Investigation of soil trace elements balance with a view to ensuring quality of crop products

Formation of microelement soil composition being developed in special bio-climatic conditions at the northern border of Mediterranean landscapes distribution are of great economic significance for viticulture evolution and growing up subtropical fruit and nut crops has been analysed by means of the concept of a soil chronofunctio

Soil and landscape changes in ancient agricultural areas (exemplified by antique Olbia)

We report results from studying the landscapes of the rural surroundings of antique Olbia and substantiate the indicators of long-term agrogenic transformation of the physicochemical properties of dry- steppe soils which have experienced long-lasting agricultural pressuresyesBelgorod State Universit

Soil catenas in archeological landscapes

Soil catenas crossing various archeological objects with an age of 360-1800 years have been studied in the subzones of dark chestnut soils and typical, ordinary, and southern chernozems in the East European PlainyesBelgorod State Universit

Interannual Variation in Productivity of Steppe Pastures as Related to Climatic Changes

The results of long-term stationary research on the assessment of aboveground phytomass and soil moisture dynamics in a steppe pasture are presented. An analysis of annual and interannual variation in meteorological parameters over the study period has been performed, and, on this basis, the dependence of productivity on climatic changes has been determined = Результаты многолетних стационарных исследований по оценке массы растительного вещества в надземном ярусе степного пастбища и динамики почвенной влаги. Анализ зависимости продуктивности от метеорологических условийyesБелГ

Peculiarities of Soils on the Sand Bar of the Evpatoria Group of Lakes = Особенности почв на песчаном баре Евпаторийской группы озер

Рассмотрено морфологическое строение и физико-химические свойства разновозрастных почв, которые сформированы на аккумулятивных формах морских берегов Северо-Западного Крым

Soil reproduction in steppe ecosystems of different ages

Features of the development of steppe chernozems were established based on the study of soils of different age groups at archaeological sites. Differences in the formation of phytomass and morphological maturity of the soil profile in the recovery of different age successions were shown. A regional model of the humus horizon steppe soil over time allowed us to estimate the time interval at which the processes of humus accumulation and morphological maturity of the soil profile are relatively at equilibriumyesBelgorod State Universit

Utilizzo come naturale antichi modelli di studio carriole pedo-geomorfologico rapporto

Definire la posizione di suoli moderne in scala temporale interno apre nuove prospettive per la comprensione delle loro capacità di informazione. Suolo, storia naturale come un corpo che serve autentici "banca" record di fondamentale importanza fasi di sviluppo dello spazio-tempo del paesaggio. Proprietà del suolo stabili e conservatori che si acquisiscono come risultato della loro evoluzione, di magazzinaggio e registrate nella memoria del terreno (pedomemory, pedorecor

Restoration of agricultural lands affected by erosional degradation

The characteristics of bioclimatic dependence of restoration of the humus horizon of soils with different degrees of its preservation are established. The prospects of using an adaptation model of ecological restoration of lands degraded as a result of erosion are shownyesБелгородский государственный университе

Periodization of anthropogenically determined evolution of steppe ecosystems

Analysis of the evolution of the vegetation cover of the Northern Black Sea Region. Dynamics of humus formation, biogeochemical transformation and erosion destructio

Quantitative substantiation of pedogenesis model key components

The presented structure of humus soil horizon formation model in time for automorphic conditions includes all the factors of soil formation. The maximum thickness of humus soil horizon is justified in terms of its dependence from climatic energy costs on soil formation and the characteristics of parent rock granulometric content (expressed in terms of particle content lesser than 0.01 mm). This allows to predict the trends of pedogenesis and speed of humus horizon soils formation in relation to global climate changes, the age of which makes a country or more than a centuryyesBelgorod State Universit