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Hyperspectral predicting model of soil salinity in Tianjin costal area using partial least square regression

机译:基于偏最小二乘回归的天津滨海地区土壤盐分高光谱预测模型

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Soil salinization is one of the most devastating land degradation process causing agricultural yields reduction. This paper presents a hyperspectral prediction model of soil salinity using partial least squares regression (PLSR) in Tianjin costal area. Soil spectral reflectance of soil samples varying in salinity was measured using an ASD Field Spec spectrometer. The treated continuum-removed (CR) reflectance and first-order derivative reflectance (FDR) were used and compared to explore the more preferable predicting model of soil salinity, which could detect subtle differences in spectral absorption features compared with original reflectance. The results showed that the soil spectra reflectance got distinct absorption feature with peaks centred at 411 nm, 475 nm, 663 nm, 868 nm, 1100 nm ∼ 1250 nm, 1400 nm, 690 nm, 1911 nm, 2206 nm and 2338 nm, representing key bands for soil salt content estimation. Through established Partial Least-Square Regression model based on treated soil spectra, the first derived-continuum-removed reflectance was the optimal spectra indexes, prediction accuracy of the optimal PLSR model was 94.4%.
机译:土壤盐渍化是最严重的土地退化过程之一,导致农业减产。本文利用偏最小二乘回归(PLSR)提出了天津沿海地区土壤盐分的高光谱预测模型。使用ASD现场光谱仪测量盐度变化的土壤样品的土壤光谱反射率。使用经过处理的连续去除率(CR)和一阶导数反射率(FDR)进行比较,以探索更理想的土壤盐分预测模型,该模型可以检测到光谱吸收特征与原始反射率之间的细微差异。结果表明,土壤光谱反射率具有明显的吸收特征,峰集中在411 nm,475 nm,663 nm,868 nm,1100 nm〜1250 nm,1400 nm,690 nm,1911 nm,2206 nm和2338 nm处。土壤盐分含量估算的关键带。通过建立基于处理后的土壤光谱的偏最小二乘回归模型,得出的第一条去除连续谱的反射率是最优光谱指标,最优PLSR模型的预测精度为94.4%。

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