4.5 Article

Recalibration of existing pedotransfer functions to estimate soil bulk density at a regional scale

期刊

EUROPEAN JOURNAL OF SOIL SCIENCE
卷 73, 期 3, 页码 -

出版社

WILEY
DOI: 10.1111/ejss.13244

关键词

pedotransfer function; recalibration; regional-scale databases; reliability test; soil properties; SoilGrids system

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Soil bulk density (rho(b)) is an important indicator of soil quality and productivity. This study evaluates the performance of recalibrating existing Pedotransfer functions (PTFs) for rho(b) estimation using new observations. The results show that recalibration of PTFs reduces errors and provides comparable or better performance than developing new PTFs. This provides a viable alternative for estimating rho(b) in data-scarce regions.
Soil bulk density (rho(b)) is an important indicator of soil quality, productivity, compaction and porosity. Despite its importance, rho(b) is often omitted from global datasets due to the costs of making many direct rho(b) measurements and the difficulty of direct measurement on rocky, sandy, very dry, or very wet soils. Pedotransfer functions (PTFs) are deployed to address these limitations. Using readily available soil properties, PTFs employ estimator equations to fit existing datasets to estimate properties like rho(b). However, PTF performance often declines when applied to soils outside those in the training dataset. Potentially, recalibrating existing PTFs using new observations would leverage the power of large datasets used in the original PTF derivation, while updating information based on new soil observations. Here, we evaluate such a recalibration approach for rho(b) estimation, benchmarking its performance against two alternatives: the original, uncalibrated PTFs, and novel, local PTFs derived solely from new soil observations. Using a rho(b) dataset of N = 360 total observations obtained in West Azerbaijan, Iran, we varied the local dataset size (with N = 15, 30, 60, and 360) and recalibrated four existing PTFs with these data. Local PTFs were generated based on stepwise multiple linear regression for the same datasets. The same PTFs (original, recalibrated, and local) were also applied to the study area, and the resulting rho(b) estimates were compared with the global SoilGrids dataset. Recalibration of PTFs reduced errors relative to the original uncalibrated PTFs; for instance, the NSE increased from -22.07 to 0.30 (uncalibrated) to 0.20-0.41 (recalibrated), and RMSE decreased from 0.12 to 0.60 Mg m(-3) (uncalibrated) to 0.10-0.13 Mg m(-3) (recalibrated). The recalibrated PTFs performance was comparable to or better than local PTFs applied to the same data. Recalibration of existing PTFs with local/regional uses provides a viable alternative to the use of global datasets or the development of local PTFs in data-scarce regions. Highlights Existing global PTFs were calibrated and tested using a small dataset for local utilisation. Several new local PTFs were also developed using the same datasets. Recalibration of existing global PTFs is comparable to or more accurate than developing new PTFs.

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