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Dielectric Properties of Vesta's Surface as Constrained by Dawn VIR Observations

机译:黎明VIR约束Vesta表面的介电性质   意见

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摘要

Earth and orbital-based radar observations of asteroids provide a uniqueopportunity to characterize surface roughness and the dielectric properties oftheir surfaces, as well as potentially explore some of their shallow subsurfacephysical properties. If the dielectric and topographic properties of asteroid'ssurfaces are defined, one can constrain their surface textural characteristicsas well as potential subsurface volatile enrichment using the observed radarbackscatter. To achieve this objective, we establish the first dielectric modelof asteroid Vesta for the case of a dry, volatile-poor regolith--employing ananalogy to the dielectric properties of lunar soil, and adjusted for thesurface densities and temperatures deduced from Dawn's Visible and InfraRedmapping spectrometer (VIR). Our model suggests that the real part of thedielectric constant at the surface of Vesta is relatively constant, rangingfrom 2.3 to 2.5 from the night- to day-side of Vesta, while the loss tangentshows slight variation as a function of diurnal temperature, ranging from 0.006to 0.008. We estimate the surface porosity to be ~55% in the upper meter of theregolith, as derived from VIR observations. This is ~12% higher than previousestimation of porosity derived from previous Earth-based X- and S-band radarobservation. We suggest that the radar backscattering properties of asteroidVesta will be mainly driven by the changes in surface roughness rather thanpotential dielectric variations in the upper regolith in the X- and S-band.
机译:基于地球和基于轨道的小行星雷达观测提供了独特的机会来表征表面粗糙度及其表面的介电特性,并有可能探索其某些浅层地下物理特性。如果定义了小行星表面的介电和形貌特性,则可以使用观测到的雷达反向散射来限制它们的表面纹理特征以及潜在的地下挥发性物质富集。为实现此目标,我们建立了干燥,挥发性差的重钙石的第一个小行星Vesta介电模型-对月球土壤的介电特性进行分析,并根据Dawn的可见光和红外测绘光谱仪推导出的表面密度和温度进行了调整(VIR)。我们的模型表明,维斯塔表面介电常数的实部是相对恒定的,从维斯塔的夜晚到白天,其介电常数在2.3到2.5之间,而损耗角正切随昼夜温度的变化显示出轻微的变化,范围为0.006到0.008。根据VIR观测,我们估计在砾岩的上部米中的表面孔隙率为〜55%。这比以前基于地球的X波段和S波段雷达观测得到的孔隙度估计值高约12%。我们建议小行星维斯塔的雷达后向散射特性将主要由表面粗糙度的变化驱动,而不是由X波段和S波段上部重石块中潜在的介电变化所驱动。

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