In this paper we investigate Charon's craters size distribution using a deep learning model. This is motivated by the recent results of Singer et al. (2019) who, using manual cataloging, found a change in the size distribution slope of craters smaller than 12 km in diameter, translating into a paucity of small Kuiper Belt objects. These results were corroborated by Robbins and Singer (2021), but opposed by Morbidelli et al. (2021), necessitating an independent review. Our MaskRCNN-based ensemble of models was trained on Lunar, Mercurian, and Martian crater catalogues and both optical and digital elevation images. We use a robust image augmentation scheme to force the model to generalize and transfer-learn into icy objects. With no prior bias or exposure to Charon, our model find best fit slopes of q =-1.47+-0.33 for craters smaller than 10 km, and q =-2.91+-0.51 for craters larger than 15 km. These values indicate a clear change in slope around 15 km as suggested by Singer et al. (2019) and thus independently confirm their conclusions. Our slopes however are both slightly flatter than those found more recently by Robbins and Singer (2021). Our trained models and relevant codes are available online on github.com/malidib/ACID .
翻译:在本文中,我们用深层学习模式调查查伦火山坑的大小分布。这是由Singer等人(2019年)最近通过人工编目发现直径小于12公里的火山坑的大小分布坡度变化引起的。这些结果得到Robbins和Singer(2021年)的证实,但Morbidelli等人(2021年)的反对,必须进行独立审查。我们的MaskRCNNN(MaskRCNNN)模型合体在月球、Mercurian和Marterian火山坑目录以及光学和数字高地图像上进行了培训。我们使用一个强大的图像增强计划迫使模型的大小分布坡度变化,将直径小于12公里的坑块变成微小的岩浆物体。我们模型在Charon(2019年)没有偏见或接触过小孔,但Morbidell等人(2033年)的斜坡度最合适,15公里以上的火山坑的斜度为q=2.91+0.51。这些数值表明,Sing 15公里左右的斜度明显变化是Sing-albins等人(2019年),因此独立证实了我们最近在Sing-clastib)的模型和网上找到的。