High methane uptake from soils of low and high density radiata pine afforestations compared to herbaceous systems
During a one-year period, methane (CH4) fluxes from soil were studied in a southern temperate region system using a static chamber technique. Four treatments on neighboring areas with similar environmental characteristics but different vegetation cover were considered: a natural grassland (NG), an a...
| Autores principales: | , , , , , , |
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| Formato: | Artículo |
| Lenguaje: | Inglés |
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Taylor and Francis
2020
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| Acceso en línea: | http://hdl.handle.net/20.500.12123/7440 https://www.tandfonline.com/doi/abs/10.1080/10549811.2020.1745653?journalCode=wjsf20 https://doi.org/10.1080/10549811.2020.1745653 |
| _version_ | 1855484009974333440 |
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| author | De Bernardi, María Priano, María Eugenia Fusé, Victoria Fernandez, María Elena Gyenge, Javier Guzmán, Sergio Julianera, María |
| author_browse | De Bernardi, María Fernandez, María Elena Fusé, Victoria Guzmán, Sergio Gyenge, Javier Julianera, María Priano, María Eugenia |
| author_facet | De Bernardi, María Priano, María Eugenia Fusé, Victoria Fernandez, María Elena Gyenge, Javier Guzmán, Sergio Julianera, María |
| author_sort | De Bernardi, María |
| collection | INTA Digital |
| description | During a one-year period, methane (CH4) fluxes from soil were studied in a southern temperate region system using a static chamber technique. Four treatments on neighboring areas with similar environmental characteristics but different vegetation cover were considered: a natural grassland (NG), an agricultural land (AL), a low tree density radiata pine afforestation (P1 – suitable for silvopastoral use), and a dense radiata pine afforestation (P2). CH4 uptake increased in the following order: AL < NG < P1 and P2 (statistically significant differences), without differences between P1 and P2. CH4 fluxes were mainly influenced by soil water content (R = 0.78; p = .0001) and bulk density (R = 0.75; p = .0004) indicating that CH4 uptake by soils is primarily connected to methane soil diffusivity. The statistical differences of these parameters could partially justify CH4 flux differences found among treatments. However, a multiple linear regression analysis indicated that other factors such as soil temperature also control CH4 fluxes (R2 = 0.86, p≪4x10−6), and could explain temporal patterns. Results suggest that the low tree density afforestations, suitable for silvopastoral use, have a functional role (CH4 uptake) similar to that of dense forests, and could be a good option to mitigate CH4 emissions by livestock and agricultural sector. |
| format | Artículo |
| id | INTA7440 |
| institution | Instituto Nacional de Tecnología Agropecuaria (INTA -Argentina) |
| language | Inglés |
| publishDate | 2020 |
| publishDateRange | 2020 |
| publishDateSort | 2020 |
| publisher | Taylor and Francis |
| publisherStr | Taylor and Francis |
| record_format | dspace |
| spelling | INTA74402024-10-15T10:02:37Z High methane uptake from soils of low and high density radiata pine afforestations compared to herbaceous systems De Bernardi, María Priano, María Eugenia Fusé, Victoria Fernandez, María Elena Gyenge, Javier Guzmán, Sergio Julianera, María Sistemas Agroforestales Agroforestry Systems Suelo Forestal Forest Soils Metano Methane Forestación Forestation Pinus Sistemas Silvopastoriles During a one-year period, methane (CH4) fluxes from soil were studied in a southern temperate region system using a static chamber technique. Four treatments on neighboring areas with similar environmental characteristics but different vegetation cover were considered: a natural grassland (NG), an agricultural land (AL), a low tree density radiata pine afforestation (P1 – suitable for silvopastoral use), and a dense radiata pine afforestation (P2). CH4 uptake increased in the following order: AL < NG < P1 and P2 (statistically significant differences), without differences between P1 and P2. CH4 fluxes were mainly influenced by soil water content (R = 0.78; p = .0001) and bulk density (R = 0.75; p = .0004) indicating that CH4 uptake by soils is primarily connected to methane soil diffusivity. The statistical differences of these parameters could partially justify CH4 flux differences found among treatments. However, a multiple linear regression analysis indicated that other factors such as soil temperature also control CH4 fluxes (R2 = 0.86, p≪4x10−6), and could explain temporal patterns. Results suggest that the low tree density afforestations, suitable for silvopastoral use, have a functional role (CH4 uptake) similar to that of dense forests, and could be a good option to mitigate CH4 emissions by livestock and agricultural sector. EEA Balcarce Fil: De Bernardi, María. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. Universidad Nacional del Centro de la Provincia de Buenos Aires. Facultad de Ciencias Exactas; Argentina. Fil: Priano, María Eugenia. Universidad Nacional del Centro de la Provincia de Buenos Aires. Facultad de Ciencias Exactas; Argentina. Fil: Fusé, Victoria. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. Universidad Nacional del Centro de la Provincia de Buenos Aires. Facultad de Ciencias Exactas; Argentina. Fil: Fernández, María Elena. Instituto Nacional de Tecnología Agropecuaria (INTA). Estación Experimental Agropecuaria Balcarce; Argentina Consejo Nacional de Investigaciones Científicas y Técnicas (CONICET); Argentina. Fil: Gyenge, Javier. Instituto Nacional de Tecnología Agropecuaria (INTA). Estación Experimental Agropecuaria Balcarce. Agencia de Extensión Rural Tandil Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas (CONICET); Argentina. Fil: Guzmán, Sergio. Instituto Nacional de Tecnología Agropecuaria (INTA). Estación Experimental Agropecuaria Balcarce. Agencia de Extensión Rural Tandil; Argentina. Fil: Julianera, María P. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. Universidad Nacional del Centro de la Provincia de Buenos Aires. Facultad de Ciencias Exactas; Argentina. 2020-06-18T19:15:14Z 2020-06-18T19:15:14Z 2020-03-26 info:ar-repo/semantics/artículo info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion http://hdl.handle.net/20.500.12123/7440 https://www.tandfonline.com/doi/abs/10.1080/10549811.2020.1745653?journalCode=wjsf20 1054-9811 1540-756X https://doi.org/10.1080/10549811.2020.1745653 eng info:eu-repo/semantics/restrictedAccess application/pdf Taylor and Francis Journal of Sustainable Forestry (2020) |
| spellingShingle | Sistemas Agroforestales Agroforestry Systems Suelo Forestal Forest Soils Metano Methane Forestación Forestation Pinus Sistemas Silvopastoriles De Bernardi, María Priano, María Eugenia Fusé, Victoria Fernandez, María Elena Gyenge, Javier Guzmán, Sergio Julianera, María High methane uptake from soils of low and high density radiata pine afforestations compared to herbaceous systems |
| title | High methane uptake from soils of low and high density radiata pine afforestations compared to herbaceous systems |
| title_full | High methane uptake from soils of low and high density radiata pine afforestations compared to herbaceous systems |
| title_fullStr | High methane uptake from soils of low and high density radiata pine afforestations compared to herbaceous systems |
| title_full_unstemmed | High methane uptake from soils of low and high density radiata pine afforestations compared to herbaceous systems |
| title_short | High methane uptake from soils of low and high density radiata pine afforestations compared to herbaceous systems |
| title_sort | high methane uptake from soils of low and high density radiata pine afforestations compared to herbaceous systems |
| topic | Sistemas Agroforestales Agroforestry Systems Suelo Forestal Forest Soils Metano Methane Forestación Forestation Pinus Sistemas Silvopastoriles |
| url | http://hdl.handle.net/20.500.12123/7440 https://www.tandfonline.com/doi/abs/10.1080/10549811.2020.1745653?journalCode=wjsf20 https://doi.org/10.1080/10549811.2020.1745653 |
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