Key Laboratory of Wetland Ecology and Environment, Northeast Institute of Geography and Agroecology, Chinese Academy of Sciences, Changchun 130102, PR China; University of Chinese Academy Sciences, Beijing 100049, PR China.
Key Laboratory of Wetland Ecology and Environment, Northeast Institute of Geography and Agroecology, Chinese Academy of Sciences, Changchun 130102, PR China.
Sci Total Environ. 2022 Oct 20;844:157176. doi: 10.1016/j.scitotenv.2022.157176. Epub 2022 Jul 5.
As an elemental carbon (C) and nitrogen (N) pool in the world, peatlands are very sensitive to environmental changes. Under global warming, the increase in available N affects the dynamic changes of plant community structure and nutrients in a permafrost peatland. This study was based on a long-term in situ N addition experiment that had been conducted for 9 years. It utilized the peatland in the permafrost area of Great Hing'an Mountain as the research object to analyze the effects of N addition on the growth characteristics, community structure, and nutrient dynamics of peatland plants. The N inputs were N1: 6 g N m·year, N2: 12 g N m·year and N3: 24 g N m·year, respectively. Our results showed that the adding N can affect the plant community structure of peatland by affecting the plant growth characteristics. The diversity and richness of plant species in the peatland decreased as the concentration of added N increased. The long-term N addition can reduce the N limitation of plants to some extent. Still, it could further aggravate their phosphorus (P) limitation, resulting in the joint limitation of N and P or the complete limitation by P. The N resorption efficiency decreased with the increase of N addition level. The P resorption efficiency of different plants had varied responses to the changes in the N nutrient environment. Our study clarified the impact of long-term N addition on the plant community structure and nutrient dynamics of peatland in a permafrost area and provided an important theoretical basis to accurately evaluate the carbon and nitrogen balance of peatland in a permafrost area owing to future climate change.
作为世界上的一种元素碳(C)和氮(N)库,泥炭地对环境变化非常敏感。在全球变暖的情况下,可用氮的增加会影响多年冻土泥炭地植物群落结构和养分的动态变化。本研究基于一项为期 9 年的长期原位氮添加实验,以大兴安岭多年冻土区的泥炭地为研究对象,分析氮添加对泥炭地植物生长特性、群落结构和养分动态的影响。氮输入分别为 N1:6 g N m·year、N2:12 g N m·year 和 N3:24 g N m·year。研究结果表明,氮添加可以通过影响植物生长特性来影响泥炭地植物群落结构。随着添加氮浓度的增加,泥炭地植物物种的多样性和丰富度降低。长期氮添加可以在一定程度上减轻植物对氮的限制,但会进一步加剧对磷(P)的限制,导致氮磷联合限制或完全受 P 限制。氮再吸收效率随氮添加水平的增加而降低。不同植物的磷再吸收效率对氮养分环境变化有不同的响应。本研究阐明了长期氮添加对多年冻土区泥炭地植物群落结构和养分动态的影响,为准确评估未来气候变化条件下多年冻土区泥炭地的碳氮平衡提供了重要的理论依据。