TRANSITIONAL HORIZONS OF SOILS WITH A CLAY-DIFFERENTIATED PROFILE RESULTING FROM PEDOGENIC DIFFERENTIATION

Gogolev AI; Targulyan VO

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TRANSITIONAL HORIZONS OF SOILS WITH A CLAY-DIFFERENTIATED PROFILE RESULTING FROM PEDOGENIC DIFFERENTIATION

机译：土生代分化导致粘土差异剖面的土壤过渡变位

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A detailed morphoanalytical study was made of the transitional horizons (A2B1) of three representatives of soils with a clay-differentiated profile: Gley-Solod, Podbel,(2) and,podzolic red-earth soils. Two morphotypes of transitional horizons were distinguished: a frontal type in the Gley-Solod and Podbel and a residual type in the Podzolic red-earth soil. Regardless of the type of structure, they are the result of ''in situ'' transformation of the upper part of the illuvial horizon by eluvial soil-formation processes.

机译：进行了详细的形态分析研究，研究了三种具有粘土差异剖面的代表土壤的过渡层（A2B1）：Gley-Solod，Podbel（2）和poldzolic红土。区分了过渡层的两种形态型：Gley-Solod和Podbel中的正面型和Podzolic红土土壤中的残余型。不论结构类型如何，它们都是通过坡地土壤形成过程对原地层上部进行“原位”转化的结果。

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《Eurasian Soil Science》 |1996年第10期|共15页
作者
Gogolev AI; Targulyan VO;
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正文语种 eng
中图分类土壤学;
关键词
Soil transitional horizons; Clay differentiated profile; Pedogenic;

机译：土壤过渡层;粘土差异剖面;成岩作用;

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1. TRANSITIONAL HORIZONS OF SOILS WITH A CLAY-DIFFERENTIATED PROFILE RESULTING FROM PEDOGENIC DIFFERENTIATION [J] . Gogolev AI, Targulyan VO Eurasian Soil Science . 1996,第10期

机译：土生代分化导致粘土差异剖面的土壤过渡变位
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TRANSITIONAL HORIZONS OF SOILS WITH A CLAY-DIFFERENTIATED PROFILE RESULTING FROM PEDOGENIC DIFFERENTIATION

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