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长白山阔叶红松林土壤无机氮空间异质性
  • ISSN号:1001-9332Call Number: 21-1253/Q
  • 期刊名称:应用生态学报
  • 时间:2010.7.7
  • 页码:1627-1634
  • 分类:S718.5[农业科学—林学]
  • 作者机构:[1]中国科学院沈阳应用生态研究所,沈阳110016, [2]中国科学院研究生院,北京100049
  • 相关基金:中国科学院知识创新工程重要方向项目(KSCX-YW-Z-1022 KZX2-YW-416); 国家自然科学基金项目(40975071 40930107)资助
  • 相关项目:CO2升高、氮沉降和降水量变化对原始阔叶红松林细根周转机制的影响
中文摘要:

利用地统计学方法,研究了长白山阔叶红松林内土壤表层(0~10cm)铵态氮和硝态氮的空间异质性.结果表明:长白山阔叶红松林内土壤表层铵态氮和硝态氮的半方差函数可用球状模型或高斯模型拟合.土壤表层铵态氮和硝态氮的空间分布均呈现中等程度的空间自相关,结构比范围分别在0.70%~41.47%和32.26%~52.66%;铵态氮的空间自相关尺度小于硝态氮,变程分别为8.87和9.76m.土壤表层铵态氮和硝态氮在空间上呈斑块状分布;铵态氮的空间异质性程度高于硝态氮,硝态氮与土壤水分呈显著负相关关系(r=-0.3743,P〈0.05),而铵态氮与土壤水分无显著的相关关系.

英文摘要:

Geostatistic methods were applied to study the spatial heterogeneity of top soil (0-10 cm) ammonium N and nitrate N in a broadleaved-Korean pine mixed forest of Changbai Mountains,Northeast China.The semi-variogram of soil ammonium N and nitrate N could be well fitted by spherical or Gaussian model.The spatial distribution of soil ammonium N and nitrate N all exhibited moderate autocorrelation,with the structural ratio being 0.70%-41.47% and 32.26%-52.66%,and the autocorrelation degree of soil ammonium N was smaller than that of soil nitrate N,with the variation distance being 8.87 and 9.76 m,respectively.Spatially,soil ammonium N and nitrate N were distributed in patches,and the spatial heterogeneity of soil ammonium N was higher than that of soil nitrate N.There was a significant negative correlation between soil nitrate N and soil moisture content,while soil ammonium N had less correlation with soil moisture.

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