Fraunhofer line-based wavelength-calibration method without calibration targets for planetary lander instruments

IF 1.8 4区 物理与天体物理 Q3 ASTRONOMY & ASTROPHYSICS Planetary and Space Science Pub Date : 2024-01-01 DOI:10.1016/j.pss.2023.105835
Shoki Mori , Yuichiro Cho , Haruhisa Tabata , Koki Yumoto , Ute Böttger , Maximilian Buder , Enrico Dietz , Till Hagelschuer , Heinz-Wilhelm Hübers , Shingo Kameda , Emanuel Kopp , Olga Prieto-Ballesteros , Fernando Rull , Conor Ryan , Susanne Schröder , Tomohiro Usui , Seiji Sugita
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Abstract

High-accuracy wavelength calibration is critical for qualitative and quantitative spectroscopic measurements. Many spectrometers employed in planetary-exploration missions have onboard calibration sources, including standard lamps and calibration targets. However, such calibration sources are not always available because planetary missions, particularly landing missions, usually have limitations in size and mass. Thus, a wavelength calibration method without requiring hardware addition can be highly beneficial. In this study, we demonstrate a method for wavelength calibration using solar Fraunhofer lines observed in the reflectance spectra of planetary surfaces. Using a Raman spectrometer prototype developed for a Phobos rover, we measured the spectrum of the sunlight reflected from a spectral standard, manufactured to provide similar reflectance spectra to the surface of Phobos. We identified 35 Fraunhofer absorption lines in the wavelength range between 530 and 700 nm and utilized these features for the wavelength calibration of the spectrometer. This approach using Fraunhofer lines achieved good results (better than +0.04/−0.06 nm), comparable to the results achieved using a conventional Ne lamp. The wavelength accuracy corresponds to a wavenumber accuracy better than ±1.5 cm−1 in the 0–4000 cm−1 Raman shift (Stokes shift) range with a 532 nm excitation laser. This result enabled the estimation of the magnesium number (Mg#) of olivine, achieving a value more precise than 1.5% based on the Raman peak positions. In addition, we examined the number of solar Fraunhofer lines detectable at different wavelength resolutions by binning the solar spectrum acquired in this study. We found that more than 10 Fraunhofer lines could be detected as prominent absorption lines when the wavelength resolution is higher than 1 nm/pix (30 cm−1/pix at 1000 cm−1). This result suggests that the target-free wavelength-calibration method using solar Fraunhofer lines can be applied to other spectrometers simply by observing sunlit planetary surfaces.

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基于弗劳恩霍夫线的波长校准方法,行星着陆器仪器无需校准目标
高精度波长校准对于定性和定量光谱测量至关重要。行星探测任务中使用的许多光谱仪都有机载校准源,包括标准灯和校准目标。然而,由于行星探测任务,尤其是着陆任务,通常在尺寸和质量上都有限制,因此并非总能获得此类校准源。因此,无需增加硬件的波长校准方法将大有裨益。在本研究中,我们展示了一种利用行星表面反射光谱中观测到的太阳弗劳恩霍夫线进行波长校准的方法。我们使用为火卫一漫游车开发的拉曼光谱仪原型,测量了光谱标准反射的太阳光光谱,该光谱标准是为提供与火卫一表面相似的反射光谱而制造的。我们确定了波长范围在 530 纳米到 700 纳米之间的 35 条弗劳恩霍夫吸收线,并利用这些特征对光谱仪进行波长校准。这种利用弗劳恩霍夫吸收线的方法取得了良好的结果(优于 +0.04/-0.06 nm),与利用传统氖灯取得的结果相当。波长精度相当于 532 nm 激发激光在 0-4000 cm-1 拉曼位移(斯托克斯位移)范围内优于 ±1.5 cm-1 的波长精度。根据这一结果,我们可以根据拉曼峰位置估算橄榄石的镁数(Mg#),其精确度高于 1.5%。此外,我们还通过对本研究中获得的太阳光谱进行分档,考察了在不同波长分辨率下可探测到的太阳弗劳恩霍夫线的数量。我们发现,当波长分辨率高于 1 nm/pix(1000 cm-1 时为 30 cm-1/pix)时,可以检测到 10 条以上的 Fraunhofer 线作为突出的吸收线。这一结果表明,利用太阳弗劳恩霍夫线进行无目标波长校准的方法可以应用于其他光谱仪,只需观测日光行星表面即可。
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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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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