Abstract

Diffuse reflectance spectroscopy (DRS), including visible and near-infrared (VNIR) and mid-infrared (MIR) radiation, is a rapid, accurate and cost-effective technique for estimating soil organic carbon (SOC). We examined 24 soil cores (0–100 cm) from the Sygera Mountains on the Qinghai–Tibet Plateau, considering field-moist intact VNIR, air-dried ground VNIR and air-dried ground MIR spectra at 5-cm intervals. Preprocessed spectra were used to predict the SOC in the soil cores using partial least squares regression (PLSR) and a support vector machine (SVM). The SVM models performed better with three predictors, with the ratio of performance to inter-quartile distance (RPIQ) and R2 values typically exceeding 1.74 and 0.73, respectively. The SVM using the DRS technique indicated accurate predictive results of SOC in each core. The RPIQ values of the shrub meadow, forest and total dataset prediction using air-dried ground VNIR were 1.97, 2.68 and 1.99, respectively; the values using field-moist intact VNIR were 1.95, 2.07 and 1.76 and those using air-dried ground MIR were 1.78, 1.96 and 1.74, respectively. We conclude that the DRS technique is an efficient and rapid method for SOC prediction and has the potential for dynamic monitoring of SOC stock density on the Qinghai–Tibet Plateau.

Highlights

  • Carbon is an essential component of all organic matter

  • We investigated the predictive ability in individual soil cores using visible and near-infrared (VNIR) and MIR spectra

  • According to research by Kuang and Mouazen[12], the variability in the range of soil organic carbon (SOC) content is a crucial factor influencing the accuracy of calibration models, and the results revealed that a larger standard deviation (SD) and wider range explained the variability of SOC content and led to a larger R2 and RPD and a larger root mean squared error in prediction (RMSEP)

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Summary

Introduction

Carbon is an essential component of all organic matter. The carbon cycle and its spatial distribution are intimately involved in the maintenance, development and stability of an ecosystem. Chen et al.[5] compared the prediction accuracy of the PLSR models using VNIR and MIR spectra of air-dried ground arable soil samples. This research focused on the following objectives: 1) to analyse soil spectral characterizations in cores under field-moist intact and air-dried ground conditions using VNIR and MIR spectra; 2) to compare the prediction accuracy using different spectral regions (VNIR and MIR), pre-treatments (field-moist intact and air-dried ground) and modelling approaches; and 3) to quantify the prediction errors of SOC at different depths and in individual soil cores, as well as the difference in organic carbon stock density (SOCD) at depths of 0–30 cm between measured and predicted values

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