自动提取月球撞击坑的多种形态参数

Meng Xiao, Teng Hu, Zhizhong Kang, Haifeng Zhao, Feng Liu
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摘要

撞击坑是广泛分布于月球表面的地貌特征。其形态参数对于研究其形成原因、撞击地点的月球碎屑厚度和撞击坑的年龄至关重要。然而,目前从广阔地理区域内的大量撞击坑中提取多种形态参数的研究面临着一些挑战,其中包括与异质数据中的坐标偏移、撞击坑剖面形态解释不足以及形态参数提取不完整有关的问题。针对上述挑战,本文提出了一种基于数字高程模型(DEM)和撞击坑数据库的形态参数自动提取方法。该方法涉及异质数据坐标偏移校正、撞击坑剖面形态模拟和各种撞击坑形态参数自动提取。该方法设计用于处理广泛地区的大量撞击坑。因此,该方法特别适用于涉及区域尺度撞击坑分析的研究。我们在不同年代的地质单元中进行了实验,并分析了该方法的准确性。分析结果表明:首先,所提出的方法能对撞击坑中心位置偏移进行相对有效的校正。其次,撞击坑轮廓形状拟合结果相对准确。R 平方值(R2)分布在 0.97 到 1 之间,平均绝对百分比误差(MAPE)在 0.032% 到 0.568% 之间,拟合度较高。最后,该方法自动提取的深度、深径比、内外坡度等 8 个形态参数与人工提取的参数基本一致。通过将所提方法与类似方法进行比较,结果表明该方法是有效的,可以为相关月面研究提供数据支持。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

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Automatic extraction of multiple morphological parameters of lunar impact craters
Impact craters are geomorphological features widely distributed on the lunar surface. Their morphological parameters are crucial for studying the reasons for their formation, the thickness of the lunar regolith at the impact site and the age of the impact crater. However, current research on the extraction of multiple morphological parameters from a large number of impact craters within extensive geographical regions faces several challenges, including issues related to coordinate offsets in heterogeneous data, insufficient interpretation of impact crater profile morphology and incomplete extraction of morphological parameters. To address the aforementioned challenges, this paper proposes an automatic extraction method of morphological parameters based on the digital elevation model (DEM) and impact crater database. It involves the correction of heterogeneous data coordinate offset, simulation of impact crater profile morphology and various impact crater morphological parameter automatic extraction. And the method is designed to handle large numbers of impact craters in a wide range of areas. This makes it particularly useful for studies involving regional‐scale impact crater analysis. Experiments were carried out in geological units of different ages and we analysed the accuracy of this method. The analysis results show that: first, the proposed method has a relatively effective impact crater centre position offset correction. Second, the impact crater profile shape fitting result is relatively accurate. The R‐squared value (R2) is distributed from 0.97 to 1, and the mean absolute percentage error (MAPE) is between 0.032% and 0.568%, which reflects high goodness of fit. Finally, the eight morphological parameters automatically extracted using this method, such as depth, depth–diameter ratio, and internal and external slope, are basically consistent with those extracted manually. By comparing the proposed method with a similar approach, the results demonstrate that it is effective and can provide data support for relevant lunar surface research.
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