AIC formulae in soil spectroscopy

Partial least squares regression (PLSR) is widely used in soil spectroscopy; however, the methodology used for selection of the optimal number of components remains inconsistent. In this study, we review and compare commonly used formulations of the Akaike Information Criterion (AIC) for selecting PLSR components. Three different AIC formulations reported in the literature were evaluated. To this end, we used visible–near-infrared (vis–NIR) spectra to predict soil organic carbon (SOC; n = 310) and soil texture ( n = 50) data. Despite substantial mathematical differences among the AIC formulations and resulting differences in selected component numbers, model performances—assessed using root mean square error (RMSE), ratio of performance to interquartile distance (RPIQ), and Nash-Sutcliffe model efficiency (NSE) for cross-validation and external validation—were largely similar. Our findings highlight the need for greater awareness regarding AIC formulation and interpretation in soil spectroscopy applications.

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Publication Details

Journal
Geoderma
Published
2026-05-10
DOI
https://doi.org/10.1016/j.geoderma.2026.117833
Primary Topic
Soil Geostatistics and Mapping
Type
article
Field-Weighted Citation Impact
0.00

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article

AIC formulae in soil spectroscopy

H.P. Piepho, T.K.D. Weber, C. Wachendorf, L. Wilke et al.
Geoderma
Soil Geostatistics and Mapping
article

AIC formulae in soil spectroscopy

H.P. Piepho, T.K.D. Weber, C. Wachendorf, L. Wilke, I. Greenberg
article en

Abstract

Partial least squares regression (PLSR) is widely used in soil spectroscopy; however, the methodology used for selection of the optimal number of components remains inconsistent. In this study, we review and compare commonly used formulations of the Akaike Information Criterion (AIC) for selecting PLSR components. Three different AIC formulations reported in the literature were evaluated. To this end, we used visible–near-infrared (vis–NIR) spectra to predict soil organic carbon (SOC; n = 310) and soil texture ( n = 50) data. Despite substantial mathematical differences among the AIC formulations and resulting differences in selected component numbers, model performances—assessed using root mean square error (RMSE), ratio of performance to interquartile distance (RPIQ), and Nash-Sutcliffe model efficiency (NSE) for cross-validation and external validation—were largely similar. Our findings highlight the need for greater awareness regarding AIC formulation and interpretation in soil spectroscopy applications.

GeodermaVol. 470
University of Kassel (DE), University of Hohenheim (DE)
Deutsche Forschungsgemeinschaft
Openalex Percentile: Top 7%
Soil Geostatistics and Mapping
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AIC formulae in soil spectroscopy — H.P. Piepho, T.K.D. Weber, et al. · Geoderma (2026) | TGRS Research Map | TGRS