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Abstract

In this chapter, exchange dynamics of greenhouse gases over Hungarian grassland ecosystems are analyzed. Carbon dioxide (CO2) exchange was measured by eddy covariance technique at three sites (Bugac, Mátra, and Hegyhátsál). Methane (CH4) and nitrous oxide (N2O) fluxes were occasionally measured by static chamber method partly at the same grassland sites and at a wetland site. Dry grasslands (Bugac and Mátra) were net sources of CO2 in extreme drought years on annual time scale, while in other years they acted as sinks. The relatively humid Hegyhátsál was a net sink of CO2 on annual time scale during the measurement period. The different soil types (light sandy soil, heavy clay soil, and loamy soil) and the variable amount of annual precipitation sums (ranging from 551 to 747 mm) provided a unique opportunity to analyze the response of CO2 dynamics of grasslands to the soil type and effect of water stress. In case of the sandy grassland (Bugac), the exclusive role of the annual precipitation sum in the determination of annual NEE is strongly coupled to the soil type. Although the sandy grassland expressed adaptation to drought, the CO2 sink--source precipitation threshold was within the standard deviation (112 mm) of the annual precipitation, showing the high risk of desertification in this ecosystem. Grassland ecosystem on heavy clay soil was more vulnerable to drought stress than the grassland on sandy soil due to the worse water management properties of the clay soil. At the grassland on loamy soil in the more rainy western part of the country, gross primary production was occasionally limited by high soil water contents. This grassland has good adaptation capabilities to uneven precipitation distribution owing to the high silt fraction of the soil resulting in high water storage capacity. CH4 flux above grasslands was within the range of −54 to 58 mg CH4 m−2 year−1 (negative flux means uptake by the soil). Wetland soils are generally CH4 emitters. Annual mean of N2O soil emission varied between 0.005 and 0.17 g N2O m−2 year−1 with 6-year averages of 0.08 and 0.03 g N2O m−2 year−1 for sandy/loess and clay soils, respectively. Mean soil flux of N2O over wetlands was similar to N2O emission over dry grasslands.

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Acknowledgments

The present work was supported by the Carboeurope-IP (EU GOCE-CT2003-505572), NITROEUROPE-IP (017810-2) of the European Comission’s 6th R&D Framework Programme, the Hungarian Ministry of Economy and Transport (GVOP-3.2.1.-2004-04-0107/3.0), and the Hungarian Scientific Research Fund (OTKA K75638). The authors highly appreciate the help and contribution of Giorgio Alberti, Alessandro Peressotti (University of Udine, Udine, Italy), István Tóth (technician at the Hegyhátsál site), Susumu Yamamoto, Hiroaki Kondo, and Nobuko Saigusa (National Institute of Advanced Industrial Science and Technology, Tsukuba, Japan).

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Correspondence to Zoltán Nagy .

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Nagy, Z. et al. (2011). Grasslands. In: Haszpra, L. (eds) Atmospheric Greenhouse Gases: The Hungarian Perspective. Springer, Dordrecht. https://doi.org/10.1007/978-90-481-9950-1_6

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