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钱江源-百山祖国家公园百山祖园区典型森林植被特征及其与土壤的关系

Characteristics of Typical Forest Vegetation and Their Relationship with Soil in Qianjiangyuan-Baishanzu National Park

  • 摘要: 为探究不同森林群落植被特征及其与土壤的关系,采用典型样地法研究钱江源-百山祖国家公园百山祖园区常绿阔叶林、针阔混交林、针叶林3种森林群落中各1200 m2的物种多样性和土壤理化性质。结果表明,常绿阔叶林、针阔混交林和针叶林的乔木层植物种类(胸径≥5 cm)分别有28、27、13种,灌木层(包括乔木层更新幼苗)植物分别有41、60、37种,草本层植物分别有7、6、7种;乔木层的物种丰富度指数、Simpson优势度指数、Shannon指数和Pielou均匀度指数大小均表现为常绿阔叶林>针阔混交林>针叶林,其中针叶林显著低于其他两种林分(P<0.05);针阔混交林中灌木层的物种丰富度指数、Simpson优势度指数、Shannon指数和Pielou均匀度指数均显著大于常绿阔叶林和针叶林(P<0.05);3种森林类型乔木层胸径大小的分布均表现为“倒J”型,树高分布呈现正偏态分布;常绿阔叶林土壤pH值显著高于针阔混交林和针叶林(P<0.05),林地土壤有机碳含量大小表现为针阔混交林>常绿阔叶林>针叶林,三者间差异显著(P<0.05)。乔木层的Simpson指数、Shannon指数、Pielou均匀度指数和土壤容重均呈显著负相关(P<0.05),和土壤总孔隙度均呈显著正相关(P<0.05),Pielou均匀度指数和土壤最大持水量呈显著正相关(P<0.05);灌木层的物种丰富度、Shannon指数与土壤有机碳呈现显著正相关(P<0.05)。综上,针叶林乔灌层植物种类较少,可对针叶林进行适当疏伐,降低林分郁闭度,有利于其他乡土树种的自然迁入、定植和生长,从而增加植物多样性。

     

    Abstract: To explore the vegetation characteristics of different forest communities and their relationships with soil, the typical plot method was used to study the species diversity and soil physical-chemical properties of three forest communities (evergreen broad-leaved forest, coniferous-broadleaved mixed forest, and coniferous forest) in Qianjiangyuan-Baishanzu National Park, with each plot area of 1200 m2 per community type. The results showed that the tree layers(with DBH ≥ 5 cm)of the above forests had 28, 27, and 13 plant species, respectively; the shrub layers (including regenerating tree seedlings) had 41, 60, and 37 plant species, respectively; and the herb layers had 7, 6, and 7 plant species, respectively. For the tree layer, the species richness index, Simpson dominance index, Shannon index, and Pielou evenness index all followed the order: evergreen broad-leaved forest > coniferous-broadleaved mixed forest > coniferous forest, with the indexes of coniferous forest being significantly lower than those of the other two forest types (P < 0.05). In the shrub layer of the coniferous-broadleaved mixed forest, the indexes of four types were significantly higher than those of the evergreen broad-leaved forest and the coniferous forest (P < 0.05). DBH distribution of the tree layer in all three forest types exhibited a “Inverted-J” shape, while tree height showed a positively skewed distribution. Soil pH in the evergreen broad-leaved forest was significantly higher than those in the coniferous–broadleaved mixed forest and the coniferous forest (P < 0.05). Soil organic carbon content showed a distinct gradient, that in coniferous-broadleaved mixed forest was the highest, followed by evergreen broad-leaved forests, and then coniferous forests, with significant differences among the three types (P < 0.05). For the tree layer, the Simpson index, Shannon index, and Pielou evenness index were significantly negatively correlated with soil bulk density (P < 0.05), significantly positively correlated with total soil porosity (P < 0.05), and the Pielou evenness index was significantly positively correlated with the maximum soil water-holding capacity (P < 0.05). For the shrub layer, species richness and Shannon index were significantly positively correlated with soil organic carbon content (P < 0.05). In summary, the tree and shrub layers in the coniferous forest had relatively few plant species. Moderate thinning of the coniferous forest to reduce canopy density is recommended, which would facilitate the natural recruitment, establishment, and growth of other native tree species, thereby increasing plant diversity.

     

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