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    雪岭云杉林地上死有机质碳和养分特征的区域差异及组分分异

    Regional variation and component-specific carbon and nutrient characteristics of aboveground dead organic matter in Picea schrenkiana forests

    • 摘要:
      目的 凋落物和粗木质残体(CWD)是森林地上死有机质库的两大主要组分,但两者在养分循环和碳储存中的响应机制及其对死有机质库组成的贡献仍缺乏区域尺度认识。明确不同死有机质组分碳与养分特征的区域变化规律,对于认识森林死有机质碳库组成及养分循环过程具有重要意义。
      方法 以天山山脉昭苏、新源、呼图壁、天池和奇台5个典型区域的天然雪岭云杉林为研究对象,测定凋落物和CWD的碳、氮、磷、钾、钙和镁含量,分析其化学计量特征及碳储量组成。
      结果 (1)凋落物养分含量和化学计量特征均存在明显区域差异,而CWD养分组成相对稳定,仅磷、钾和镁表现出区域差异。(2)与凋落物相比,CWD具有较高的碳氮比和碳磷比以及更大的化学计量变异幅度,表明长期腐解过程中元素迁移增强。(3)不同区域地上死有机质碳储量差异主要来源于凋落物,且沿天山山脉由西向东逐渐增加。尽管凋落物和CWD贡献比例存在明显差异,但总地上死有机质碳储量在区域间未表现出显著变化。其中,凋落物和CWD对总地上死有机质碳储量贡献率分别为57.2% ~ 86.6%和13.4% ~ 42.8%。
      结论 凋落物和CWD的碳养分特征及其碳储量占比的区域差异,共同塑造了雪岭云杉林地上死有机质碳库的空间格局。研究结果有助于深化对干旱区山地森林地上死有机质碳库形成过程及养分循环特征的认识。

       

      Abstract:
      Objective Litter and coarse woody debris (CWD) are the two major components of forest aboveground dead organic matter pools. However, their responses in nutrient dynamics and carbon storage, as well as their relative contributions to dead organic matter pools, remain poorly understood across regional scales. Understanding the spatial variation in carbon and nutrient characteristics of different dead organic matter components is essential for elucidating the composition of forest carbon pools and nutrient cycling processes.
      Method Natural Schrenk spruce (Picea schrenkiana) forests located in five representative regions of the Tianshan Mountains, including Zhaosu, Xinyuan, Hutubi, Tianchi, and Qitai, were selected for this study. Concentrations of carbon (C), nitrogen (N), phosphorus (P), potassium (K), calcium (Ca), and magnesium (Mg) in litter and CWD were determined to evaluate their stoichiometric characteristics and carbon storage patterns.
      Result (1) Significant regional differences were observed in nutrient concentrations and stoichiometric characteristics of litter, whereas nutrient composition in CWD was comparatively stable, with only P, K, and Mg varying significantly among regions. (2) Compared with litter, CWD exhibited higher C∶N and C∶P ratios and greater stoichiometric variability, indicating enhanced elemental losses and retention during long-term decomposition. (3) Regional variation in aboveground dead organic matter carbon storage was primarily driven by litter and generally increased from west to east across the Tianshan Mountains. Although the relative contributions of litter and CWD differed substantially among regions, total aboveground dead organic matter carbon storage showed no significant regional differences. Litter and CWD accounted for 57.2% ~ 86.6% and 13.4% ~ 42.8% of total aboveground dead organic matter carbon storage, respectively.
      Conclusion The spatial pattern of the aboveground dead organic matter C pool in Tianshan spruce forests is jointly shaped by regional variation in the C and nutrient characteristics of litter and CWD and in their relative contributions to C storage. These findings improve our understanding of the formation and nutrient cycling processes of aboveground dead organic matter pools in mountain forests of arid regions.

       

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