Relevant bibliographies by topics / Dnieper River

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Academic literature on the topic 'Dnieper River'

Author: Grafiati
Published: 4 June 2021
Last updated: 30 May 2022

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Journal articles on the topic "Dnieper River"

1

Semenchenko, V. P., T. P. Lipinskaya, and A. I. Makarenko. "SPREAD RATE OF ALIEN AMPHIPODS AND MYSIDS IN THE MAIN RIVERS OF BELARUS." Russian Journal of Biological Invasions 14, no. 2 (June 11, 2021): 85–92. http://dx.doi.org/10.35885/1996-1499-2021-14-2-85-92.

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The spread rates of alien species of Amphipoda and Mysida were calculated for the Dnieper, Pripyat and Neman rivers in the territory of Belarus. The maximal values of spread rate were obtained for Dikerogammarus villosus (in the Pripyat River - 37.8 km/year, in the Dnieper River - 17 km/year) and Dikerogammarus haemobaphes (in the Pripyat River - 53.6 km/year, in the Dnieper River - 17 km/year), while the minimal values of spread rate were calculated for mysids Paramysis lacustris (in the Dnieper River - 0.4 km/year) and Limnomysis benedeni (in the Dnieper River - 0.6 km/year), also for amphipods Chelicorophium robustum (in the Dnieper River - 0.5 km/year) and Echinogammarus trichiatus (in the Dnieper River - 1.3 km/year). The differences in the spread rates of species connected with the time of their first records at the monitoring points and the intensity of economic activities in the studied rivers.
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KHILCHEVSKYI, V. K., and V. V. GREBIN. "LARGE AND SMALL RESERVOIRS OF UKRAINE: REGIONAL AND BASIN DISTRIBUTION FEATURES." Hydrology, hydrochemistry and hydroecology, no. 2 (60) (2021): 6–17. http://dx.doi.org/10.17721/2306-5680.2021.2.1.

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The aim of the study was to establish the territorial patterns of the distribution of reservoirs in administrative regions and river basin districts, to identify the role of large, medium and small reservoirs in the balance of river flow regulation in Ukraine. In Ukraine, there are only 1054 reservoirs, among which there are six large reservoirs of the Dnieper cascade and the Dniester reservoir, and all the remaining 99.3% (1047 reservoirs) belong to the middle (M), small (S) and very small (VS) categories. For convenience, we call this group with the abbreviation MSVS-reservoirs. All reservoirs have a total volume of 55.13 km3. Thus, reservoirs regulate 32% of the total river flow of the country, amounting to 170.3 km3 per year. There are two main patterns of territorial distribution of reservoirs: large reservoirs are located on large rivers (Dnieper and Dniester) and are of national importance; MSVS-reservoirs – were created to provide water to industrial regions (for example, Donetsk, Kharkiv) and have regional or local significance. In terms of the volume of accumulated water, Ukraine is a country of large reservoirs. The six reservoirs of the Dnieper cascade contain 79% of the water, in the Dniester – 6%, in the MSVS-reservoirs – 15%. The volume of reservoirs in the Dnieper cascade is 43.71 km3, which is 82% of the average long-term runoff of the Dnieper (53.5 km3 per year). The operation of the Dniester reservoir (3.0 km3), which was created in the transboundary city of Dniester (Ukraine – Moldova), is carried out taking into account the water management interests of the two countries. MSVS-reservoirs are unevenly distributed over the territory of Ukraine. The largest number of them is concentrated in the arid central and southeastern regions of Ukraine, 45% of the total number of MSVS-reservoirs is located in the region of the river basin Dnieper. The largest total values of the total volume and area of MSVS-reservoirs is in the Odesa region due to the Danube lakes, which have been granted the status of reservoirs. In the use of territorial communities in Ukraine, there are 72% of the MSVS-reservoirs, 28% – leased. Among the regions of Ukraine, most of all are rented MSVS-reservoirs in the Transcarpathian region – 78%. In the Zaporizhye region, 56% of the MSVS-reservoirs are leased, in the Ternopil region – 54%. There are leases of MSVS-reservoirs in Ivano-Frankivsk and Lviv regions. Low values of the lease indicator were in the Autonomous Republic of Crimea (4%), in Kherson (7%), Vinnitsa (8%) and Volyn regions (10% each). Among the regions of river basins, there are more leased MSVS-reservoirs in the regions of the river basins. Southern Bug – 35%, Dnieper – 32%. The minimum rental rate was in the region of the Crimean river basin (4%). There is a lease of MSVS-reservoirs in the area of the river basin. Vistula.
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MILYUKIN, M. V., M. V. Gorban, and M. M. Skrynnyk. "Monitoring And Distribution Of Organochlorine Pesticides, Polychlorinated Biphenyls And Polycyclic Aromatic Hydrocarbons In Surface River Water And Suspended Particulate Matter." Methods and Objects of Chemical Analysis 14, no. 3 (2019): 117–29. http://dx.doi.org/10.17721/moca.2019.117-129.

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The monitoring results of organochlorine pesticides (OCPs), polychlorinated biphenyls (PCBs) and polycyclic aromatic hydrocarbons (PAHs) in Ukranian and world surface river waters were summarized. Total concentrations of OCPs, PCBs and PAHs in surface waters of Ukrainian rivers (Dnieper and Dniester) were 1.4–17.1; 2.8–57.2; 7.5–378.6 ng/dm3 , respectively. These pollution levels are medium on a global scale. Higher concentrations were recorded in the surface water of China, India and other Asian countries. Distribution of these organic ecotoxicants between water and suspended particulate matter (dispersionphase distribution) was analyzed and it was shown that in the majority of river waters ≥50% of them are associated with suspended particles. By the case of River Dnieper antibate correlations between watersoluble parts of individual OCPs, PCBs and PAHs and coefficient of their hydrophobicity were recorded. These correlations were presented graphically. In addition, relevant correlation coefficients and criterions of probability were calculated. The clearest correlation was established for PCBs.
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Sarnavskyi, S. P., and Grebin V.V. "RETROSPECTIVE ANALYSIS OF STUDIES OF THE RIVER NETWORK OF THE LEFT BANK OF THE MIDDLE DNIEPER (FROM THE FIRST MENTIONS TO DETAILED DESCRIPTIONS – IV CENTURY BC – THE END OF THE XVIII CENTURY)." Hydrology, hydrochemistry and hydroecology, no. 4 (62) (2021): 46–66. http://dx.doi.org/10.17721/2306-5680.2021.4.4.

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The article presents the history of research of the left tributaries of the Middle Dnieper. The periodization of research by chronological periods from the IV century is developed. B.C. until the end of the XVIII century. The periods and key stages of river research during the corresponding period are highlighted. The issues of description of the respective rivers in antiquity and the Middle Ages are covered, in particular the elements of the geographical position of their river systems, water regime, feeding conditions, economical use, elements of river valleys and the organic world of their basins. Chronicle data and original works of scientists and politicians of these time periods are processed. The issues of geographical position of the river network, number and names of rivers of the studied sub-basin of the Middle Dnieper according to the maps of the XVI-XVIII centuries are covered in detail. Cartographic works of cartographers from France, the Netherlands, Italy, and Muscovy have been studied. Particular attention is paid to the cartographic works of the French cartographer Guillaume Levasser de Beauplan, who began a new stage in the mapping of the main left tributaries of the Middle Dnieper and their smaller tributaries. For the first time, 137 rivers of the Left Bank of the Middle Dnieper were marked on his maps. He put forward the theory of the formation of the channels of the left tributaries of the Middle Dnieper. On the maps of 1680 – 1760, we notice the beginning of the stage of stagnation in the image of the hydrographic grid of the left tributaries of the Middle Dnieper. The information according to the descriptive data of the Left Bank of Ukraine of the end of the XVIII century is singled out. The first detailed descriptions of the rivers – Kyiv, Chernihiv, Kharkiv governorates and Little Russia Governorate in the period from 1775 to 1800 were developed. A complete catalog of rivers of the I, II, III and IV order of the Middle Dnieper sub-basin according to descriptive data within the river basins with indication of their length is given.
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Khilchevskyi, V. K. "THE HYDROECOLOGICAL STATUS OF SMALL HISTORICAL RIVERS LYBED AND POCHAYNA IN THE BASIN OF THE DNIEPER AND VOLGA AT THE BEGINNING OF THE XXI CENTURY." Hydrology, hydrochemistry and hydroecology, no. 4 (55) (2019): 74–88. http://dx.doi.org/10.17721/2306-5680.2019.4.6.

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A survey study of the general hydroecological status of the historical small rivers of the same name Lybed and Pochayna, known since the Middle Ages (10th-11th centuries) in the Dnieper basin in Ukraine and in the Volga basin in the Russian Federation (RF), has been carried out. These rivers, many centuries ago, were natural objects around which cities formed, and in our time they turned out to be “absorbed” by cities. The state of six small rivers was analyzed: Lybed and Pochayna – tributaries of the Dnieper, Kiev, Ukraine; Lybed and Pochayna – Klyazma tributaries (Volga basin), Vladimir, Russia; Lybed – a tributary of the Oka (Volga basin), Ryazan, Russia; Pochayna – a tributary of the Volga, Nizhny Novgorod, Russia. According to hydromorphological indicators of the state of the rivers (catchment area and water content), the studied ones relate to rivers of very small size and very low water content. A significant part of the channel of these rivers is enclosed in a reservoir (41-100%). The hydroecological condition of these rivers is unsatisfactory, water is prone to pollution. The Pochaina River – a tributary of the Dnieper in Kiev (Ukraine) and the Pochaina River – a tributary of the Volga in Nizhny Novgorod (RF) turned into lost natural heritage sites. Given the involvement in urban infrastructure, the morphometric parameters of the six rivers considered are the greatest prerequisites for being more or less revitalized in the river Lybed – the right tributary of the Dnieper in Kiev (Ukraine).
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Gudkov, D. I., and M. I. Kuzmenko. "The distribution of tritium in the Dnieper River." River Systems 10, no. 1-4 (September 18, 1996): 555–58. http://dx.doi.org/10.1127/lr/10/1996/555.

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7

Son, M. O., R. A. Novitsky, and V. G. Dyadichko. "Recent State and Mechanisms of Invasions of Exotic Decapods in Ukrainian Rivers." Vestnik Zoologii 47, no. 1 (February 1, 2013): 45–50. http://dx.doi.org/10.2478/vzoo-2013-0004.

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Abstract Lower reaches of largest Ukrainian rivers are zones of migrations for exotic euryhaline decapods. During 2000s new records of invasions of three euryhaline exotic decapods, Rhithropanopeus harrisii (Gould, 1841), Eriocheir sinensis Milne-Edwards, 1853 and Macrobrachium nipponense (De Haan, 1849), were made in the channels of Ukrainian rivers. Chinese mitten crab, E. sinensis, spread in the Danube Delta and reservoirs of the Dnieper River; Rh. harrisii - in the channels of the Danube, Dnieper, Southern Bug and small river Gruzskij Yelanchik in the Azov Sea Basin; M. nipponense that was introduced in the Kuchurgan Liman (cooler reservoir of the Moldavian Hydro-power Station) - in the Dniester Delta. The migration zone of the established population can cover significant part of river watershed; it is necessary to take this fact into account at an estimation of biological invasion risk. Main problem in the investigation of exotic decapods in Ukrainian waters is absence of specialized methods used in the standard ecological monitoring. Among euryhaline exotic decapods, only Rh. harrisii is sometimes sampled with the equipment used in the monitoring of macrozoobenthos. A few records of these species at the large extent of their supposed ways of migration are the result of gaps in the study of their distribution in Ukrainian inland waters. Realistic attitude toward this fact is very important for the estimation of invasions in the inland waters of this region.
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Khilchevskyi, V. K. "MODERN CHARACTERISTICS OF WATER BODIES IN UKRAINE: WATERCOURSES AND RESERVOIRS." Hydrology, hydrochemistry and hydroecology, no. 1 (59) (2021): 17–27. http://dx.doi.org/10.17721/2306-5680.2021.1.2.

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According to the assessment made in the article, the current data on the number of water bodies on the territory of Ukraine are: 63119 rivers; about 20 thousand lakes; 1054 reservoirs; 50793 ponds. There are rivers in Ukraine: large (> 50 thousand km2) – 8 rivers: Dnieper, Dniester, Danube, Desna, Pripyat, Southern Bug, Seversky Donets, Tisa; medium (2.0-50 thousand km2) – 82 rivers; small (<2.0 thousand km2) – 63,029 rivers (99.87%). There are lakes in Ukraine: very large (> 100 km2) – 1 lake: Yalpug; large (10-100 km2) – 21 lakes; medium (1-10 km2) – about 70; small (0.5-1.0 km2) and very small (<0.5 km2) - all other lakes (99.54%). There are reservoirs in Ukraine: very large (10-50 km3) – 2 reservoirs: Kremenchug and Kakhovskoe – on the river.Dnipro (0.2%); large (1.0-10 km3) – 5 reservoirs; Kievskoe,Kanevskoe, Kamenskoe, Dneprovskoe (on the Dnieper river), Dnestrovsky – on the Dniester (0.5%); medium (0.1-1.0 km3) – 11 reservoirs (1.0%); small (0.01-0.1 km3) – 88 reservoirs (8.4%); small (<0.01 km3) – 948 reservoirs (89.9%). There are ponds in Ukraine: very large (> 500 thousand m3) and large (200-500 thousand m3) – 13%; medium (50-200 thousand m3) – 29%; small (10-50 thousand m3) and very small (<10 thousand m3) - 58%. Of great importance was the approval by the Verkhovna Rada of Ukraine in 2016 of the hydrographic zoning of the territory of Ukraine with the allocation of 9 regions of river basins: the Dnieper, Dniester, Danube, Southern Bug, Don, Vistula, Crimean rivers Black Sea rivers, Azov rivers. Almost all rivers of Ukraine belong to the basin of the Black and Azov seas. In addition to the area of the river basin Vistula (Western Bug and San rivers) which belongs to the Baltic Sea basin and occupies only 2.5% of the country's territory. It is shown that since hydrographic studies in Ukraine were carried out more than 50 years ago, modern hydrographic surveys of the country’s territory with the creation of a modern water cadastre and the establishment of real morphometric parameters of water bodies (rivers, lakes, reservoirs, ponds) are necessary. The main organizations dealing with these issues are the State Agency for Water Resources of Ukraine and the Ukrainian Hydrometeorological Center of the State Service of Ukraine for Emergency Situations. It is also necessary to regulate a number of concepts that are used a priori, but do not have a definition, clear parameters (for example, a stream, a source, a digging pond, etc.). This is difficult to implement through the Water Code of Ukraine or state standards, but it can be easier to do through the officially approved methods in which these terms are used.
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Roshchyna, N. O., and B. O. Baranovski. "Hydrological and hydrobotanic typology of the lake of North-Steppe Dnieper region." Ecology and Noospherology 30, no. 2 (September 20, 2019): 125–31. http://dx.doi.org/10.15421/031921.

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This article is devoted to the typology of lakes of the North-Steppe Dnieper. In developing the typology of lakes, the parameters were taken into account: landscape location, hydro-chemical and hydro-biological characteristics and the degree of their anthropogenic transformation. The data presented are based on the processing of stationary and route research materials from 1998 to 2018 on the lakes of river valleys: Dnieper, Samara, and Orel. Hydrological indicators are analyzed according to the literature, cartographic and archival data of the Dneprodiprovodkhoz Institute and the Biology Research Institute of Oles Honchar Dnipropetrovsk National University. Floristic studies were carried out using general botanical methods of collection and herbarization, and in the study of typical aquatic flora - special hydro-botanical methods. Geo-botanical studies were carried out according to geo-botanical and special hydro-botanical methods. The article presents the hydrological and hydro-botanical features of the lakes of the valley of a large river (Dnieper) and medium rivers (Samara, Orel). Lakes are located exclusively in valley-terrace landscapes in the northern part of the steppe zone of Ukraine. Despite this, based on cartographic materials, we proposed zoning of the territory of the lakes of the North-Steppe Dnieper according to the criteria: their location in lake regions, in various landscapes and the degree of anthropogenic transformation. The following districts and subareas were identified: Dnieper Lake District (Dnieper floodplain lake subarea with slight flooding of the floodplain, Dnieper Lake subarea of floodplain terraces, Dievsky floodplain lake subarea); Samara Lake District (Lake Subarea of Samara Coniferous forest, Lake Subarea of Estuary part of Samara); Orel Lake District. Lakes are located in various physical and geographical conditions of the floodplain, arena and third saline terrace. The typology of the lakes of the North-Steppe Dnieper basin was developed on the basis of regionalization of the location of the lakes, distribution according to the ecological and topographic profile, hydrological, hydro-chemical regimes, degree and nature of overgrowing. 11 types of lakes are identified based on the above criteria. 6 types were identified for the valley of a large river: floodplain lakes (3 types) with a long-flow regime, lakes of the second (sandy) terrace (2 types) and highly mineralized lakes of the third (saline) terrace. 5 types were identified for the valleys of middle rivers: floodplain lakes (3 types) with an episodic short-burial regime, lakes of the second (sandy) terrace (low-mineralized) and excessively mineralized lakes of the third (saline) terrace.
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Vasilyuk, O. M. "ВПЛИВ РЕГУЛЯТОРУ РОСТУ НА ФЕРМЕНТИ АНТИОКСИДАНТНОГО ЗАХИСТУ ЗА УМОВ ДІІ АНТРОПОГЕННИХ ЕМІСІЙ." Biological Bulletin of Bogdan Chmelnitskiy Melitopol State Pedagogical University 6, no. 3 (November 4, 2016): 80–87. http://dx.doi.org/10.15421/201674.

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The paper presents analysis of general (GА, Px, ΔЕ, ml∙sec) and specific (SA, Px, ΔЕ, mg∙sec) of oxidoreductase enzyme activity (Peroxidase, Px, EC 1.11.1.7), which together with Catalase (Cat, EC 1.11.1.6) forms a double link antioxidant protection of cells in the organisms of different levels of organization (non-specific response to stress) in the conditions of increasing redox processes under the exogenous stress. These markers of changeable environmental factors were sampled in the leaves of Salix alba L., which grew along Mokra Sura River (anthropogenically polluted with high level of salinity, experiment) and Shpakova River (without anthropogenic impact, control). These rivers belong to the basin of the Dnieper River (Steppe Dnieper region) that has high industrial load. We used plant growth regulator "Kornevin" in order to accelerate the rooting and reduce the exogenous pressures on the plants. We detected nonspecific reaction towards peroxidase in anthropogenic pressure conditions and determined significant differences between experiment and control regards antioxidant protection depending on growth and development conditions.
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Dissertations / Theses on the topic "Dnieper River"

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Самойленко, Євген Анатолійович, Евгений Анатольевич Самойленко, and Yevhen Anatoliiovych Samoilenko. "The principle of freedom of international river navigation and problems of regime of navigational usage of international rivers, which flow through the territory of Ukrainian State." Thesis, Севастопольський інститут банківської справи УАБС НБУ, 2012. http://essuir.sumdu.edu.ua/handle/123456789/64216.

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The article is dedicated to analysis of the principle of freedom of international river navigation and problems of regime of navigational usage of international rivers, which flow through the territory of Ukrainian State.
Стаття присвячена характеристиці принципу свободи навігації на міжнародних ріках та проблемі режиму судноплавного використання міжнародних рік, що протікають по території України.
Статья посвящена анализу принципа свободы судоходства по международным рекам, а также проблемам становления режима навигационного использования тех из них, которые протекают по территории Украины.
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Waddell, Steve Robert. "Drive to the Dnieper: the Soviet 1943 summer campaign." 1985. http://hdl.handle.net/2097/27570.

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Books on the topic "Dnieper River"

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Gozhik, P. F. Geologicheskie uslovii͡a︡ stroitelʹstva Dneprovsko-Bugskogo gidrouzla. Kiev: Nauk. dumka, 1989.

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Cossacks of the brotherhood: The Zaporog Kosh of the Dniepr River. New York: P. Lang, 1990.

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Rothberg, Judith. Meet the rivers of historic Russia, then and now: The Volga and the Dnieper. New York: Vantage Press, 1993.

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John, Philipps. The Germans by the Black Sea between the Bug and Dniester rivers. Fargo, N.D: Germans from Russia Heritage Collection, North Dakota State University Libraries, 2000.

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Andronati, S. A. Managementul bazinului transfrontalier al fl. Nistru și Directiva-cadru a apelor a Uniunii Europene: Materialele conferinței internaționale, Chișinaŭ, 2-3 octombrie 2008 = Upravlenie basseĭnom transgranichnoĭ reki Dnestr i Vodnai︠a︡ ramochnai︠a︡ direktiva Evropeĭskogo Soi︠u︡za : materialy mezhdunarodnoĭ konferent︠s︡ii, Kishinev, 2-3 okti︠a︡bri︠a︡ 2008 g. = Transboundary Dniester River Basin management and the EU Water Framework Directive : proceedings of the international conference, Chișinaŭ, October 2-3, 2008. Chișinău: Eco-TIRAS, 2008.

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1936-, Robchuk Ivan, ed. Ukraïnsʹki hovory Rumuniï: Dii︠a︡lektni teksty. Edmonton: Kanadsʹkyĭ in-t ukraïnsʹkykh studiĭ, 2003.

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I︠A︡stremsʹka, Teti︠a︡na. Tradyt︠s︡iĭne hut︠s︡ulʹsʹke pastukhuvanni︠a︡. Lʹviv: Instytut Ukraïnoznavstva im. I. Kryp'i︠a︡kevycha, 2008.

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Instytut ukraïnoznavstva im. I. Kryp'i︠a︡kevycha. and Shevchenko Scientific Society (U.S.), eds. Naddnistri︠a︡nsʹkyĭ rehionalʹnyĭ slovnyk. Lʹviv: Instytut Ukraïnoznavstva im. I. Kryp'i︠a︡kevycha NAN Ukraïny, 2008.

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Agency, International Atomic Energy, ed. Radiological conditions in the Dnieper River basin: Assessment by an international expert team and recommendations for an action plan. Vienna: International Atomic Energy Agency, 2006.

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D, Romanenko V., Grodzinskiĭ Dmitriĭ Mikhaĭlovich, and Institut gidrobiologii (Akademii͡a︡ nauk Ukraïny), eds. Radioaktivnoe i khimicheskoe zagri͡a︡znenie Dnepra i ego vodokhranilishch posle avarii na Chernobylʹskoĭ AĖS. Kiev: Nauk. dumka, 1992.

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Book chapters on the topic "Dnieper River"

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Dolin, V., O. Shevchenko, and J. Brittain. "Artificial Radionuclides Speciation in River Water of Dnieper Basin." In Role of Interfaces in Environmental Protection, 135–44. Dordrecht: Springer Netherlands, 2003. http://dx.doi.org/10.1007/978-94-010-0183-0_9.

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Goncharuk, V. V., and M. V. Milyukin. "Evaluation of Contamination Level of Dnieper River Basin by Organic and Inorganic Toxicants." In Bioavailability of Organic Xenobiotics in the Environment, 35–56. Dordrecht: Springer Netherlands, 1999. http://dx.doi.org/10.1007/978-94-015-9235-2_2.

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Poletto, D., and K. Babcock. "The Dnieper River Basin Challenge: Local and International Response to an Environmental and Human Health Crisis." In Role of GIS in Lifting the Cloud Off Chernobyl, 13–23. Dordrecht: Springer Netherlands, 2002. http://dx.doi.org/10.1007/978-94-010-0518-0_2.

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Kovalskyy, Valeriy, and Geoffrey Henebry. "Recent Trends in Land Surface Phenologies Within the Don and Dnieper River Basins from the Perspective of MODIS Collection 4 Products." In Regional Aspects of Climate-Terrestrial-Hydrologic Interactions in Non-boreal Eastern Europe, 183–89. Dordrecht: Springer Netherlands, 2009. http://dx.doi.org/10.1007/978-90-481-2283-7_20.

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Milyukin, M. V. "Determination of Isomeric-Specific Composition of Polychlorinated Biphenyls in Natural and Drinking Waters of Dnieper River Basin in Kiev Region Using Gas Chromatography and Mass-Spectrometry." In Role of Interfaces in Environmental Protection, 103–20. Dordrecht: Springer Netherlands, 2003. http://dx.doi.org/10.1007/978-94-010-0183-0_6.

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Shulyarenko, A., M. Yatsyuk, and L. Shulyarenko. "Causes and Peculiarities of Recent Floods on the Dniester River." In Flood Issues in Contemporary Water Management, 95–100. Dordrecht: Springer Netherlands, 2000. http://dx.doi.org/10.1007/978-94-011-4140-6_10.

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Jeleapov, Ana, Orest Melniciuc, and Iurie Bejan. "Assessment of Flood Risk Areas in the Dniester River Basin (in the Limits of the Republic of Moldova)." In Water Science and Technology Library, 157–73. Cham: Springer International Publishing, 2014. http://dx.doi.org/10.1007/978-3-319-02708-1_8.

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Markova, Anastasia K. "A New Early Middle Pleistocene Locality of Small Mammals (Lower Dniester River) and its Position in the Early Middle Pleistocene Sequence." In Springer Geology, 1017–18. Cham: Springer International Publishing, 2014. http://dx.doi.org/10.1007/978-3-319-04364-7_193.

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"In the garden of Gethsemane on the Dnieper river." In Words for War, edited by Oksana Maksymchuk and Max Rosochinsky, 56. Boston, USA: Academic Studies Press, 2019. http://dx.doi.org/10.1515/9781618116673-028.

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"In the garden of Gethsemane on the Dnieper river." In Words for War, translated by Oksana Maksymchuk and Max Rosochinsky, 56. Academic Studies Press, 2017. http://dx.doi.org/10.2307/j.ctv1zjg8p9.30.

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Conference papers on the topic "Dnieper River"

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Voronenko, Oleg. "Mesolithic settlement in the lower reaches of the Berezina River (Dnieper)." In SUBSISTENCE STRATEGIES IN THE STONE AGE, DIRECT AND INDIRECT EVIDENCE OF FISHING AND GATHERING. Institute for the History of Material Culture Russian Academy of Science, 2018. http://dx.doi.org/10.31600/978-5-907053-00-7-2018-58-59.

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Slepchuk, Kira, Kira Slepchuk, Tatyana Khmara, Tatyana Khmara, Ekaterina Mankovskaya, and Ekaterina Mankovskaya. "EXTREME DETERIORATION OF WATER QUALITY AND FISH SUFFOCATION PHENOMENA IN THE MARINE ESTUARY." In Managing risks to coastal regions and communities in a changing world. Academus Publishing, 2017. http://dx.doi.org/10.21610/conferencearticle_58b4315dd0f08.

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The factors that provoke fish suffocation in an estuary, namely: natural (small river runoff, high air and water temperature, water stratification) and anthropogenic (regulation of river, etc.) were marked. Taking into account these factors the calculations were carried out and the possible areas of the Dnieper-Bug estuary, where fish kill of different scale and genesis is found out were identified.
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Slepchuk, Kira, Kira Slepchuk, Tatyana Khmara, Tatyana Khmara, Ekaterina Mankovskaya, and Ekaterina Mankovskaya. "EXTREME DETERIORATION OF WATER QUALITY AND FISH SUFFOCATION PHENOMENA IN THE MARINE ESTUARY." In Managing risks to coastal regions and communities in a changing world. Academus Publishing, 2017. http://dx.doi.org/10.31519/conferencearticle_5b1b93c33e64c4.27067986.

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The factors that provoke fish suffocation in an estuary, namely: natural (small river runoff, high air and water temperature, water stratification) and anthropogenic (regulation of river, etc.) were marked. Taking into account these factors the calculations were carried out and the possible areas of the Dnieper-Bug estuary, where fish kill of different scale and genesis is found out were identified.
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Shakhman, I. "ASSESSMENT OF ECOLOGICAL STATE AND ECOLOGICAL RELIABILITY OF THE LOWER SECTION OF THE DNIEPER RIVER." In 18th International Multidisciplinary Scientific GeoConference SGEM2018. Stef92 Technology, 2018. http://dx.doi.org/10.5593/sgem2018/5.2/s20.015.

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Korneev, V., and I. Bulak. "HYDROPOWER POTENTIAL OF MEDIUM AND SMALL RIVERS OF BELARUS ON THE EXAMPLE OF RIVER BASINS OF WESTERN DVINA, DNIEPER, PRIPYAT." In SAKHAROV READINGS 2020:ENVIRONMENTAL PROBLEMS OF THE XXI CENTURY. Minsk, ICC of Minfin, 2020. http://dx.doi.org/10.46646/sakh-2020-2-3385-388.

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Korneev, V., and I. Bulak. "HYDROPOWER POTENTIAL OF MEDIUM AND SMALL RIVERS OF BELARUS ON THE EXAMPLE OF RIVER BASINS OF WESTERN DVINA, DNIEPER, PRIPYAT." In SAKHAROV READINGS 2020:ENVIRONMENTAL PROBLEMS OF THE XXI CENTURY. Minsk, ICC of Minfin, 2020. http://dx.doi.org/10.46646/sakh-2020-2-385-388.

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Loktyev, Valentyn, Sanzhar Zharkeshov, Oleg Gotsynets, Oleksandr Davydenko, Mikhailo Machuzhak, Kuzmenko Pavlo, Vitalii Repryntsev, and Oksana Kabatova. "Modern Analogues of Sedimentation of Lower Permian Reservoirs in the Dnieper-Donets Depression." In SPE Eastern Europe Subsurface Conference. SPE, 2021. http://dx.doi.org/10.2118/208505-ms.

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Abstract The paper considers the problematics of identifying proper analogues for understanding carbonate and clastic reservoir distribution and prediction in the Lower Permian and Upper and Lower Carboniferous within the Dnieper-Donets basin. The focus of the exploration team was finding meandering rivers. This choice was proven good in mapping reservoirs and finding traps deeper in the Upper and Middle Carboniferous, although for Permian clastic section the approach was not helpful. The second option was desert dunes, but poor sorting of reservoirs suggests a more complex picture. Analogues such as desert environment is quite logical for describing Lower Permian as aridic climate, with red and brown shales and sands. Lower Permian reservoirs have a moon-like shape in the vertical sections that could be easily mistaken for river channels, but in such a dry climate, it is very likely water flow channels with sporadic hurricane-related activities. Core and logs shows chaotic grain sizes, but more with fine grains with almost no coarse grains. The source of sedimentary material could be mountains of Ukrainian Rock Shield from the South and Voronezh massif from the North. This conceptual model is proposing not to look for meandering channels, but more for braided channels with poorly sorted material. The current time analogue could be the Oman desert between the mountains and peninsula. From satellite images, braided channels are clearly visible in the direction towards the Indian Ocean. The channels’ internal structure is quite heterogeneous. This method suggests exploration targets with possible widths of the channels as big as hundreds of meters and their lengths under 10 and between 10-20 kilometres maximum.
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Bricheva, Svetlana, and Kirill Efremov. "Combining ground penetrating radar and electrical resistivity tomography for the study of history of relief development in Dnieper River valley." In 2018 17th International Conference on Ground Penetrating Radar (GPR). IEEE, 2018. http://dx.doi.org/10.1109/icgpr.2018.8441545.

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Khabanets, Ivan, Benjamin Medvedev, Carlo D'Aguanno, Diego Scapin, and Marco Mantova. "The Importance of Seismic Attributes in Complex Area, Case Study from Vodianivske Field, Dnieper-Donets Basin, Ukraine." In SPE Eastern Europe Subsurface Conference. SPE, 2021. http://dx.doi.org/10.2118/208506-ms.

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Abstract The Dnieper-Donets Basin (DDB) is the principal producer of hydrocarbons in Ukraine and reserves are found in lower Permian and in Visean-Serpukhovian from Lower Carboniferous. The Vodianivske field is located halfway between Poltava and Kharkiv in east Ukraine with proven reserves at depth of 5-6km. Previous studies based on legacy seismic data show thickness changes of the upper Visean towards the main structure and dim small-scale structures on the block boundary. A recent 3D data reprocessing using 5D interpolation and advanced prestack time migration provides a broad frequency content image and imparts detailed high-resolution geological events. While traditional exploration is focused on gas traps in the Visean and below, current study aims to scan for potential traps in the Serpukhovian and above. In order to reveal thin section features, multiple seismic attributes were tested, and spectral decomposition was found to be a powerful tool that delineated thin sand bodies in river valleys and allowed interpretation of high-resolution small-scale faults and pinch-outs not seen before. Frequency tuning analysis on mapped horizons associated with upper Serpukhovian supported the presence of a large deltaic structure revealing SE-NW thin ∼1km wide sand body and developed set of crossing meanders. Similar approach was applied on legacy data expanding to the east and while seismic quality was limited, it was possible to identify a narrow ∼25km length meander and highlight a fault set. Upon seismic attribute study we were able to identify and map thin units associated with sands that can be considered as future targets in hydrocarbon exploration in the area.
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Voitsekhovich, O., T. Lavrora, A. S. Skalskiy, and V. F. Ryazantsev. "The Strategy on Rehabilitation of the Former Uranium Facilities at the “Pridneprovsky Chemical Plant” in Ukraine." In The 11th International Conference on Environmental Remediation and Radioactive Waste Management. ASMEDC, 2007. http://dx.doi.org/10.1115/icem2007-7196.

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This paper describes current status of the former Uranium Facilities at the Pridneprovsky Chemical Plant in Ukraine, which are currently under development of action plan for its territory rehabilitation. The monitoring data carried out during recent several years show its impact to the Environment and gives a basis for justification of the number of measures aiming to reduce radiological and ecological risks of the Uranium tailings situated at the territory of PChP. The monitoring data and strategy for its remediation are considered in the presentation. Uranium mining has been intensively conducted in Ukraine since the end of the 40-s. Most of the uranium deposits have been explored in the Dnieper river basin, shown in Figure 1, while some smaller deposits can be found within the basins of the Southern Bug and Severskiy Donets rivers. There also several large Uranium Milling facilities were in operation since the end of the 40-s till 1991, when due to disintegration of the former Soviet Union system the own uranium production has been significantly declined. The Milling Plant and Uranium extraction Facilities in ZhevtiVody is still in operation with UkrAtomprom Industrial Consortium. Therefore rehabilitation programme for all Uranium facilities in this site are in duty of the East Mining Combine and the Consortium. The most difficult case is to provide rehabilitation Action Plan for Uranium tailings and number of other facilities situated in Dnieprodzerzhinsk town and which were in operation by the former State Industrial Enterprise Pridneprovskiy Chemical Plant (PChP).
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Reports on the topic "Dnieper River"

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Novichkova, Tatiana. The Dnieper. Basin of the river. Edited by Nikolay Komedchikov. Entsiklopediya, January 2012. http://dx.doi.org/10.15356/dm2015-12-28-1.

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Voitsekhovitch, O. V., M. J. Zheleznyak, and Y. Onishi. Chernobyl nuclear accident hydrologic analysis and emergency evaluation of radionuclide distributions in the Dnieper River, Ukraine, during the 1993 summer flood. Office of Scientific and Technical Information (OSTI), June 1994. http://dx.doi.org/10.2172/10168428.

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Alokhina, Tetiana, and Vadym Gudzenko. Distribution of radionuclides in modern sediments of the rivers flowing into the Dnieper-Bug Estuary. EDP Sciences, 2021. http://dx.doi.org/10.31812/123456789/4617.

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The article presents the results of large-scale studies of the content and distribution of natural and man-made radionuclides in the sediments of the rivers flowing into the Dnieper-Bug estuary. The article also presents the results of the granulometric analysis of the surveyed water bodies. The data about natural radioactive elements in the sediments rivers flowing into the Dnieper-Bug estuary obtained in this research are demonstrated moderate specific activity, which, however, clearly correlates with the granulometric composition of sediments. The 137Cs determined by us is contained in the sediments of all studied water bodies and the places of it greatest concentration coincide with the areas in which the sediment is represented mainly by the pelitic fraction. The data obtained in this research can serve as a baseline data in natural radionuclides concentration in sediments rivers flowing into the Dnieper-Bug estuary. The obtained data can also be used for further monitoring of the specific activity of man-made radionuclides, in particular 137Cs.
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