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Resumen
Upland soils are the only known biological sink for methane (CH4) by methanotrophic bacteria consumption. This process is mainly limited by the diffusion processes related to the soil's physical characteristics, which can be modified because of changes in land use depending on the soil type, the original system and the new land use converted. Our study focused on determining the differences in soil CH4 uptake because of changes in land use (from natural [ver mas...]
dc.contributor.authorDe Bernardi, María
dc.contributor.authorPriano, María Eugenia
dc.contributor.authorFernandez, María Elena
dc.contributor.authorGyenge, Javier
dc.contributor.authorJuliarena, Maria Paula
dc.date.accessioned2024-03-04T17:29:35Z
dc.date.available2024-03-04T17:29:35Z
dc.date.issued2024-01-30
dc.identifier.issn1475-2743 (Online)
dc.identifier.issn0266-0032 (Print)
dc.identifier.otherhttps://doi.org/10.1111/sum.13017
dc.identifier.urihttp://hdl.handle.net/20.500.12123/16916
dc.identifier.urihttps://bsssjournals.onlinelibrary.wiley.com/doi/10.1111/sum.13017
dc.description.abstractUpland soils are the only known biological sink for methane (CH4) by methanotrophic bacteria consumption. This process is mainly limited by the diffusion processes related to the soil's physical characteristics, which can be modified because of changes in land use depending on the soil type, the original system and the new land use converted. Our study focused on determining the differences in soil CH4 uptake because of changes in land use (from natural grassland to agricultural land and two Pinus radiata afforestation, differing in thinning management) and on determining which are the main drivers that control CH4 uptake in the studied soil type (Hapludoll), with focus on the diffusion process. CH4 fluxes were measured 12 times with the static chamber technique between October 2015 and April 2019. Also, CH4 gradient concentration in the soil profile and physical and chemical variables were measured on the same dates. All land uses studied acted as net CH4 sinks. Land-use change from grassland to agriculture decreased soil CH4 uptake (~37% ± 19), whereas afforestation increased (~85% ± 73) this environmental service related to natural grassland. We found that the main drivers that control CH4 uptake in this soil are water and air-filled pore space, variables that govern soil CH4 diffusion; they are mostly related to differences in bulk density (compaction) among land uses. Organic matter was also an important driver, mainly related to soil structure. Land-use change affected all of these drivers. CH4 concentration presented differences at deeper soil layers only in the two afforestations, which differed in management (pruning and thinning vs. no management). However, CH4 uptake did not present significant differences between them, suggesting that there is no need for a high tree cover to increase the CH4 sink of the soil. This mixed tree and herbaceous cover may result in a similar environmental service output, increasing the options of land uses.eng
dc.formatapplication/pdfes_AR
dc.language.isoenges_AR
dc.publisherWileyes_AR
dc.rightsinfo:eu-repo/semantics/restrictedAccesses_AR
dc.rights.urihttp://creativecommons.org/licenses/by-nc-sa/4.0/es_AR
dc.sourceSoil Use and Management 40 (1) : e13017 (January 2024)es_AR
dc.subjectPastizal Naturales_AR
dc.subjectNatural Pastureseng
dc.subjectSuelos Agrícolases_AR
dc.subjectAgricultural Soilseng
dc.subjectPlantación Forestales_AR
dc.subjectForest Plantationseng
dc.subjectMetanoes_AR
dc.subjectMethaneeng
dc.subjectSueloes_AR
dc.subjectSoileng
dc.subjectPinuseng
dc.titleNatural grassland conversion to agriculture or pine plantations: Effects on soil methane uptakees_AR
dc.typeinfo:ar-repo/semantics/artículoes_AR
dc.typeinfo:eu-repo/semantics/articlees_AR
dc.typeinfo:eu-repo/semantics/publishedVersiones_AR
dc.rights.licenseCreative Commons Attribution-NonCommercial-ShareAlike 4.0 International (CC BY-NC-SA 4.0)es_AR
dc.description.origenEEA Balcarcees_AR
dc.description.filFil: De Bernardi, María. Universidad Nacional del Centro de la Provincia de Buenos Aires. Facultad de Ciencias Exactas; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. Comisión de Investigaciones Científicas de la Provincia de Buenos Aires; Argentina. Centro de Investigaciones en Física e Ingeniería del Centro de la Provincia de Buenos Aires; Argentina.es_AR
dc.description.filFil: Priano, Maria Eugenia. Universidad Nacional del Centro de la Provincia de Buenos Aires. Facultad de Ciencias Exactas; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. Comisión de Investigaciones Científicas de la Provincia de Buenos Aires; Argentina. Centro de Investigaciones en Física e Ingeniería del Centro de la Provincia de Buenos Aires; Argentina.es_AR
dc.description.filFil: Fernández, María Elena. Instituto Nacional de Tecnología Agropecuaria (INTA). Estación Experimental Agropecuaria Balcarce; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. Instituto de Innovación para la Producción Agropecuaria y el Desarrollo Sostenible; Argentina.es_AR
dc.description.filFil: Gyenge, Javier. Instituto Nacional de Tecnología Agropecuaria (INTA). Estación Experimental Agropecuaria Balcarce; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. Instituto de Innovación para la Producción Agropecuaria y el Desarrollo Sostenible; Argentina.es_AR
dc.description.filFil: Juliarena, Maria Paula. Universidad Nacional del Centro de la Provincia de Buenos Aires. Facultad de Ciencias Exactas; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. Comisión de Investigaciones Científicas de la Provincia de Buenos Aires; Argentina. Centro de Investigaciones en Física e Ingeniería del Centro de la Provincia de Buenos Aires; Argentina.es_AR
dc.subtypecientifico


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