THE ASSIMILATIVE CAPACITY OF THE MARGINAL FILTER OF THE VOLGA RIVER IN RELATION TO ORGANOCHLORINE PESTICIDES

Author(s):  
Tatarnikov Vitaly ◽  
◽  
Dairova Dinara ◽  
Ocheretny Maxim ◽  
◽  
...  
2006 ◽  
Vol 406 (1) ◽  
pp. 97-102 ◽  
Author(s):  
I. A. Nemirovskaya ◽  
V. F. Brekhovskikh

Oceanology ◽  
2019 ◽  
Vol 59 (3) ◽  
pp. 381-391
Author(s):  
V. N. Lukashin ◽  
M. D. Kravchishina ◽  
A. A. Klyuvitkin ◽  
A. N. Novigatsky ◽  
N. V. Politova

2021 ◽  
Vol 82 (3) ◽  
pp. 49-55
Author(s):  
SVETASHEVA DIANA R. ◽  
◽  
TATARNIKOV VITALY O. ◽  
OCHERETNY MAXIM A. ◽  
◽  
...  

According to the data of long-term observations, the assessment of the degree of impact of copper and zinc on the ecosystem of the shallow part of the estuarine coast of the Volga River was carried out. There are the ideas of the marginal filter and the assimilation capacity were used in the article. The calculation of the assimilation capacity for a marginal filter significantly based on the dimensional characteristics, such as the estuarine region of the Volga River, was carried out at several points located within the estuarine seashore. In this work the century-old sections of the state observation network were used. It can be seen from the calculated data that the value of the assimilation capacity is subject to significant intra-and inter-annual fluctuations. The main parameter determining the volume of the assimilation capacity of copper and zinc is fairly called the flow of the Volga River. According to the results of the study, it can be argued that the observed level of copper and zinc runoff into the Caspian Sea is completely assimilated in the shallow part of the seashore.


2019 ◽  
Vol 59 (3) ◽  
pp. 421-432
Author(s):  
V. N. Lukashin ◽  
M. D. Kravchishina ◽  
A. A. Klyuvitkin ◽  
A. N. Novigatsky ◽  
N. V. Politova

The first data on the long-term study of marginal filter (MF) of the Volga River is presented. The concentrations of suspended particulate matter, suspendforming chemical elements and microelements are considered. Ratios of enrichment suspension by chemical elements relative to the upper lithosphere are calculated. as well as their interrelations at different stages of the MF. It is shown that the sedimentary substance supplied by the sea with river flow, changes radically, both quantitatively and qualitatively.


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.


Human Ecology ◽  
2016 ◽  
pp. 3-8
Author(s):  
S. A. Ivanov ◽  
O. F. Dmitrieva ◽  
N. I. Kulmakova ◽  
Yu. O. Dimitriev

Author(s):  
Yelena I. Polyakova ◽  
Yekaterina I. Novichkova ◽  
Tatiana S. Klyuvitkina ◽  
Elizaveta A. Agafonova ◽  
Irina M. Kryukova

Presented the results of long-term studies of diatoms and aquatic palynomorphs in surface sediments of the Arctic seas and the possibility of their use for the reconstructions of paleocirculation water masses, advection of Atlantic and Bering sea water into the Arctic ocean, changes in the river runoff to the seas, sedimentary processes in the marginal filter of the largest rivers, seasonal sea ice cover and other hydrological parameters.


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