论文标题

原始崩溃:形成富含灰尘的原球盘的条件

Protostellar collapse: the conditions to form dust rich protoplanetary disks

论文作者

Lebreuilly, Ugo, Commerçon, Benoît, Laibe, Guillaume

论文摘要

尘埃在恒星,磁盘和行星形成期间起着关键作用。然而,它在原始的崩溃中的动态仍然是一个未经研究的领域。最近的研究似乎表明,在这些早期阶段,灰尘可能会有效地与气体有效地脱成相结合。我们的目标是了解在原恒星塌陷的早期阶段,尘埃晶粒集中了多少,并查看它如何依赖于初始云和固体颗粒的性质。我们使用基于网格的代码公羊的多种物种灰尘动力学求解器来执行各种尘土崩溃的模拟。我们执行流体动力学和MHD模拟,其中我们改变了最大晶粒尺寸,热量与重力能比和云的磁性。我们模拟了十种中性粉尘晶粒物种的同时进化,其晶粒尺寸从几nm到几百微米不等。我们在典型尺寸的几个10微米的谷物的气体和灰尘之间获得了显着的解耦。这种脱钩很大程度上取决于热与重力能比,晶粒大小或磁场的包含。通过对我们的结果校准的半分析模型,我们表明尘埃比主要因初始stokes数字而变化,其速率取决于局部云特性。我们发现,较大的谷物倾向于在第一核和新形成的磁盘中有效地定居和漂移。这可以产生尘埃与气体比的初始值几倍。尘埃集中在高密度区域,并在低密度区域耗尽。从气体中谷物切换的大小取决于云的初始特性。由于粉尘不一定被用作崩溃期间气体的代理,因此我们强调有必要将其动态处理在崩溃模拟中。

Dust plays a key role during star, disk and planet formation. Yet, its dynamics during the protostellar collapse remains a poorly investigated field. Recent studies seem to indicate that dust may decouple efficiently from the gas during these early stages. We aim to understand how much and in which regions dust grains concentrate during the early phases of the protostellar collapse, and see how it depends on the properties of the initial cloud and of the solid particles. We use the multiple species dust dynamics solver of the grid-based code RAMSES to perform various simulations of dusty collapses. We perform hydrodynamical and MHD simulations where we vary the maximum grain size, the thermal-to-gravitational energy ratio and the magnetic properties of the cloud. We simulate the simultaneous evolution of ten neutral dust grains species with grain sizes varying from a few nm to a few hundredth of microns. We obtain a significant decoupling between the gas and the dust for grains of typical sizes a few 10 microns. This decoupling strongly depends on the thermal-to-gravitational energy ratio, the grain sizes or the inclusion of a magnetic field. With a semi-analytic model calibrated on our results, we show that the dust ratio mostly varies exponentially with the initial Stokes number at a rate that depends on the local cloud properties. We find that larger grains tend to settle and drift efficiently in the first-core and in the newly formed disk. This can produce dust-to-gas ratios of several times the initial value. Dust concentrates in high density regions and is depleted in low density regions. The size at which grains decouple from the gas depends on the initial properties of the clouds. Since dust can not necessarily be used as a proxy for gas during the collapse, we emphasize on the necessity of including the treatment of its dynamics in collapse simulations.

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