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Cartographic Assessment of Soil Diversity in Russia

机译:俄罗斯土壤多样性的制图评估

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The paper describes approaches assessing the diversity of soils in Russia, as well as algorithms for quantitatively assessing the differentiation of soil bodies and covers. To assess soil diversity (or the degree of differentiation of parent rock materials into soil bodies and soil covers), two indices have been introduced: the vertical differentiation index ( Ird ) and the spatial lateral differentiation index ( Ild ( red )). These indices were computed based on the soil cover structure shown on the Soil Map of the Russian Federation on a scale of 1: 2.5 M within the spatial framework of the Map of Soil-Ecological Zoning of the Russian Federation on a scale of 1: 2.5 M. Based on the data obtained, the most complex soil covers and soil profiles on plains were identified at the boundary of the Boreal and Subboreal geographical belts in the zones of soddy-podzolic soils (umbric albeluvisols/umbric podzols) of the southern taiga and gray forest soils (albic luvisols/luvic greyic phaeozems) of deciduous forests characterized by widespread occurrence of dynamically mature soils, as well as in mountainous soil provinces of the Altai and Caucasus.
机译:本文介绍了评估俄罗斯土壤多样性的方法,以及定量评估土壤和盖子分化的算法。为了评估土壤多样性(或家长岩材料分化为土体和土壤覆盖物),已经介绍了两种指标:垂直分化指数(IRD)和空间横向分化指数(ILD(红色))。这些索引基于俄罗斯联邦的土壤地图上显示的土壤覆盖结构,以1:2.5米在俄罗斯联邦的土壤 - 生态分区地图的空间框架内,以1:2.5的规模基于所得数据,在南部南部南部和阵容的陶醉土壤(乌古亚溴脲/翁陶氏陶器)区域的北部和亚伯尔地理带的边界处鉴定了最复杂的土壤覆盖和土壤曲线。落叶林的灰林土(Albic Luvisols / Luvic Grey Phaeozems),其特征在于普遍发生动态成熟的土壤,以及阿尔泰和高加索的山区土壤省份。

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