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Responses of soil respiration to elevated carbon dioxide and nitrogen addition in young subtropical forest ecosystems in China

机译:中国年轻亚热带森林生态系统升高二氧化碳和氮含量的土壤呼应

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Global climate change in the real world always exhibits simultaneous changes in multiple factors. Prediction of ecosystem responses to multi-factor global changes in a future world strongly relies on our understanding of their interactions. However, it is still unclear how nitrogen (N) deposition and elevated atmospheric carbon dioxide concentration [CO2] would interactively influence forest floor soil respiration in subtropical China. We assessed the main and interactive effects of elevated [CO2] and N addition on soil respiration by growing tree seedlings in ten large open-top chambers under CO2 (ambient CO2 and 700 mol mol1) and nitrogen (ambient and 100 kg N ha1 yr1) treatments. Soil respiration, soil temperature and soil moisture were measured for 30 months, as well as above-ground biomass, root biomass and soil organic matter (SOM). Results showed that soil respiration displayed strong seasonal patterns with higher values observed in the wet season (April–September) and lower values in the dry season (October–March) in all treatments. Significant exponential relationships between soil respiration rates and soil temperatures, as well as significant linear relationships between soil respiration rates and soil moistures (below 15%) were found. Both CO2 and N treatments significantly affected soil respiration, and there was significant interaction between elevated [CO2] and N addition (p0.001, p=0.003, and p=0.006, respectively). We also observed that the stimulatory effect of individual elevated [CO2] (about 29% increased) was maintained throughout the experimental period. The positive effect of N addition was found only in 2006 (8.17% increased), and then had been weakened over time. Their combined effect on soil respiration (about 50% increased) was greater than the impact of either one alone. Mean value of annual soil respiration was 5.32 0.08, 4.54 0.10, 3.56 0.03 and 3.53 0.03 kg CO2 m2 yr1 in the chambers exposed to elevated [CO2] and high N deposition (CN), elevated [CO2] and ambient N deposition (CC), ambient [CO2] and high N deposition (NN), and ambient [CO2] and ambient N deposition (CK as a control), respectively. Greater above-ground biomass and root biomass was obtained in the CN, CC and NN treatments, and higher soil organic matter was observed only in the CN treatment. In conclusion, the combined effect of elevated [CO2] and N addition on soil respiration was apparent interaction. They should be evaluated in combination in subtropical forest ecosystems in China where the atmospheric CO2 and N deposition have been increasing simultaneously and remarkably.
机译:现实世界的全球气候变化总是在多个因素中表现出同时变化。对未来世界的多因素全球变化的生态系统反应的预测强烈依赖于我们对其互动的理解。然而,尚不清楚氮气(n)沉积和升高的大气二氧化碳浓度[CO2]将如何在亚热带地区互动地影响森林地板土壤呼吸。通过CO 2(环境CO2和700mol Mol1)和氮气(环境和100kg n Ha1 YR1),在10个大的俯视室中的树苗中,评估了升高的[CO2]和N添加对土壤呼吸的主要和互动的影响治疗。测量土壤呼吸,土壤温度和土壤水分30个月,以及地上生物质,根生物质和土壤有机物(SOM)。结果表明,在湿季(4月至9月)(4月至9月)和旱季(10月至3月)在所有治疗中展示了较高价值的土壤呼吸呈现出强烈的季节性模式。发现土壤呼吸率和土壤温度之间的显着指数关系,以及土壤呼吸率和土壤水分之间的显着线性关系(低于15%)。二氧化碳和N治疗均显着影响土壤呼吸,并且在升高的[CO 2]和N加(P0.001,P = 0.003和P = 0.006之间,显着相互作用。我们还观察到,在整个实验期间,将个体升高的刺激作用(CO2]升高(升高约29%增加)保持。 N添加的阳性效果仅在2006年(增加8.17%),然后随着时间的推移被削弱。它们对土壤呼吸的综合影响(约50%增加)大于单独的任何一种的影响。每年土壤呼吸的平均值为5.32 0.08,4.54 0.10,3.56 0.03和3.53 0.03kg CO2m2 YR1,暴露于升高的[CO2]和高N沉积(CN),升高的[CO 2]和环境N沉积(CC) ,环境[CO2]和高N沉积(NN)和环境[CO2]和环境N沉积(CK作为对照)。在CN,CC和NN处理中获得更大的地上生物质和根生物质,并且仅在CN处理中观察到更高的土壤有机物质。总之,升高的[CO2]和N添加土壤呼吸的综合作用是表观相互作用。它们应在中国的亚热带林生态系统中组合进行评估,其中大气二氧化碳二氧化碳和N沉积同时且显着地增加。

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