Impact of land use change on soil methane fluxes and diffusivity in Pampean plains, Argentina

Upland soils are the main methane (CH4) biological sink, and may be affected by land-use change. Changes in land uses and soil management affect soil properties that control diffusion of gases, which in combination with microbial activity, determine CH4 flux (fCH4) through the soil. Net CH4 fluxes a...

Descripción completa

Detalles Bibliográficos
Autores principales: De Bernardi, María, Priano, María Eugenia, Fernandez, María Elena, Gyenge, Javier, Juliarena, Maria Paula
Formato: info:ar-repo/semantics/artículo
Lenguaje:Inglés
Publicado: Elsevier 2023
Materias:
Acceso en línea:http://hdl.handle.net/20.500.12123/15192
https://www.sciencedirect.com/science/article/pii/S0167880922000159
https://doi.org/10.1016/j.agee.2022.107866
_version_ 1855037263266709504
author De Bernardi, María
Priano, María Eugenia
Fernandez, María Elena
Gyenge, Javier
Juliarena, Maria Paula
author_browse De Bernardi, María
Fernandez, María Elena
Gyenge, Javier
Juliarena, Maria Paula
Priano, María Eugenia
author_facet De Bernardi, María
Priano, María Eugenia
Fernandez, María Elena
Gyenge, Javier
Juliarena, Maria Paula
author_sort De Bernardi, María
collection INTA Digital
description Upland soils are the main methane (CH4) biological sink, and may be affected by land-use change. Changes in land uses and soil management affect soil properties that control diffusion of gases, which in combination with microbial activity, determine CH4 flux (fCH4) through the soil. Net CH4 fluxes and diffusivity -estimated by the CH4 diffusion coefficient- were measured in three common land uses typical from Pampean plains, South America (natural grassland NG; Eucalyptus globulus Labill. afforestation E; and agricultural land AL: oat, soybean and red clover in successive cultivation) during two years (March 2017–March 2019). Methane fluxes in the soil-atmosphere interface were measured using the static chamber technique, and a diffusion model was applied to estimate soil CH4 diffusivity from soil porosity. We aimed to quantify the effect of land use change (both E and AL vs. NG, the reference system) on fCH4 and gas diffusivity due to changes in the soil parameters. Soils were net sinks in the three land uses, with mean CH4 flux higher in the afforestation, intermediate in the natural grassland and lower in the agricultural land (− 10.99 ± 5.85, − 8.9 ± 5.32 and − 4.58 ± 4.19 ng CH4 m−2 s−1, respectively). CH4 fluxes varied significantly through seasons and space coinciding with variations in water-filled pore space and air-filled pore space variables (ρ > 0.7 and <−0.7 respectively; p < 0.05). Land-use change metric for methane flux ΔfCH4 was − 2.1 ± 3.7 and 4.4 ± 2.5 for NG-E and NG-AL, respectively, indicating a significant increment in net CH4 uptake when the natural grassland is afforested and a decrease when it was converted to agricultural use. This change was mainly explained by changes in soil physical properties (bulk density, soil water content, WFPS and air filled porosity). In relation to this, soil CH4 diffusion coefficient followed the same pattern as fCH4 (0.024 ± 0.011; 0.015 ± 0.007 and 0.008 ± 0.007 cm2 s−1 for E, NG and AL respectively); and allowed us to recalculate mean CH4 fluxes. Theoretical and in situ measured CH4 fluxes were similar and followed the same patterns across land uses, suggesting the possibility to determine CH4 fluxes by means of simple measures of soil properties (bulk density and soil water content) and soil CH4 gradient concentration.
format info:ar-repo/semantics/artículo
id INTA15192
institution Instituto Nacional de Tecnología Agropecuaria (INTA -Argentina)
language Inglés
publishDate 2023
publishDateRange 2023
publishDateSort 2023
publisher Elsevier
publisherStr Elsevier
record_format dspace
spelling INTA151922023-09-13T11:00:30Z Impact of land use change on soil methane fluxes and diffusivity in Pampean plains, Argentina De Bernardi, María Priano, María Eugenia Fernandez, María Elena Gyenge, Javier Juliarena, Maria Paula Gases de Efecto Invernadero Reforestación Pastizal Forestal Suelo Propiedades del Suelo Greenhouse Gases Refosteration Forest Range Soil Soil Properties Región Pampeana Upland soils are the main methane (CH4) biological sink, and may be affected by land-use change. Changes in land uses and soil management affect soil properties that control diffusion of gases, which in combination with microbial activity, determine CH4 flux (fCH4) through the soil. Net CH4 fluxes and diffusivity -estimated by the CH4 diffusion coefficient- were measured in three common land uses typical from Pampean plains, South America (natural grassland NG; Eucalyptus globulus Labill. afforestation E; and agricultural land AL: oat, soybean and red clover in successive cultivation) during two years (March 2017–March 2019). Methane fluxes in the soil-atmosphere interface were measured using the static chamber technique, and a diffusion model was applied to estimate soil CH4 diffusivity from soil porosity. We aimed to quantify the effect of land use change (both E and AL vs. NG, the reference system) on fCH4 and gas diffusivity due to changes in the soil parameters. Soils were net sinks in the three land uses, with mean CH4 flux higher in the afforestation, intermediate in the natural grassland and lower in the agricultural land (− 10.99 ± 5.85, − 8.9 ± 5.32 and − 4.58 ± 4.19 ng CH4 m−2 s−1, respectively). CH4 fluxes varied significantly through seasons and space coinciding with variations in water-filled pore space and air-filled pore space variables (ρ > 0.7 and <−0.7 respectively; p < 0.05). Land-use change metric for methane flux ΔfCH4 was − 2.1 ± 3.7 and 4.4 ± 2.5 for NG-E and NG-AL, respectively, indicating a significant increment in net CH4 uptake when the natural grassland is afforested and a decrease when it was converted to agricultural use. This change was mainly explained by changes in soil physical properties (bulk density, soil water content, WFPS and air filled porosity). In relation to this, soil CH4 diffusion coefficient followed the same pattern as fCH4 (0.024 ± 0.011; 0.015 ± 0.007 and 0.008 ± 0.007 cm2 s−1 for E, NG and AL respectively); and allowed us to recalculate mean CH4 fluxes. Theoretical and in situ measured CH4 fluxes were similar and followed the same patterns across land uses, suggesting the possibility to determine CH4 fluxes by means of simple measures of soil properties (bulk density and soil water content) and soil CH4 gradient concentration. EEA Balcarce Fil: De Bernardi, María. Universidad Nacional de la la Provincia de Buenos Aires; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. Comisión de Investigaciones Cientificas; Argentina. Centro de Investigaciones en Física e Ingeniería del Centro de la Provincia de Buenos Aires. Fil: Priano, María Eugenia. Universidad Nacional de la la Provincia de Buenos Aires; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. Comisión de Investigaciones Cientificas; Argentina. Centro de Investigaciones en Física e Ingeniería del Centro de la Provincia de Buenos Aires. Fil: 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. Fil: 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. Fil: Juliarena, María Paula. Universidad Nacional de la la Provincia de Buenos Aires; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. Comisión de Investigaciones Cientificas; Argentina. Centro de Investigaciones en Física e Ingeniería del Centro de la Provincia de Buenos Aires. 2023-09-13T10:55:41Z 2023-09-13T10:55:41Z 2022-05 info:ar-repo/semantics/artículo info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion http://hdl.handle.net/20.500.12123/15192 https://www.sciencedirect.com/science/article/pii/S0167880922000159 0167-8809 (print) 1873-2305 (online) https://doi.org/10.1016/j.agee.2022.107866 eng info:eu-repo/semantics/restrictedAccess http://creativecommons.org/licenses/by-nc-sa/4.0/ Creative Commons Attribution-NonCommercial-ShareAlike 4.0 International (CC BY-NC-SA 4.0) application/pdf Elsevier Agriculture, Ecosystems & Environment 329 : 107866 ( May 2022)
spellingShingle Gases de Efecto Invernadero
Reforestación
Pastizal Forestal
Suelo
Propiedades del Suelo
Greenhouse Gases
Refosteration
Forest Range
Soil
Soil Properties
Región Pampeana
De Bernardi, María
Priano, María Eugenia
Fernandez, María Elena
Gyenge, Javier
Juliarena, Maria Paula
Impact of land use change on soil methane fluxes and diffusivity in Pampean plains, Argentina
title Impact of land use change on soil methane fluxes and diffusivity in Pampean plains, Argentina
title_full Impact of land use change on soil methane fluxes and diffusivity in Pampean plains, Argentina
title_fullStr Impact of land use change on soil methane fluxes and diffusivity in Pampean plains, Argentina
title_full_unstemmed Impact of land use change on soil methane fluxes and diffusivity in Pampean plains, Argentina
title_short Impact of land use change on soil methane fluxes and diffusivity in Pampean plains, Argentina
title_sort impact of land use change on soil methane fluxes and diffusivity in pampean plains argentina
topic Gases de Efecto Invernadero
Reforestación
Pastizal Forestal
Suelo
Propiedades del Suelo
Greenhouse Gases
Refosteration
Forest Range
Soil
Soil Properties
Región Pampeana
url http://hdl.handle.net/20.500.12123/15192
https://www.sciencedirect.com/science/article/pii/S0167880922000159
https://doi.org/10.1016/j.agee.2022.107866
work_keys_str_mv AT debernardimaria impactoflandusechangeonsoilmethanefluxesanddiffusivityinpampeanplainsargentina
AT prianomariaeugenia impactoflandusechangeonsoilmethanefluxesanddiffusivityinpampeanplainsargentina
AT fernandezmariaelena impactoflandusechangeonsoilmethanefluxesanddiffusivityinpampeanplainsargentina
AT gyengejavier impactoflandusechangeonsoilmethanefluxesanddiffusivityinpampeanplainsargentina
AT juliarenamariapaula impactoflandusechangeonsoilmethanefluxesanddiffusivityinpampeanplainsargentina