Current status of the Russian desman habitats in small rivers of the Don River Basin in Saratov oblast and the abundance of this species

2013 ◽  
Vol 40 (10) ◽  
pp. 854-861 ◽  
Author(s):  
O. S. Oparina ◽  
E. I. Filinova ◽  
E. E. Sonina ◽  
Yu. A. Malinina ◽  
M. L. Oparin
2021 ◽  
Author(s):  
Ilia Lobzenko ◽  
Dina Nevidomskaya ◽  
Elizaveta Konstantinova ◽  
Tatiana Minkina ◽  
Tatiana Bauer ◽  
...  

<p>Large rivers and their deltaic parts and adjacent coastal zones are subjected to strong anthropogenic influence and are often considered as hotspots of environmental pollution. The Don River basin is a highly urbanized area with developed agriculture and industry which negatively affect water quality, aquatic ecosystems and soils. The main objectives of the proposed research were to determine the levels of potentially toxic elements (PHEs) in soils of various aquatic landscapes of the study area, as well as to reveal the relationships between the content of exchangeable PTEs and the physical-chemical properties of floodplain soils.</p><p>Depending on the soil-landscape and hydrological conditions and taking into account the intensity of anthropogenic influence, the following zones were identified: the lower Don floodplain from the Tsimlyansk Reservoir to the source of the Mertvy Donets River, Don Delta, the coastal zone of the Taganrog Bay, the mouths of small rivers flowing into the bay, and Taganrog city, an industrial port center on the northern coast of the bay.</p><p>The floodplain and coastal landscapes of the study area are dominated by Fluvisols. Solonchaks, Arenosols and Haplic Chernozems which are background soils of the region are less common. Soil samples were collected in summer 2020 from the surface soil horizon (0–20 cm deep). The particle size analysis was conducted using the pipette method; the total organic carbon content in the soils was determined using the dichromate oxidation; the pH was measured by potentiometry in the supernatant suspension of soil and water in a ratio of 1:2.5. The total concentrations of Cr, Mn, Ni, Cu, Zn, Cd, and Pb were determined by X-ray fluorescence analysis using a Spectroscan MAX-GV spectrometer (Spectron, Russia), and the content of exchangeable forms extracted from the soil by NH4Ac buffer solution with pH 4.8 and soil/solution ratio of 1:10 for 18 h was determined by atomic absorption spectrophotometry.</p><p>The obtained results showed that soils of the Lower Don and Taganrog Bay coastal zone are rather contrasted in terms of properties and metal contents, which indicates the variability of landscapes, natural and anthropogenic processes in the studied systems. High CV values for Pb, Zn, Cd and Cr indirectly indicate strong anthropogenic influence on these environments. The results of PCA analysis showed that there are two association of metals in terms of geochemical behaviour and sources. The first one included Cr-Zn-Pb-Cd, the elements of anthropogenic origin, the second Mn, Ni, and Cu, which are probably of mixed origin. The obtained results showed that the coastal zone is a diverse and complex system subjected to anthropogenic activities, which is pronounced in the enrichment of aquatic soils with a number of metals and higher proportions of exchangeable forms from different types of sources.</p><p>This work was funded by the Russian Science Foundation, grant no. 20-14-00317.</p>


Author(s):  
B. Korzhenevsky ◽  
Gleb Tolkachev ◽  
Nikolay Kolomiycev

The problems of modern geological ecology associated with the study of pollution of sediments of water bodies by heavy metals are considered. The Volga River basin is quite heterogeneous, both in geomorphological and hydrological terms, and in thechnogenical development and usage. A fourrank taxonomy is presented for the selection of sites for monitoring, based on a combination of natural, landscape, climatic and thechnogenical factors. To the largest – the highest taxon – sites of the Ist category – bowls of reservoirs with the slopes and the urban zones, industrial and agricultural structures located within them are carried. Within these areas are allocated to smaller taxa, areas category IInd are the industrial and urban zones, areas category IIIrd are the small rivers without significant contamination and areas category IVth to conduct special observations. The examples of special observations in the study of the annual migration of heavy metals in the system «bottom sediments – water column» on the Ivankovo reservoir are highlighted. The investigations were carried out under the conditions of the standard flow rate for this reservoir and in the conditions of slow water exchange.


Author(s):  
V.B. Buber

Рассмотрены методы и приведены результаты построения прогнозной оценки стока реки Дон на период 2020-2030 гг. При построении прогноза использованы метод построения разностных интегральных кривых и статистический анализ стока за период с 1881 по 2018гг.Considered methods and given the results of making a forecast estimation of Don River basin flow for the 2020-2030 years period. The forecast is based on the difference integral curves constructing method and flow statistical analysis for the period from 1881 to 2018.


2013 ◽  
Vol 40 (6) ◽  
pp. 573-584 ◽  
Author(s):  
R. G. Dzhamalov ◽  
N. L. Frolova ◽  
M. B. Kireeva

2020 ◽  
Author(s):  
Pol Shutov

<p>The aim of the study is the spatial analysis of the structure of the river basin in identifying anthropogenic-transformed landscapes. The object of the study is the water catchment basin of the «Yayva» river, which is a left, mountain-taiga tributary of the «Kama» river and flows in the Perm region, in the Russian Federation. The river basin covers an area of km<sup>2 </sup> 6502, long main river, 304 km, the average slope of the basin 1,85<sup>0</sup>, height difference is significant and is 687 meters. the Catchment has a high degree of ruggedness of 0.91 km/km2. The sharp asymmetry of the catchment basin is expressed, so the left part of the basin is more pronounced.</p><p>With the use of remote sensing satellite images with high spatial resolution Landsat – 8 and Sentinel – 2, based on digital elevation model and GIS tools identify the types of land cover of the basin. In the ArcGis 10.4 software environment, morphometric indicators of the river basin at the level of small rivers are determined. The map of the basin territorial structure is developed on the basis of a vector relief model with a section height of 25 meters. The areas of morphological elements of river basins are unevenly distributed over the absolute height and slope of the terrain, causing spatial heterogeneity of landscape structures.</p><p>In the zones of the sources of watercourses, water-collecting funnels of a rounded shape are formed, the boundaries of which are clearly deciphered from space images. In the direction from the mouth to the source along the main river, the average absolute height of the terrain increases from 170 to 540 meters, the height differences also increase, while the area of the catchment funnels increases from 0.04 km<sup>2</sup> to 13.4 km<sup>2</sup>.</p><p>On well-drained slopes with average humidity, fern spruce-fir forests are represented, and on wet slopes and areas with temporary watercourses, sparse high-forest taiga and raw horsetail spruce forests are developed. Also, waterlogging is manifested in flat areas with poorly developed river network, where drainage is insufficient, so in the lower reaches of the basin, the wide valley of the river is swamped.</p><p>For each morphological element of the catchment area, a characteristic type of vegetation is determined. The most common wetland landscapes are confined to catchment funnels (37%), which is especially pronounced in mountainous conditions (upper reaches of the basin at an altitude of 500 meters or more); less wetlands (17%) occur in inland river valleys.</p><p>Transformed landscapes (cuttings and secondary forests) are confined to the upper parts of the slopes of the catchment surface (14%) and arcs of the watershed system (10%). The largest share of urbanized areas corresponds to inland river valleys (3%). Areal dynamics of anthropogenically transformed landscapes is determined. As a result of the analysis of the dynamics of vegetation cover, the growth of the area of cuttings, secondary forests and anthropogenic objects that form the basins of river systems was established.</p><p>The work was carried out with the financial support of The Russian Foundation for basic research No. 19-05-00363 A.</p>


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