Carrillo-Sánchez J D, Plane J M C, Feng W, Nesvorný D, Janches D
School of Chemistry University of Leeds Leeds UK.
School of ChemistryUniversity of LeedsLeedsUK; National Centre for Atmospheric ScienceUniversity of LeedsLeedsUK.
Geophys Res Lett. 2015 Aug 16;42(15):6518-6525. doi: 10.1002/2015GL065149. Epub 2015 Aug 13.
The size and velocity distribution of cosmic dust particles entering the Earth's atmosphere is uncertain. Here we show that the relative concentrations of metal atoms in the upper mesosphere, and the surface accretion rate of cosmic spherules, provide sensitive probes of this distribution. Three cosmic dust models are selected as case studies: two are astronomical models, the first constrained by infrared observations of the Zodiacal Dust Cloud and the second by radar observations of meteor head echoes; the third model is based on measurements made with a spaceborne dust detector. For each model, a Monte Carlo sampling method combined with a chemical ablation model is used to predict the ablation rates of Na, K, Fe, Mg, and Ca above 60 km and cosmic spherule production rate. It appears that a significant fraction of the cosmic dust consists of small (<5 µg) and slow (<15 km s) particles.
进入地球大气层的宇宙尘埃颗粒的大小和速度分布尚不确定。在此我们表明,中间层上部金属原子的相对浓度以及宇宙球粒的表面堆积速率,为这种分布提供了灵敏的探测手段。选取了三种宇宙尘埃模型作为案例研究:两种是天文学模型,第一种受黄道尘埃云的红外观测约束,第二种受流星头部回波的雷达观测约束;第三种模型基于星载尘埃探测器的测量结果。对于每个模型,采用蒙特卡罗抽样方法并结合化学烧蚀模型来预测60公里以上钠、钾、铁、镁和钙的烧蚀率以及宇宙球粒的产生率。看来相当一部分宇宙尘埃由小颗粒(<5微克)和低速颗粒(<15公里/秒)组成。