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Error propagation in spectrometric functions of soil organic carbon

机译:土壤有机碳光谱函数中的误差传播

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Abstract. Soil organic carbon (SOC) plays a major role concerning chemical, physical,and biological soil properties and functions. To get a better understandingof how soil management affects the SOC content, the precise monitoring ofSOC on long-term field experiments (LTFEs) is needed. Visible andnear-infrared (Vis–NIR) reflectance spectrometry provides an inexpensive andfast opportunity to complement conventional SOC analysis and has often beenused to predict SOC. For this study, 100 soil samples were collected at anLTFE in central Germany by two different sampling designs. SOC values rangedbetween 1.5 % and 2.9 %. Regression models were built using partial leastsquare regression (PLSR). In order to build robust models, a nested repeated5-fold group cross-validation (CV) approach was used, which comprised modeltuning and evaluation. Various aspects that influence the obtained errormeasure were analysed and discussed. Four pre-processing methods werecompared in order to extract information regarding SOC from the spectra.Finally, the best model performance which did not consider error propagationcorresponded to a mean RMSE _(MV) of 0.12 % SOC ( R ~(2)=0.86 ). This model performance was impaired by Δ RMSE _(MV)=0.04 % SOC while considering input data uncertainties ( ΔR ~(2)=0.09 ), and by Δ RMSE _(MV)=0.12 % SOC( ΔR ~(2)=0.17 ) considering an inappropriatepre-processing. The effect of the sampling design amounted to a Δ RMSE _(MV) of 0.02 % SOC ( ΔR ~(2)=0.05 ). Overall,we emphasize the necessity of transparent and precise documentation of themeasurement protocol, the model building, and validation procedure in orderto assess model performance in a comprehensive way and allow for acomparison between publications. The consideration of uncertaintypropagation is essential when applying Vis–NIR spectrometry for soilmonitoring.
机译:抽象。土壤有机碳(SOC)在涉及化学,物理和生物土壤特性和功能方面起着重要作用。为了更好地了解土壤管理如何影响SOC含量,需要对长期田间试验(LTFE)进行精确的SOC监测。可见和近红外(Vis–NIR)反射光谱法为常规SOC分析提供了廉价且快速的机会,并且经常被用来预测SOC。在本研究中,德国中部的anLTFE通过两种不同的采样设计收集了100个土壤样品。 SOC值介于1.5%和2.9%之间。回归模型是使用偏最小二乘回归(PLSR)建立的。为了构建健壮的模型,使用了嵌套的重复5倍组交叉验证(CV)方法,其中包括模型调整和评估。分析和讨论了影响获得的错误度量的各个方面。为了从光谱中提取关于SOC的信息,比较了四种预处理方法。最后,没有考虑误差传播的最佳模型性能对应于0.12%SOC的平均RMSE _(MV)( R〜(2) = 0.86)。在考虑输入数据不确定性(ΔR〜(2)= 0.09)的情况下,此模型性能会因ΔRMSE _(MV)= 0.04%SOC和ΔRMSE _(MV)= 0.12%SOC(Δ< i> R〜(2)= 0.17)考虑到不合适的预处理。采样设计的影响总计为0.02%SOC的ΔRMSE _(MV)(ΔR〜(2)= 0.05)。总的来说,我们强调必须透明,精确地记录测量规程,模型构建和验证程序,以便以全面的方式评估模型性能并允许出版物之间进行比较。当使用Vis-NIR光谱仪进行土壤监测时,必须考虑不确定度传播。

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