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The 2004 Las Campanas/Lowell Observatory campaign II. Surface properties of Hayabusa target Asteroid 25143 Itokawa inferred from Hapke modeling

机译:2004年拉斯坎帕纳斯/洛厄尔天文台运动II。 Hapke建模推论Hay鸟靶小行星25143 Itokawa的表面特性

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We present an analysis of Hapke photometric modeling applied to uniform ground-based UBVRIJHK broadband data of asteroid 25143 Itokawa collected over a wide range of solar phase angles (4°-130°) during the 2004 apparition (Thomas-Osip et al. , this issue, hereafter Paper I). Our photometric analyses indicate that Itokawa has a blocky surface with properties different from other, albeit larger, S-class asteroids studied using similar Hapke modeling analyses. Images from the Hayabusa spacecraft affirm the Hapke modeling results, demonstrating the ability of Hapke photometric modeling to predict a rocky asteroid surface correctly; this is the first time that a predicted rocky surface has been observed by a spacecraft. The single particle scattering functions are dominantly forward scattering, suggesting the surface material is composed primarily of clear particles whose scattering is dictated by the particle's surface as opposed to internal scatterers (more typical of S-class asteroids), while the opposition parameters indicate that the regolith may be more compact than most of the limited number of asteroids visited by spacecraft to date. The roughness properties, single particle scattering properties, and opposition surge characteristics are all indicative of a surface where multiple scattering does not play a major role in defining the photometric properties of the regolith
机译:我们对Hapke光度模型进行了分析,该光度模型适用于2004年幻影期间在广泛的太阳相位角(4°-130°)上收集的小行星25143 Itokawa的统一地面UBVRIJHK宽带数据。问题,以下为论文I)。我们的光度分析表明,线川的块状表面与使用相似的Hapke建模分析研究的其他大型S级小行星的性质不同。 Hayabusa太空船的影像证实了Hapke建模的结果,证明了Hapke光度学建模能够正确预测岩石小行星表面的能力。这是航天器首次观测到预测的岩石表面。单个粒子的散射函数主要是前向散射,这表明表面材料主要由透明粒子组成,其散射是由粒子的表面而不是内部散射体(S类小行星的典型代表)决定的,而相反的参数则表明与迄今为止航天器访问的有限数量的小行星中的大多数小行星相比,雷格石更紧凑。粗糙度特性,单粒子散射特性和相反的喘振特性均表示表面,其中多重散射在定义硬脂石的光度特性中不发挥主要作用

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