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月表高纬的月船三号 APXS 元素丰度测量。

Chandrayaan-3 APXS elemental abundance measurements at lunar high latitude.

机构信息

Physical Research Laboratory (PRL), Ahmedabad, India.

Department of Geology, Hemvati Nandan Bahuguna University, Srinagar Garhwal, India.

出版信息

Nature. 2024 Sep;633(8029):327-331. doi: 10.1038/s41586-024-07870-7. Epub 2024 Aug 21.

DOI:10.1038/s41586-024-07870-7
PMID:39169194
Abstract

The elemental composition of the lunar surface provides insights into mechanisms of the formation and evolution of the Moon. The chemical composition of lunar regolith have so far been precisely measured using the samples collected by the Apollo, Luna and Chang'e 5 missions, which are from equatorial to mid-latitude regions; lunar meteorites, whose location of origin on the Moon is unknown; and the in situ measurement from the Chang'e 3 and Chang'e 4 missions, which are from the mid-latitude regions of the Moon. Here we report the first in situ measurements of the elemental abundances in the lunar southern high-latitude regions by the Alpha Particle X-ray Spectrometer (APXS) experiment aboard the Pragyan rover of India's Chandrayaan-3 mission. The 23 measurements in the vicinity of the Chandrayaan-3 landing site show that the local lunar terrain in this region is fairly uniform and primarily composed of ferroan anorthosite (FAN), a product of the lunar magma ocean (LMO) crystallization. However, observation of relatively higher magnesium abundance with respect to calcium in APXS measurements suggests the mixing of further mafic material. The compositional uniformity over a few tens of metres around the Chandrayaan-3 landing site provides an excellent ground truth for remote-sensing observations.

摘要

月球表面的元素组成提供了关于月球形成和演化机制的深入了解。迄今为止,对阿波罗、月球和嫦娥五号任务采集的样本进行了精确的化学组成测量,这些样本来自赤道到中纬度地区;对月球陨石进行了测量,这些月球陨石的起源位置未知;还对嫦娥三号和嫦娥四号任务进行了原位测量,这些任务来自月球的中纬度地区。在这里,我们报告了印度 Chandrayaan-3 任务 Pragyan 漫游者上的 Alpha 粒子 X 射线光谱仪 (APXS) 实验首次对月球南部高纬度地区元素丰度的原位测量结果。在 Chandrayaan-3 着陆点附近的 23 次测量结果表明,该地区的当地月球地形相当均匀,主要由斜长质富铁辉长岩 (FAN) 组成,这是月球岩浆海洋 (LMO) 结晶的产物。然而,APXS 测量中观察到镁相对于钙的相对较高丰度表明存在进一步的镁铁质物质混合。Chandrayaan-3 着陆点周围几十米范围内的组成均匀性为遥感观测提供了极好的地面实况。

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本文引用的文献

1
A changing thermal regime revealed from shallow to deep basalt source melting in the Moon.月球浅层至深层玄武岩源区熔融所揭示的热状态变化
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