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亚热带红壤丘陵典型区土壤全氮的空间变异特征

路鹏, 黄道友, 宋变兰, 黄敏, 刘守龙, 苏以荣, 肖和艾, 吴金水

路鹏, 黄道友, 宋变兰, 黄敏, 刘守龙, 苏以荣, 肖和艾, 吴金水. 亚热带红壤丘陵典型区土壤全氮的空间变异特征[J]. 农业工程学报, 2005, 21(8): 181-183.
引用本文: 路鹏, 黄道友, 宋变兰, 黄敏, 刘守龙, 苏以荣, 肖和艾, 吴金水. 亚热带红壤丘陵典型区土壤全氮的空间变异特征[J]. 农业工程学报, 2005, 21(8): 181-183.
Lu Peng, Huang Daoyou, Song Bianlan, Huang Min, Liu Shoulong, Su Yirong, Xiao He′ai, Wu Jinshui. Characteristics of spatial variability of total soil nitrogen in the typical subtropical red soil hilly areas[J]. Transactions of the Chinese Society of Agricultural Engineering (Transactions of the CSAE), 2005, 21(8): 181-183.
Citation: Lu Peng, Huang Daoyou, Song Bianlan, Huang Min, Liu Shoulong, Su Yirong, Xiao He′ai, Wu Jinshui. Characteristics of spatial variability of total soil nitrogen in the typical subtropical red soil hilly areas[J]. Transactions of the Chinese Society of Agricultural Engineering (Transactions of the CSAE), 2005, 21(8): 181-183.

亚热带红壤丘陵典型区土壤全氮的空间变异特征

基金项目: 中国科学院知识创新工程重要方向项目(KZCX3-SW-426);国家自然科学基金重点项目(40235057);国家重点基础研究发展规划(973)项目(2002CB412503)

Characteristics of spatial variability of total soil nitrogen in the typical subtropical red soil hilly areas

  • 摘要: 在GIS支持下,运用地统计学方法分析了耕层土壤全氮的空间变异特征,并在此基础上利用Kriging插值方法绘制了土壤全氮的空间分布图。结果表明,在步长间隔60 m下,土壤全氮具有较强的空间相关性,其相关距离为208 m。在NE30°、NE120°两个方向上具有典型的几何异向性结构特点;在NE60°、NE150°两个方向上具有典型的带状异向性结构特点。Kriging插值结果表明,研究区土壤全氮的空间分布表现为条带状和斑块状分布。土壤全氮高值斑块区的分布与地势相对低洼的地形部位相吻合。地形是影响土壤全氮空间变化的主要因素。
    Abstract: A geostatistics method combined with GIS was applied to analyze and map the spatial variability of total soil N in topsoil. The results showed that total soil N had strong spatial relativity at 60 m lag interval and its range of autocorrelation extended to 208 m. The variogram of total soil N was characterized by geometric anisotropy in NE30° and NE120° directions and zonal anisotropy in NE60° and NE150° directions. The spatial distribution map of total soil N interpolated by Kriging interpolation showed apparently strip and block. The "hot spots" of high soil N content were consistent with the low locations of the field. The spatial distribution of total soil N was controlled by topology.
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出版历程
  • 收稿日期:  2005-01-05
  • 修回日期:  2005-06-05
  • 发布日期:  2005-08-30

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