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首页> 外文期刊>Journal of Geophysical Research. Biogeosciences >Color and polarization as indicators of comet dust properties and evolution in the near-nucleus coma
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Color and polarization as indicators of comet dust properties and evolution in the near-nucleus coma

机译:颜色和极化是彗核粉尘特性和近核昏迷演变的指标

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摘要

We present CCD colorimetric and polarimetric observations of comets Hale-Bopp, Hyakutake, and Tabur and an analysis of their change in color and polarization with the distance from the nucleus that may indicate dust evolution in the coma. We concentrate on trends along the solar-antisolar direction in the innermost coma, where all three observed comets demonstrate a correlation between color and polarization. Comparisons to laboratory studies of scattering by complex dust structures reveal that the observed correlation is most likely a result of evaporation/destruction of a dark (organic) material. We study the evolution and properties of the dust in the central coma of these comets using a tentative model of cometary dust as an ensemble of core-mantle particles with sublimating mantles. Calculations for a variety of optical properties, core-mantle mass ratios, and dust size distributions showed that this model could describe the observed change in color and polarization in cometary comae when realistic ranges of input parameters are used. The best fit particles have silicate cores of radius 0.05-0.2 mum with a porous organic-carbon mantle of mantle/core mass ratio 0.5-1. Within the frames of the model the peculiarity of the color and polarization for comet Hale-Bopp (both increase with the distance from the nucleus unlike the decrease observed in comets Hyakutake and Tabur) can be understood in terms of a compact organic mantle on the Hale-Bopp dust grains, whereas the Hyakutake and Tabur dust have more porous mantles. We show how polarimetric color restricts the range of satisfactory refractive indices of both the core and the mantle materials. [References: 38]
机译:我们介绍了彗星Hale-Bopp,Hyakutake和Tabur的CCD比色和极化观测,并分析了它们的颜色和极化变化以及与核的距离,这可能表明彗星出现了尘埃。我们集中在最内层昏迷中沿太阳-反日向的趋势,其中观察到的所有三个彗星都显示出颜色和偏振之间的相关性。与实验室研究复杂粉尘结构散射的比较表明,观察到的相关性很可能是深色(有机)物质蒸发/破坏的结果。我们使用彗星尘埃的初步模型研究了彗星中央彗形尘埃的演变和性质,将其作为具有升华地幔的核幔幔粒子的集合。通过计算各种光学特性,芯-幔质量比和粉尘尺寸分布,可以看出,该模型可以描述当使用实际输入参数范围时,彗星彗星观察到的颜色和偏振态变化。最合适的颗粒具有半径为0.05-0.2微米的硅酸盐核,以及多孔质/核质量比为0.5-1的多孔有机碳幔。在该模型的框架内,可以通过黑尔的紧凑有机幔来理解黑尔-波普彗星的颜色和极化的独特性(与离核的距离都增加,这与彗星Hyakutake和Tabur的减少不同)。 -Bopp尘埃颗粒,而Hyakutake和Tabur尘埃具有更多的多孔披风。我们展示了偏光色如何限制纤芯和地幔材料令人满意的折射率范围。 [参考:38]

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