Using magnetic susceptibility mapping for assessing soil degradation due to water erosion

This study focused on developing a method for estimating topsoil organic carbon content from measured mass-specific magnetic susceptibility in Chernozems heavily affected by water erosion. The study was performed on a 100 ha area, whereby 202 soil samples were taken. A set of soil samples was divide...

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Main Authors: Ondřej JAKŠÍK, Radka KODEŠOVÁ, Aleš KAPIČKA, Aleš KLEMENT, Miroslav FÉR, Antonín NIKODEM
Format: Article
Language:English
Published: Czech Academy of Agricultural Sciences 2016-06-01
Series:Soil and Water Research
Subjects:
Online Access:https://swr.agriculturejournals.cz/artkey/swr-201602-0005_using-magnetic-susceptibility-mapping-for-assessing-soil-degradation-due-to-water-erosion.php
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author Ondřej JAKŠÍK
Radka KODEŠOVÁ
Aleš KAPIČKA
Aleš KLEMENT
Miroslav FÉR
Antonín NIKODEM
author_facet Ondřej JAKŠÍK
Radka KODEŠOVÁ
Aleš KAPIČKA
Aleš KLEMENT
Miroslav FÉR
Antonín NIKODEM
author_sort Ondřej JAKŠÍK
collection DOAJ
description This study focused on developing a method for estimating topsoil organic carbon content from measured mass-specific magnetic susceptibility in Chernozems heavily affected by water erosion. The study was performed on a 100 ha area, whereby 202 soil samples were taken. A set of soil samples was divided into 3 subsets: A (32 samples), B (67 samples), and C (103 samples). The mass-specific magnetic susceptibility using low (χlf) and high (χhf) frequency, and organic carbon content were measured at all soil samples. The contents of iron and manganese, extracted with a dithionite-citrate solution (Fed, Mnd) and ammonium oxalate (Feo, Mno), were quantified in A and B samples. Models for predicting organic carbon content from magnetic susceptibilities were designed as follows: (1) subset A was used as the training set for calibration, and subsets B and C were used as the test sets for model validation, either separately (subset B only), or together (merged subsets B and C); (2) merged subsets A and B were used as the training set and subset C was used as the test set. Results showed very close correlations between organic carbon content and all measured soil properties. Obtained models relating organic carbon content to mass-specific magnetic susceptibility successfully predicted soil organic carbon contents.
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spelling doaj.art-5df0eb525a8b445bb132ac51a3d035612023-02-23T03:48:32ZengCzech Academy of Agricultural SciencesSoil and Water Research1801-53951805-93842016-06-0111210511310.17221/233/2015-SWRswr-201602-0005Using magnetic susceptibility mapping for assessing soil degradation due to water erosionOndřej JAKŠÍK0Radka KODEŠOVÁ1Aleš KAPIČKA2Aleš KLEMENT3Miroslav FÉR4Antonín NIKODEM5Department of Soil Science and Soil Protection, Faculty of Agrobiology, Food and Natural Resources, Czech University of Life Sciences Prague, Prague, Czech Republic;Department of Soil Science and Soil Protection, Faculty of Agrobiology, Food and Natural Resources, Czech University of Life Sciences Prague, Prague, Czech Republic;Institute of Geophysics of the CAS, Prague, Czech RepublicDepartment of Soil Science and Soil Protection, Faculty of Agrobiology, Food and Natural Resources, Czech University of Life Sciences Prague, Prague, Czech Republic;Department of Soil Science and Soil Protection, Faculty of Agrobiology, Food and Natural Resources, Czech University of Life Sciences Prague, Prague, Czech Republic;Department of Soil Science and Soil Protection, Faculty of Agrobiology, Food and Natural Resources, Czech University of Life Sciences Prague, Prague, Czech Republic;This study focused on developing a method for estimating topsoil organic carbon content from measured mass-specific magnetic susceptibility in Chernozems heavily affected by water erosion. The study was performed on a 100 ha area, whereby 202 soil samples were taken. A set of soil samples was divided into 3 subsets: A (32 samples), B (67 samples), and C (103 samples). The mass-specific magnetic susceptibility using low (χlf) and high (χhf) frequency, and organic carbon content were measured at all soil samples. The contents of iron and manganese, extracted with a dithionite-citrate solution (Fed, Mnd) and ammonium oxalate (Feo, Mno), were quantified in A and B samples. Models for predicting organic carbon content from magnetic susceptibilities were designed as follows: (1) subset A was used as the training set for calibration, and subsets B and C were used as the test sets for model validation, either separately (subset B only), or together (merged subsets B and C); (2) merged subsets A and B were used as the training set and subset C was used as the test set. Results showed very close correlations between organic carbon content and all measured soil properties. Obtained models relating organic carbon content to mass-specific magnetic susceptibility successfully predicted soil organic carbon contents.https://swr.agriculturejournals.cz/artkey/swr-201602-0005_using-magnetic-susceptibility-mapping-for-assessing-soil-degradation-due-to-water-erosion.phparable landgeomorphologically diverse areaschernozemmagnetic susceptibilitysoil organic carbonspatial variability
spellingShingle Ondřej JAKŠÍK
Radka KODEŠOVÁ
Aleš KAPIČKA
Aleš KLEMENT
Miroslav FÉR
Antonín NIKODEM
Using magnetic susceptibility mapping for assessing soil degradation due to water erosion
Soil and Water Research
arable land
geomorphologically diverse areas
chernozem
magnetic susceptibility
soil organic carbon
spatial variability
title Using magnetic susceptibility mapping for assessing soil degradation due to water erosion
title_full Using magnetic susceptibility mapping for assessing soil degradation due to water erosion
title_fullStr Using magnetic susceptibility mapping for assessing soil degradation due to water erosion
title_full_unstemmed Using magnetic susceptibility mapping for assessing soil degradation due to water erosion
title_short Using magnetic susceptibility mapping for assessing soil degradation due to water erosion
title_sort using magnetic susceptibility mapping for assessing soil degradation due to water erosion
topic arable land
geomorphologically diverse areas
chernozem
magnetic susceptibility
soil organic carbon
spatial variability
url https://swr.agriculturejournals.cz/artkey/swr-201602-0005_using-magnetic-susceptibility-mapping-for-assessing-soil-degradation-due-to-water-erosion.php
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