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Comparison of Field and Laboratory Wet Soil Spectra in the Vis-NIR Range for Soil Organic Carbon Prediction in the Absence of Laboratory Dry Measurements

机译:在缺失实验室干测量中的土壤有机碳预测中的域和实验室湿土光谱比较

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摘要

Spectroscopy has demonstrated the ability to predict specific soil properties. Consequently, it is a promising avenue to complement the traditional methods that are costly and time-consuming. In the visible-near infrared (Vis-NIR) region, spectroscopy has been widely used for the rapid determination of organic components, especially soil organic carbon (SOC) using laboratory dry (lab-dry) measurement. However, steps such as collecting, grinding, sieving and soil drying at ambient (room) temperature and humidity for several days, which is a vital process, make the lab-dry preparation a bit slow compared to the field or laboratory wet (lab-wet) measurement. The use of soil spectra measured directly in the field or on a wet sample remains challenging due to uncontrolled soil moisture variations and other environmental conditions. However, for direct and timely prediction and mapping of soil properties, especially SOC, the field or lab-wet measurement could be an option in place of the lab-dry measurement. This study focuses on comparison of field and naturally acquired laboratory measurement of wet samples in Visible (VIS), Near-Infrared (NIR) and Vis-NIR range using several pretreatment approaches including orthogonal signal correction (OSC). The comparison was concluded with the development of validation models for SOC prediction based on partial least squares regression (PLSR) and support vector machine (SVMR). Nonetheless, for the OSC implementation, we use principal component regression (PCR) together with PLSR as SVMR is not appropriate under OSC. For SOC prediction, the field measurement was better in the VIS range with R2CV = 0.47 and RMSEPcv = 0.24, while in Vis-NIR range the lab-wet measurement was better with R2CV = 0.44 and RMSEPcv = 0.25, both using the SVMR algorithm. However, the prediction accuracy improves with the introduction of OSC on both samples. The highest prediction was obtained with the lab-wet dataset (using PLSR) in the NIR and Vis-NIR range with R2CV = 0.54/0.55 and RMSEPcv = 0.24. This result indicates that the field and, in particular, lab-wet measurements, which are not commonly used, can also be useful for SOC prediction, just as the lab-dry method, with some adjustments.
机译:光谱学证明了预测特定土壤性质的能力。因此,这是一个有希望的途径,以补充昂贵且耗时的传统方法。在近似红外(Vis-NIR)区域中,光谱学已广泛用于快速测定使用实验室干燥(实验室干)测量的有机组分,尤其是土壤有机碳(SOC)。然而,在环境(房间)温度和湿度下的收集,研磨,筛分和土壤干燥等步骤,这是一个重要的过程,使实验室干燥制剂与现场或实验室潮湿相比有点慢(Lab-湿)测量。由于土壤湿度变化和其他环境条件不受控制地,在现场直接测量的土壤光谱或在湿样品上的使用仍然具有挑战性。然而,对于直接和及时的预测和映射土壤性质,特别是SOC,现场或实验室或实验室湿法测量可以是一种选择实验室干测量。该研究专注于使用包括正交信号校正(OSC)的几种预处理方法(OSC)的视野(VI),近红外(NIR)和Vis-NIR范围的田间和自然获得的湿式样品的实验室测量。基于偏最小二乘回归(PLSR)和支持向量机(SVMR)的SOC预测的验证模型的开发结论了比较。尽管如此,对于OSC实现,我们将主成分回归(PCR)与PLSR一起使用,因为SVMR不适合OSC。对于SOC预测,在VI的VIS范围内具有R2CV = 0.47和RMSEPCV = 0.24的磁场测量,而在VIS-NIR范围内,使用SVMR算法,R2CV = 0.44和RMSEPCV = 0.25的实验室湿测量更好。然而,预测精度随着两个样品的引入而改善了。使用R2CV = 0.54 / 0.55和RMSEPCV = 0.24,使用NIR中的实验室湿数据集(使用PLSR)获得最高预测。该结果表明该字段和尤其是实验室 - 湿测量,不常用,也可用于SoC预测,即作为实验室干法,有一些调整。

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