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首页> 外文期刊>The Astrophysical journal >THE CANADA-FRANCE ECLIPTIC PLANE SURVEY—L3 DATA RELEASE: THE ORBITAL STRUCTURE OF THE KUIPER BELT*
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THE CANADA-FRANCE ECLIPTIC PLANE SURVEY—L3 DATA RELEASE: THE ORBITAL STRUCTURE OF THE KUIPER BELT*

机译:加拿大法国信噪比平面调查-L3数据发布:Kuiper带的轨道结构*

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We report the orbital distribution of the trans-Neptunian comets discovered during the first discovery year of the Canada-France Ecliptic Plane Survey (CFEPS). CFEPS is a Kuiper Belt object survey based on observations acquired by the Very Wide component of the Canada-France-Hawaii Telescope Legacy Survey (LS-VW). The first year's detections consist of 73 Kuiper Belt objects, 55 of which have now been tracked for three years or more, providing precise orbits. Although this sample size is small compared to the world-wide inventory, because we have an absolutely calibrated and extremely well-characterized survey (with known pointing history) we are able to de-bias our observed population and make unbiased statements about the intrinsic orbital distribution of the Kuiper Belt. By applying the (publically available) CFEPS Survey Simulator to models of the true orbital distribution and comparing the resulting simulated detections to the actual detections made by the survey, we are able to rule out several hypothesized Kuiper Belt object orbit distributions. We find that the main classical belt's so-called 'cold' component is confined in semimajor axis (a) and eccentricity (e) compared to the more extended "hot" component; the cold component is confined to lower e and does not stretch all the way out to the 2:1 resonance but rather depletes quickly beyond a = 45 AU. For the cold main classical belt population we find a robust population estimate of N(Hg < 10) = 50 ± 5 × 103 and find that the hot component of the main classical belt represents ~60% of the total population. The inner classical belt (sunward of the 3:2 mean-motion resonance) has a population of roughly 2000 trans-Neptunian objects with absolute magnitudes Hg < 10, and may not share the inclination distribution of the main classical belt. We also find that the plutino population lacks a cold low-inclination component, and so, the population is somewhat larger than recent estimates; our analysis shows a plutino population of N(Hg < 10)~ 25+25 –12 × 103compared to our estimate of the size of main classical Kuiper Belt population of N(Hg < 10) ~ (126+50 –46) × 103.
机译:我们报告了在加拿大-法国黄道平面调查(CFEPS)的第一个发现年发现的跨海王星彗星的轨道分布。 CFEPS是基于加拿大-法国-夏威夷望远镜遗产调查(LS-VW)的甚宽部分获得的观测结果的柯伊伯带天体调查。第一年的探测包括73个柯伊伯带天体,其中55个已经被追踪了三年或更长时间,提供了精确的轨道。尽管与全球范围内的样本相比,该样本量很小,但是由于我们进行了绝对校准且特征非常明确的调查(具有已知的定点历史),因此我们能够对观测到的种群进行反偏,并对本征轨道做出无偏见的陈述。柯伊伯带的分布。通过将(公开可用的)CFEPS勘测模拟器应用于真实轨道分布的模型,并将得到的模拟探测结果与勘测结果进行的实际探测结果进行比较,我们可以排除几种假设的柯伊伯带天体轨道分布。我们发现,与更扩展的“热”分量相比,古典主带的所谓“冷”分量被限制在半长轴(a)和偏心率(e)中。冷成分被限制在较低的e值,并不会一直延伸到2:1共振,而是会很快耗尽,超过a = 45 AU。对于寒冷的主要古典带人口,我们找到了一个可靠的人口估计值N(Hg <10)= 50±5×103,并且发现主要古典带的热部分约占总人口的60%。内部古典带(3:2平均运动共振的向阳)拥有大约2000个跨海王星天体,绝对量Hg <10,并且可能不共享主要古典带的倾角分布。我们还发现,plutino种群缺乏寒冷的低倾角分量,因此,该种群比最近的估计数要大。我们的分析显示,相比于我们对经典柯伊伯带主要N(Hg <10)〜(126 + 50 –46)×103的主要种群的估计,我们发现了N(Hg <10)〜25 + 25 –12×103的plutino种群。 。
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