成都平原水稻土中铁的分异特点
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DIFFERENTIATION OF IRON OXIDES IN PADDY SOILS OF CHENGDU PLAIN
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    摘要:

    本文研究了成都平原发育于岷江冲积物、紫色土沉积物和黄壤残积物三种不同母质的六个主要水稻土剖面中各种形态氧化铁含量及其在剖面中的分异特点,探讨了各种形态氧化铁之间的关系及其与环境条件、成土母质的关系。此外,根据全铁含量在剖面中的分异,讨论了发生层的形成。

    Abstract:

    Sia paddy soils derived from three different parent materials were sampled from the Chengdu Plain which was one of the most important rice-growing regions in China to study the characteristics of the differentiation of iron oxides in various forms and its relation to the formation of the specific genetic horizon. Tlte results showed that the extent of the variation of iron oxides in various forms in the paddy profiles studied decreased in the following order: amor. iron oxide > free iron oxide > total iron. It was revealed that the content of total iron was closely related to the parent material from which the paddy soil was derived, and the content of free iron was positively linearly related to the content of total iron in the paddy soil, which suggested that it was also related to the parent materials to some extent, but the content of amor iron oxide was greatly influenced by the environmental conditions.

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赵红挺.成都平原水稻土中铁的分异特点[J].土壤学报,1992,29(2):191-198. Zhao Hongting. DIFFERENTIATION OF IRON OXIDES IN PADDY SOILS OF CHENGDU PLAIN[J]. Acta Pedologica Sinica,1992,29(2):191-198.

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  • 在线发布日期: 2013-02-25
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