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首页> 外文期刊>Moscow University Soil Science Bulletin >The genesis, classification, and melioration of gleyed podzolic chernozem-like soils in the north of the forest-steppe zone of European Russia
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The genesis, classification, and melioration of gleyed podzolic chernozem-like soils in the north of the forest-steppe zone of European Russia

机译：欧洲俄罗斯森林草原带北部的格状荚果类黑钙质类土壤的成因，分类和改良

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摘要

Chernozem-like soils with light-colored acid eluvial horizons are widespread in the forest-steppe zone of European Russia. Their formation is related to gleying under the conditions of a stagnant-percolative water regime on leached rocks. It is closely associated with the evolution of salinized soils (Gedroitss scheme). However, these soils have not been included in the soil classifications of the Soviet Union and Russia. Based on the principles of substantial-genetic classification, one of the authors of this article [35, 10] referred them to gleyed podzolic chernozem-like soils, which are considered as an individual genetic soil type. With respect to agroecological aspects, they are different from the leached chernozems in their low productivity and difficulty of tillage. This article covers the problems of genesis, classification, and melioration of gleyed podzolic chernozem-like soils in the north of the forest-steppe zone of European Russia and their possible association with dark-colored podbels.
机译：浅色酸性坡地层的黑钙土状土壤广泛分布在欧洲俄罗斯的森林草原地区。它们的形成与沥滤岩石上的滞渗水状态下的regime曲有关。它与盐渍化土壤的演化密切相关（Gedroitss方案）。但是，这些土壤尚未包括在苏联和俄罗斯的土壤分类中。根据实质遗传分类的原则，本文的一位作者[35，10]将它们称为带格状的梯形黑钙土样土壤，被认为是个体遗传土壤类型。在农业生态方面，它们与沥滤黑钙土的区别在于生产率低和耕作困难。本文讨论了欧洲俄罗斯森林草原带北部的格状荚果类黑钙质类土壤的成因，分类和改良问题，以及它们与深色荚果的可能联系。

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