4.5 Article

Density of soil observations in digital soil mapping: A study in the Mayenne region, France

Journal

GEODERMA REGIONAL
Volume 24, Issue -, Pages -

Publisher

ELSEVIER
DOI: 10.1016/j.geodrs.2021.e00358

Keywords

Digital soil mapping; Topsoil particle-size distribution; Sampling strategy; Sampling density; Prediction performance; Multiple soil classes; France

Categories

Funding

  1. French Scientific Group of Interest on Soils, the GIS Sol
  2. French Ministry for Ecology and Sustainable Development
  3. French Ministry of Agriculture
  4. French Agency for Energy and Environment (ADEME)
  5. French National Research Institute for Agriculture, Food and Environment (INRAE)
  6. French Institute for Research and Development (IRD)
  7. French National Forest Inventory (IFN)
  8. French Agency for Biodiversity
  9. CNES TOSCA program
  10. French Ministry in charge of agriculture
  11. LE STUDIUM Loire Valley Institute for Advanced Studies

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The study found that with increasing density of observations, ordinary kriging (OK) may perform as well or even better than quantile random forest (QRF), depending on particle-size distribution. For silt prediction, OK was systematically better than QRF. However, the prediction intervals were much larger for OK than for QRF, and OK did not seem to estimate uncertainty correctly.
The density of soil observations is a major determinant of digital soil mapping (DSM) prediction accuracy. In this study, we investigated the effect of soil sampling density on the performance of DSM to predict topsoil particle-size distribution in the Mayenne region of France. We tested two prediction algorithms, namely ordinary kriging (OK) and quantile random forest (QRF). The study area is a region of similar to 5000 km(2) with the highest density of field soil observations in France (1 profile per 0.64 km(2)). The number of training sites was progressively reduced (from n = 7500 to n = 400, corresponding to 1 profile per 0.7 km(2) to 1 profile per 13 km(2)) to simulate the different density of observations. For OK and QRF, we tested random subsampling for splitting the data into training and testing datasets using k-fold cross validation. For QRF we also tested conditioned Latin hypercube sampling based on the point coordinates or the covariates. The results indicated that, with increasing density of observations, OK performed as well or even better than QRF, depending on the particle-size fraction. For silt prediction, OK was systematically better than QRF. However, the prediction intervals were much larger for OK than for QRF, and OK did not seem to estimate uncertainty correctly. Overall, the performance indicators increased with the density of observations with a threshold at about 1 profile per 2 km(2) which suggests that the main limitation of DSM prediction accuracy using QRF is the amount of data collected in the field, not the type of calibration sampling strategy. Future DSM activities should focus on gathering more field observations. (C) 2021 Elsevier B.V. All rights reserved.

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