Pedosphere (5): 834--845, 2025
ISSN 1002-0160/CN 32-1315/P
©2025 Soil Science Society of China
Published by Elsevier B.V. and Science Press
Accessing global soil raster images and equal-area splines to estimate soil organic carbon stocks on the regional scale
Trevan FLYNN1, Rosana KOSTECKI2, Ansa REBI3, Taqi RAZA4
1 Department of Research, add1Technologies, 11531 Slick Rock Dr., Richmond TX 77406 (USA)
2 Department of Geography, State University of Londrina, Londrina 86055 (Brazil)
3 Jianshui Research Station, School of Soil and Water Conservation, Beijing Forestry University, Beijing 100083 (China)
4 Biosystems Engineering & Soil Science, University of Tennessee, Knoxville TN 37996 (USA)
Corresponding Author:Trevan FLYNN
ABSTRACT
      Soil carbon stock research has gained prominence in environmental studies amidst climate change concerns, especially given that soil is one of the largest terrestrial carbon reserves. Accurate predictions necessitate comprehensive soil profile measurements, which are resource-intensive to obtain. To address this, depth functions are employed to derive continuous estimates, aligning with standardized depths. However, global datasets employing depth functions in raster format have not been widely utilized, which could lower financial costs and improve accuracy in data-scarce regions. Furthermore, research into aggregating depth functions for realistic carbon stock estimations remains limited, offering opportunities to streamline cost and time. The aim of this study was to apply equal-area splines to estimate soil carbon stocks, utilizing SoilGrids and iSDAsoil datasets in a 317-km2 Quaternary catchment (30°48′ E, 29°18′ S) in KwaZulu-Natal, South Africa. Both datasets were resampled to a 250-m resolution, and the splines were interpolated to a depth of 50 cm per pixel. Various aggregation methods were employed in calculation, including the cumulative sum (definite integral), discrete sum (sum of 1-cm spline predictions), and the mean carbon stock (mean to 50 cm). Quantitative evaluation was performed with 310 external soil samples. SoilGrids showed higher predictions (100-546 kg m-2) than iSDAsoil (66.9-225 kg m-2) for the cumulative sum. The discrete sum also exhibited higher prediction values for SoilGrids (293-789 kg m-2) compared to iSDAsoil (228-557 kg m-2). SoilGrids aggregated with the discrete sum closely matched previous studies, estimating total carbon stock for the catchment at 7 126 t, albeit with spatial inconsistencies. However, when evaluating with an external dataset, the results were not satisfactory for any method according to Lin's concordance correlation coefficient (CCC, correlation of a 1:1 line), with all models obtaining a CCC below 0.01. Similarly, all models had a root mean squared error larger than 59 kg m-2. It was concluded that SoilGrids and iSDAsoil were spatially inaccurate in the catchment but can still provide information about the total carbon stock. This method could be improved by obtaining more soil samples for the datasets, incorporating local data into the spline, making the method more computationally efficient, and accounting for discrete horizon boundaries.
Key Words:  depth distribution,depth function,global dataset,Google Earth Engine,normalized difference prediction index,South Africa
Citation: Flynn T, Kostecki R, Rebi A, Raza T. 2025. Accessing global soil raster images and equal-area splines to estimate soil organic carbon stocks on the regional scale. Pedosphere. 35(5):834-845.
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