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Evaluation of a curve-fitting method for diffuse reflectance spectra in the UV-Visible-NIR wavelength region

机译:评估紫外 - 可见 - 近红外波长区域中漫反射光谱的曲线拟合方法

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摘要

The Modified Gaussian Method (MGM) proposed by Sunshine et al. [Sunshine, J.M., Pieters, C.M., Pratt, S.F., 1990. Deconvolution of mineral absorption bands: an improved approach. Journal of Geophysical Research 95, 6955–6966.] is generally used to decompose spectra in the UV–Visible–NIR wavelength region into the characteristic absorption bands of minerals. Here, we compare the optimized results obtained using different curve-fitting methods for this spectrum. The result obtained using the Gaussian function for the absorption band shows a better fit than that obtained using the Lorentzian function. The background continuum of a quadratic polynomial for the wavenumber provides a better result than does the linear function for the wavenumber. We successfully decomposed the spectra of ordinary chondrites and eucrites into the absorption bands of olivine and pyroxene. The wavelength positions of these absorption bands are broadly consistent with the Fe contents of olivine and pyroxene. Although the present results are derived from a limited number of spectra, they are of use in terms of the decomposition of diffuse reflectance spectra.
机译:Sunshine等人提出的改进高斯方法(MGM)。 [Sunshine,J.M.,Pieters,C.M.,Pratt,S.F.,1990。矿物质吸收谱带的反卷积:一种改进的方法。地球物理研究杂志95,6955–6966。]通常用于将UV-Visible-NIR波长区域中的光谱分解为矿物的特征吸收带。在这里,我们比较了使用该曲线的不同曲线拟合方法获得的优化结果。使用高斯函数得到的吸收带结果比使用洛伦兹函数得到的结果更好。与波数的线性函数相比,波数的二次多项式的背景连续性提供了更好的结果。我们成功地将普通球粒陨石和真核晶体的光谱分解为橄榄石和辉石的吸收带。这些吸收带的波长位置与橄榄石和辉石中的Fe含量大致一致。尽管目前的结果是从有限数量的光谱中得出的,但它们在漫反射光谱的分解方面很有用。

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