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Spatial variability of soil organic carbon fractions in areas under cultivation of Amazonian species in the southern region of Amazonas state, Brazil

dc.contributorCNPq, CAPESen-US
dc.creatorPraça, José Igor Silva Praça Igor Silva
dc.creatorEnck, Bruna Firmino
dc.creatorCampos, Milton Cesar Costa
dc.creatorPereira, Marcos Gervasio
dc.creatorSouza, Fernando Gomes
dc.creatorMantovanelli, Bruno Campos
dc.creatorBrito Filho, Elilson Gomes
dc.creatorSilva, Laercio Santos
dc.creatorCunha, Jose Mauricio
dc.date2023-08-29
dc.date.accessioned2024-03-11T15:11:46Z
dc.date.available2024-03-11T15:11:46Z
dc.identifierhttps://www.rcia.uc.cl/index.php/ijanr/article/view/2446
dc.identifier10.7764/ijanr.v50i2.2446
dc.identifier.urihttps://revistaschilenas.uchile.cl/handle/2250/240586
dc.descriptionSoil organic carbon (OC) is heterogeneous and sensitive to agricultural management, so knowledge of its spatial variability can improve the monitoring of areas under anthropogenic influence, as OC can serve as a sensitive indicator of changes in the environment. The objective of this study was to evaluate the spatial variability of soil OC fractions in areas of cultivation with Amazonian species in the southern region of Amazonas state. A total of 256 georeferenced data points were collected in the 0.0–0.05 m and 0.05–0.10 m layers in the following agricultural systems: areas with cultivation of Guaraná, Annatto, Cupuaçu and forest. The OC contents were analyzed, and the chemical fractionation of soil organic matter was performed. The analytical results were evaluated through descriptive statistical analysis, and the spatial pattern was evaluated through geostatistical analysis. The conversion of natural ecosystems to agricultural systems affected the rates of addition and decomposition of soil organic matter. Changes in soil organic carbon stocks (SOC stock) due to the uses of different agricultural systems were determined by evaluating the free light fraction of soil organic matter. For the chemical fractions of organic matter, there was a predominance of the humin fraction (C-HU) in relation to the fractions of humic acid (C-FAH), fulvic acid (C-FAF) and OC associated with minerals (COAM) in the different land uses and soil layers analyzed. The geostatistical procedures proved to be important in determining the degree of carbon dependence and its fractionation in the context of spatial variability, and this information is useful in soil quality monitoring.en-US
dc.formatapplication/pdf
dc.languageeng
dc.publisherPontificia Universidad Católica de Chileen-US
dc.relationhttps://www.rcia.uc.cl/index.php/ijanr/article/view/2446/1433
dc.relationhttps://www.rcia.uc.cl/index.php/ijanr/article/downloadSuppFile/2446/857
dc.relationhttps://www.rcia.uc.cl/index.php/ijanr/article/downloadSuppFile/2446/858
dc.relationhttps://www.rcia.uc.cl/index.php/ijanr/article/downloadSuppFile/2446/859
dc.rightsCopyright (c) 2023 International Journal of Agriculture and Natural Resourcesen-US
dc.rightshttp://creativecommons.org/licenses/by/4.0en-US
dc.sourceInternational Journal of Agriculture and Natural Resources; Vol 50, No 2 (2023)en-US
dc.sourceInternational Journal of Agriculture and Natural Resources; Vol 50, No 2 (2023)es-ES
dc.source2452-5731
dc.source2452-5731
dc.subjectsoil science, natural resources, soil carbonen-US
dc.subjectsoil attributes, chemical fractionation, forest, geostatistics, mapping.en-US
dc.titleSpatial variability of soil organic carbon fractions in areas under cultivation of Amazonian species in the southern region of Amazonas state, Brazilen-US
dc.typeinfo:eu-repo/semantics/article
dc.typeinfo:eu-repo/semantics/publishedVersion
dc.typeen-US
dc.typees-ES


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