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Use of clustering with partial least squares regression for predictions based on hyperspectral data

机译:基于高光谱数据的预测,使用群集与部分最小二乘回归

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Visible and near-infrared (VNIR) diffuse reflectance spectroscopy (DRS) has proven to be effective tools of estimation of soil properties. Regression models are usually calibrated on the entire datasets without its stratification. This paper discusses how clustering of the soil spectra improves prediction of basic soil properties: contents of sand, clay, soil organic carbon (SOC) and total nitrogen, as well as the cation exchange capacity (CEC) and total exchangeable bases (TEB). The analysis was performed on a set of 212 soil samples collected from surface horizons throughout the area of arable lands in Poland. Spectral measurements were done using ASD Fildspec PRO with attached Source Probe Mug-Lite in the wavelength range of 350-2500 nm. First, partial least squares (PLS) regression models using the raw spectra and their first derivatives were calibrated on the entire dataset. Then, the observations (soil samples) were clustered using the Ward and K-mean methods based both on the raw and the transformed spectral data. The PLS regression modeling fitted separately within each cluster was performed. Our findings indicate that clustering is potentially useful to enhance the prediction of soil properties based on the DSR data when using the PLS regression modeling. In a practical application to a given set of soil samples, one needs to implement a two-step procedure recommended in this paper. In the first step, one runs a cross-validation analysis in order to identify the best combination of the spectra transformation, the type of the clustering method, and the number of clusters. In the second step, the best combination is applied to the whole dataset for prediction purposes. The improvement achieved by the described procedure ranges from 24 to 49 % reduction in the cross validation root mean squared error.
机译:可见和近红外(VNIR)漫反射光谱(DRS)已被证明是有效的土壤性质估算工具。回归模型通常在整个数据集上校准而无需其分层。本文讨论了土壤光谱的聚类如何改善基本土壤性质的预测:砂,粘土,土壤有机碳(SoC)和总氮的含量,以及阳离子交换能力(CEC)和总可交换碱(TEB)。在波兰耕地面积的各个地区从地表视野中收集的一组212种土壤样品进行了分析。使用ASD FIDSPEC PRO与连接源探针杯Lite的波长范围为350-2500nm的光谱测量。首先,校正使用原始光谱的部分最小二乘(PLS)回归模型在整个数据集上校准。然后,使用基于RAW和变换的光谱数据的病房和K均值方法聚集观察(土壤样品)。执行PLS回归建模在每个集群内部拟合。我们的研究结果表明,在使用PLS回归建模时,聚类可能在基于DSR数据的基于DSR数据来增强土壤性质的预测。在给定一套土壤样本的实际应用中,需要实施本文推荐的两步程序。在第一步中,一个运行交叉验证分析,以识别光谱转换的最佳组合,聚类方法的类型和簇的数量。在第二步中,最佳组合应用于整个数据集以进行预测目的。所描述的过程实现的改进范围为24至49±49 %的交叉验证根均方平方误差。

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