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Constraints on the subsurface structure and density of the nucleus of Comet 67P/Churyumov-Gerasimenko from Arecibo radar observations

机译:阿雷西博雷达观测对67P / Churyumov-Gerasimenko彗星地下结构和核密度的约束

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Context. Little is known about the internal structure of cometary nuclei. In addition to understanding their accretion in the early solar nebula and their subsequent evolution in the solar system, we find this question to be of acute and timely interest in the case of 67P/Churyumov-Gerasimenko (hereafter 67P/C-G) due to be visited by the Rosetta spacecraft in the second half of 2014. In particular, the successful landing of the Philae surface module depends critically upon the bulk density of the nucleus and the structure of its surface layer. Aims. In addition to fostering our general knowledge of these properties, it is important to exploit all possible information to assist in preparing the delivery of Philae. Methods. We performed an in-depth analysis of the observations done with the radar system of the Arecibo Observatory in November 1982 when comet 67P/C-G had a close encounter with Earth at a geocentric distance of 0.4AU taking our present knowledge of the properties of its nucleus (size, rotational state) into account. Results. In the absence of a detectable radar echo, we determined a maximum radar cross section of 0.7 km2, leading to a maximum radar albedo of 0.05. This low albedo probably results from a combination of a low radar reflectivity material and a lightly packed upper layer of the nucleus with substantial roughness (rms slope of ≈55°), consistent with its low thermal inertia. Based on radar observations of other cometary nuclei and asteroids, it is unlikely that the albedo can be lower than 0.04 so that we were able to constrain the dielectric permittivity of the subsurface layer to a narrow range of 1.9 to 2.1. Laboratory measurements and our modeling of mixtures of ice and dust have led to a porosity in the range of approximately 55 to 65% and a density in the range of ≈600 to ≈1000 kg m-3 for the top ≈2.5 m layer of the nucleus. This would be the bulk density range for a homogeneous nucleus and would place the success of the landing at risk, but an inhomogeneous nucleus with an overall density below this range remains a possibility.
机译:上下文。关于彗核的内部结构知之甚少。除了了解它们在早期太阳星云中的增生及其随后在太阳系中的演化外,我们还发现,对于即将访问的67P / Churyumov-Gerasimenko(以下称67P / CG),这个问题引起了人们的关注。由Rosetta太空飞船在2014年下半年完成。特别是,菲莱(Philae)表面模块的成功降落关键取决于原子核的堆积密度及其表面层的结构。目的除了增强我们对这些属性的一般知识外,重要的是利用所有可能的信息来帮助准备Philae的交付。方法。我们对1982年11月阿雷西博天文台的雷达系统进行的观测进行了深入分析,当时彗星67P / CG在地心距为0.4AU的情况下与地球亲密接触,这是根据我们对它的原子核特性的了解(大小,旋转状态)。结果。在没有可检测到的雷达回波的情况下,我们确定最大雷达横截面为0.7 km2,从而导致最大雷达反照率为0.05。这种低反照率可能是由于低雷达反射率材料和原子核的上层轻堆积而造成的,该上层具有相当大的粗糙度(均方根斜率≈55°),并且具有较低的热惯性。根据其他彗星核和小行星的雷达观测结果,反照率不可能低于0.04,这样我们就能够将地下层的介电常数限制在1.9到2.1的窄范围内。实验室测量和我们对冰和尘埃混合物的建模已导致孔隙的最高层约2.5 m的孔隙率在约55%至65%的范围内,密度在≈600至≈1000kg m-3的范围内核。这将是同质核的堆积密度范围,并将成功着陆置于危险之中,但总密度低于该范围的不均质核仍然是可能的。

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