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Background nitrogen deposition controls the effects of experimental nitrogen addition on soil gross N transformations in forest ecosystems

机译:背景技术氮沉积对森林生态系统中的土壤总转化进行了实验氮的影响

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摘要

Nitrogen (N) deposition can profoundly alter soil N transformation processes and the long-term productivity of forest ecosystems. The response of soil gross N transformations to N deposition in forest ecosystems has been well studied through simulated N addition experiments. Simulated N addition experiments are conducted under a wide range of background N deposition rates. However, it remains unclear whether the response of soil gross N transformation rates to simulated N addition is dependent on background N deposition rates. Here, we collate results from the literature in forest ecosystems, and found, for the first time, that the responses of gross rates of N mineralization, nitrification, and NO3- immobilization to experimental N addition changed from positive to negative with increasing background N deposition rates with the thresholds for such changes were 3.23, 6.02, 1.90 kg N ha(- 1) yr(- 1), respectively. Our results suggest that background N deposition rates shall be incorporated into ecosystem models to better predict forest ecosystem N cycling under future N deposition scenarios.
机译:氮沉降可以深刻地改变土壤氮的转化过程和森林生态系统的长期生产力。通过模拟施氮试验,研究了森林生态系统土壤全氮转化对氮沉降的响应。模拟氮添加实验在大范围的背景氮沉积速率下进行。然而,目前尚不清楚土壤总氮转化率对模拟氮添加量的响应是否取决于背景氮沉降率。在这里,我们整理了森林生态系统中的文献结果,并首次发现,随着背景氮沉积速率的增加,氮矿化、硝化和NO3-固定化的总速率对实验氮添加量的响应从正变为负,这些变化的阈值分别为3.23、6.02和1.90 kg N ha(-1)yr(-1)。我们的结果表明,为了更好地预测未来氮沉降情景下的森林生态系统氮循环,应将背景氮沉降率纳入生态系统模型。

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