论文标题
银河灰尘:建模火中的灰尘演化
The Galactic Dust-Up: Modeling Dust Evolution in FIRE
论文作者
论文摘要
最近的进步已经开发了用于银河形成模拟的尘埃演化模型,但是这些方法的假设和复杂程度各不相同。在这里,我们介绍并比较了两个单独的尘埃演化模型(以最近的方法为标记的“元素”和“物种”),并将其纳入Gizmo代码中,并与Fire-2 Stellar Refectback和ISM物理学结合使用。这两种模型都可以解释湍流的灰尘扩散,尘埃产生出色的产生,通过气盘积聚的粉尘生长以及时间分辨的超新星,热气体中的热溅射和挤压剂的粉尘破坏。 “元素”模型跟踪了广义粉尘物种的演变,并利用了一个简单的“可调”灰尘生长程序,而“物种”模型跟踪具有集合化学成分的特定灰尘物种的演变,并结合了一个有力动机的两相尘埃生长常规。我们在理想化的银河系质量银河系中测试和比较这些模型,发现两者都会产生合理的星系集成粉尘到金属(D/Z)比率(D/Z)比率,并预测作为主要粉尘生长机制的气粉积分,但需要化学动机的模型来重现单个元素耗竭和D/Z with d/Z with D/d local Dentail and Commind Density and Local Denty Density and Denty Density dementy dementy dementy dementy dementy and Z and Z and Z and Z and。我们还发现,在特定的灰尘物种的情况下,需要纳入理论金属铁和含含粉的灰尘,以匹配O和Fe耗竭的观察结果,并且需要匹配观察到的C耗竭并确保在致密的环境中不能过量生产碳质粉尘,需要进行亚分辨率密集的分子气/CO方案。
Recent strides have been made developing dust evolution models for galaxy formation simulations but these approaches vary in their assumptions and degree of complexity. Here we introduce and compare two separate dust evolution models (labelled 'Elemental' and 'Species'), based on recent approaches, incorporated into the GIZMO code and coupled with FIRE-2 stellar feedback and ISM physics. Both models account for turbulent dust diffusion, stellar production of dust, dust growth via gas-dust accretion, and dust destruction from time-resolved supernovae, thermal sputtering in hot gas, and astration. The "Elemental" model tracks the evolution of generalized dust species and utilizes a simple, 'tunable' dust growth routine, while the "Species" model tracks the evolution of specific dust species with set chemical compositions and incorporates a physically motivated, two-phase dust growth routine. We test and compare these models in an idealized Milky Way-mass galaxy and find that while both produce reasonable galaxy-integrated dust-to-metals (D/Z) ratios and predict gas-dust accretion as the main dust growth mechanism, a chemically motivated model is needed to reproduce the observed scaling relation between individual element depletions and D/Z with column density and local gas density. We also find the inclusion of theoretical metallic iron and O-bearing dust species are needed in the case of specific dust species in order to match observations of O and Fe depletions, and the integration of a sub-resolution dense molecular gas/CO scheme is needed to both match observed C depletions and ensure carbonaceous dust is not overproduced in dense environments.