MINERAL TRANSFORMATION IN SOILS OF THE TAIGA-FOREST ZONE AS A FUNCTION OF THEIR DEGREE OF HYDROMORPHISM

Zvereva TS

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MINERAL TRANSFORMATION IN SOILS OF THE TAIGA-FOREST ZONE AS A FUNCTION OF THEIR DEGREE OF HYDROMORPHISM

机译：太原林区土壤的矿物转化作用及其对水溶斜度的作用

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Mineralogical analysis of coarse and fine particles in soils on homogeneous materials revealed consistent variation in the basic groups of minerals for soils with increasing degrees of hydromorphism, from Brown to Podzolic to eluvial-gley to Bog-gley soils. The role of the principal mineral transformation mechanisms in the genesis of soils in the taiga-forest zone is described.

机译：从均质材料上对土壤中的粗颗粒和细颗粒进行的矿物学分析表明，从棕壤到波佐利奇到坡格利到博格格利地带，随着水同溶度的增加，土壤基本矿物质的含量也发生了一致的变化。描述了主要的矿物转化机制在针叶林林带土壤成因中的作用。

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《Eurasian Soil Science》 |1996年第10期|共10页
作者
Zvereva TS;
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原文格式 PDF
正文语种 eng
中图分类土壤学;
关键词
Mineral transformation; Taiga forest zone soils; Hydromorphism;

机译：矿物转化;针叶林林带土壤;同质性;

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专利

1. MINERAL TRANSFORMATION IN SOILS OF THE TAIGA-FOREST ZONE AS A FUNCTION OF THEIR DEGREE OF HYDROMORPHISM [J] . Zvereva TS Eurasian Soil Science . 1996,第10期

机译：太原林区土壤的矿物转化作用及其对水溶斜度的作用
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MINERAL TRANSFORMATION IN SOILS OF THE TAIGA-FOREST ZONE AS A FUNCTION OF THEIR DEGREE OF HYDROMORPHISM

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