scholarly journals Genesis problems of chernozems of the Galicia

Author(s):  
I. Papish ◽  
S. Pozniak

The problems of genesis and classification of chernozems of Galicia is being considerated within the common theory of the evolution of chernozems of the forest-steppe zone of Ukraine. In the soilbotanical conditions of the West forest-steppe of Ukraine the character and trend direction of the last Holocene evolution of chernozems is diverse. Key words: chernozems, pheozems, soil cover, Galicia, soil evolution, classification, soil horizon, morphological features.

Author(s):  
Erofey Krasekha

Questions of settling and development of territory of Ukraine during prehistoric time are considered. Specialities of development of agriculture and cattle breeding by different archaeological cultures in the steppe zone depending on paleogeographic stages are covered. Features of the development of agriculture in the steppe zone of Ukraine are determined primarily by physical and geographical factors and, above all, the climate, the nature of the relief, the specifics of vegetation and soil cover. At the same time the Ukrainian steppe of thousand years was arena on which arose, some time existed, and then disappeared, practically leaving nothing after itself ethnic cultures which were engaged mainly in cattle breeding. Key words: paleogeography, agriculture, cattle breeding, steppe zone.


2019 ◽  
Vol 75 ◽  
pp. 02002
Author(s):  
Yuliya V. Gorbunova ◽  
Tatyana N. Demyanenko ◽  
Valentina V. Chuprova

The possibilities of using data of Earth remote sensing for the construction of a geomorphological profile for the purpose of agroecological assessment of soil cover patterns and subsequent land typification as a basis for the design of adaptive landscape agriculture in the Krasnoyarsk Territory are considered. The geomorphological profile illustrates the features of the relief and regularities in the distribution of soil structures with a certain set of agro-ecological conditions and limiting factors that determine the choice of agro-technologies and farming systems.


Ekosistemy ◽  
2021 ◽  
pp. 5-11
Author(s):  
L. A. Novikova ◽  
E. V. Mikhailova ◽  
V. M. Vasjukov ◽  
T. V. Gorbushina

Halophytic vegetation is very rare in the forest-steppe zone. It was studied in the tract Serdobsky solonetsin the vicinity of Serdobsk (Serdobsky district, Penza region). The studies were conducted in the years 2009–2018, using the technique of geobotanical profiling. 80 trial areas were laid (35 in 2009 and 45 in 2008). Ecological and phytocenotic classification of plant communities is performed on the dominant principle. Comparison of two descriptions of vegetation with an interval of 10 years allows us to trace the transformation of halophytic vegetation after intensive anthropogenic impact (grazing and partial plowing) in different environmental conditions. The flora of Serdobsky solonets consists of 179 species of vascular plants, of which 13 species are included in the Red book of the Penza region (2013). The share of halophytic vegetation on the territory of Serdobsky solonetshas changed over 10 years: from 97.0 % to 63.8 %. Moreover, halophyte meadows occupied 67.0 % and halophyte steppes 30.0 % of the area in 2009. Now (2018) halophytic steppes make up 30.8 %, and halophytic meadows 33.0 %.The main stages of demutation of halophytic steppe and meadow vegetation were identified in various environmental conditions (meadows and steppes). The same stages of demutation were identified earlier for the South-Eastern Solonets (Neverskinsky district of the Penza region). However, a special stage of annual saline grasslands has been identified.This place requires protection due to the high level of floral and phytocenotic diversity. We offer to organize here a natural monument called “Serdobsky solonets”.


Author(s):  
S. V. Lukin

Studies were conducted in the forest-steppe zone of the Belgorod region. The soil cover was represented by Haplic Chernozems and Luvic Сhernozems. The aim of the research was to analyze and assess the accumulation in pea, white lupine and soybean plants of the main macro- and microelements. The materials of local agroecological monitoring 2015-2017 years were used for pea, white lupin and soybean sowings. It has been established that the highest average content of the main macroelements: nitrogen (6,26%), phosphorus (1,88%), potassium (2,52%), sulfur (0,3%) and trace elements: copper (11,7 mg / kg), nickel (5,15 mg / kg), chromium (0,42 mg / kg) are characterized by soy beans. The highest content of zinc (43,2 mg / kg), cobalt (0,88 mg / kg) and molybdenum (6,73 mg / kg) was recorded in white lupine beans. The lowest average nitrogen content (3,3%), potassium (1,38%), sulfur (0,14%), zinc (26,5 mg / kg), copper (3,85 mg / kg), molybdenum 0,39 mg / kg) was noted in pea beans. The lowest content of cobalt (0,14 mg / kg) was characteristic of soybeans. The mean phosphorus content, nickel and chromium in the white lupine beans and peas was similar and significantly lower than in soy beans.


2010 ◽  
Vol 17 (1) ◽  
pp. 47-52 ◽  
Author(s):  
Barbara Sudnik-Wójcikowska ◽  
Ivan Moysiyenko

Zonal character of the flora of kurgans in central and southern UkraineIn the years 2004-2010 floristic studies were carried out on kurgans in 4 different climatic/vegetation zones: 3 steppe zones (west and central Pontic desert steppe, west Pontic grass steppe, west and central Pontic herb-rich grass-steppe) and a forest steppe zone. Among the 450 kurgans surveyed, 106 barrows met the selection criteria. The species composition and the contribution of different life forms to the flora of kurgans changed along the north-south gradient. Jaccard's similarity coefficient and Wards clustering method were used to compare the qualitative composition of flora in particular zones. The results of this comparison confirmed floristic differences between kurgans located in the four zones. Kurgans in the desert steppe zone proved to have the most distinct flora among the floras considered. The biggest similarities were found between the flora of kurgans in the forest steppe zone and that of barrows in the west and central Pontic herb rich grass steppe.


Author(s):  
N. A. Sokolova ◽  
◽  
E. N. Smolentseva ◽  

Plowing up is a widespread type of anthropogenic transformation of soils and soil cover (SC) in the forest-steppe zone of Western Siberia. As a result of plowing up agrogenic transformation (agrotransformation) of soils causes their form and properties change, as well as the spatial characteristics of the SC. In the example of a model territory the features of changes in the component composition and structure of the SC of the Pre-Salair drained plain under the influence of arable press are studied. Automorphic soil formation prevails in the studied area, and zonal natural soils here are chernozems (clay-illuvial and migrate-micellar) and dark grays. These soils have an upper dark humus horizon, which in arable soils becomes an agro-dark humus horizon. In the studied area, an increase in number of the SC components was found due to the soils of the agrozems section and different types of agricultural soils, which leads to a diversification of the component composition. It was found that the component composition of SC shows high degree of its agrotransformation: area of arable soils is 55.6% of total area of SC. We also showed the sequence of agrotransformation for the chernozems of the model territory: chernozems, agrochernozems, agrozems, abraded agrozems, agroabrazems. Agrozems occupy a large area and have a classification diversity. Factors affecting the diversity of agrozems at the type and subtype classification level are identified: the degree of agrogenic transformation of clay-illuvial and migrate-micellar chernozems are distinguished. The low thickness of the humus horizon of soils in the pre-agrarian period during plowing leads to various degrees of their agrotransformation and classification divergence of soils. The SC structure is characterized by geometric parameters in accordance with the concept of V.M. Friedland. These are areas and dissection coefficients (minimum, maximum, average and median) of elementary soil areal (ESA) and soil combinations areal (SCA). Geometries of ESA and SCA are caused by the combined influence of terrain features and anthropogenic impact. ESA of agrotransformed soils (agrograys, agrochernozems, agrozems) have largest sizes, besides undisturbed automorphic soils; ESA of strongly transformed soils developed in temporary flow hollows have smallest sizes. The overall result of the agrogenic transformation of the SC on the studied area is a new spatial agrogenic structure. In the component composition of SC specific soils of different taxonomic levels appear.


2014 ◽  
pp. 45-70 ◽  
Author(s):  
A. Yu. Korolyuk

The West-Siberian Plain extends more than 1200 km from west to east. Its southern part is occupied by steppe and forest-steppe zones with pre-dominance of herbaceous plant communities. Steppes and xeric meadows are widespread on this territory and characterized by a high diversity and complex spatial structure. This study presents the analysis of 874 relevés describing xeric meadows and steppes of the class Festuco-Brometea from the West Siberian Plain. Numerical analysis with using of plant indicator values showed that some ecological factors, such as soil moisture, salinity and sand content are important in differentiation of grasslands. Three zonal associations form the sequence on the latitudinal gradient from 56º to 51º of northern latitude: Galatello biflorae–Calamagrostietum epigeii (xeric meadows and meadow steppes on solonetz soils in forest-steppe zone), Helictotricho desertori–Stipetum rubentis (rich bunchgrass steppes of southern part of forest-steppe zone and northern part of steppe zone), Artemisio austriacae–Stipetum capillatae (typical bunchgrass steppes of steppe zone). Zonal associations form complexes with other grasslands of Festuco-Brometeae. In forest-steppe landscapes zonal communities usually adjoined with Galio borealis–Artemisietum ponticae in more mesic habitats and with halophyte association Limonio gmelini–Phleetum phleoides. In steppe regions zonal associations make an assemblage with relatively mesic grasslands of Trommsdorffio maculatae–Stipetum pennatae and halophyte communities of Limonio gmelini–Stipetum capillatae on solonetz soils. Three associations form the sequence related with increasing of sand content in soils: Gypsophilo paniculatae–Artemisietum glaucae, Sileno borysthenicae–Cleistogenetum squarrosae, Scorzonero ensifoliae–Festucetum valesiacae. All grasslands usually are under intense grazing that cause changes in plant communities, first of all, the reduction of meso-xerophyte species diversity. The class Festuco-Brometea in the West Siberian plain is divided into two orders. The order Festucetalia valesiacae unites xeric meadows and meadow steppes in forest-steppe landscapes. The class and order are diagnosed mainly by meso-xerophyte species with wide Eurosiberian distribution: Anemone sylvestris, Artemisia glauca, A. latifolia, Astragalus danicus, Campanula sibirica, Centaurea scabiosa, Dianthus versicolor, Festuca pseudovina, Festuca valesiaca, Filipendula vulgaris, Fragaria viridis, Galium ruthenicum, Galium verum, Koeleria cristata, Medicago falcata, Phleum phleoides, Phlomoides tuberosa, Plantago urvillei, Poa angustifolia, Polygala comosa, Scabiosa ochroleuca, Seseli libanotis, Stipa capillata, Stipa pennata, Tephroseris integrifolia, Trommsdorffia maculata, Veronica spicata. This order is presented by the alliance Galatellion biflorae located to the west from the Ob River (Korolyuk, Kiprijanova, 1998). Its communities differ from others by presence of salt-tolerant species: Artemisia pontica, Artemisia rupestris, Carex caryophyllea, Galatella biflora, Inula britannica, Melampyrum cristatum, Peucedanum morisonii, Plantago maxima, Silene multiflora. To the east from the Ob River this alliance is replaced by Poo urssulensis–Artemision glaucae, in the South Urals by Festucion valesiacae. The xeric meadows of Festuco-Brometea north from forest-steppe zone are replaced by mesic meadows of Molinio-Arrhenatheretea. The order Helictotricho-Stipetalia represents the typical steppes and xeric variants of meadow steppes. Its distribution covers steppe zone and southern part of forest-steppe zone. The main part of its diagnostic combination is formed by xerophyte steppe plants: Achillea nobilis, Adonis villosa, Androsace maxima, Artemisia austriaca, Carex supina, Galatella angustissima, Helictotrichon desertorum, Jurinea multiflora, Onosma simplicissima, Oxytropis pilosa, Pilosella echioides, Potentilla bifurca, P. humifusa, Salvia stepposa, Scorzonera austriaca, Seseli ledebourii, Spiraea crenata, Stipa zalesskii, Taraxacum erythrospermum, Thymus marschallianus, Verbascum phoeniceum, Veronica incana. Three alliances form the sequence along moisture gradient: more mesic rich steppes of Helictotricho desertori–Stipion rubentis (diagnostic species: Helictotrichon desertorum, Stipa zalesskii, Thymus marschallianus, Artemisia latifolia, Filipendula vulgaris, Fragaria viridis, Phlomoides tuberosa, Plantago urvillei, Seseli libanotis, Artemisia pontica, A. rupestris, Galatella biflora, Peucedanum morisonii, Silene multiflora), typical steppes of Artemisio austriacae–Festucion valesiacae (diagnostic species: Androsace maxima, Artemisia austriaca, Carex supina, Po­ten­tilla bifurca, Scorzonera austriaca, Taraxacum erythrospermum), and dry steppes of Stipion korshinskyi Toman1969 (diagnostic species: Kochia prostrata, Krascheninnikovia ceratoides, Leymus ramosus, Phlomoides agraria, Stipa korshinskyi, Stipa lessingiana).


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