4.7 Article

Comparison on Quantitative Analysis of Olivine Using MarSCoDe Laser-Induced Breakdown Spectroscopy in a Simulated Martian Atmosphere

Journal

REMOTE SENSING
Volume 14, Issue 21, Pages -

Publisher

MDPI
DOI: 10.3390/rs14215612

Keywords

MarSCoDe; Tianwen-1; laser-induced breakdown spectroscopy; preprocessing; quantitative analysis; olivine; simulated Martian atmosphere

Funding

  1. National Natural Science Foundation of China (NSFC) [11904378]
  2. Key Laboratory of Space Active Opto-electronics Technology, CAS [CXJJ22S019]
  3. Key Laboratory of Lunar and Deep Space Exploration, CAS [LDSE201904]
  4. NaturalScience Foundation of Shanghai [22ZR1472400]
  5. Pre-research project on Civil Aerospace Technologies [D020102]
  6. China National Space Administration (CNSA)
  7. National Natural Science Foundation [U1931211]

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MarSCoDe instrument on Zhurong rover utilizes LIBS to conduct rapid multi-elemental analysis of minerals, rocks and soils on Mars surface. By testing olivine samples with gradient concentrations, it is found that methods like elastic net and PLSR are more effective in analysis.
A Mars Surface Composition Detector (MarSCoDe) instrument mounted on Zhurong rover of Tianwen-1, adopts Laser-Induced Breakdown Spectroscopy (LIBS), with no sample preparation or dust and coatings ablation required, to conduct rapid multi-elemental analysis and characterization of minerals, rocks and soils on the surface of Mars. To test the capability of MarSCoDe LIBS measurement and quantitative analysis, some methods of multivariate analysis on olivine samples with gradient concentrations were inspected based on the spectra acquired in a Mars-simulated environment before the rover launch in 2020. Firstly, LIBS spectra need preprocessing, including background subtraction, random signal denoising, continuum baseline removal, spectral drift correction and wavelength calibration, radiation calibration, and multi-channel spectra subset merging. Then, the quantitative analysis with univariate linear regression (ULR) and multivariate linear regression (MLR) are performed on the characteristic lines, while principal component regression (PCR), partial least square regression (PLSR), ridge, least-absolute-shrinkage-and-selection-operator (LASSO) and elastic net, and nonlinear analysis with back-propagation (BP) are conducted on the entire spectral information. Finally, the performance on the quantitative olivine analyzed by MarSCoDe LIBS is compared with the mean spectrum and all spectra for each sample and evaluated by some statistical indicators. The results show that: (1) the calibration curve of ULR constructed by the characteristic line of magnesium and iron indicates the linear relationship between the spectral signal and the element concentration, and the limits of detection of forsterite and fayalite is 0.9943 and 2.0536 (c%) analyzed by mean spectra, and 2.3354 and 3.8883 (c%) analyzed by all spectra; (2) the R-2 value on the calibration and validation of all the methods is close to 1, and the predicted concentration estimated by these calibration models is close to the true concentration; (3) the shrinkage or regularization technique of ridge, LASSO and elastic net perform better than the ULR and MLR, except for ridge overfitting on the testing sample; the best results can be obtained by the dimension reduction technique of PCR and PLSR, especially with PLSR; and BP is more applicable for the sample measured with larger spectral dataset.

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