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The first monograph of Ukrainian soil scientists on the Holocene evolution of soilsReview of the first monograph of Ukrainian soil scientists on Holocene evolution of soils

Change in the Soil Structure of Gray Forest Soils of the Moscow Region in Conditions of a Postagrogenic EvolutionStructural analysis of the samples gray forest soils of different ages deposits was carried out

Anthropogenic evolution of dark gray forest-steppe soils in the southern part of the central russian uplandA sequence of dark gray forest soils developing under a virgin broadleaved forest and under

Soils with the second humus horizon, paleochernozems, and the history of pedogenesis at the border between forest and steppe areasSoils with the second humus horizon, paleochernozems, and the history of pedogenesis at the border

Soils with the second humus horizon, paleochernozems, and the history of pedogenesis at the border between forest and steppe areasSoils with the second humus horizon, paleochernozems, and the history of pedogenesis at the border

Contrasting variants of soil development at archaeological sites on floodplains in the forest-steppe of the Central Russian Upland soil evolution in the south and north of the forest-steppe zone on the Central Russian Upland have been

Evolution of the carbonate state of agrogenically transformed dark gray forest soils in the central forest-steppeThe integrated study of the carbonate state of soils, which involves all the forms of soil

Environmental monitoring of sod-podzolic soils under the forest stands over one hundred year period: The case study at the forest experimental station in Moscow, Russia Agrarian University of Moscow Agricultural Academy reveals the evolution of a soil profile over a 100-year

Early stages of the evolution of chernozems under forest vegetation (Belgorod Oblast)Early stages of the evolution of chernozems under forest vegetation (Belgorod Oblast)

К вопросу о пространственной неоднородности почвенных свойств и способах ее оценкиThe evaluative quantitative method of soil compared and graded in their differences is suggested

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