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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
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.
作者姓名:路鹏  黄道友  宋变兰  黄敏  刘守龙  苏以荣  肖和艾  吴金水
作者单位:1. 中国科学院水利部水土保持研究所,杨凌,712100;中国科学院亚热带农业生态研究所,长沙,410125
2. 中国科学院亚热带农业生态研究所,长沙,410125
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)
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。

关 键 词:土壤全氮    空间变异性    Kriging插值法    GIS    亚热带典型区
文章编号:1002-6819(2005)08-0181-03
收稿时间:1/6/2005 12:00:00 AM
修稿时间:6/6/2005 12:00:00 AM

Characteristics of spatial variability of total soil nitrogen in the typical subtropical red soil hilly areas
Lu Peng,Huang Daoyou,Song Bianlan,Huang Min,Liu Shoulong,Su Yirong,Xiao Heai,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,2005,21(8):181-183.
Authors:Lu Peng  Huang Daoyou  Song Bianlan  Huang Min  Liu Shoulong  Su Yirong  Xiao Heai  Wu Jinshui
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.
Keywords:total soil nitrogen  spatial variability  Kriging interpolation  GIS  typical subtropical areas
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