Wu Yu-Ping, Ding Ming-Jun, Zhang Hua, Zhang Yue-Ju, Xu Huan, Huang Peng
School of Geography and Environment, Jiangxi Normal University, Nanchang 330022, China.
Key Laboratory of Poyang Lake Wetland and Watershed Research, Ministry of Education, Jiangxi Normal University, Nanchang 330022, China.
Huan Jing Ke Xue. 2024 Oct 8;45(10):6050-6060. doi: 10.13227/j.hjkx.202310130.
An in-depth understanding of the soil nutrient status and balance relationship can help the effective recovery and management of alpine degraded meadows. In order to study the balance relationship among soil carbon, nitrogen, and phosphorus nutrients during the heavy degradation stage of meadows, field sampling and investigation, indoor analysis, and mathematical statistics were used to explore the characteristics and driving factors of changes in soil carbon, nitrogen, and phosphorus content, storage, and ecological stoichiometry during the heavy degradation stage of alpine meadows in the Sanjiangyuan region. The results showed that in the heavy degradation stage, miscellaneous grass plants occupied absolute dominance, soil C∶N∶P was approximately 32.83∶3.87∶0.67, and there was certain nitrogen limitation. The coefficients of variation of soil carbon, nitrogen, and phosphorus content were in the following order: organic carbon (1.09) > total nitrogen (0.63) > total phosphorus (0.29). The organic carbon content and the carbon and nitrogen ratio showed a significant linear decreasing trend with the increase in the grassland degradation index (GDI), while the total phosphorus content and organic carbon storage showed a significant non-linear change, in which the total phosphorus content showed a significant gentle U-shaped distribution, and the organic carbon storage decreased more gently at the beginning of the heavy degradation stage and then decreased sharply when the GDI was 57.9. The results of Mantel correlation analysis showed that the soil carbon to nitrogen ratio, carbon to phosphorus ratio, and nitrogen to phosphorus ratio showed significant correlation with organic carbon content and storage and total nitrogen storage. The results of structural equation modeling indicated that soil water content had direct effects as well as indirect through vegetation factors, soil carbon, nitrogen, and phosphorus ecological stoichiometry ratios, and soil water content and vegetation factors (height, cover, and biomass) were key environmental factors affecting soil ecological stoichiometry. The research results can provide scientific basis and practical guidance for the restoration of heavily degraded grassland in alpine meadows.
深入了解土壤养分状况及平衡关系有助于高寒退化草甸的有效恢复与管理。为研究草甸重度退化阶段土壤碳、氮、磷养分的平衡关系,采用野外采样调查、室内分析及数理统计方法,探究三江源地区高寒草甸重度退化阶段土壤碳、氮、磷含量、储量及生态化学计量比的变化特征及驱动因素。结果表明,在重度退化阶段,杂草植物占据绝对优势,土壤C∶N∶P约为32.83∶3.87∶0.67,存在一定的氮限制。土壤碳、氮、磷含量的变异系数排序为:有机碳(1.09)>全氮(0.63)>全磷(0.29)。有机碳含量及碳氮比随草地退化指数(GDI)的增加呈显著线性下降趋势,而全磷含量及有机碳储量呈显著非线性变化,其中全磷含量呈显著平缓的U形分布,有机碳储量在重度退化初期下降较平缓,当GDI为57.9时急剧下降。Mantel相关性分析结果表明,土壤碳氮比、碳磷比和氮磷比与有机碳含量、储量及全氮储量显著相关。结构方程模型结果表明,土壤含水量既有直接影响,也通过植被因子、土壤碳、氮、磷生态化学计量比产生间接影响,土壤含水量和植被因子(高度、盖度和生物量)是影响土壤生态化学计量比的关键环境因子。研究结果可为高寒草甸重度退化草地的恢复提供科学依据和实践指导。