2003
DOI: 10.1086/377367
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Fragmentation of a Molecular Cloud Core versus Fragmentation of the Massive Protoplanetary Disk in the Main Accretion Phase

Abstract: The fragmentation of molecular cloud cores a factor of 1.1 denser than the critical Bonnor-Ebert sphere is examined though three-dimensional numerical simulations. A nested grid is employed to resolve fine structure down to 1 AU while following the entire structure of the molecular cloud core of radius 0.14 pc. A barotropic equation of state is assumed to take account of the change in temperature during collapse, allowing simulation of the formation of the first core. A total of 225 models are shown to survey … Show more

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Cited by 141 publications
(165 citation statements)
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“…Starting with a level of rotation consistent with observations, hydrodynamical numerical simulations discovered that centrifugally supported disks form with characteristic diameters of the order of a few hundred AU (Matsumoto & Hanawa 2003;Hennebelle et al 2004;Goodwin et al 2007;Commerçon et al 2008). These structures are the unavoidable consequence of angular momentum conservation during the collapse phase.…”
Section: Introductionmentioning
confidence: 65%
“…Starting with a level of rotation consistent with observations, hydrodynamical numerical simulations discovered that centrifugally supported disks form with characteristic diameters of the order of a few hundred AU (Matsumoto & Hanawa 2003;Hennebelle et al 2004;Goodwin et al 2007;Commerçon et al 2008). These structures are the unavoidable consequence of angular momentum conservation during the collapse phase.…”
Section: Introductionmentioning
confidence: 65%
“…In the former scenario, fragments may share the core's net angular momentum vector (Matsumoto & Hanawa 2003). We note that while equal inclinations is a necessary condition for aligned angular momenta, it is not a sufficient one, unless the inclinations are zero.…”
Section: Discussion: Implications For Formationmentioning
confidence: 84%
“…To construct the BE profile, we set the central density as n = 10 4 cm −3 in all models and adopt different isothermal temperatures that are estimated by a one-zone calculation (see below). To promote contraction, we enhance the cloud density by a factor of 1.8 (Matsumoto & Hanawa 2003). For each initial cloud, the mass and radius are different, while the initial cloud stability (the ratio of thermal to gravitational energy), which affects the fragmentation condition, is the same (for details, see §5.2).…”
Section: Model and Numerical Methodsmentioning
confidence: 99%