树冠对奥地利松人工林土壤特性的影响

Plamen Glogov, Simeon Bogdanov, Stela Gyudorova
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引用次数: 0

摘要

本研究的目的是跟踪奥地利松(Pinus nigra Arn.研究对象是位于索非亚地区五座山的低温橡树带中树龄为 50-80 年的奥地利松人工种植园。每座山都有三块试验田(SP),每块面积为 400 平方米(表 1)。选择 PP 的主要原因是第一层的覆盖丰度。在每个试验小区内测量以下指标:每层植被的覆盖度-丰度(%);植物废弃物的覆盖度(%)。在所有 SP 中,土壤样本取自三个深度:0-10 厘米、10-20 厘米和 20-30 厘米。对土壤有机质含量进行了分析,包括:全氮(N)、C/N 比值(计算方法)、水提取物中土壤溶液的反应(pH 值)和土壤的机械成分。 研究结果表明,所研究土壤的性质会随着植被的丰度发生很大程度的变化,尤其是在植被的第一层。土壤有机质含量、碳/氮比和机械成分是最能反映冠层和植物废弃物覆盖与土壤特性之间关系的指标。经证实,这些指标值在统计意义上的显著差异强调了植被在土壤形成过程、土壤肥力的形成和变化中的作用。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Canopy influence on soil properties in Austrian pine artificial stands
The aim of the present study is to track changes in the canopy (cover-abundance of the tree layer) of vegetation and cover of the forest litter, and the relationship between them and the dynamics of soil parameters in Austrian pine (Pinus nigra Arn.) plantations. The objects of study are 50-80-year-old artificial plantations of Austrian pine located in the xerothermic oak belt of five mountains in the area of Sofia. In each mountain, three test plots (SPs) were laid out, each measuring 400 m2 (Table 1). The main reason for choosing PP is the cover abundance of the first layer. Within each SP, the following metrics are measured: cover-abundance (%) of vegetation in each layer; the cover of plant litter (%). From all SPs, soil samples were taken from three depths: 0-10 cm, 10-20 cm and 20 -30 cm. An analysis of the content of soil organic matter was carried out, including: total nitrogen (N), the C/N ratio – calculation method, the reaction of the soil solution (pH) in the aqueous extract and the mechanical composition of the soil. The results show that the properties of the studied soils change to a significant extent in accordance with the cover abundance, especially in the first floor of the vegetation. Soil organic matter content, C/N ratio and mechanical composition are the indicators that most clearly reflect the relationship between the canopy and the cover of plant litter on the one hand, and soil properties. The proven, statistically significant differences in the values of these indicators emphasize the role of vegetation in soil-forming processes, the formation and change of soil fertility.
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