祁连山5种典型灌丛土壤生态化学计量特征
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甘肃省自然科学基金(20JR5RE641);


Soil Ecological Stoichiometry of Five Typical Shrubs in Qilian Mountain
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    摘要:

    土壤C、N、P生态化学计量特征是体现生态系统变化过程的重要依据。该研究以分布于祁连山北麓中段的甘青锦鸡儿、鲜黄小檗、金露梅、鬼箭锦鸡儿、吉拉柳等5种典型灌丛群落为研究对象,通过野外调查采样,测定土壤有机C、N、P含量,分析了不同灌丛群落土壤C、N、P含量及其生态化学计量比的垂直分布特征,并探讨了各指标间的耦合关系,为祁连山地区土壤植物养分关系及退化植被恢复与重建提供理论依据。结果表明:(1)祁连山北麓中段5种灌丛群落土壤有机C(45.29 g/kg)、全N(3.85 g/kg)、全P含量(0.70 g/kg)较高,均高于全国平均水平。(2)相关性分析表明,土壤有机C与全N之间呈极显著正相关(P<0.01),但土壤有机C与全P以及全N与全P之间没有明显的相关性,且土壤C、N含量变化几乎完全同步。(3)各灌丛类型土壤有机C、全N含量均表现为表层高于下层,而全P含量土层间差异不显著;各灌丛群落土壤有机C、全N含量均随土层加深呈现“倒金字塔”的分布格局,但不同灌丛类型全P含量随土层加深的变化规律却不一致,且土层对全P含量的影响不显著。(4)5种灌丛群落土壤整体C∶N、C∶P、N∶P(11.29、66.99、5.67)均低于全国平均水平,各灌丛群落土壤C∶P、N∶P随土层加深均呈不同程度的下降趋势,但不同灌丛群落土壤C∶N随土层加深的变化规律有所不同。(5)土壤有机C、全N与C∶N、C∶P、N∶P之间均具有极显著的二次函数关系(P<0.01),土壤全P与C∶N、C∶P、N∶P之间关系不显著。研究认为,祁连山北麓中段土壤C∶N和P含量的稳定性较高(CV=3.99%和2.66%),C∶P、N∶P是判断研究区限制性养分的重要指标,祁连山北麓中段灌丛群落土壤主要受N素的限制。

    Abstract:

    The ecological stoichiometric of soil carbon (C), nitrogen (N), and phosphorus (P) is an important basis to reflect the process of ecosystem change. This study selected Caragana tangutica, Berberis diaphana, Potentilla fruticosa, Caragana jubata and Salix gilashanica which lived in northern piedmont of the central Qilian Mountain as object, to determine the contents of soil C, N and P by field investigation and sampling, analyze the vertical distribution characteristics of soil C, N and P contents and their ecological stoichiometry in different shrub communities, and discuss the coupling relationship among the indexes. It could provid a theoretical basis for the relationship between soil and plant nutrients and the restoration and reconstruction of degraded vegetation in Qilian Mountain. The results showed that: (1) the mean contents of soil C, N and P were 45.29, 3.85, 0.70 g/kg, respectively, which were higher than the national average levels. (2) According to the correlation analysis, soil C and N presented extremely significant positive correlation (P<0.01), but there was no significant correlation between soil C and P or between soil N and P, Furthermore, C and N showed almost synchronous variation. (3) The contents of soil C and N in the surface layer were higher than those in the lower layer, while there was no significant difference in soil P between soil layers in all shrub types. The contents of soil C and N showed an inverted pyramid distribution pattern with the deepening of soil layer in different shrub types, but the changes of soil P were not consistent with the deepening of soil layer in different shrub types, and the effect of soil layer on soli P was not significant. (4) The mean soil C∶N, C∶P and N∶P ratios were 11.29, 66.99 and 5.67, respectively, which were all below the national level. The soil C∶P and N∶P showed a decreasing trend with the deepening of soil layer to different degrees in all shrub types, but the change rule of soil C∶N was different with the deepening of soil layer in all shrub types. (5) Soil C, N and C∶N, C∶P, N∶P had extremely significant quadratic function relationship (P<0.01), but the relationship between soil P and C∶N, C∶P, N∶P was not significant. According to the research, the soil C∶N and P content have high stability (3.99% and 2.66%), whereas the C∶P and N∶P are important indicators for determining nutrient limitation. The soil of shrub community is mainly restricted by N element in northern piedmont of the central Qilian Mountain.

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马 剑,刘贤德,金 铭,等.祁连山5种典型灌丛土壤生态化学计量特征[J].西北植物学报,2021,41(8):1391-1400

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  • 在线发布日期: 2021-09-10
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