Floodplain soils on the soil map of the Russian Federation, scale 1 : 2.5 M, 1988, in the Russian soil classification

Q4 Agricultural and Biological Sciences Biulleten'' Pochvennogo instituta im VV Dokuchaeva Pub Date : 2021-10-19 DOI:10.19047/0136-1694-2021-108-5-30
N. Savitskaya, T. Ananko, M. Gerasimova
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Abstract

The development of the digital model of the soil map of Russia derived of the map of the Soviet Russian Federation, 1988, compiled in Dokuchaev Soil Science Institute, comprises the transfer of soil names in the initial legend to those in the new classification system of Russian soils (2004). Floodplain soils (only native) are represented by seven legend units (out of 205) that were named in terms of soil classification of USSR, 1977, and part of their names indicated ‘landscapes’ rather than soils, which disagrees with the principles of the new classification system. Basing on numerous publications and following the rules of the new system, soils were renamed. Most of them were referred to alluvial soil types within the synlithogenic trunk (Fluvisols), and their new names indicate both their properties and their zonal attachment. In order to obtain more adequate patterns of soils in river valleys additional soils were introduced including stratified-alluvial soils in the trunk of primary pedogenesis (Regosols). Simultaneously, the composition of polygons in the database was revised in accordance with regional data; human-modified soils were introduced (agro-soils and urbo-soils). 
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俄罗斯联邦土壤地图上的泛滥平原土壤,比例尺1:2.5M,1988年,俄罗斯土壤分类
根据Dokuchaev土壤科学研究所编制的1988年苏联-俄罗斯联邦地图开发的俄罗斯土壤地图数字模型,包括将最初图例中的土壤名称转换为俄罗斯土壤新分类系统中的名称(2004年)。洪泛平原土壤(仅为原生土壤)由七个传说单元(205个)表示,这些单元是根据1977年苏联的土壤分类命名的,它们的部分名称表示“景观”而非土壤,这与新分类系统的原则不一致。根据大量出版物并遵循新系统的规则,土壤被重新命名。它们中的大多数被称为同成因树干内的冲积土类型(Fluvisols),它们的新名称表明了它们的性质和地带性附着。为了在河谷中获得更合适的土壤模式,引入了额外的土壤,包括初级土壤形成主干中的分层冲积土(Regosols)。同时,根据区域数据修订了数据库中多边形的组成;引入了人类改良土壤(农用土壤和urbo土壤)。
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CiteScore
0.90
自引率
0.00%
发文量
15
审稿时长
8 weeks
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