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Prediction of soil salinity with soil-reflected spectra: A comparison of two regression methods

机译:用土壤反射光谱预测土壤盐分:两种回归方法的比较

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摘要

To achieve the best high spectral quantitative inversion of salt-affected soils, typical saline-sodic soil was selected from northeast China, and the soil spectra were measured; then, partial least-squares regression (PLSR) models and principle component regression(PCR) models were established for soil spectral reflectance and soil salinity, respectively. Modelling accuracies were compared between two models and conducted with different spectrum processing methods and different sampling intervals. Models based on all of the original spectral bands showed that the PLSR was superior to the PCR; however, after smoothing the spectra data, the PLSR did not continue outperforming the PCR. Models established by various transformed spectra after smoothing did not continue showing superiority of the PCR over the PLSR; therefore, we can conclude that the prediction accuracies of the models were not only determined by the smoothing methods, but also by spectral mathematical transformations. The best model was the PCR based on the median filtering data smoothing technique (MF) + log (1/X) + baseline correction transformation (R2 = 0.7206 and RMSE = 0.3929). To keep the information loss becoming too large, this suggested that an 8 nm sampling interval was the best when using soil spectra to predict soil salinity for both the PLSR and PCR models.
机译:为了获得最佳的盐分土壤高光谱定量反演,从中国东北选择了典型的盐碱土,并测量了土壤光谱。然后分别建立了土壤光谱反射率和盐度的偏最小二乘回归模型和主成分回归模型。比较两个模型之间的建模精度,并使用不同的频谱处理方法和不同的采样间隔进行建模。基于所有原始光谱带的模型表明,PLSR优于PCR。但是,在对光谱数据进行平滑处理后,PLSR并没有继续超过PCR。平滑后通过各种变换光谱建立的模型没有继续显示出PCR优于PLSR的优势;因此,我们可以得出结论,模型的预测精度不仅由平滑方法确定,而且还由频谱数学变换确定。最好的模型是基于中值滤波数据平滑技术(MF)+ log(1 / X)+基线校正变换(R 2 = 0.7206和RMSE = 0.3929)的PCR。为了使信息丢失变得太大,这表明在使用土壤光谱预测PLSR和PCR模型的土壤盐度时,最好使用8?nm的采样间隔。

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