• ISSN 1008-505X
  • CN 11-3996/S

柴达木盆地白刺沙堆剖面土壤化学计量特征

Stoichiometry characteristics of Nitraria tangutorum nebkhas profile soil in Qaidam Basin

  • 摘要:
    目的 植物沙堆广泛分布于荒漠生态系统中,具有减缓风蚀、提高土壤肥力、促进生物多样性等维持区域生态稳定的重要作用,其土壤化学计量学特征是沙堆系统养分循环动态和生态系统恢复力的重要指标。本研究以干旱区优势灌丛白刺(Nitraria tangutorum)为研究对象,探讨其土壤化学计量特征及其驱动因素。
    方法 以柴达木盆地东缘5个相对独立的白刺沙堆为研究对象,通过采集白刺沙堆及其堆间、堆下剖面的土样,研究白刺沙堆土壤碳(C)、氮(N)、磷(P)化学计量特征及其在剖面的垂直变化,采用逐步回归分析确定影响化学计量比的关键土壤因子,通过Spearman相关分析评估了养分比与环境变量之间的关系,最后利用结构方程模型量化了土壤理化性质对土壤化学计量比的直接和间接影响。
    结果 1)研究区白刺沙堆土壤全氮(TN)、全磷(TP)和有机碳(SOC)的平均含量分别为0.11~0.13、0.38~0.43和1.48~1.76 g/kg,TN和SOC含量均低于其他荒漠土壤,沙堆剖面土壤TP含量显著小于堆间地下剖面(P<0.05);速效氮(AN)、速效磷(AP)、速效钾(AK)的平均含量为2.98~4.31、2.67~3.93、68.68~87.03 mg/kg,分别处于极贫乏、贫乏和适量水平,沙堆剖面AP含量显著高于堆间地下剖面(P<0.05),AK含量显著高于沙堆地下剖面(P<0.05)和堆间地下剖面(P<0.001)。C/N、C/P、N/P的平均值分为14.64~15.45、3.86~4.48、0.25~0.32,土壤C、N、P元素的缺乏程度为N>C >P;C/N略高于自然荒漠土壤但低于荒漠绿洲人工林土壤,C/P和N/P均低于其他荒漠土壤,沙堆剖面N/P含量显著高于堆间地下剖面(P<0.05)。2)白刺沙堆剖面土壤TN、SOC、AN、AP、AK含量和C/P、N/P均随土层深度增加整体呈先减小后增加再减小趋势,TP含量整体呈减少趋势,C/N整体呈增加趋势;沙堆土壤养分在0—5 cm表层和较深土层(110—130 cm)均存在积聚现象;土壤含水量、白刺根系体积、平均直径、重量和枯落物重量在不同土层之间具有显著差异(P<0.05),100—135 cm土层具有大量根系和较高的土壤含水量。3)白刺沙堆土壤化学计量比不仅受AN、TP和SOC含量的影响,还受CEC、容重、土壤含水量、根系体积和枯落物重量的影响。
    结论 白刺沙堆土壤全量和速效氮磷以及有机碳含量均较贫乏,尤其氮素限制了白刺的生长发育。沙堆剖面垂直养分动态显示出分层模式:随土层深度增加,土壤全P含量呈减少趋势,全N、速效氮磷钾以及有机碳含量均呈先减小后增加再减小趋势。白刺根系和枯落物在剖面不均匀分布导致的不同土层间土壤含水量的差异,是影响沙堆土壤剖面土壤化学计量特征的主要原因。本研究强调了沙堆生态系统对养分胁迫的脆弱性以及优先考虑土壤肥力恢复和地下生物多样性保护的保护策略的必要性。

     

    Abstract:
    Objectives Nebkhas, which are widely distributed in desert ecosystems, play a pivotal role in sustaining regional ecological stability by mitigating wind erosion, enhancing soil fertility, and fostering biodiversity. Soil stoichiometric characteristics serve as critical indicators of nutrient cycling dynamics and ecosystem resilience within nebkha systems. This study focuses on the Nitraria tangutorum nebkhas, a dominant shrub species in arid regions, aiming to elucidate soil stoichiometric patterns and their underlying drivers.
    Methods Field sampling was conducted across five spatially distinct nebkhas in the eastern Qaidam Basin, China. Soil samples were collected from three microhabitats: within nebkha mounds, the subsurface zone beneath nebkhas, and the inter-nebkha substrate. Vertical profiles (0−135 cm) were analyzed for total nitrogen (TN), total phosphorus (TP), organic carbon (SOC), available nitrogen (AN), available phosphorus (AP), and available potassium (AK). Stepwise regression analysis identified key soil factors influencing stoichiometric ratios, while Spearman correlation analysis assessed relationships between nutrient ratios and environmental variables. Structural equation modeling (SEM) quantified the direct and indirect effects of soil physicochemical properties (e.g., cation exchange capacity, bulk density, soil moisture, root biomass, and litter accumulation) on stoichiometric dynamics.
    Results 1) The average contents of TN, TP and SOC in Nitraria tangutorum nebkhas were 0.11−0.13 g/kg, 0.38−0.43 g/kg, and 1.48−1.76 g/kg, respectively, lower than other deserts in TN and SOC. TP content in nebkhas was significantly depleted compared to underground section of inter-nebkhas (P<0.05). AN, AP and AK contents are in range of 2.98−4.31 mg/kg, 2.67−3.93 mg/kg, and 68.68−87.03 mg/kg, respectively, at the levels of extreme deficiency, deficiency and slight deficiency. AP content in nebkhas was significantly higher than in underground section (P<0.05), and AK content in nebkhas was significantly higher than underground section beneath (P<0.05) and inter-nebkhas (P<0.001). The mean Stoichiometric ratios values (C/N: 14.64−15.45, C/P: 3.86−4.48, and N/P 0.25−0.32) revealed the deficiency degree of nutrients in order of N>C>P. C/N ratios exceeded those in natural deserts but were lower than in oasis plantations, while C/P and N/P ratios were universally lower than in other desert soils. N/P in nebkha mounds surpassed subsurface values (P<0.05). 2) TN, SOC, AN, AP, AK, C/P, and N/P exhibited a "decrease-increase-decrease" trend with depth, whereas TP declined uniformly and C/N increased. Nutrient accumulation peaked in surface (0−5 cm) and deep (110−130 cm) layers. Root volume, diameter, biomass, and litter weight as well as soil moisture varied significantly across soil layers (P<0.05), with the 100−135 cm layer harboring dense root networks and elevated moisture. 3) Soil stoichiometry was jointly influenced by nutrient availability (AN, TP, SOC) and physicochemical factors (cation exchange capacity, bulk density, moisture, root biomass, litter mass). SEM highlighted root distribution and litter accumulation as primary mediators of moisture heterogeneity, thereby regulating nutrient cycling and stoichiometric ratios.
    Conclusions The Nitraria tangutorum nebkhas exhibit pronounced nutrient scarcity (TN, TP, SOC, AN, AP), with nitrogen emerging as the primary growth-limiting factor. Vertical nutrient dynamics reveal a stratified pattern: subsurface P depletion, surface and deep nutrient enrichment, and mid-profile minima. The heterogeneous distribution of roots and litter, coupled with soil moisture gradients, drives these stoichiometric shifts. These findings underscore the vulnerability of nebkha ecosystems to nutrient stress and emphasize the need for conservation strategies that prioritize soil fertility restoration and belowground biodiversity protection.

     

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