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首页> 外文期刊>Polish journal of ecology >Effects of CO2 fumigation and nitrogen addition on soil respiration in a wetland ecosystem: experimental approach with top open chambers
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Effects of CO2 fumigation and nitrogen addition on soil respiration in a wetland ecosystem: experimental approach with top open chambers

机译:CO2熏蒸和氮气添加对湿地生态系统土壤呼吸的影响:顶部开放腔室的实验方法

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摘要

Soil respiration plays a crucial role in global carbon cycling of terrestrial ecosystems. Changes in atmospheric CO2 and nitrogen (N) addition across the globe are likely to affect soil respiration. However, the effects of elevated CO2 and N addition on soil respiration are not fully understood especially in wetland ecosystems. To evaluate the effects of atmospheric CO2 and N availability on soil respiration, a paired, nested manipulative in situ experiment was performed, using CO2 fumigation within Open-Top Chambers as the primary factor, and N (as NH4NO3) as the secondary factor in a temperate wetland in northeastern China in 2010 and 2011. CO2 fumigation significantly enhanced soil respiration, according to repeated-measures ANOVA, and the stimulatory effect of CO2 fumigation on soil respiration was sustained during the whole experimental period regardless of N addition. However, the positive soil respiration effect of N addition alone weakened over time. Moreover, there was a significant interaction between CO2 fumigation and N addition. Soil temperature explained 50-66% of the variation in soil respiration. Moreover, soil respiration was positively correlated with the root N content and litter decomposition rate. The results suggested that elevated CO2 concentrations will accelerate soil respiration and ecosystem carbon cycling, thus, limiting soil carbon sequestration, especially when coupled with increasing N deposition.
机译:土壤呼吸在陆地生态系统的全球碳循环中起着至关重要的作用。整个地球上的大气二氧化碳和氮气(n)的变化可能会影响土壤呼吸。然而,在湿地生态系统中,升高的CO2和N添加对土壤呼吸的影响尤其是完全理解的。为了评估大气CO2和N可用性对土壤呼吸的影响,在敞开的腔室内使用CO 2熏蒸作为原位实验,作为主要因子,N(AS NH 4 NO 3)作为次要因素进行配对的嵌套操纵2010年和2011年的中国东北部温带湿地。根据重复措施Anova,CO2熏蒸显着增强了土壤呼吸,并且在整个实验期内,无论添加多少,CO2熏蒸对土壤呼吸的刺激作用。然而,单独添加N添加的正土壤呼吸效应随着时间的推移而减弱。此外,CO 2熏蒸和N添加之间存在显着的相互作用。土壤温度解释了土壤呼吸变异的50-66%。此外,土壤呼吸与根部N含量和凋落物分解率呈正相关。结果表明,升高的CO2浓度将加速土壤呼吸和生态系统碳循环,从而限制土壤碳封存,特别是当加上增加N沉积时。

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