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Considerations regarding the colors and low surface albedo of comets using the Hapke methodology

机译:使用Hapke方法对彗星的颜色和低表面反照率的考虑

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The single scattering albedos (SSA's) determined for 9P/Tempel 1 are interpreted in terms of the Hapke model of irregular particle scattering efficiencies. Absorption coefficients versus wavelength from 0.31 to 2.5 mu m are obtained. It is shown that the colors and exceedingly low reported SSA's in the UV region of the spectrum below 0.4 mu m cannot be reproduced with the geometric Hapke scattering model for irregular particles. However, by increasing the reported SSA's by a small amount, absorption coefficients for particle radii of 10-1001 mu m versus wavelength from 0.31 to 2.5 mu m can be fitted. Several reasons are given for slightly increasing the SSA's, such as neglect of the effects of porosity, having a more complex phase function for the particles, uncertainties in the absolute calibration and the uncertainties associated with the complex treatment of surface roughness. The absorption coefficients determined show good agreement with potential surface constituents, Mg rich olivine and pyroxene with some amount of darkening iron or organic component. (C) 2015 Elsevier Inc. All rights reserved.
机译:根据不规则粒子散射效率的Hapke模型解释了针对9P / Tempel 1确定的单个散射反照率(SSA)。获得相对于波长为0.31至2.5μm的吸收系数。结果表明,在不规则粒子的几何Hapke散射模型下,无法在低于0.4微米的光谱的UV区中报告颜色和极低的SSA值。但是,通过少量增加报告的SSA,可以拟合10-1001μm的粒子半径相对于0.31至2.5μm波长的吸收系数。给出了稍微增加SSA的一些原因,例如忽略了孔隙率的影响,对粒子具有更复杂的相函数,绝对校准的不确定性以及与表面粗糙度的复杂处理相关的不确定性。测得的吸收系数与潜在的表面成分,富含镁的橄榄石和辉石以及一定量的变黑铁或有机成分表现出良好的一致性。 (C)2015 Elsevier Inc.保留所有权利。

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