Abstract

Many national and international initiatives rely on spatially explicit information on soil organic carbon (SOC) stock change at multiple scales to support policies aiming at land degradation neutrality and climate change mitigation. In this study, we used regression cokriging with random forest and spatial stochastic cosimulation to predict the SOC stock change between two years (i.e. 1992 and 2010) in Hungary at multiple aggregation levels (i.e. point support, 1 × 1 km, 10 × 10 km square blocks, Hungarian counties and entire Hungary). We also quantified the uncertainty associated with these predictions in order to identify and delimit areas with statistically significant SOC stock change. Our study highlighted that prediction of spatial totals and averages with quantified uncertainty requires a geostatistical approach and cannot be solved by machine learning alone, because it does not account for spatial correlation in prediction errors. The total topsoil SOC stock for Hungary was predicted to increase between 1992 and 2010 with 14.9Tg, with lower and upper limits of a 90% prediction interval equal to 11.2Tg and 18.2Tg, respectively. Results also showed that both the predictions and uncertainties of the average SOC stock change were smaller for larger spatial supports, while spatial aggregation also made it easier to obtain statistically significant SOC stock changes. The latter is important for carbon accounting studies that need to prove in Measurement, Reporting and Verification protocols that observed SOC stock changes are not only practically but also statistically significant.

Highlights

  • Soil is the largest terrestrial pool of organic carbon (Stockmann et al, 2013)

  • We found that parent material, geomorphometric parameters and climate attributes were informative covariates in both random forest (RF) models

  • This could be important from a practical point of view because it means that the absolute value of Soil organic carbon (SOC) stock change decreases as the size of area for which spatial prediction is required increases

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Summary

Introduction

Soil is the largest terrestrial pool of organic carbon (Stockmann et al, 2013). Soil organic carbon (SOC) directly or indirectly influences various soil-related functions and services, such as food production and climate change mitigation. If the ob­ servations on SOC stock are only detailed in space and not so much in time (e.g. SOC stock was only measured at two points in time), building an explicit space–time model is not possible. In such a case, a different approach must be used.

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