Finzi Adrien C, DeLucia Evan H, Hamilton Jason G, Richter Daniel D, Schlesinger William H
Department of Biology, Boston University, 5 Cummington Street, Boston, MA, 02215, USA.
Department of Plant Biology, University of Illinois, Urbana, IL, 61801, USA.
Oecologia. 2002 Aug;132(4):567-578. doi: 10.1007/s00442-002-0996-3. Epub 2002 Aug 1.
Elevated concentrations of atmospheric CO increase plant biomass, net primary production (NPP) and plant demand for nitrogen (N). The demand for N set by rapid plant growth under elevated CO could be met by increasing soil N availability or by greater efficiency of N uptake. Alternatively, plants could increase their nitrogen-use efficiency (NUE), thereby maintaining high rates of growth and NPP in the face of nutrient limitation. We quantified dry matter and N budgets for a young pine forest exposed to 4 years of elevated CO using free-air CO enrichment technology. We addressed three questions: Does elevated CO increase forest NPP and the demand for N by vegetation? Is demand for N met by greater uptake from soils, a shift in the distribution of N between plants, microbes, and soils, or increases in NUE under elevated CO? Will soil N availability constrain the NPP response of this forest as CO fumigation continues? A step-function increase in atmospheric CO significantly increased NPP during the first 4 years of this study. Significant increases in NUE under elevated CO modulated the average annual requirement for N by vegetation in the first and third growing seasons under elevated CO; the average stimulation of NPP in these years was 21% whereas the average annual stimulation of the N requirement was only 6%. In the second and fourth growing seasons, increases in NPP increased the annual requirement for N by 27-33%. Increases in the annual requirement for N were largely met by increases in N uptake from soils. Retranslocation of nutrients prior to senescence played only a minor role in supplying the additional N required by trees growing under elevated CO. NPP was highly correlated with between-plot variation in the annual rate of net N mineralization and CO treatment. This demonstrates that NPP is co-limited by C availability, as CO from the atmosphere, and N availability from soils. There is no evidence that soil N mineralization rates have increased under elevated CO. The correlation between NPP and N mineralization rates and the increase in the annual requirement for N in certain years imply that soil N availability may control the long-term productivity response of this ecosystem to elevated CO. Although we have no evidence suggesting that NPP is declining in response to >4 years of CO fumigation, if the annual requirement of N continues to be stimulated by elevated CO, we predict that the productivity response of this forest ecosystem will decline over time.
大气中二氧化碳(CO)浓度升高会增加植物生物量、净初级生产力(NPP)以及植物对氮(N)的需求。在CO浓度升高的情况下,植物快速生长所产生的氮需求,可以通过增加土壤氮有效性或提高氮吸收效率来满足。或者,植物可以提高其氮利用效率(NUE),从而在养分限制的情况下保持较高的生长速率和NPP。我们使用自由空气CO2富集技术,对一片暴露于4年高浓度CO环境中的年轻松林的干物质和氮收支进行了量化。我们探讨了三个问题:CO浓度升高是否会增加森林NPP以及植被对氮的需求?对氮的需求是通过从土壤中更多地吸收、植物、微生物和土壤之间氮分配的变化,还是通过CO浓度升高时NUE的增加来满足?随着CO熏蒸的持续,土壤氮有效性是否会限制这片森林的NPP响应?在本研究的前4年中,大气CO浓度的阶跃式增加显著提高了NPP。在CO浓度升高的情况下,NUE的显著增加调节了CO浓度升高时第一和第三个生长季节植被对氮的年均需求量;这些年份中NPP的平均刺激率为21%,而氮需求的年均刺激率仅为6%。在第二和第四个生长季节,NPP的增加使氮的年需求量增加了27 - 33%。氮年需求量的增加在很大程度上通过土壤氮吸收的增加得到满足。衰老前养分的重新转运在为CO浓度升高条件下生长的树木提供额外所需氮方面仅起次要作用。NPP与地块间净氮矿化年速率和CO处理的变化高度相关。这表明NPP受到碳有效性(如大气中的CO)和土壤氮有效性的共同限制。没有证据表明在CO浓度升高的情况下土壤氮矿化速率有所增加。NPP与氮矿化速率之间的相关性以及某些年份氮年需求量的增加意味着土壤氮有效性可能控制该生态系统对CO浓度升高的长期生产力响应。虽然我们没有证据表明在超过4年的CO熏蒸后NPP正在下降,但如果氮的年需求量继续受到CO浓度升高的刺激,则我们预测这片森林生态系统的生产力响应将随时间下降。