黑垆土的形成环境
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GENETIC ENVIRONMENT OF DARK LOESSIAL SOIL
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    摘要:

    根据成土年龄、土壤中植物孢粉鉴定、腐殖质组成、碳酸钙含量、粘土矿物类型、土壤微形态,土壤剖面形态和其它特征,分析了黑垆土的形成环境。研究表明,黑垆土是一种古土壤,它的许多特征是古生物气候条件的产物。

    Abstract:

    Base on the determination of soil age, spore-pollen in soil, composition of humus, soil micromorphology, X-ray diffraction, soil profile morphological character, soil physical and chemical properties, the genetic environment of dark loessial soil are discussed. The results show that dark loessial soil is a palesol. Many characteristics of dark loessial soil are the result of paleontology,climatic conditions. 14C soil age. The genesis of dark loessial soil includes three year ranges: 8100-8500 4600-7400, and 2000-3000 years B.P., which were cold in the climate. Spore-pollen appraisal. According to the appraisal of spore-pollen in Xian Luo-chuan, Ansai, Longxi and Xifeng,a conclusion can be drawn that the herb is predominant and the environment is cold and damp in the geneticperiod of dark loessial soil.

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季耿善.黑垆土的形成环境[J].土壤学报,1992,29(2):113-125. Ji Genshan. GENETIC ENVIRONMENT OF DARK LOESSIAL SOIL[J]. Acta Pedologica Sinica,1992,29(2):113-125.

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  • 在线发布日期: 2013-02-25
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