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Combination of soil texture with Nix color sensor can improve soil organic carbon prediction

•SOC of 371 soil samples was predicted via Nix, PXRF-Rb, and texture.•Combining Nix color parameters and texture showed the best prediction of SOC.•Using PXRF-Rb as a proxy for clay could not produce satisfactory SOC prediction.•Color variables b* and a* extracted by Nix appeared influential in pred...

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Bibliographic Details
Published in:Geoderma 2021-01, Vol.382, p.114775, Article 114775
Main Authors: Swetha, R.K., Chakraborty, Somsubhra
Format: Article
Language:English
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Summary:•SOC of 371 soil samples was predicted via Nix, PXRF-Rb, and texture.•Combining Nix color parameters and texture showed the best prediction of SOC.•Using PXRF-Rb as a proxy for clay could not produce satisfactory SOC prediction.•Color variables b* and a* extracted by Nix appeared influential in predicting SOC. The optimum ecosystem functioning is reliant on soil organic carbon (SOC) content which is traditionally measured in the laboratory via a cumbersome wet-chemistry method. This preliminary research tested whether a combination of Nix color sensor and portable X-ray fluorescence (PXRF) spectrometer data with soil texture data can improve soil SOC prediction accuracy relative to using them independently. A total of 371 samples representing diverse soil texture and SOC content were collected from three different ecoregions of eastern India: coastal saline zone, red and lateritic zone, and Gangetic alluvial zone. All dried, ground, and sieved samples were scanned via Nix and PXRF and random forest (RF) regression was used to predict soil SOC with different combinations of data. Soils were grouped into nine textural classes while soil SOC content exhibited substantial variability (0.08–2.26%). Comparing soil SOC with texture (sand + silt + clay), satisfactory prediction accuracy was observed (validation R2 = 0.70). Combining Nix extracted color parameters with texture substantially improved the model performance, producing the validation determination coefficient of 0.81. In contrast, PXRF-Rb, as a proxy of soil clay content was unable to achieve satisfactory prediction performance (R2 = 0.24), indicating the heterogeneity in soil mineralogical composition. The RF variable importance plot using Nix alone identified redness (a*) and yellowness to blueness (b*) as influential predictors, manifesting the impact of red color from Fe and Al-oxides and their significant negative correlation with soil SOC (r = −0.62 and −0.57 for a* and b*, respectively). These color parameters were again identified by the RF variable importance plot of (Texture + Nix)-model, implying that the SOC prediction improvement may be linked with the Nix sensor’s capability of extracting useful information in the visible range. Summarily, a combination of Nix color variables and texture data was adept at predicting soil SOC in lieu of traditional laboratory analysis. The robustness of the (Texture + Nix)-based SOC prediction model can be augmented by incorporating more soil samples repre
ISSN:0016-7061
1872-6259
DOI:10.1016/j.geoderma.2020.114775