Abstract

In this paper, a self-made, mineral, multi-angle, spectrum measurement device is employed to measure the multi-angle spectra of olivine and plagioclase; the multi-angle spectra of ilmenite in the Reflectance Experiment Laboratory (RELAB) Spectral Library are collected; and the optimized retrieval of the photometric parameters of the Hapke model is realized. Importantly, the derived result of the single-scattering albedo (SSA) is stable and has both mathematical meaning and physical meaning. The derived Legendre polynomial coefficients of the phase function can better simulate the variation in the mineral spectra with angle. This paper compares the effects of multi-angle and single-angle spectral data on the photometric parameter derived results. The setting of the Legendre polynomial coefficient of the scattering phase function mainly affects the simulation accuracy of the mineral spectra as a function of angle. Using this coefficient to optimize the retrieval, the simulation accuracy is moderately improved compared with the single-angle simulation. The estimation of photometric parameters based on multi-angle spectral data can provide a basis for setting the empirical values of the phase function parameters from single-angle spectral calculations, which can more truly reflect the law of reflectance spectra changing with angle than Lucey’s traditional empirical value of the phase function (b = −0.4 and c = 0.25). The results of multi-angle spectra retrieval in this paper show that the Legendre polynomial coefficients of the phase function vary with wavelength rather than being constant and that different minerals differ greatly.

Highlights

  • IntroductionWhen light enters a mineral, part of the light is absorbed, and part of the light is reflected, showing spectral features that are dependent on internal and external factors unique to a sample

  • The results show that the integral of the phase function in the range of 0–4π is not constant to 4π, and the amount of change cπ has nothing to do with the phase angle g

  • Optimized retrieval of the photometric parameters of the Hapke model can be realized by using the multi-angle spectral data

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Summary

Introduction

When light enters a mineral, part of the light is absorbed, and part of the light is reflected, showing spectral features that are dependent on internal and external factors unique to a sample. This behavior is the result of the combined effect of the internal and external conditions of the mineral [1,2]. Studying the variation in spectral features over a range of physical, compositional, and experimental parameters is important for interpreting the internal attributes and external conditions implicit in the spectra [3,4,5,6]

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