OH

Different species have different distributions - H 2 O extended along outflow, but OH peaking on source - [O I] falling off rapidly along outflow Note: orientation outflow switched in RA compared with Spitzer image

Origin of hot CO? Protostellar Envelope model Visser, Bruderer, Kristensen, van Kempen et al. PACS fluxes Shock Photon-heated, disk?

Which physical component dominates PACS lines? Protostellar envelope with hot core: Low-J CO UV irradiated cavity walls, disk surface: Mid-J CO? Quiescent O I? Outflow shocks: High-J CO, Hot water High velocity O I PDR Disk

- Strong H 2 O, OH, CO and [O I] lines detected - Cannot be fit with protostellar envelope model only Intermediate mass YSO NGC 7129 FIRS2

Spitzer image Megeath et al. Johnstone, Fich, Fuente, et al. Need HIFI to disentangle different components!