森林土壤C:N:P生态化学计量垂直格局及理化驱动OA
Vertical patterns of C:N:P ecological stoichiometric in forest soils and their physicochemical drivers
[目的]为揭示藏东昌都地区大果圆柏林、川西云杉林、川滇高山栎林等3种典型森林类型土壤C、N、P含量及生态化学计量特征的垂直分异规律,明确土壤理化性质对其空间变异的驱动机制,为藏东高海拔森林生态系统养分循环过程解析与可持续管理提供科学支撑.[方法]采集3种森林类型0~20 cm、20~40 cm 和40~60 cm土层土壤样品,测定土壤理化性质和C、N、P含量,并结合冗余分析(RDA)和主成分分析(PCA)探讨驱动机制.[结果]结果显示(1)3种森林类型土壤理化性质存在显著林型差异与垂直分异,川西云杉林具有"低容重、高含水率、高孔隙度"特征,川滇高山栎林pH值和黏粒含量最低、砂粒含量最高,容重表层显著低于中深层,pH值呈深层酸化趋势;(2)C、N含量均呈表层富集的垂直递减规律,大果圆柏林与川西云杉林C、N含量显著高于川滇高山栎林,P含量垂直分异平缓,C/P比垂直分异最一致(均显著递减),川西云杉林表层呈磷限制、整体与大果圆柏林为氮限制,川滇高山栎林无明显养分限制;(3)理化性质对计量特征的驱动具有林型特异性和深度依赖性,大果圆柏林受砂粒、pH值和孔隙度影响;川西云杉林以容重和含水率为主导;川滇高山栎林受黏粒和孔隙度调控,表层理化性质与计量特征关联更直接.[结论]在昌都地区进行森林土壤环境监测时,可选取土壤pH值、砂粒、容重、孔隙度、含水率和有机质作为土壤生态化学计量特征垂直分异的关键监测指标,进行监测以及后续土壤的改良.
[Objective]This study aimed to reveal the vertical variation patterns of soil carbon(C),nitrogen(N),phosphorus(P)contents and their ecological stoichiometric characteristics in three typical forest types(Juniperus tibetica forest,Picea balfouriana forest,and Quercus aquifolioides forest)in Qamdo,eastern Xizang,clarify the driving mechanisms of soil physicochemical properties on their spatial variability,and provide scientific support for analyzing nutrient cycling processes and sustainable management of high-altitude forest ecosystems in eastern Xizang.[Method]Collect soil samples from the 0-20 cm,20-40 cm,and 40-60 cm soil layers in three forest types.Soil physicochemical properties and C,N,P contents were determined,and redundancy analysis(RDA)and principal component analysis(PCA)were combined to explore the driving mechanisms.[Result]The results showed that:(1)There were significant forest type differences and vertical variations in soil physicochemical properties among the three forest types.Picea balfouriana forest exhibited the characteristics of"low bulk density,high water content,and high porosity";Quercus aquifolioides forest had the lowest pH value and clay content but the highest sand content;bulk density was significantly lower in the topsoil than in the middle and deep layers,and pH value showed a deep-layer acidification trend.(2)C and N contents showed a consistent vertical decreasing pattern with surface enrichment;C and N contents in Juniperus tibetica forest and Picea balfouriana forest were significantly higher than those in Quercus aquifolioides forest;the vertical variation of P content was gentle;the vertical variation of C/P ratio was the most consistent(all significantly decreasing).The topsoil of Picea balfouriana forest showed P limitation,while Picea balfouriana forest and Juniperus tibetica forest showed N limitation overall,and Quercus aquifolioides forest had no obvious nutrient limitation.(3)The driving effects of physicochemical properties on stoichiometric characteristics were forest type-specific and depth-dependent:Juniperus tibetica forest was affected by sand content,pH value,and porosity;Picea balfouriana forest was dominated by bulk density and water content;Quercus aquifolioides forest was regulated by clay content and porosity;the correlation between topsoil physicochemical properties and stoichiometric characteristics was more direct.[Conclusion]Soil pH value,sand content,bulk density,porosity,water content,and organic matter can be selected as key monitoring indicators for the vertical variation of soil ecological stoichiometric characteristics in Qamdo during forest soil environmental monitoring,and provide references for subsequent soil improvement.
罗浩杰;万丹;陈嵚崟
西藏农牧大学资源与环境学院/高寒水土保持研究中心,西藏 林芝 860000西藏农牧大学资源与环境学院/高寒水土保持研究中心,西藏 林芝 860000西藏农牧大学资源与环境学院/高寒水土保持研究中心,西藏 林芝 860000
农业科技
森林类型土壤生态化学计量垂直分异理化性质冗余分析主成分分析
forest typesoilecological stoichiometryvertical differentiationphysicochemical propertiesredundancy analysis(RDA)principal component analysis(PCA)
《东南园艺》 2026 (1)
23-34,12
国家自然科学基金资助项目(32241036)
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