Abstract

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.

Highlights

  • Soils are significant natural resources for the survival of humanity

  • Studies have shown over the years that the conservation of soil organic carbon (SOC) concentrations is strongly linked to biological activity and agricultural productivity [2]

  • The spectra measured in the field slightly differ from those measured in the laboratory wet conditions, which may be caused by differences in environmental conditions, mainly soil water content, as anticipated, such as soil moisture generally increasing spectral absorption of soil compared to dry samples [46]; water replacing the air within soil voids, causing an increase in the forward scattering of light and increasing the absorption of soil at each wavelength [47,48]

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Summary

Introduction

Soils are significant natural resources for the survival of humanity. Substantially more carbon is stockpiled in the world’s soils than is present in global vegetation and atmosphere combined [1]. Maintaining SOC contents above critical limits for specific ecological and climatic zones will help to protect soil resources and maintain crop yields, contributing to global food security [3]. Spectroscopy, being the analysis of the interaction of visible-infrared wavelengths with soil properties, provides information on soil particle size and information on the soil matrix. Another attractive feature of spectroscopy is that spectra can be recorded, at points or by imaging, from different platforms; by proximal sensing in the field, in the laboratory using sampled material, or from remote sensing platforms with multi- and hyperspectral capabilities. In laboratory and field environments, the spectroscopy technique is increasingly used to predict numerous soil constituents based on their diagnostic spectral features and approaches to statistical regression [8]

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