Key Laboratory of Land Surface Pattern and Simulation, Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101, China; University of Chinese Academy of Sciences, Beijing 100049, China.
Key Laboratory of Land Surface Pattern and Simulation, Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101, China.
Sci Total Environ. 2022 Oct 20;844:157115. doi: 10.1016/j.scitotenv.2022.157115. Epub 2022 Jul 1.
Litter decomposition is a major method in which nutrients are recycled, especially carbon and nitrogen elements, in terrestrial ecosystems. However, how the responses of litter quality and soil microbial communities to global changes alter litter decomposition remains unclear. A 4-year field manipulative experiment based on the litterbag method was conducted in a typical temperate semiarid grassland in China to explore how increased precipitation and nitrogen deposition affect decomposition processes via litter quality and soil microbial communities. Our results showed that water and nitrogen addition treatments could accelerate litter carbon release and promote mass loss through different pathways. Water addition had a direct positive effect on litter decomposition. However, nitrogen addition could indirectly promote litter decomposition by improving litter quality and increasing the bacterial and fungal ratios. The water addition treatment increased litter mass loss by 7.37 %, and the N addition treatments increased litter mass loss by 5.83 %-16.93 %. Moreover, water and nitrogen additions had antagonistic effects on litter decomposition. These findings revealed that litter quality and the soil bacterial to fungal ratio were the factors controlling litter decomposition. The changes in precipitation and nitrogen deposition will impact ecosystem carbon and nitrogen cycling by altering litter decomposition processes in semiarid grassland ecosystems under the context of climate change.
凋落物分解是陆地生态系统中养分(特别是碳和氮元素)循环的主要方式。然而,凋落物质量和土壤微生物群落对全球变化的响应如何改变凋落物分解仍不清楚。本研究采用凋落袋法,在中国典型的温带半干旱草原上进行了为期 4 年的野外控制实验,以探讨增加降水和氮沉降如何通过凋落物质量和土壤微生物群落来影响分解过程。结果表明,水分和氮添加处理可以通过不同途径加速凋落物碳的释放和促进质量损失。水分添加对凋落物分解有直接的积极影响。然而,氮添加可以通过改善凋落物质量和增加细菌与真菌的比例,间接促进凋落物分解。水分添加处理使凋落物质量损失增加了 7.37%,氮添加处理使凋落物质量损失增加了 5.83%-16.93%。此外,水分和氮添加处理对凋落物分解有拮抗作用。这些发现表明,凋落物质量和土壤细菌与真菌的比例是控制凋落物分解的因素。在气候变化背景下,降水和氮沉降的变化将通过改变半干旱草原生态系统的凋落物分解过程,影响生态系统碳和氮循环。