Soil carbon dioxide fluxes following tillage in semiarid Mediterranean agroecosystems

dc.contributor.author
Álvaro-Fuentes, Jorge
dc.contributor.author
Cantero-Martínez, Carlos
dc.contributor.author
López Sánchez, María Victoria
dc.contributor.author
Arrúe, José Luis
dc.date.accessioned
2024-12-05T22:36:51Z
dc.date.available
2024-12-05T22:36:51Z
dc.date.issued
2018-11-12T09:57:40Z
dc.date.issued
2018-11-12T09:57:40Z
dc.date.issued
2007
dc.identifier
https://doi.org/10.1016/j.still.2007.08.003
dc.identifier
0167-1987
dc.identifier
http://hdl.handle.net/10459.1/65076
dc.identifier.uri
http://hdl.handle.net/10459.1/65076
dc.description.abstract
In semiarid Mediterranean agroecosystems, low and erratic annual rainfall together with the widespread use of mouldboard ploughing (conventional tillage, CT), as the main traditional tillage practice, has led to a depletion of soil organic matter (SOM) and with increases in CO2 emissions from soil to the atmosphere. In this study, we evaluated the viability of conservation tillage: RT, reduced tillage (chisel and cultivator ploughing) and, especially, NT (no-tillage) to reduce short-term (from 0 to 48 h after a tillage operation) and mid-term (from 0 h to several days since tillage operation) tillage-induced CO2 emissions. The study was conducted in three long-term tillage experiments located at different sites of the Ebro river valley (NE Spain) across a precipitation gradient. Soils were classified as: Fluventic Xerocrept, Typic Xerofluvent and Xerollic Calciorthid. Soil temperature and water content were also measured in order to determine their influence on tillage-induced CO2 fluxes. The majority of the CO2 flux measured immediately after tillage ranged from 0.17 to 6 g CO2 m−2 h−1 and was from 3 to 15 times greater than the flux before tillage operations, except in NT where soil CO2 flux was low and steady during the whole study period. Mid-term CO2 emission showed a different trend depending on the time of the year in which tillage was implemented. Microclimatic soil conditions (soil temperature and water content) had little impact on soil CO2 emission following tillage. In the semiarid Mediterranean agroecosystems studied, NT had low short-term soil CO2 efflux compared with other soil tillage systems (e.g., conventional and reduced tillage) and therefore can be recommended to better manage C in soil.
dc.description.abstract
This research was supported by the Comisión Interministerial de Ciencia y Tecnología of Spain (Grants AGL 2001-2238-C02-01 and AGL 2004-07763-C02-02) and the European Union (FEDER funds). The first author was awarded a FPI fellowship by the Spanish Ministry of Science and Education.
dc.language
eng
dc.publisher
Elsevier
dc.relation
info:eu-repo/grantAgreement/MICYT//AGL2001-2238-C02-01/ES/
dc.relation
info:eu-repo/grantAgreement/MEC//AGL2004-07763-C02-02/ES/
dc.relation
Versió postprint del document publicat a https://doi.org/10.1016/j.still.2007.08.003
dc.relation
Soil and Tillage Research, 2007, vol. 96, núm. 1-2, p. 331-341
dc.rights
cc-by-nc-nd (c) Elsevier, 2007
dc.rights
info:eu-repo/semantics/openAccess
dc.rights
http://creativecommons.org/licenses/by-nc-nd/4.0/
dc.subject
Tillage
dc.subject
Soil CO2 fluxes
dc.subject
No-tillage
dc.subject
Mediterranean agroecosystems
dc.title
Soil carbon dioxide fluxes following tillage in semiarid Mediterranean agroecosystems
dc.type
info:eu-repo/semantics/article
dc.type
info:eu-repo/semantics/acceptedVersion


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