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Effects of Water and Nitrogen Addition on Ecosystem Carbon Exchange in a Meadow Steppe

机译:水和氮的添加对草地草原生态系统碳交换的影响

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摘要

A changing precipitation regime and increasing nitrogen deposition are likely to have profound impacts on arid and semiarid ecosystem C cycling, which is often constrained by the timing and availability of water and nitrogen. However, little is known about the effects of altered precipitation and nitrogen addition on grassland ecosystem C exchange. We conducted a 3-year field experiment to assess the responses of vegetation composition, ecosystem productivity, and ecosystem C exchange to manipulative water and nitrogen addition in a meadow steppe. Nitrogen addition significantly stimulated aboveground biomass and net ecosystem CO2 exchange (NEE), which suggests that nitrogen availability is a primary limiting factor for ecosystem C cycling in the meadow steppe. Water addition had no significant impacts on either ecosystem C exchange or plant biomass, but ecosystem C fluxes showed a strong correlation with early growing season precipitation, rather than whole growing season precipitation, across the 3 experimental years. After we incorporated water addition into the calculation of precipitation regimes, we found that monthly average ecosystem C fluxes correlated more strongly with precipitation frequency than with precipitation amount. These results highlight the importance of precipitation distribution in regulating ecosystem C cycling. Overall, ecosystem C fluxes in the studied ecosystem are highly sensitive to nitrogen deposition, but less sensitive to increased precipitation.
机译:不断变化的降水状况和增加的氮沉降可能会对干旱和半干旱生态系统的C循环产生深远影响,而这通常受到水和氮的时间和可用性的限制。然而,关于降水量和氮的增加对草地生态系统碳交换的影响知之甚少。我们进行了为期3年的野外实验,以评估植被成分,生态系统生产力和生态系统碳交换对草甸草原中水和氮的操纵性的响应。氮的添加显着刺激了地上生物量和生态系统净二氧化碳交换(NEE),这表明氮的有效性是草地草原生态系统碳循环的主要限制因素。在三个实验年中,添加水对生态系统碳交换或植物生物量均无显着影响,但生态系统C通量与生长早期降水而不是整个生长季节降水密切相关。将加水量纳入降水机制后,我们发现月平均生态系统碳通量与降水频率的相关性大于与降水量的相关性。这些结果突出了降水分布在调节生态系统碳循环中的重要性。总体而言,所研究生态系统中的生态系统碳通量对氮沉积高度敏感,但对增加的降水较不敏感。

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