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    青藏高原-黄土高原过渡带人工林土壤生态化学计量特征

    Ecological stoichiometric characteristics of plantation soil in the Tibetan Plateau-Loess Plateau transition zone

    • 摘要: 选取青藏高原-黄土高原过渡带青海云杉、祁连圆柏、油松、华北落叶轮、青杨、白桦6种人工林土壤作为研究对象,并以荒草地作为对照,探究人工林土壤碳(C)、氮(N)和磷(P)生态化学计量特征及其影响因素。结果表明:6种人工林土壤C、N和P质量分数范围分别为11.34~20.86、1.16~1.74和0.51~0.72 g/kg,人工林土壤养分质量分数均高于荒草地,表明植被对研究区土壤养分有一定改良作用。林型及土层深度对土壤化学计量比具有一定影响。6种人工林土壤C/N和C/P范围分别为9.30~11.60和16.56~41.98,阔叶林土壤C/N和C/P大于针叶林,其中青杨林显著高于其他林型(P < 0.05),表现为较强的固磷潜力。土壤C/N随土层的加深而减小,变异系数较小,C和N随土层深度的变化具有趋同性;不同林型C/P和N/P随土层深度的变化无明显规律。N/P值在1.71~3.64之间,N素是该区域土壤养分主要限制元素。土壤养分及其化学计量比与土壤饱和导水率及碱解氮有显著相关性(P < 0.05)。研究区人工林对土壤养分具有改良作用,且阔叶林优于针叶林,研究成果可为该区植被恢复建设及人工林抚育管理提供理论参考。

       

      Abstract:
      Background Due to the special geographical location, the ecological environment of Tibet Plateau-Loess Plateau transition zone is fragile and its soil fertility is quite poor. Plantation is the main measure of ecological restoration in this area. Studying the soil ecological stoichiometric characteristics of plantation is conducive to understanding the effect of vegetation improvement in this area and revealing the limiting elements of vegetation growth, providing theoretical basis and technical guidance for vegetation restoration and reconstruction.
      Methods The study selected 5 standard plots (20 m×20 m) for each plantation(Picaea crassifolia, Sabina przewalskii, Pinus tabuliformis Carr., Larix principis-rupperchii, Populus cathayana Rehd, and Betula platyphylla Suk) in this area, and selected 3 standard plots (20 m×20 m) of grassland as a control. We collected 0-60 cm soil samples to determine their C, N and P contents, using one way ANOVA and Pearson correlation analysis to explore the soil ecological stoichiometric characteristics of typical plantations and their influencing factors.
      Results 1) The soil C, N and P contents of 6 plots were 11.34-20.86, 1.16-1.74 and 0.51-0.72 g/kg. The soil nutrient contents of each plantation were higher than that of grassland, while the soil nutrient of broad-leaved forest was higher than that of coniferous forest. 2) The soil C/N, C/P and N/P of 6 plantations were 9.30-11.60, 16.56-41.98 and 1.71-3.64. The soil C/P and N/P were lower than the average level of soil in China. 3) Soil C, N and P decreased with the increase of soil depth, and there were significant differences between different soil layers (P < 0.05). Soil C/N decreased with the deepening of the soil depth, and its coefficient of variation was small. Soil C/P and N/P of different plantations showed different trend of soil depth, while they had no significant difference between different soil layers. 4) The correlation analysis showed that there was a very significant positive correlation between soil C and N, indicating that the changes of their contents were consistent. C/P and N/P were more affected by P. Soil nutrients and their stoichiometric ratio were significantly correlated with soil saturated hydraulic conductivity and alkali-decomposed nitrogen (P < 0.05).
      Conclusions This study indicates that plantation has a certain improvement effect on soil nutrients, while broad-leaved forests are better than coniferous forests. N is found to be the main restricted nutrient in this area. In the process of plantation management, attention should be paid to the supplement of N to promote the healthy development of plantation ecosystem.

       

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