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April 12, 2026Remote Sensing2 citationsOpen Access

A Hapke Physics-Guided Deep Autoencoder for Lunar Hyperspectral Unmixing

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QLQing LinCLChengbao LiuDHDong Han

Key Points

  • The study aims to improve the accuracy of mineral distribution mapping on the Moon using a deep learning approach.
  • Developed PGU-Net, a physics-guided deep autoencoder for nonlinear unmixing of hyperspectral data.
  • Utilized a dual-attention mechanism to enhance spectral feature discrimination.
  • Employed linear mixing in the SSA domain followed by a nonlinear reflectance reconstruction module.
  • Tested on synthetic lunar regolith and terrestrial AVIRIS Cuprite datasets.
  • PGU-Net yielded lower endmember SAD and abundance aRMSE compared to existing methods.
  • Validation on M3 observations showed physically plausible mineral distributions.
  • M3 mineral maps were consistent with Kaguya MI products, supporting PGU-Net's effectiveness.

Abstract

Accurate mapping of lunar mineral distributions is essential for understanding the Moon’s origin and evolution and for enabling future in situ resource utilization (ISRU). Yet mineralogical inversion from orbital hyperspectral observations remains challenging due to limited spatial resolution, complex photometric conditions, and sparse returned samples. We present PGU-Net, a Hapke physics-guided deep autoencoder for nonlinear blind unmixing of lunar hyperspectral data. The encoder adopts a dual-attention design to enhance discriminative spectral features. The decoder performs linear mixing in the SSA domain and then reconstructs reflectance through a lightweight nonlinear module, while physics-consistent losses encourage radiative-transfer plausibility. Experiments on a synthetic lunar regolith dataset demonstrate that PGU-Net achieves consistently lower endmember SAD and abundance aRMSE than representative baselines across multiple noise levels. Additional validations on the terrestrial AVIRIS Cuprite benchmark and on Moon Mineralogy Mapper (M3) observations near the Chang’e-5 (CE-5) and Chang’e-6 (CE-6) landing regions yield physically plausible mineral distributions. The M3 maps are broadly consistent with Kaguya MI mineral products and returned-sample constraints, supporting the practicality of PGU-Net for lunar mineralogical mapping.

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Cite This Study

Lin et al. (2026) studied this question.

synapsesocial.com/papers/69db37f94fe01fead37c616ehttps://doi.org/10.3390/rs18081123
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