论文标题
研究橄榄石诊断光谱特征的改良高斯模型及其在太空风化实验中的应用
Study of the Modified Gaussian Model on olivine diagnostic spectral features and its applications in space weathering experiments
论文作者
论文摘要
橄榄石在可见和近红外(VNIR)反射光谱中的吸收特征是其矿物学研究中的关键频谱参数。通常,这些光谱参数可以通过使用适当的连续性去除来利用修饰的高斯模型(MGM)来获得。但是,不同的连续图可能会改变这些参数的反卷积结果。本文研究了具有多种化学成分的橄榄石的诊断光谱特征。提出了使用MGM的四种不同的连续性去除方法,用于获得反卷积结果,并引入了预测MG数(FO#)的回归方程。结果表明,在矿物质吸收特征上叠加的不同连续性将使吸收中心移动以及吸收带的形状,宽度和强度发生明显变化。此外,还发现,二阶多项式连续体的对数可以与对数空间中光谱的整体形状相匹配,并且应用的改进的回归方程式用于估计橄榄石主导光谱的化学成分也具有更好的性能。作为一个应用示例,改进的方法应用于脉冲激光辐照的橄榄石晶粒,以模拟和研究对橄榄石诊断光谱特征的空间风化影响。实验证实,空间风化可以使吸收带中心向更长的波长移动。因此,从遥感光谱中估计的FO#可能小于其实际的化学成分。这些结果可能会提供有价值的信息,以揭示橄榄石晶粒光谱与以橄榄石为主的小行星之间的差异。
The absorption features of olivine in visible and near-infrared (VNIR) reflectance spectra are the key spectral parameters in its mineralogical studies. Generally, these spectral parameters can be obtained by exploiting the Modified Gaussian Model (MGM) with a proper continuum removal. However, different continua may change the deconvolution results of these parameters. This paper investigates the diagnostic spectral features of olivine with diverse chemical compositions. Four different continuum removal methods with MGM for getting the deconvolution results are presented and the regression equations for predicting the Mg-number (Fo#) are introduced. The results show that different continua superimposed on the mineral absorption features will make the absorption center shift, as well as the obvious alterations in shape, width, and strength of the absorption band. Additionally, it is also found that the logarithm of a second-order polynomial continuum can match the overall shape of the spectrum in logarithmic space, and the improved regression equations applied to estimate the chemical composition of olivine-dominated spectra also have a better performance. As an application example, the improved approach is applied to pulse laser irradiated olivine grains to simulate and study the space weathering effects on olivine diagnostic spectral features. The experiments confirm that space weathering can make the absorption band center shift toward longer wavelength. Therefore, the Fo# estimated from remote sensing spectra may be less than its actual chemical composition. These results may provide valuable information for revealing the difference between the spectra of olivine grains and olivine-dominated asteroids.