固碳
温带气候
生态系统
环境科学
沉积(地质)
氮气
温带森林
温带雨林
营养物
碳纤维
农学
航程(航空)
生态系统模型
营养循环
陆地生态系统
森林生态学
自行车
环境化学
生态学
大气科学
碳循环
土壤科学
化学
全球变化
生物量(生态学)
氮气循环
生物地球化学循环
作者
B. Liu,Xianlei Fan,Ziping Liu,Qing Chang,Jiancheng Chen,Yuanzi Huo,Edith Bai
标识
DOI:10.1073/pnas.2533999123
摘要
Anthropogenic nitrogen (N) deposition comprising reduced (NH x ) and oxidized (NO y ) forms, differentially influences ecosystem processes. However, their long-term fates and collective impacts on ecosystem nitrogen use efficiency (NUE) and carbon (C) sequestration remain unresolved. Here, using a decade-long paired labeling ( 15 NH 4 + and 15 NO 3 − ) experiment in a temperate forest, we demonstrate that initially distinct fates of different N forms converged within 2 y due to low initial loss rates prior to organic incorporation. After 10 y, overall ecosystem retention was remarkably similar (55.3 to 65.6%) for both N forms. A process -based N-cycling model was built and parameterized by our 15 N recovery data and the model predicted declining ecosystem NUE with increasing N deposition level. We further identified a deposition-induced C sequestration potential of 41.41 kg C kg −1 N under an incremental deposition of 10 kg N ha −1 y −1 , exceeding prior estimates at comparable loads. This study provides mechanistic, high-resolution temporal data critical for refining N-cycle models and reveals an optimal N deposition range (20 to 30 kg N ha −1 y −1 ) that maximizes C sequestration while minimizing environmental risks (e.g., nutrient imbalance, eutrophication) in temperate forests.
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