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应用生态学报 ›› 2026, Vol. 37 ›› Issue (6): 1830-1840.doi: 10.13287/j.1001-9332.202606.011

• 研究论文 • 上一篇    下一篇

增温对高山灌木凋落叶分解和土壤有机碳稳定性的影响

王宁宁1, 罗长菊1, 刘丽鸽1, 宋思宇1, 李聪1, AsmaAtta1, AjayoPleasurechisom1, 崔宁洁2, 刘洋1*   

  1. 1四川农业大学林学院长江上游森林生态与保育四川省重点实验室/四川峨眉山森林生态系统国家定位观测研究站, 成都 611130;
    2四川省林业和草原调查规划院, 成都 610084
  • 收稿日期:2025-09-01 修回日期:2026-04-22 出版日期:2026-06-18 发布日期:2026-12-18
  • 通讯作者: *E-mail: sicauliuyang@163.com
  • 作者简介:王宁宁, 女, 2000年生, 硕士研究生。主要从事全球变化与凋落叶分解研究。E-mail: 2017495451@qq.com
  • 基金资助:
    国家自然科学基金项目(32371850,4251101400)和四川省科技计划项目(2025YFHZ0168)

Effects of warming on leaf litter decomposition and soil organic carbon stability in alpine shrubs

WANG Ningning1, LUO Changju1, LIU Lige1, SONG Siyu1, LI Cong1, ASMA Atta1, AJAYO Pleasure chisom1, CUI Ningjie2, LIU Yang1*   

  1. 1Sichuan Province Key Laboratory of Forest Ecology and Conservation in the Upper Reaches of the Yangtze River/Sichuan Mt. Emei Forest Ecosystem National Observation and Research Station, College of Forestry, Sichuan Agricultural University, Chengdu 611130, China;
    2Sichuan Forestry and Grassland Survey and Planning Institute, Chengdu 610084, China
  • Received:2025-09-01 Revised:2026-04-22 Online:2026-06-18 Published:2026-12-18

摘要: 凋落叶分解是调控土壤有机碳形成与稳定性的核心过程,而气候变暖背景下,高山灌丛扩张通过改变凋落叶输入特征(分解速率、化学组成)影响高寒生态系统碳平衡的内在机制尚未明确。本研究以红毛花楸(高质量,低C/N、低木质素含量)和高山杜鹃(低质量,高C/N、高木质素含量)凋落叶为研究对象,设置常温(白天10 ℃/夜间5 ℃)和增温(白天20 ℃/夜间15 ℃)两种温度处理,开展为期180 d的室内控温培养试验,探究增温对不同凋落叶分解动态、碳组分变化及土壤有机碳稳定性的影响。结果表明:增温加速两种灌木凋落叶分解,红毛花楸和高山杜鹃分解速率较常温分别提升47.9%和21.0%;有机溶性组分、酸溶组分分别平均降低9.7%和14.7%,酸不溶组分平均增加16.9%。增温显著提高土壤溶解性有机碳含量,显著降低惰性有机碳含量,对土壤总有机碳含量无影响。增温条件下,红毛花楸凋落叶输入下土壤碳库指数和碳库活度较常温提升2.5%和53.4%,高山杜鹃凋落叶输入下提升3.2%和79.5%,两者土壤碳库管理指数较常温分别降低13.6%和7.3%。综上,增温加速了高山灌木凋落叶分解并且降低了土壤有机碳稳定性,而低质量的凋落叶输入比高质量的凋落叶能更好地维持高寒土壤有机碳的稳定性。

关键词: 增温, 高山灌木, 凋落叶分解, 土壤有机碳稳定性, 碳库管理指数

Abstract: Litter decomposition is a core process regulating the formation and stability of soil organic carbon. Under the background of climate warming, the intrinsic mechanisms by which the expansion of alpine shrubs affects carbon balance of alpine ecosystems by altering litter input characteristics (decomposition rate and chemical composition) remains unclear. We explored the effects of warming on the decomposition dynamics, carbon fraction changes of litters with different qualities and the stability of soil organic carbon, taking the leaf litters of Sorbus rufopilosa (high-quality, low C/N ratio and low lignin content) and Rhododendron lapponicum (low-quality, high C/N ratio and high lignin content) in the alpine regions of western Sichuan as the research objects. We conducted a 180-day laboratory controlled-temperature incubation experiment, with two temperature treatments: ambient temperature (10 ℃ in the daytime / 5 ℃ at night) and warming (20 ℃ in the daytime / 15 ℃ at night). The results showed that warming significantly accelerated the decomposition of the litters of two shrub species, with the decomposition rates of S. rufopilosa and R. lapponicum being increased by 47.9% and 21.0%, respectively. There was an average decrease of 9.7% and 14.7% in the non-polar extractives and acid-hydrolyzable carbohydrates and an average increase of 16.9% in the acid-unhydrolyzable residue. Warming significantly increased the content of soil dissolved organic carbon and decreased the content of soil recalcitrant organic carbon, but did not affect the content of soil total organic carbon. Under warming conditions, soil carbon stock index and carbon stock activity increased by 2.5% and 53.4% compared to normal temperature under S. rubra litters input, and increased by 3.2% and 79.5% for R. alpinum litters input, while the soil carbon stock management index decreased by 13.6% and 7.3%, respectively. In conclusion, warming accelerated the decomposition of alpine shrub litters and reduced the stability of soil organic carbon, while the input of low-quality litter could better maintain the stability of soil organic carbon in alpine meadows compared with high-quality litter.

Key words: warming, alpine shrub, litter decomposition, soil organic carbon stability, carbon pool management index