Low-velocity shocks traced by extended sio emission along the w43 ridges: witnessing the formation of young massive clusters
Author
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Nguyen-Luong, Q.
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Motte, F.
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Carlhoff, P.
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Louvet, F.
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Lesaffre, P.
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Schilke, P.
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Hill, T.
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Hennemann, M.
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Gusdorf, A.
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Didelon, P.
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Schneider, N.
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Bontemps, S.
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Duarte Cabral, A.
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Menten, K. M.
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Martin, P. G.
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Wyrowski, F.
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Bendo, G.
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Roussel, H.
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Bernard, J. P.
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Bronfman Aguiló, Leonardo
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Henning, Thomas
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Kramer, C.
Author
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Heitsch, F.
Admission date
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2015-06-16T19:33:37Z
Available date
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2015-06-16T19:33:37Z
Publication date
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2013-10-01
Cita de ítem
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The Astrophysical Journal, 775:88 (21pp), 2013 October 1
en_US
Identifier
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doi:10.1088/0004-637X/775/2/88
Identifier
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https://repositorio.uchile.cl/handle/2250/131148
General note
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Artículo de publicación ISI
en_US
Abstract
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The formation of high-mass stars is tightly linked to that of their parental clouds. Here, we focus on the high-density
parts of W43, a molecular cloud undergoing an efficient event of star formation. Using a column density image
derived from Herschel continuum maps, we identify two high-density filamentary clouds, called the W43-MM1
and W43-MM2 ridges. Both have gas masses of 2.1 × 104 M and 3.5 × 104 M above >1023 cm−2 and within
areas of ∼6 and ∼14 pc2, respectively. The W43-MM1 and W43-MM2 ridges are structures that are coherent in
velocity and gravitationally bound, despite their large velocity dispersion measured by the N2H+ (1–0) lines of
the W43-HERO IRAM large program. Another intriguing result is that these ridges harbor widespread (∼10 pc2)
bright SiO (2–1) emission, which we interpret to be the result of low-velocity shocks (10 km s−1). We measure
a significant relationship between the SiO (2–1) luminosity and velocity extent and show that it distinguishes
our observations from the high-velocity shocks associated with outflows. We use state-of-the-art shock models to
demonstrate that a small percentage (10%) of Si atoms in low-velocity shocks, observed initially in gas phase or in
grain mantles, can explain the observed SiO column density in the W43 ridges. The spatial and velocity overlaps
between the ridges of high-density gas and the shocked SiO gas suggest that ridges could be forming via colliding
flows driven by gravity and accompanied by low-velocity shocks. This mechanism may be the initial conditions for
the formation of young massive clusters.