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北京松山自然保护区不同母质油松林土壤氮、磷、钾含量垂直分布

苟丽晖1,孙兆地3,聂立水1**,罗盼盼1,吴记贵2,许武德3   

  1. (1北京林业大学水土保持与荒漠化防治教育部重点实验室, 北京 100083; 2北京松山国家级自然保护区, 北京 102115; 3辽宁省水利水电勘测设计研究院, 沈阳 110062)
  • 出版日期:2013-04-18 发布日期:2013-04-18

Vertical distribution patterns of nitrogen, phosphorus, and potassium in Chinese pine forest soils developed from different parent materials in Songshan Mountain Nature Reserve, Beijing of China.

GOU Li-hui1, SUN Zhao-di3, NIE Li-shui1, LUO Pan-pan1, WU Ji-gui2, XU Wu-de3   

  1. (1Ministry of Education Key Laboratory of Soil and Water Conservation and Desertification Combating, Beijing Forestry University, Beijing 100083, China; 2Beijing Songshan National Nature Reserve, Beijing 102115, China; 3Liaoning Investigation and Design Institute of Water Resources and Hydropower, Shenyang 110062, China)
  • Online:2013-04-18 Published:2013-04-18

摘要: 以北京市松山自然保护区同海拔油松林下两种母质(花岗岩和石灰岩)上发育的土壤为对象,研究了土壤的全氮、有效磷、速效钾含量在剖面的垂直变化.结果表明: 花岗岩母质发育的土壤0~20 cm土层的全氮、有效磷和速效钾含量分别为1.61~2.35 g·kg-1、5.84~10.74 mg·kg-1和39.33~93.66 mg·kg-1,石灰岩母质发育的土壤分别为1.69~2.36 g·kg-1、4.45~8.57 mg·kg-1和60.66~124.00 mg·kg-1.两种母质发育的土壤0~10 cm土层的全氮、有效磷和速效钾含量均最大,且与各土层之间差异均极显著,并随土层深度的增加而下降,说明土壤全氮、有效磷和速效钾含量的分布有很强的表聚性,而且石灰岩母质发育的土壤的表聚性更强.对同土层土壤进行配对t检验,全氮含量在各土层之间无显著性差异,有效磷含量在0~10 cm土层差异极显著,速效钾含量在10~20 cm土层之间差异显著.

Abstract: Taking the soils developed from two kinds of parent materials (granite and limestone) under Pinus tabulaeformis forest at the same altitude in Songshan Mountain Nature Reserve of Beijing as test objects, this paper studied the vertical distribution patterns of soil total nitrogen, available phosphorus, and available potassium. The soil developed from granite had the total nitrogen, available phosphorus, and available potassium contents being 1.61-2.35 g·kg-1, 5.84-1074 mg·kg-1, and 39.33-93.66 mg·kg-1, while that developed from limestone had the total nitrogen, available phosphorus, and available potassium contents being 1.69-2.36 g·kg-1, 4.45-8.57 mg·kg-1, and 60.66-124.00 mg·kg-1, respectively. The total nitrogen, available phosphorus, and available potassium contents in the two soils were the highest in 0-10 cm layer, decreased with increasing depth, and had significant differences between different layers, showing that the soil total nitrogen, available phosphorus, and available potassium had a strong tendency to accumulate in surface layer. Such a tendency was more obvious for the soil developed from limestone. The paired ttest for the two soils indicated that the total nitrogen content in different layers had no significant difference, whereas the available phosphorus content in 0-10 cm layer and the available potassium content in 10-20 cm layer differed significantly.