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Ecosystem CO2 Exchange in Response to Nitrogen and Phosphorus Addition in a Restored, Temperate Grassland

机译:恢复的温带草原中氮和磷添加对生态系统CO2交换的响应

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摘要

Nitrogen (N) and phosphorus (P) affect the structure and function of grasslands by altering plant competitive interactions, shifting patterns of above and below ground biomass allocation, and increasing net primary production. However, the influence of N and P on net ecosystem CO2 exchange (NEE) is poorly understood. In a field-based factorial N- and P-addition experiment, we measured shallow soil moisture, leaf area index, and component fluxes of midday ecosystem CO2 exchange throughout the growing season in a restored temperate grassland near Buffalo, New York. Throughout the growing season, N-addition increased gross ecosystem CO2 exchange (GEE) and correspondingly altered NEE to increase ecosystem CO2 uptake. In contrast N-addition caused a seasonally dynamic decline in leaf area adjusted GEE, a pattern consistent with increased photosynthetic light limitation. P-addition did not significantly increase Re, and N- and P-addition interacted to significantly weaken the ecosystem as a midday CO2 sink. Moreover, water limitation and phenological constraints during the middle and late growing season appear to limit plant responses to nutrient addition. These results suggest influences of N -and P-addition on ecosystem processes are seasonally dynamic and by differentially influencing above and below ground components of ecosystems, the availability of N and P in soils may interact to influence ecosystem CO2 exchange.
机译:氮(N)和磷(P)通过改变植物之间的竞争性相互作用,改变地面和地下生物量分配的方式以及增加净初级生产力来影响草原的结构和功能。但是,关于氮和磷对生态系统净二氧化碳交换量(NEE)的影响知之甚少。在基于田间的阶乘N和P的附加实验中,我们在纽约布法罗附近的一个恢复温带草原上,测量了整个生长季节的浅层土壤水分,叶面积指数和午间生态系统CO2交换的通量。在整个生长季节,氮的添加增加了生态系统的总CO2交换量(GEE),并相应地改变了NEE以增加生态系统的CO2吸收量。相反,氮的添加导致叶面积调整的GEE随季节动态下降,这种模式与增加的光合光限制一致。磷的添加并没有显着增加Re,氮和磷的添加会相互作用,从而显着削弱生态系统,这是午间的CO2吸收。此外,生长中期和后期的水分限制和物候约束似乎限制了植物对养分添加的反应。这些结果表明,氮和磷的添加对生态系统过程的影响是季节性变化的,并且通过不同地影响生态系统的地面和地下组成部分,土壤中氮和磷的有效性可能相互作用,从而影响生态系统的二氧化碳交换。

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