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WU Xing, ZHOU Xiang, LI Keyi, LIU Yang. Principles, Current Status and Prospects of Hydrated Minerals Detection on Mars with Hyperspectral Remote Sensing (in Chinese). Chinese Journal of Space Science, 2025, 45(6): 1482-1491 doi: 10.11728/cjss2025.06.2024-0173
Citation: WU Xing, ZHOU Xiang, LI Keyi, LIU Yang. Principles, Current Status and Prospects of Hydrated Minerals Detection on Mars with Hyperspectral Remote Sensing (in Chinese). Chinese Journal of Space Science, 2025, 45(6): 1482-1491 doi: 10.11728/cjss2025.06.2024-0173

Principles, Current Status and Prospects of Hydrated Minerals Detection on Mars with Hyperspectral Remote Sensing

doi: 10.11728/cjss2025.06.2024-0173 cstr: 32142.14.cjss.2024-0173
  • Received Date: 2024-11-26
  • Rev Recd Date: 2025-01-15
  • Available Online: 2025-01-16
  • Mars is the most Earth-like terrestrial planet in the solar system and a primary focus of deep space exploration. Hydrated minerals, formed through water-rock interactions, are crucial for understanding the planet’s ancient aqueous environments, geological changes, and capacity to support life. Their study offers vital insights into Mars’ climatic evolution and surface processes. Hyperspectral remote sensing, which collects detailed spectral data across hundreds of continuous bands, serves as a powerful tool for detecting and analyzing these minerals. Despite its advantages, hyperspectral detection on Mars faces significant challenges. The sparse distribution and low abundance of hydrated minerals, combined with spectral mixing and noise, diminish the clarity of diagnostic spectral features. Consequently, traditional methods primarily rely on spectral parameter mapping and visual interpretation, which are labor-intensive and struggle to process the vast hyperspectral datasets effectively. Recent advances in machine learning for terrestrial hyperspectral remote sensing offer innovative approaches to Martian mineral mapping, yet their application remains at an early stage. This review first introduces Mars orbital spectral datasets such as the Observatoire pour la Minéralogie, l’Eau, les Glaces et l’Activité (OMEGA) and the Compact Reconnaissance Imaging Spectrometer for Mars (CRISM), and diagnostic spectral features of common hydrated minerals. The current state of Martian hydrated mineral detection is then explored, covering both qualitative identification and quantitative abundance retrieval methods. It evaluates the advantages and limitations of existing approaches and highlights key challenges, such as spectral variability and validation constraints. To advance this field, future work should focus on developing adaptable algorithms, integrating multi-source data, and establishing robust validation frameworks. These efforts will enhance the efficiency and reliability of mineral mapping, providing deeper insights into Mars’ aqueous history and its implications for planetary habitability.

     

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