首页> 外文期刊>Icarus: International Journal of Solar System Studies >Density waves in Cassini UVIS stellar occultations. 1. The Cassini Division
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Density waves in Cassini UVIS stellar occultations. 1. The Cassini Division

机译:卡西尼号UVIS恒星掩星中的密度波。 1.卡西尼分部

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We analyze density waves in the Cassini Division of Saturn's rings revealed by multiple stellar occultations by Saturn's rings observed with the Cassini Ultraviolet Imaging Spectrograph. The dispersion and damping of density waves provide information on the local ring surface mass density and viscosity. Several waves in the Cassini Division are on gradients in the background optical depth, and we find that the dispersion of the wave reflects a change in the underlying surface mass density. We find that over most of the Cassini Division the ring opacity (the ratio of optical depth to surface mass density) is nearly constant and is ~5 times higher than the opacity in the A ring where most density waves are found. However, the Cassini Division ramp, a 1100-km-wide, nearly featureless region of low optical depth that connects the Cassini Division to the inner edge of the A ring, has an opacity like that of the A ring and significantly less than that in the rest of the Cassini Division. This is consistent with particles in the ramp originating in the A ring and being transported into the Cassini Division through ballistic transport processes. Damping of the waves in the Cassini Division suggests a vertical thickness of 3-6 m. Using a mean opacity of 0.1 cm~2/g we find the mass of the Cassini Division, excluding the ramp, is 3.1 × 10~(16) kg while the mass of the Cassini Division ramp, with an opacity of 0.015 cm~2/g, is 1.1 × 10~(17) kg. Assuming a power-law size distribution for the ring particles, the larger opacity of the main Cassini Division is consistent with the largest ring particles there being ~5 times smaller than the largest particles in the ramp and A ring.
机译:我们通过卡西尼紫外成像光谱仪观察到的土星环的多次恒星掩星分析了土星环的卡西尼分区中的密度波。密度波的色散和阻尼提供了有关局部环表面质量密度和粘度的信息。卡西尼分部中的几个波在背景光学深度上处于梯度上,我们发现波的色散反映了底层表面质量密度的变化。我们发现,在大多数卡西尼分部中,环的不透明度(光学深度与表面质量密度之比)几乎恒定,比发现大多数密度波的A环的不透明度高约5倍。但是,卡西尼分区的坡度是1100公里,光学深度很深,几乎没有任何特征,将卡西尼分区连接到A环的内边缘,其不透明度类似于A环,并且比A环要小得多。卡西尼分部的其余部分。这与源自A环并通过弹道运输过程被运输到卡西尼分部的坡道中的颗粒一致。卡西尼分区中的波浪阻尼表明垂直厚度为3-6 m。使用平均不透明度0.1 cm〜2 / g,我们发现卡西尼分部的质量(不包括坡道)为3.1×10〜(16)kg,而卡西尼分部的质量为不透明度为0.015 cm〜2 / g为1.1×10〜(17)kg。假设环粒子具有幂律尺寸分布,则主要的卡西尼分部的不透明度与最大的环粒子一致,比最大的环粒子小约5倍,比坡道和A环中的最大粒子小。

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