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应用生态学报 ›› 2026, Vol. 37 ›› Issue (3): 897-906.doi: 10.13287/j.1001-9332.202603.018

• 研究论文 • 上一篇    下一篇

环青海湖地区牦牛与藏羊粪便降解对土壤-植物养分循环的影响

李梦棋1, 董全民1,2, 刘玉祯1,2, 吕卫东1, 孙彩彩1, 许蔚1, 刘文亭1,2, 季海明1, 杨晓霞1,2*   

  1. 1青海大学畜牧兽医科学院/青海省高寒草地适应性管理重点实验室, 西宁 810016;
    2青海大学三江源区高寒草地生态教育部重点实验室, 西宁 810016
  • 收稿日期:2025-07-02 接受日期:2026-01-29 出版日期:2026-03-18 发布日期:2026-09-18
  • 通讯作者: *E-mail: xxyang@qhu.edu.cn
  • 作者简介:李梦棋, 女, 1998年生, 硕士研究生。主要从事草地放牧生态学研究。E-mail: 379155294@qq.com
  • 基金资助:
    青海大学研究生导师创新团队项目(qddt-2508)

Effect of yak and Tibetan sheep dung decomposition on the nutrient of soil-plant system in the Qinghai Lake Region

LI Mengqi1, DONG Quanmin1,2, LIU Yuzhen1,2, LYU Weidong1, SUN Caicai1, XU Wei1, LIU Wenting1,2, JI Haiming1, YANG Xiaoxia1,2*   

  1. 1Qinghai Academy of Animal Science and Veterinary/Qinghai Provincial Key Laboratory of Adaptive Management on Alpine Grassland, Qinghai University, Xining 810016, China;
    2Key Laboratory of Alpine Grassland Ecosystem in the Three-River-Source, Ministry of Education, Qinghai University, Xining 810016, China
  • Received:2025-07-02 Accepted:2026-01-29 Online:2026-03-18 Published:2026-09-18

摘要: 牦牛粪便(YD)和藏羊粪便(SD)的降解过程均会影响高寒草地生态系统的养分循环过程,但二者对土壤-植物体系养分循环影响的差异及机制尚不明确。本研究在环青海湖高寒草地开展了为期270 d的牦牛和藏羊新鲜粪便降解试验,通过测定不同降解时期粪便、土壤和植物养分含量,解析两种粪便降解对土壤-植物养分传递的影响。结果表明:1)YD的降解速率显著高于SD,两者全碳、全氮、全磷含量随降解时间线性下降,且YD的全氮含量始终高于SD;降解90 d后,YD中硝态氮和速效磷含量显著高于SD。2)土壤全氮和全磷含量的变化主要受粪便类型影响,解释率分别为57.1%和71.5%;YD处理土壤硝态氮和速效磷含量在90 d降解期间持续显著高于SD处理。3)植物养分吸收具有功能群特异性,植物功能群是主导植物全氮含量变化的关键因子,解释率为40.2%,YD处理禾本科全氮含量较SD处理响应更快。4)结构方程模型表明,粪便主要通过“粪便全效养分→土壤速效养分”的间接路径影响植物养分吸收,土壤速效养分是该过程的关键中介。牦牛粪降解较快,有利于早期速效养分释放与禾草氮素利用;藏羊粪降解较慢,其养分释放过程更为迟缓。本研究阐明了不同牲畜粪便降解驱动土壤-植物养分循环的关键过程,可为高寒草地放牧管理优化提供科学依据。

关键词: 牦牛, 藏羊, 粪便降解, 养分循环, 高寒草地, 土壤-植物体系

Abstract: The decomposition of yak dung (YD) and Tibetan sheep dung (SD) affects nutrient cycling in alpine grasslands, but the mechanisms underlying the differences in their impacts on plant-soil nutrient cycling remain unclear. In this study, a 270 day decomposition experiment using fresh YD and SD was conducted in an alpine grassland near the Qinghai Lake. By measuring nutrient contents in dung, soil, and plants at different decomposition stages, we analyzed the effects of the two dung types on nutrient transfer along the soil-plant continuum. The results showed that: 1) The decomposition rate of YD was significantly higher than that of SD. Total carbon (TC), total nitrogen (TN), and total phosphorus (TP) in YD decreased linearly over time (TC declined from 333.39 g·kg-1 to 211.24 g·kg-1), with TN consistently higher in YD than in SD. After 90 days of decomposition, nitrate (NO3--N) and available phosphorus (AP) contents were significantly higher in YD than in SD. 2) Changes in soil TN and TP were mainly influenced by dung type, accounting for 57.1% and 71.5% of the variance, respectively. Soil NO3--N and AP under YD treatment remained significantly higher than those under SD throughout the 90 day decomposition period. 3) Plant nutrient uptake showed functional group specificity. Plant functional group was the key factor driving variation in plant TN, explaining 40.2% of the variance. The TN of grasses responded more rapidly under YD treatment than under SD treatment. 4) Structural equation modeling revealed that dung affected plant nutrient uptake mainly through the indirect pathway “dung total nutrients → soil available nutrients”, with soil available nutrients acting as the critical mediator. In summary, yak dung decomposed faster, favoring early release of available nutrients and grass nitrogen utilization, whereas Tibetan sheep dung decomposed more slowly, leading to a more prolonged nutrient release process. This study clarified key processes through which different livestock dung types drive soil-plant nutrient cycling and could provide a scientific basis for optimizing grazing management in alpine grasslands.

Key words: yak, Tibetan sheep, dung decomposition, nutrient cycling, alpine grassland, soil-plant system