Mapping the spatial distributions of oxide abundances and Mg# on the lunar surface using multi-source data and a new ensemble learning algorithm

IF 1.8 4区 物理与天体物理 Q3 ASTRONOMY & ASTROPHYSICS Planetary and Space Science Pub Date : 2024-04-12 DOI:10.1016/j.pss.2024.105894
Chaofa Bian , Kefei Zhang , Yunzhao Wu , Suqin Wu , Yu Lu , Hongtao Shi , Huaizhan Li , Dongsheng Zhao , Yabo Duan , Ling Zhao , Huajing Wu
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Abstract

The spatial distribution of oxide abundances and Mg# (Mg/(Mg + Fe)) on the lunar surface is of great significance for in-depth understanding the origin and evolution of the Moon. China's Chang’E−5 (CE-5) mission returned young lunar soils for the first time, providing a new ground truth for the inversion of oxide abundances. In this study, the relationship between multi-source remote sensing data (including Chang’E−1 Interference Imaging Spectrometer (CE-1 IIM) data and the new global Christiansen feature (CF) product, named IIM-CF data), and the abundances of six oxides (FeO, TiO2, MgO, SiO2, Al2O3 and CaO) measured at 40 lunar sampling sites including CE-5 were analyzed. The use of IIM-CF data as the input features of the selected inversion models for obtaining the abundances of oxides, and the oxide abundances measured at the 40 sampling sites were used as the ground truth. The models selected for this investigation contain three typical algorithms − random forest (RF), extreme gradient boosting (XGBoost) and partial least squares regression (PLSR), and a new method integrates RF, XGBoost and PLSR together named RXP was developed in this study. The modeling results of the abundances of the six oxides derived from the above four algorithms show that the RXP algorithm outperforms the other three algorithms. The distributions of the six oxides and Mg# on the lunar surface covering the range from 70° N to 70° S (70° N/S) with a resolution of about 200 m/pixel were generated using the proposed RXP algorithm. Our results indicate that, compared with the result of a single data source, the use of IIM-CF data improved the accuracy of the modeling of oxide abundances and Mg#. It is expected that the CE-5 samples can bring additional references to the studies of the inversion for the oxides of the lunar surface and deepen our understanding over this issue.

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利用多源数据和新的集合学习算法绘制月球表面氧化物丰度和镁的空间分布图
月球表面氧化物丰度和镁#(镁/(镁+铁))的空间分布对深入了解月球的起源和演化具有重要意义。中国的嫦娥五号(CE-5)任务首次返回了年轻的月球土壤,为氧化物丰度的反演提供了新的地面实况。本研究分析了多源遥感数据(包括嫦娥一号干涉成像光谱仪(CE-1 IIM)数据和新的全球克里斯琴森特征(CF)产品,即 IIM-CF 数据)与包括 CE-5 在内的 40 个月球采样点测量的六种氧化物(FeO、TiO2、MgO、SiO2、Al2O3 和 CaO)丰度之间的关系。使用 IIM-CF 数据作为所选反演模型的输入特征,以获得氧化物丰度,并将在 40 个采样点测得的氧化物丰度作为地面实况。本研究选择的模型包含三种典型算法--随机森林(RF)、极梯度提升(XGBoost)和偏最小二乘回归(PLSR),并开发了一种将 RF、XGBoost 和 PLSR 集成在一起的新方法,命名为 RXP。上述四种算法得出的六种氧化物丰度的建模结果表明,RXP 算法优于其他三种算法。利用提出的 RXP 算法生成了月球表面六种氧化物和 Mg# 的分布图,覆盖范围为北纬 70°至南纬 70°(北/南 70°),分辨率约为 200 米/像素。结果表明,与单一数据源的结果相比,使用 IIM-CF 数据提高了氧化物丰度和 Mg# 建模的准确性。预计 CE-5 样品能为月球表面氧化物的反演研究提供更多参考,并加深我们对这一问题的理解。
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来源期刊
Planetary and Space Science
Planetary and Space Science 地学天文-天文与天体物理
CiteScore
5.40
自引率
4.20%
发文量
126
审稿时长
15 weeks
期刊介绍: Planetary and Space Science publishes original articles as well as short communications (letters). Ground-based and space-borne instrumentation and laboratory simulation of solar system processes are included. The following fields of planetary and solar system research are covered: • Celestial mechanics, including dynamical evolution of the solar system, gravitational captures and resonances, relativistic effects, tracking and dynamics • Cosmochemistry and origin, including all aspects of the formation and initial physical and chemical evolution of the solar system • Terrestrial planets and satellites, including the physics of the interiors, geology and morphology of the surfaces, tectonics, mineralogy and dating • Outer planets and satellites, including formation and evolution, remote sensing at all wavelengths and in situ measurements • Planetary atmospheres, including formation and evolution, circulation and meteorology, boundary layers, remote sensing and laboratory simulation • Planetary magnetospheres and ionospheres, including origin of magnetic fields, magnetospheric plasma and radiation belts, and their interaction with the sun, the solar wind and satellites • Small bodies, dust and rings, including asteroids, comets and zodiacal light and their interaction with the solar radiation and the solar wind • Exobiology, including origin of life, detection of planetary ecosystems and pre-biological phenomena in the solar system and laboratory simulations • Extrasolar systems, including the detection and/or the detectability of exoplanets and planetary systems, their formation and evolution, the physical and chemical properties of the exoplanets • History of planetary and space research
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