Increasing nitrogen addition rates suppressed long-term litter decomposition in a temperate meadow steppe

IF 4.3 3区 材料科学 Q1 ENGINEERING, ELECTRICAL & ELECTRONIC
Pei Zheng, R. Zhao, Liangchao Jiang, Guojiao Yang, Yinliu Wang, Ruzhen Wang, Xingguo Han, Qiushi Ning
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Abstract

Plant litter decomposition is critical for the carbon (C) balance and nutrient turnover in terrestrial ecosystems and sensitive to the ongoing anthropogenic nitrogen (N) input. Previous studies evaluating the N effect on litter decomposition relied mostly on short-term experiments (< 2 years), which probably masked the real N effect on litter decomposition. Therefore, long-lasting experiments are imperative for the overall evaluation of the litter decomposition dynamics under N enrichment. We conducted a long-term (4-year) N addition experiment with N levels from 0 – 50 g N m -2 yr -1 to examine the potential abiotic and biotic factors in regulating the decomposition process of litterfall from the dominant species Leymus chinensis. The long-term experiment exhibited a consistent decrease of decomposition rate with increasing N addition rates, providing strong evidence showing the inhibitory effect of N addition on decomposition. The N-induced alterations in soil environment (acidification and nutrient stoichiometry), microbial activity (microbial biomass and enzyme activity), changes of litter quality (residual lignin and nutrient content) and plant community (aboveground productivity and species richness) jointly contributed to the lowered decomposition. During the whole decomposition process, the changes of litter quality, including accumulation of lignin and the concentrations of nutrient, were mainly driven by the soil environment and microbial activity in this N-enriched environment. The findings help clarify how increasing N input rates affect long-term litter decomposition, and improve the mechanistic understanding of the linkages between ecosystem N enrichment and C cycling.
增加氮添加量可抑制温带草甸草原凋落物的长期分解
植物凋落物分解对陆地生态系统碳(C)平衡和养分周转至关重要,对持续的人为氮(N)输入非常敏感。以往评价N对凋落物分解影响的研究大多依赖于短期实验(< 2年),这可能掩盖了N对凋落物分解的真实影响。因此,长期实验是全面评价富氮条件下凋落物分解动态的必要条件。为了研究优势种羊草凋落物分解过程中可能存在的非生物和生物因素,我们进行了长期(4年)N添加试验,N水平为0 ~ 50 g N m -2 yr -1。长期实验显示,随着N添加量的增加,分解速率一致降低,为N添加对分解的抑制作用提供了强有力的证据。氮诱导的土壤环境(酸化和养分化学计量)、微生物活性(微生物生物量和酶活性)、凋落物质量(残余木质素和养分含量)和植物群落(地上生产力和物种丰富度)的变化共同导致了分解的降低。在整个分解过程中,凋落物质量的变化,包括木质素积累和养分浓度的变化,主要受土壤环境和富氮环境下微生物活动的驱动。这些发现有助于阐明增加N输入率如何影响凋落物的长期分解,并提高对生态系统N富集与C循环之间联系的机制理解。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
CiteScore
7.20
自引率
4.30%
发文量
567
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