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福建若干山地土壤不同形态氧化铁的主组元分析
引用本文:林幼光,陈益,周性敦,陈君月. 福建若干山地土壤不同形态氧化铁的主组元分析[J]. 福建农林大学学报(自然科学版), 1992, 0(4)
作者姓名:林幼光  陈益  周性敦  陈君月
作者单位:福建农学院基础部,福建农学院基础部,福建农学院土壤农化系,福建农学院基础部 福州 350002
摘    要:研究福建4条代表性山地土壤垂直带谱中铁的形态的结果表明,氧化铁的活化度和游离度随海拔升高而呈现规律性的变化,应用主组元分析法,前两个主组元全铁和游离铁的累计贡献率已达85%以上。据此认为,氧化铁的活化度可以作为划分常湿润铁铝土亚纲和湿润铁铝土亚纲的一项参考依据。

关 键 词:氧化铁活化度  主组元分析  土壤系统分类

The Principal Component Analysis of Different Forms of Iron Oxides in Some Mountain Soil
Lin Youguang Chen Yi Zhou Xingdun Chen Junyue. The Principal Component Analysis of Different Forms of Iron Oxides in Some Mountain Soil[J]. Journal of Fujian Agricultural and Forestry University, 1992, 0(4)
Authors:Lin Youguang Chen Yi Zhou Xingdun Chen Junyue
Affiliation:Lin Youguang~1 Chen Yi~1 Zhou Xingdun~2 Chen Junyue~1
Abstract:Different forms of iron oxides of four vertically distributed spectra of mountain soils in Fujian Province were studied.The degree of activation and the degree of segregation of iron oxide varied with the variation of altitude.The result of principal component analysis showed that the accumulative contribution of the first two principal component was more than 85% (Fe_t and Fe_d).Therefore, it is considered that the degree of activation of iron oxide can be used as an refereutial index for classifying peruelic ferrallisols and udic ferrallisols.
Keywords:degree of activation of iron oxide  principal component analysis  soil taxonomia classification
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