Soil Mapping of Small Fields with Limited Number of Samples by Coupling EMI and NIR Spectroscopy

Precision agriculture relies on highly detailed soil maps to optimize resource use. Proximal sensing methods, such as EMI, require a certain number of soil samples and laboratory analysis to interpolate the characteristics of the soil. NIR diffuse reflectance spectroscopy offers a rapid, low-cost al...

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Main Authors: Leonardo Pace, Simone Priori, Monica Zanini, Valerio Cristofori
Format: Article
Language:English
Published: MDPI AG 2024-12-01
Series:Soil Systems
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Online Access:https://www.mdpi.com/2571-8789/8/4/128
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author Leonardo Pace
Simone Priori
Monica Zanini
Valerio Cristofori
author_facet Leonardo Pace
Simone Priori
Monica Zanini
Valerio Cristofori
author_sort Leonardo Pace
collection DOAJ
description Precision agriculture relies on highly detailed soil maps to optimize resource use. Proximal sensing methods, such as EMI, require a certain number of soil samples and laboratory analysis to interpolate the characteristics of the soil. NIR diffuse reflectance spectroscopy offers a rapid, low-cost alternative that increases datapoints and map accuracy. This study tests and optimizes a methodology for high-detail soil mapping in a 2.5 ha hazelnut grove in Grosseto, Southern Tuscany, Italy, using both EMI sensors (GF Mini Explorer, Brno, Czech Republic) and a handheld NIR spectrometer (Neospectra Scanner, Si-Ware Systems, Menlo Park, CA, USA). In addition to two profiles selected by clustering, another 35 topsoil augerings (0–30 cm) were added. Laboratory analyses were performed on only five samples (two profiles + three samples from the augerings). Partial least square regression (PLSR) with a national spectral library, augmented by the five local samples, predicted clay, sand, organic carbon (SOC), total nitrogen (TN), and cation exchange capacity (CEC). The 37 predicted datapoints were used for spatial interpolation, using the ECa map, elevation, and DEM derivatives as covariates. Kriging with external drift (KED) was used to spatialize the results. The errors of the predictive maps were calculated using five additional validation points analyzed by conventional methods. The validation showed good accuracy of the predictive maps, particularly for SOC and TN.
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spelling doaj-art-3ba7c6f273c74eb5bef2084655274ef02025-08-20T02:57:21ZengMDPI AGSoil Systems2571-87892024-12-018412810.3390/soilsystems8040128Soil Mapping of Small Fields with Limited Number of Samples by Coupling EMI and NIR SpectroscopyLeonardo Pace0Simone Priori1Monica Zanini2Valerio Cristofori3Department of Agriculture and Forest Sciences (DAFNE), University of Tuscia, Via San Camillo de Lellis Snc, 01100 Viterbo, ItalyDepartment of Agriculture and Forest Sciences (DAFNE), University of Tuscia, Via San Camillo de Lellis Snc, 01100 Viterbo, ItalyDepartment of Agriculture and Forest Sciences (DAFNE), University of Tuscia, Via San Camillo de Lellis Snc, 01100 Viterbo, ItalyDepartment of Agriculture and Forest Sciences (DAFNE), University of Tuscia, Via San Camillo de Lellis Snc, 01100 Viterbo, ItalyPrecision agriculture relies on highly detailed soil maps to optimize resource use. Proximal sensing methods, such as EMI, require a certain number of soil samples and laboratory analysis to interpolate the characteristics of the soil. NIR diffuse reflectance spectroscopy offers a rapid, low-cost alternative that increases datapoints and map accuracy. This study tests and optimizes a methodology for high-detail soil mapping in a 2.5 ha hazelnut grove in Grosseto, Southern Tuscany, Italy, using both EMI sensors (GF Mini Explorer, Brno, Czech Republic) and a handheld NIR spectrometer (Neospectra Scanner, Si-Ware Systems, Menlo Park, CA, USA). In addition to two profiles selected by clustering, another 35 topsoil augerings (0–30 cm) were added. Laboratory analyses were performed on only five samples (two profiles + three samples from the augerings). Partial least square regression (PLSR) with a national spectral library, augmented by the five local samples, predicted clay, sand, organic carbon (SOC), total nitrogen (TN), and cation exchange capacity (CEC). The 37 predicted datapoints were used for spatial interpolation, using the ECa map, elevation, and DEM derivatives as covariates. Kriging with external drift (KED) was used to spatialize the results. The errors of the predictive maps were calculated using five additional validation points analyzed by conventional methods. The validation showed good accuracy of the predictive maps, particularly for SOC and TN.https://www.mdpi.com/2571-8789/8/4/128precision agriculturedigital soil mappingelectrical conductivityspectroscopysoil monitoring
spellingShingle Leonardo Pace
Simone Priori
Monica Zanini
Valerio Cristofori
Soil Mapping of Small Fields with Limited Number of Samples by Coupling EMI and NIR Spectroscopy
Soil Systems
precision agriculture
digital soil mapping
electrical conductivity
spectroscopy
soil monitoring
title Soil Mapping of Small Fields with Limited Number of Samples by Coupling EMI and NIR Spectroscopy
title_full Soil Mapping of Small Fields with Limited Number of Samples by Coupling EMI and NIR Spectroscopy
title_fullStr Soil Mapping of Small Fields with Limited Number of Samples by Coupling EMI and NIR Spectroscopy
title_full_unstemmed Soil Mapping of Small Fields with Limited Number of Samples by Coupling EMI and NIR Spectroscopy
title_short Soil Mapping of Small Fields with Limited Number of Samples by Coupling EMI and NIR Spectroscopy
title_sort soil mapping of small fields with limited number of samples by coupling emi and nir spectroscopy
topic precision agriculture
digital soil mapping
electrical conductivity
spectroscopy
soil monitoring
url https://www.mdpi.com/2571-8789/8/4/128
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AT simonepriori soilmappingofsmallfieldswithlimitednumberofsamplesbycouplingemiandnirspectroscopy
AT monicazanini soilmappingofsmallfieldswithlimitednumberofsamplesbycouplingemiandnirspectroscopy
AT valeriocristofori soilmappingofsmallfieldswithlimitednumberofsamplesbycouplingemiandnirspectroscopy