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白龙江上游不同海拔梯度云杉人工林土壤生态化学计量特征

Soil Ecological Stoichiometry of Picea asperata Plantation at Different Altitudes in Upstream of Bailongjiang River

  • 摘要: 为探讨不同海拔梯度云杉Picea asperata人工林土壤养分的生态化学计量特征及限制因子,旨在提升不同海拔云杉人工林的生产力及水源涵养力。以白龙江上游6个不同海拔的云杉人工林土壤为研究对象,采用野外取样法和室内分析法,测定不同土层(0~20 cm和20~40 cm)土壤有机C、全N、全P、全K含量,并分析了其化学计量特征的垂直变化规律及其与海拔的相关性。结果表明:(1)海拔对云杉人工林土壤养分影响显著(P<0.05),随着海拔梯度的升高,土壤有机C、全N、全P含量呈先增长后减少的趋势,土壤全K含量无明显变化;各海拔梯度土壤有机C、全P含量随着土层加深而减少,全N、全K含量变化规律不明显;土壤养分最大值出现在海拔2 600 m、2 710 m处。(2)C/N、C/P、N/P、C/K的变化范围分别为4.48~36.78、10.37~36.78、1.42~6.82、0.41~2.32,其随海拔升高变化规律各异,均属于中度变异;除C/N、N/P无明显变化规律外,C/P、C/K值0~20 cm土层大于20~40 cm土层;研究区各海拔土壤养分均受N素控制。(3)相关性分析表明,海拔与土壤全N含量、全P含量、N/P、C/N有着显著相关性,有机C含量是影响C/P、C/K的关键因子,全N含量是影响C/N的关键因子,全P含量是影响N/P的关键因子。

     

    Abstract: Exploring the ecological stoichiometric characteristics and nutrient limiting factors of Picea asperata plantations at different altitudes aims to increase the productivity and water conservation capacity of P. asperata plantations. Soil samples of 0−20 cm and 20−40 cm layers were collected from six P. asperata plantations at different altitudes in the upstream of the Bailong River to measure contents of soil organic C total N, total P, total K and to analyze the vertical variation of their stoichiometric characteristics and the correlation with altitude, using the field sampling method and the indoor analysis method. The results were summarized as follows: (1) Altitude had significant effect on soil physical and chemical properties of P. asperata plantations (P<0.05). With the increase of altitude gradient, soil organic C, total N and total P increased first and then decreased, soil total K did not change significantly. The content of soil organic C and total P decreased with the deepening of soil layer, while the total N and total K changed in an unobvious rule with the maximum value of soil nutrients appearing at altitude of 2600 m and 2710 m. (2) The variable range of C/N, C/P, N/P and C/K were 4.48~36.78, 10.37~36.78, 1.42~6.82 and 0.41~2.32, respectively, the variation rules of which were different with the attitude elevating, and all belonged to moderate variation. Except C/N and N/P, the ratios of C/P and C/K of 0−20 cm layer were greater than those of 20−40 cm layer. Soil nutrients in the study area were controlled by N. (3) Correlation analysis showed that altitude was significantly correlated with soil total N, total P, N/P and C/N. Organic C was the key factor affecting ratios of C/P and C/K, total N was the crucial factor affecting ratio of C/N, while total P was the dominant factor affecting ratio of N/P.

     

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