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The Cosmological Evolution of Dust Clouds inBrown Dwarf Atmospheres

机译:尘埃云中的宇宙论演变矮小气氛

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We present our latest DRIFT-PHOENIX model results for dust cloud formation in coolatmospheres and investigate the influence of the metallicity [MM] on the dust cloud structure onthe example of a typical mid-L dwarf (Teff=2000K, log(g)=5.0). Our new dust model simulates theformation of TiO_2seed particles (nucleation) and their subsequent gravitational settling, accompa-nied by kinetic growth and evaporation of seven solid species on top of these seeds. The gas phasedepletion by each of the considered surface reactions and the element replenishment by convectiveup-mixing are consistently coupled into this mechanism. The result is a stationary cloud structure inphase-non-equilibrium. We observe a comparably low decrease of the dust particle number densityand a weak increase of the mean grain size in the lower dust cloud for decreasing metallicities downto [M/H]=-4.0. For even lower metallicities to [M/H]=-6.0, these trends are reversed.
机译:我们展示了我们最新的漂移 - 菲尼克斯模型结果,在Coolatmospheres中进行尘云形成,并调查金属性[mm]对典型中间Ldwarf的示例的粉尘云结构的影响(Teff = 2000k,log(g)= 5.0 )。我们的新型粉尘模型模拟了TiO_2Seed颗粒(成核)的形式及其随后的重力沉降,通过动力学生长和七种固体物种在这些种子顶部的蒸发。通过对流混合的每种考虑的表面反应和元素补充,通过对流混合的气体促进剂始终偶联。结果是静止云结构依然 - 非平衡。我们观察到灰尘颗粒数密度的相对低的降低,下尘云中的平均晶粒尺寸的弱增加,用于降低金属性下降至[m / h] = - 4.0。对于甚至降低金属性至[M / H] = - 6.0,这些趋势是逆转的。

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