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    典型高寒灌丛草甸区海拔对草甸生物量和土壤养分的影响——以青藏高原东南缘折多山东坡为例

    Effects of Altitude on Meadow Biomass and Soil Nutrients in a Typical Alpine Shrub Meadow Area: A Case Study of the Eastern Slope of Zheduo Mountain, Qinghai-Tibet Plateau

    • 摘要: 海拔对草甸生态系统的生物量、土壤养分及其相互关系产生重要影响,深入揭示其作用机制有助于理解极端环境下草甸植被的响应过程,为保护高海拔地区生态系统提供科学依据。本文以青藏高原东南缘折多山东坡草甸生态系统为研究对象,沿海拔梯度依次选取8块以嵩草为优势种的典型草甸样地,采集不同深度土壤与植被样品,测定地上生物量、土壤总氮(TN)、总磷(TP)、有机碳(SOC)、pH值及含水率等指标,结合方差分析、相关性分析及灰色关联度分析,探讨海拔对土壤养分和草甸生物量的影响。结果表明:(1)随着海拔升高,草甸地上生物量与土壤TP、氮磷比(N:P)呈先增后减的单峰型趋势,土壤TN、SOC、碳氮比(C:N)和含水率则呈先减后增的变化趋势,土壤碳氮比(C:P)变化不显著;(2)土壤养分沿剖面分布表现出明显的表层累积效应,土壤TN和SOC在浅层(0~10 cm)土壤含量最高,且该表聚现象随海拔升高逐渐减弱;(3)深层(10~20cm)土壤的养分变化对草甸生物量的调控作用比浅层(0~10cm)土壤更为显著,且深层土壤的TP含量是影响草甸地上生物量的关键正向因子,深层土壤的SOC含量是影响草甸地下生物量的关键正向因子。研究成果揭示了折多山草甸土壤养分与地上生物量对海拔变化的响应机制,明确了驱动生物量变化的核心因子,可为区域高寒草甸生态保护与可持续管理提供科学依据。

       

      Abstract: Altitude variation exerts significant impacts on meadow ecosystem biomass, soil nutrients and their interrelationships. Delving into these mechanisms is crucial for understanding vegetation response processes in extreme environments and provides scientific basis for protecting high-altitude ecosystems. This study focused on the meadow ecosystem of Zheduo Mountain in the southeastern edge of the Qinghai-Tibet Plateau. Eight typical meadow plots with <italic>Carex myosuroides</italic> as the dominant species were systematically selected along an altitudinal gradient. Soil and vegetation samples from different depths were collected to measure aboveground biomass, soil total nitrogen (TN), total phosphorus (TP), organic carbon (SOC), pH, and moisture content. By integrating Analysis of Variance, correlation analysis and grey relational analysis, we investigated how soil nutrients affect meadow biomass under altitudinal variation.The results indicate that: (1) With increasing altitude, the aboveground biomass of meadows, soil TP, and N:P exhibit a unimodal trend of first increasing and then decreasing, whereas soil TN, SOC, C:N, and water content demonstrate a pattern of first decreasing and then increasing; the change in soil C:P was relatively inconspicuous. (2) Nutrients exhibited distinct surface accumulation, with maximum TN, and SOC concentrations in the 0-10 cm soil layer. This surface enrichment weakened progressively with increasing altitude. (3) Nutrient variations in deep soil layers (10~20 cm) have a more pronounced regulatory effect on meadow biomass than those in surface soil layers (0~10 cm). Specifically, soil TP in the 10~20 cm layer is a key positive factor influencing aboveground meadow biomass, while soil SOC in the same layer is a critical positive factor affecting belowground meadow biomass. In contrast, the pH value of surface soil has minimal influence on meadow biomass. This study elucidates altitudinal response mechanisms between soil nutrients and biomass in Zheduo Mountain meadows, identifying the core driver of biomass variation. These findings provide scientific support for ecological conservation and sustainable management of alpine meadow ecosystems.

       

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