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首页> 外文期刊>Eurasian Soil Science >Soils of the Lena-Angara Plateau in the Area of the Kovykta Gas Condensate Field
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Soils of the Lena-Angara Plateau in the Area of the Kovykta Gas Condensate Field

机译:Kovykta凝析气田地区Lena-Angara高原的土壤

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摘要

It is shown that soil-foiming rocks—red calcareous silicate Lower Ordovician and Upper Cambrian deposits—play the leading role in the formation of unique long lastingly frozen mountainous taiga soils of Central Siberia. The functional role of the litter horizon forming under dark coniferous forests is analyzed. This horizon is sensitive to the bioclimatic factor. The genetic specificity of the predominating prepodzolic soils, podburs, soddy burozems, and soddy-calcareous soils and of the locally forming shallow pink-colored podzols is shown.
机译:结果表明,形成土壤的岩石(红色钙质硅酸盐钙质下奥陶纪和上寒武统)在形成独特而持久的西伯利亚中部山区高山针叶林土壤中起着主导作用。分析了暗针叶林下凋落物水平形成的功能作用。这个视野对生物气候因素敏感。显示了优势的前坡地土壤,豆荚,泥泞的burozems和泥泞的钙质土壤以及局部形成的浅粉红色的足动物的遗传特异性。

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