Soil-atmosphere greenhouse gases (CO2, CH4 and N2O) exchange in evergreen oak woodland in southern Portugal

A 10-20% decrease in annual precipitation is predicted in the Mediterranean basin, and in particular to the Iberian Peninsula, with foreseen effects on the exchange of soil-atmosphere greenhouse gases (GHGs; CO2, CH4, and N2O). To simulate this scenario, we setup an experimental design in the partic...

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Main Authors: A. Shvaleva, R. Lobo-do-Vale, C. Cruz, S. Castaldi, A.P. Rosa, M.M. Chaves, J.S. Pereira
Format: Article
Language:English
Published: Czech Academy of Agricultural Sciences 2011-10-01
Series:Plant, Soil and Environment
Subjects:
Online Access:https://pse.agriculturejournals.cz/artkey/pse-201110-0005_soil-atmosphere-greenhouse-gases-co2-ch4-and-n2o-exchange-in-evergreen-oak-woodland-in-southern-portugal.php
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author A. Shvaleva
R. Lobo-do-Vale
C. Cruz
S. Castaldi
A.P. Rosa
M.M. Chaves
J.S. Pereira
author_facet A. Shvaleva
R. Lobo-do-Vale
C. Cruz
S. Castaldi
A.P. Rosa
M.M. Chaves
J.S. Pereira
author_sort A. Shvaleva
collection DOAJ
description A 10-20% decrease in annual precipitation is predicted in the Mediterranean basin, and in particular to the Iberian Peninsula, with foreseen effects on the exchange of soil-atmosphere greenhouse gases (GHGs; CO2, CH4, and N2O). To simulate this scenario, we setup an experimental design in the particularly dry period of 2008-2009 using rainfall exclusion and irrigation, to obtain plots receiving 110% (538 mm), 100% (493 mm) and 74% (365 mm) of the natural precipitation. Soil CO2 fluxes showed a strong increase from summer to autumn as a consequence of increasing soil heterotrophic respiration that resulted from rewetting. Fluxes of N2O were negligible. According to our data, soil was a permanent CH4 sink independent of the soil water content (in the range between 6-26% WFPS - water-filled pore space) and of soil temperature (in the range of 7-28°C), supporting the concept that seasonally dry ecosystems (Mediterranean) may represent a significant sink of atmospheric CH4. The study provides evidence that the 26% decrease or 10% increase in the ambient rainfall from annual precipitation of ca 500 mm did not significantly affect soil functionality and had a limited impact on soil-atmosphere net GHGs exchange in evergreen oak woodlands in southern Portugal.
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spelling doaj.art-951f4229b3054176a5bd10e612788a622023-02-23T03:45:45ZengCzech Academy of Agricultural SciencesPlant, Soil and Environment1214-11781805-93682011-10-01571047147710.17221/223/2011-PSEpse-201110-0005Soil-atmosphere greenhouse gases (CO2, CH4 and N2O) exchange in evergreen oak woodland in southern PortugalA. Shvaleva0R. Lobo-do-Vale1C. Cruz2S. Castaldi3A.P. Rosa4M.M. Chaves5J.S. Pereira6Institute of Technological Chemistry and Biology, New University of Lisbon, Av. República, Oeiras, PortugalInstitute of Agronomy, Technical University of Lisbon, Tapada da Ajuda, Lisbon, PortugalFaculty of Sciences, University of Lisbon (CBA), Lisbon, PortugalSecond University, Caserta, ItalyFaculty of Sciences, University of Lisbon (CBA), Lisbon, PortugalInstitute of Technological Chemistry and Biology, New University of Lisbon, Av. República, Oeiras, PortugalInstitute of Agronomy, Technical University of Lisbon, Tapada da Ajuda, Lisbon, PortugalA 10-20% decrease in annual precipitation is predicted in the Mediterranean basin, and in particular to the Iberian Peninsula, with foreseen effects on the exchange of soil-atmosphere greenhouse gases (GHGs; CO2, CH4, and N2O). To simulate this scenario, we setup an experimental design in the particularly dry period of 2008-2009 using rainfall exclusion and irrigation, to obtain plots receiving 110% (538 mm), 100% (493 mm) and 74% (365 mm) of the natural precipitation. Soil CO2 fluxes showed a strong increase from summer to autumn as a consequence of increasing soil heterotrophic respiration that resulted from rewetting. Fluxes of N2O were negligible. According to our data, soil was a permanent CH4 sink independent of the soil water content (in the range between 6-26% WFPS - water-filled pore space) and of soil temperature (in the range of 7-28°C), supporting the concept that seasonally dry ecosystems (Mediterranean) may represent a significant sink of atmospheric CH4. The study provides evidence that the 26% decrease or 10% increase in the ambient rainfall from annual precipitation of ca 500 mm did not significantly affect soil functionality and had a limited impact on soil-atmosphere net GHGs exchange in evergreen oak woodlands in southern Portugal.https://pse.agriculturejournals.cz/artkey/pse-201110-0005_soil-atmosphere-greenhouse-gases-co2-ch4-and-n2o-exchange-in-evergreen-oak-woodland-in-southern-portugal.phpclimate changedroughtmediterraneanprecipitation
spellingShingle A. Shvaleva
R. Lobo-do-Vale
C. Cruz
S. Castaldi
A.P. Rosa
M.M. Chaves
J.S. Pereira
Soil-atmosphere greenhouse gases (CO2, CH4 and N2O) exchange in evergreen oak woodland in southern Portugal
Plant, Soil and Environment
climate change
drought
mediterranean
precipitation
title Soil-atmosphere greenhouse gases (CO2, CH4 and N2O) exchange in evergreen oak woodland in southern Portugal
title_full Soil-atmosphere greenhouse gases (CO2, CH4 and N2O) exchange in evergreen oak woodland in southern Portugal
title_fullStr Soil-atmosphere greenhouse gases (CO2, CH4 and N2O) exchange in evergreen oak woodland in southern Portugal
title_full_unstemmed Soil-atmosphere greenhouse gases (CO2, CH4 and N2O) exchange in evergreen oak woodland in southern Portugal
title_short Soil-atmosphere greenhouse gases (CO2, CH4 and N2O) exchange in evergreen oak woodland in southern Portugal
title_sort soil atmosphere greenhouse gases co2 ch4 and n2o exchange in evergreen oak woodland in southern portugal
topic climate change
drought
mediterranean
precipitation
url https://pse.agriculturejournals.cz/artkey/pse-201110-0005_soil-atmosphere-greenhouse-gases-co2-ch4-and-n2o-exchange-in-evergreen-oak-woodland-in-southern-portugal.php
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