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ISSN 1993-3916

Arid Ecosystems

The “Arid Ecosystems” journal was organized by the decision of General Biology Division of the Russian Academy of Sciences.

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Архив метки: chestnut soils

REGIONAL CLIMATE CHANGES IN DRY STEPPES AND THEIR CONNECTION TO DROUGHTS

Arid Ecosystems

UDC 551.583:632.125

Pugacheva A.M., Belyaev A.I., Trubakova K.Yu., Romadina O.D. Regional Climate Changes in Dry Steppes and their Connection to Droughts // Arid Ecosystems. 2022. Vol. 28. № 4 (93). P. 13-21. | PDF

The authors carried out an analysis of the regional climate for separate administrative districts of the Volgograd region for the first time. Differences were revealed based on temperature data and incoming precipitation. The study of the Volgograd region in the context of natural and climatic zones and subzones is of particular interest. This makes it possible to analyze multidirectional trends of climate change in a limited area. The open data of the climatic archive (VNIIGMI-MCD) on 5 reference weather stations of the region located in the dry steppes of chestnut soils were used in the work. The droughts were calculated on the basis of temperature and precipitation anomalies using Pedj Drought Index. Regional changes in the climate were identified in terms of the flow of precipitation during the seasons of active vegetation (spring, summer) according to long-term time series of data from registered meteorological stations. Regression analysis showed an increase in their reception in the spring and a decrease in the summer. Also, an increase in the number of droughts in the summer period was revealed with a decrease in aridity. This effect increases the intensity using Pedj Drought Index, the value of which reaches 3 units. A slight inverse correlation was found between the amount of incoming precipitation and the number of droughts in the summer in Volgograd, Surovikinsky, Ilovlinsky and Kamyshinsky districts and dry phenomena in the Surovikinsky district, as well as a direct moderate dependence on droughts in the Kamyshinsky district in summer. Areas with the maximum number of drought events have been identified, therefore, having the maximum risks of agricultural production. In Kamyshinsky district there were 21 drought events in spring, 115 in summer and in Surovikinsky district there were 4 drought events in spring, 70 in summer. In accordance with the results obtained, especially in the regions most susceptible to the influence of droughts, it is necessary to adjust the existing crop rotation schemes, the range of cultivated crops and a shift in emphasis towards conducting reclamation agriculture in these territories in order to eliminate the risks of agricultural production with the effective use of land resources. Regional climate studies are necessary for conducting effective agricultural activities. This makes it possible to objectively assess the situation with climate change at the level of administrative districts. The information obtained is necessary for the purpose of making managerial, risk-free decisions for agricultural production for agricultural regions.

Keywords: climate change, seasons of active vegetation, moisture availability during the seasons of active vegetation, droughts, aridity, dry steppe, chestnut soils.

Acknowledgements. The authors are grateful to the research engineer of the Laboratory of Geoinformation Modeling and Mapping of Agroforestry Landscapes of the Federal Research Center of Agroecology of the Russian Academy of Sciences A.A. Vasilchenko for the cartographic material prepared for the article.

Funding.The work was carried out within the framework of the State Task of the Federal Research Center of Agroecology of the Russian Academy of Sciences «Theoretical foundations of the functioning and natural-anthropogenic transformation of agroforestry complexes in transitional natural-geographical zones, patterns and forecast of their degradation and desertification based on geoinformation technologies, aerospace methods and mathematical cartographic modeling in modern conditions».:

DOI: 10.24412/1993-3916-2022-4-13-21

EDN: ZNQHLZ

HEAVY METALS IN ECOSYSTEMS OF CRYOARID LANDSCAPES OF THE WESTERN TRANSBAIKALIA

Arid Ecosystems

UDC  631.4

Chimitdorzhieva G.D., Bodeeva E.A., Chimitdorzhieva E.O. HEAVY METALS IN ECOSYSTEMS OF CRYOARID LANDSCAPES OF THE WESTERN TRANSBAIKALIA // Arid ecosystems. 2022. V.28. № 2 (91). P. 62-70. | PDF

The results of experimental work on the study of the transformation flux of heavy metals: copper, zinc, nickel and lead from parent rocks into chestnut soils, then into virgin grass stand and humic substances are presented. The soil-forming rocks are deluvial and deluvial-proluvial deposits, as well as deposits of sands and pebbles, which, as a result of their weathering, movement and redeposition, determine the unequal granulometric, mineralogical and chemical composition of rocks, affecting the composition of the soil cover. Chestnut soils are characterized by an arid climate, a long stay in a frozen state, low bioproductivity, low power, light particle size distribution, and low humus content. For the extraction of humic substances, the Grimme method was used. The determination of the content of trace elements was carried out by the atomic absorption method with direct electrothermal atomization of samples. Heavy metals were determined on an atomic absorption spectrophotometer – AAS-15 Perkin Elmer. It was revealed that, due to the depletion of rocks in copper and nickel, there are few of them in the soils, and there is more zinc and lead, which, respectively, is reflected in the vegetation and humus.

Keywords: heavy metals, humic substances, parent rocks, vegetation, chestnut soils, Western Transbaikalia.

Financing. The work was carried out on the topic of state task No. 121030100228-4 «Evolutionary-genetic, biogeochemical and productive functions of soils of the Baikal region as a component of the biosphere, assessment of their resource potential and development of technologies for rational use and protection» 2021-2022.

DOI: 10.24412/1993-3916-2022-2-62-70

MANIFESTATIONS OF SALINITY AND SOLONETZICITY IN ZONAL SOILS OF MONGOLIAN DRY STEPPES

Arid Ecosystems

Pankova E.I., Yamnova I.A. MANIFESTATIONS OF SALINITY AND SOLONETZICITY IN ZONAL SOILS OF MONGOLIAN DRY STEPPES // Arid ecosystems. 2021. V. 27. № 1 (86). P. 43-53. | PDF

The taxonomic position of dry-steppe (chestnut) soils mentioned in the books Classification and Diagnostics of Soils of the USSR (1977), Classification and Diagnostics of Soils of Russia (2004), and World Reference Base for Soil Resources (2014) is discussed. Based on the example of the soils of Mongolia, it is shown that the soils of dry steppes that formed on arenic nonsaline parent rocks are normally nonsaline and nonsolonetzic. The soils of Mongolian dry steppes that formed on saline rocks are saline and solonetzic. The soils with profiles that include loamy layers (even those with a predominantly light granulometric composition and formed on nonsaline rocks) normally feature signs of solonetzicity in the loamy horizons.

Keywords: chestnut soils, cryoarid soils, kastanozems, salic and solonetz (natrik) horizons.

DOI: 10.24411/1993-3916-2021-10136

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