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Temporal Dynamics of CO 2 Fluxes over a Non-Irrigated Vineyard

Author

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  • Aysan Badraghi

    (Institute of Landscape Engineering, Slovak University of Agriculture in Nitra, Tr. A. Hlinku 2, 949 76 Nitra, Slovakia
    Institute for Environmental Studies, Charles University, Fac. Sci. Benatska 2, 128 00 Prague 2, Czech Republic)

  • Beáta Novotná

    (Institute of Landscape Engineering, Slovak University of Agriculture in Nitra, Tr. A. Hlinku 2, 949 76 Nitra, Slovakia)

  • Jan Frouz

    (Institute for Environmental Studies, Charles University, Fac. Sci. Benatska 2, 128 00 Prague 2, Czech Republic
    Institute of Soil Biology and Biogeochemistry, Biology Centre CAS, Na Sadkach 7, 370 05 Ceske Budejovice, Czech Republic)

  • Koloman Krištof

    (Institute of Agricultural Engineering, Transport and Bioenergetics, Slovak University of Agriculture in Nitra, Tr. A. Hlinku 2, 949 76 Nitra, Slovakia)

  • Martin Trakovický

    (TRAKO, s.r.o. Pod lesom 11, 949 01 Nitra, Slovakia)

  • Martin Juriga

    (Institute of Agronomic Sciences, Slovak University of Agriculture in Nitra, Tr. A. Hlinku 2, 949 76 Nitra, Slovakia)

  • Branislav Chvila

    (Meteorological and Climatological Monitoring, Slovak Hydrometeorological Institute, Jeséniova 17, 833 15 Bratislava, Slovakia)

  • Leonardo Montagnani

    (Faculty of Science and Technology, Free University of Bozen-Bolzano, Piazza Università 1, 39100 Bolzano, Italy
    Forest Services, Autonomous Province of Bolzano, Via Brennero 6, 39100 Bolzano, Italy)

Abstract

Some knowledge gaps still remain regarding carbon sequestration in non-irrigated agroecosystems, where plants may experience drought stress during summertime. Therefore, by the combination of the eddy covariance (EC) and soil chamber techniques, we determined the role of a non-irrigated grassed vineyard in carbon sequestration in the Slovak Republic. Based on the EC data, the cumulative net uptake of CO 2 (NEE) for the whole growing season was weak and was ca. −97 (g C m −2 ). This value resulted from −796 (g C m −2 ) carbon uptake from the atmosphere through photosynthesis (GEE) and 699 (g C m −2 ) carbon released to the atmosphere through respiration (Reco). Carbon emissions through Reco were considerable and accounted for ca. 88% of GEE, which points out the importance of Reco for managing non-irrigated agroecosystems. Data from the soil chamber indicated that ca. 302 g C m −2 was released by the vineyard through soil respiration (Rsoil) over a growing season, which was constantly lower than Reco and accounted for ca. 44 ± 18% of Reco. This finding implies that the vineyard soil was not a main source of carbon emissions. Rsoil was mainly driven by temperature (exponentially ca. 69–85%). Meanwhile, vapour pressure deficit (VPD) and temperature appeared to be the most important limiting factors for GEE, NEE, and Reco, particularly when they exceeded a certain threshold (e.g., temperature > 17 °C, and VPD > 10 hPa).

Suggested Citation

  • Aysan Badraghi & Beáta Novotná & Jan Frouz & Koloman Krištof & Martin Trakovický & Martin Juriga & Branislav Chvila & Leonardo Montagnani, 2023. "Temporal Dynamics of CO 2 Fluxes over a Non-Irrigated Vineyard," Land, MDPI, vol. 12(10), pages 1-16, October.
    • Handle: RePEc:gam:jlands:v:12:y:2023:i:10:p:1925-:d:1260460
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    References listed on IDEAS

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