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List of Dams and Reservoirs 1 List of Dams and Reservoirs
List of dams and reservoirs 1 List of dams and reservoirs The following is a list of reservoirs and dams, arranged by continent and country. Africa Cameroon • Edea Dam • Lagdo Dam • Song Loulou Dam Democratic Republic of Congo • Inga Dam Ethiopia Gaborone Dam in Botswana. • Gilgel Gibe I Dam • Gilgel Gibe III Dam • Kessem Dam • Tendaho Irrigation Dam • Tekeze Hydroelectric Dam Egypt • Aswan Dam and Lake Nasser • Aswan Low Dam Inga Dam in DR Congo. Ghana • Akosombo Dam - Lake Volta • Kpong Dam Kenya • Gitaru Reservoir • Kiambere Reservoir • Kindaruma Reservoir Aswan Dam in Egypt. • Masinga Reservoir • Nairobi Dam Lesotho • Katse Dam • Mohale Dam List of dams and reservoirs 2 Mauritius • Eau Bleue Reservoir • La Ferme Reservoir • La Nicolière Reservoir • Mare aux Vacoas • Mare Longue Reservoir • Midlands Dam • Piton du Milieu Reservoir Akosombo Dam in Ghana. • Tamarind Falls Reservoir • Valetta Reservoir Morocco • Aït Ouarda Dam • Allal al Fassi Dam • Al Massira Dam • Al Wahda Dam • Bin el Ouidane Dam • Daourat Dam • Hassan I Dam Katse Dam in Lesotho. • Hassan II Dam • Idriss I Dam • Imfout Dam • Mohamed V Dam • Tanafnit El Borj Dam • Youssef Ibn Tachfin Dam Mozambique • Cahora Bassa Dam • Massingir Dam Bin el Ouidane Dam in Morocco. Nigeria • Asejire Dam, Oyo State • Bakolori Dam, Sokoto State • Challawa Gorge Dam, Kano State • Cham Dam, Gombe State • Dadin Kowa Dam, Gombe State • Goronyo Dam, Sokoto State • Gusau Dam, Zamfara State • Ikere Gorge Dam, Oyo State Gariep Dam in South Africa. • Jibiya Dam, Katsina State • Jebba Dam, Kwara State • Kafin Zaki Dam, Bauchi State • Kainji Dam, Niger State • Kiri Dam, Adamawa State List of dams and reservoirs 3 • Obudu Dam, Cross River State • Oyan Dam, Ogun State • Shiroro Dam, Niger State • Swashi Dam, Niger State • Tiga Dam, Kano State • Zobe Dam, Katsina State Tanzania • Kidatu Kihansi Dam in Tanzania. -
Analysis of the Constructive Features of the Earth Dam
MATEC Web of Conferences 196, 02002 (2018) https://doi.org/10.1051/matecconf/201819602002 XXVII R-S-P Seminar 2018, Theoretical Foundation of Civil Engineering Analysis of the Constructive Features of the Earth Dam Mikhail Balzannikov1, 1Samara State University of Economics, 443090 Samara, 141 Sovetskoi Armii St, Russia Abstract. The article considers the earth dam of the run-of-river unit – Kuibyshev hydroelectric power station on the Volga river (Russia). The main parameters of the earth dam, peculiarities of its erection and operation are described. The article notes the importance of ensuring a high degree of reliability of water structures constructed near major cities. It is especially important to monitor the condition of retaining structures with long service life. The factors influencing the change of the initial design conditions of operation of the Kuibyshev run-of-river unit dam are discussed. The results of examination of the geometric parameters of the body of the dam, performed at different periods of its maintenance, are analyzed. Examination results revealed significant deviations of the elevation marks of the earth dam surface on the upstream side from the design values. Possible causes of the discrepancy between these parameters and the design solutions are considered. The conclusion is drawn that the most likely reason for these features of the dam design lies in the initial incompleteness of construction. The measures for carrying out repair work to improve the reliability of the earth dam are being recommended. 1 Introduction At present, ensuring reliable operation of retaining water structures is a very urgent requirement for both operating enterprises and design organizations [1, 2]. -
For Classification and Construction of Ships (Rccs)
RULES FOR CLASSIFICATION AND CONSTRUCTION OF SHIPS (RCCS) Part 0 CLASSIFICATION 4 RCCS. Part 0 “Classification” 1 GENERAL PROVISIONS 1.1 The present Part of the Rules for the materials for the ships except for small craft Classification and Construction of Inland and used for non-for-profit purposes. The re- Combined (River-Sea) Navigation Ships (here quirements of the present Rules are applicable and in all other Parts — Rules) defines the to passenger ships, tankers, pushboats, tug- basic terms and definitions applicable for all boats, ice breakers and industrial ships of Parts of the Rules, general procedure of ship‘s overall length less than 20 m. class adjudication and composing of class The requirements of the present Rules are formula, as well as contains information on not applicable to small craft, pleasure ships, the documents issued by Russian River Regis- sports sailing ships, military and border- ter (hereinafter — River Register) and on the security ships, ships with nuclear power units, areas and seasons of operation of the ships floating drill rigs and other floating facilities. with the River Register class. However, the River Register develops and 1.2 When performing its classification and issues corresponding regulations and other survey activities the River Register is governed standards being part of the Rules for particu- by the requirements of applicable interna- lar types of ships (small craft used for com- tional agreements of Russian Federation, mercial purposes, pleasure and sports sailing Regulations on Classification and Survey of ships, ekranoplans etc.) and other floating Ships, as well as the Rules specified in Clause facilities (pontoon bridges etc.). -
New Records of the Chinese Mitten Crab, Eriocheir Sinensis H. Milne Edwards, 1853, from the Volga River, Russia
Aquatic Invasions (2007) Volume 2, Issue 3: 169-173 Open Access doi: http://dx.doi.org/10.3391/ai.2007.2.3.3 © 2007 The Author(s). Journal compilation © 2007 REABIC Research Article New records of the Chinese mitten crab, Eriocheir sinensis H. Milne Edwards, 1853, from the Volga River, Russia Firdauz M. Shakirova1, Vadim E. Panov2* and Paul F. Clark3 1Federal State Scientific Institute “GosNIORKh”, Tatarstan Branch, Kazan, Tatarstan, Russia 2St.Petersburg State University, St. Petersburg, Russia 3Department of Zoology, The Natural History Museum, Cromwell Road, London SW7 5BD, England E-mail: [email protected] (FMS), [email protected](VEP), [email protected] (PFC) *Corresponding author Received: 10 July 2007 / Accepted: 7 September 2007 Abstract Single adult specimens of the Chinese mitten crab have been regularly found in the Volga River since the mid-1970s, most likely originating from the eastern Baltic Sea via the Volga-Baltic Canal. Three new records of Eriocheir sinensis H. Milne Edwards, 1853 are reported from the Kuibyshev Reservoir, Volga River, Russia, found in fishing nets in October 2002 and April-May 2007. The origins and possible vectors for the introduction of these crabs are discussed. Key words: Crustacea, Brachyura, Eriocheir sinensis, Volga River basin, migration, hull fouling Introduction the eastern Baltic Sea have increased, with the estuaries of north-western Europe (Ojaveer et al. The Chinese mitten crab Eriocheir sinensis H. 2007) serving as a breeding area for crabs found Milne Edwards, 1853 (Crustacea: Brachyura: in the brackish water of the Baltic Sea and its Varunidae) was introduced into Europe at the basin. -
Sediment Balance of the Volga Reservoirs
Sediment balance of the Volga reservoirs IM. A. Ziminova Abstract. The main input component of the Volga Reservoir sediment balance is the product of bank and bed abrasion (60—80 per cent of the total input). The second component is the river suspended sediment discharge (20-40 per cent}. Only 1 -S per cent of the total sediment input is derived from plankton and the higher aquatics. The main component of the output is sedimentation (60-98 per cent). Suspended sediment discharge from reservoirs varies from 2 to 40 per cent of the total output. Résumé. La plus grande partie des entrés dans le bilan de sédiments des réservoirs de la Volga se compose des produits d'affouillement des beiges et du lit, il en résulte 60-80 pour cent du total des entrées. La deuxième place est occupée par l'écoulement des matières en suspension transportées par les rivières (20-40 pour cent). Le poids qui résulte de la production du phy to plankton et des plantes aquatiques supérieures constitue 1-5 pour cent de la rentrée générale. La principale partie des sorties est la sédimentation (60-98 pour cent). Les transports solides en suspension sortant des réservoirs constituent de 2 à 40 pour cent du total des sorties. Sediment balances of reservoirs are being compiled to estimate the silting of reservoirs and to forecast the tendency of this process. These balances allow one to determine the value of and to reveal the causes of quantitive changes in the sediment discharge under the conditions of flow regulation, and to consider possible changes in the composition of sediments. -
European River Lamprey Lampetra Fluviatilis in the Upper Volga: Distribution and Biology
European River Lamprey Lampetra Fluviatilis in the Upper Volga: Distribution and Biology Aleksandr Zvezdin AN Severtsov Institute of Ecology and Evolution Aleksandr Kucheryavyy ( [email protected] ) AN Severtsov Institute of Ecology and Evolution https://orcid.org/0000-0003-2014-5736 Anzhelika Kolotei AN Severtsov Institute of Ecology and Evolution Natalia Polyakova AN Severtsov Institute of Ecology and Evolution Dmitrii Pavlov AN Severtsov Institute of Ecology and Evolution Research Keywords: Petromyzontidae, behavior, invasion, distribution, downstream migration, upstream migration Posted Date: February 12th, 2021 DOI: https://doi.org/10.21203/rs.3.rs-187893/v1 License: This work is licensed under a Creative Commons Attribution 4.0 International License. Read Full License Page 1/19 Abstract After the construction of the Volga Hydroelectric Station and other dams, migration routes of the Caspian lamprey were obstructed. The ecological niches vacated by this species attracted another lamprey of the genus Lampetra to the Upper Volga, which probably came from the Baltic Sea via the system of shipways developed in the 18 th and 19 th centuries. Based on collected samples and observations from sites in the Upper Volga basin, we provide diagnostic characters of adults, and information on spawning behavior. Silver coloration of Lampetra uviatilis was noted for the rst time and a new size-related subsample of “large” specimens was delimited, in addition to the previously described “dwarf”, “small” and “common” adult resident sizes categories. The three water systems: the Vyshnii Volochek, the Tikhvin and the Mariinskaya, are possible invasion pathways, based on the migration capabilities of the lampreys. Dispersal and colonization of the Caspian basin was likely a combination of upstream and downstreams migrations. -
Translation Series No
, ARCHIVES FISHERIES RESEARCH BOARD OF CANADA Transla^ion Series No. 363 RESULTS OF THREE YEARS OF OBSERVATIONS ON FISH BELOW THE LENIN,.HYDROELECTRIC STATION ON THE VOLQA By A.. T. Diûzhikov (Saratov Branch at the State Institute-for Lake and River Fisheries--GosNIORKh) Original title: Rezultaty t^ekhletnikh nabliûdeni^ za rybami v nizhnem befe volzhskoi GES im. V. I. Lenina. From: Voprosy Ikhtiologii, Vol. 1, No. 1(18), pp. 69-78,: 1961. Moscow. Preliminary translation by W. E. Ricker Distributed by the,.AFisherdes, Res:éaroh:,Board of Canada Biological Station, Nanaimo, B. C. 1961 .e* This is a preliminary translation prepared for the use of the Fisheries Research Board of Canada. It is not a definitive English version of the article, and it has not been checked or approved by the author. The Volga River below the ci^y of Kuibyshev was closed off by.the Volga Hydroelectric Station in the autumn of 1955. The Kui.byshev reservoir was filled in three stages: autumn 1955, spring 1956, and spring 1957. The right bank below the hydro- electric station is steep: the Zhigulev Mountains.come ri,ght down to the water. On the left side, for 12 km the river is held back by the dam of the navigation canal, which prevents the exit of the water from the main channel into the system of side channels. On the side of the river adjacent to the hydro- electric station there is an accelerated current speed especially at high water. In addition to its seasonal fluctua- tions, the level of the water below the dam is subject to sharp weekly changes, caused by the working plan of the hydroelectric $tation, In comparison with the former regime of the Volga, below the dam there has been some reduction in the height of high water, and some increase in the mean level, as well as slower warming of the water in spring and cooling off in autumn. -
Translation Series No.1248
7%1, cgivEs FISHERIES RESEARCH BOARD OF CANADA Translation Series No. 1248 Formation of ecological conditions in the shoals of reservoirs in spring. I I By G.L. Mel l nikova Original title: Formirovanie ekologicheskoi obstanovki na melkovod l yakh vodokhranilishch v vesennii From: Biologiya Vnutrennikh yod, Informatsionnyi , Byullete .Akadèmiya Nauk SSSR. (2): 18-21, 1968. • Translated by the Translation Bureau(GM) Foreign Languages Division Department of the Secretary of State of Canada Fisheries Research Board of Canada • Freshwatér Institute. Winnipeg, Man., . 1969 9 pages typescript SECRÉTARIA T D'ÉTAT DEPARTMENT OF THE SECRETARY OF STATE TRANSLATION BUREAU BUREAU DES TRADUCTIONS FOREIGN LANGUAGES DIVISION DIVISION DES LANGUES ÉTRANGÈRES CANADA DI VI S ION/RANC H CITY YOUR NO. DEPARTMENT VILLE VOTRE N ° MINISTRE DIVISION/DIRECTION • Freshwater InstitutelWinnipeg # Manitoba F.R.B. i • TRANSLATOR (INITIALS) DATE OUR NO. LANGUAGE f TRADUCTEUR (INITIALES) NOTRE N ° LANGUE i ' S u 1 April 16, 1969. Formirovanie ekologicheskoi_obstanovki ma melkovodlyakh vodokhranilisheh v vesennii period, published in.Biologiya vnutrennikh vod, Informatsionny ByUlletent, The Formation of Ecological Conditions on the Shoals of Reservoirs in_Spring by G.L. Melvnikov mom.grommmairoil Within the confines of large reservoirs an . 1 flatland rivers the shoals with depths of up to 2 metres often account for more than i of the area of the water body, and by our calculations this means 21% of the Rybinsk 1To obtain comparative data on the scale of large regions or an entire country it seems most sensible to us to adopt the.following constant criterion: "the interactio n between the waves and the bcttom within stable boundaries from the normal water level (XWL) to a depth of 2 metres". -
PP-77-2 PECULIARITIES of SHALLOWS in REGULATED RESERVOIRS Ga1ina L. Me1nikova January 1977
PP-77-2 PECULIARITIES OF SHALLOWS IN REGULATED RESERVOIRS Ga1ina L. Me1nikova January 1977 Professional Papers are not official publications of the International Institute for Applied Systems Analysis, but are reproduced and distributed by the Institute as an aid to staff members in furthering their professional activities. Views or opinions expressed herein are those of the author and should not be interpreted as representing the view of either the Institute or the National Member Organizations supporting the Institute. ABSTRACT This paper is concerned with the shallows of water reservoirs, which are located between the shore line and the deep water area. The intermediate loca tion of these shallows is the reason that their for mation, especially at large amplitude of water level oscillations, is a very complex process. At the same time the role of these shallows is subject to con siderable discussion in the relevant literature. Comprehensive investigations of water quality at present include not only the technological aspects of pollution control (waste treatment, water purifica tion, etc.), but also the relevant ecological problems which in turn are closely related to social problems and to the conditions of human life. This paper describes the role of reservoir shallows, taking into consideration the entire spec trum of the aqove mentioned aspects. Special stress is given to the filtering role of shallows; they act as natural filter~ protecting water in the reservoir against the nonpoint source pollutants of agricultural origin which are difficult to control. The degree to which the reservoir shallows can act as the "natural filters" depends on their structure, which in turn depends on the regime of water level oscillations in the reservoir. -
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Sergey P. Gorshkov1*, Laurent Touchart2, Olga I. Mochalova3, Andrey Yu. Ozerskiy4, Larissa S. Evseeva1 1 Faculty of Geography, Lomonosov Moscow State University * Corresponding author, e-mail: [email protected] 2 The University of Orleans 3 Environmental Initiatives Centre, Design Bureau, LLC 4 Krasnoyarsk Mining and Geological Company FROM PONDS TO MAN-MADE SEAS ENVIRONMENT IN RUSSIA 65 ABSTRACT. Russia has more than 2200 development, which was only natural reservoirs and large ponds. As time went by, under the existing totalitarian regime. The ponds lost their importance in some aspects Civil War of 1917–1922, confiscation of food of human life, while newly created man-made by the government, crop failures and famines seas impacted the nature and the people in in the early 1920s and 1930s, dekulakization two ways. The costs involved in designing, and collectivization, and industrialization constructing, and operating the artificial seas, aimed at developing the military industry especially on the plains, have been too high to took place amid the repressive crackdown consider them as an undisputed achievement and GULAG camps. Under the circumstances, of the Soviet scientists transforming the nature. the authorities had to make some highly This paper discusses the problem of ponds and questionable decisions relating to land man-made seas in Russia. ownership and the public. Josef Stalin and his henchmen took extremely tough social and KEY WORDS: mega projects, quantum leap, economic measures to make a quantum leap in overflowing, giant reservoir, large industrial the military and industrial development using complex, environmental damage, drift wood, coercion, punitive measures, and propaganda. abrasion, landslide processes, intensification Providing economy with electric power was of karst, disintegration of family relationships. -
Easychair Preprint Modern Approaches to Protecting Urban Areas from Flooding
EasyChair Preprint № 5470 Modern Approaches to Protecting Urban Areas from Flooding Mikhail Balzannikov and Andrey Mikhasek EasyChair preprints are intended for rapid dissemination of research results and are integrated with the rest of EasyChair. May 6, 2021 Modern Approaches to Protecting Urban Areas from Flooding M.I. Balzannikov1 and A.A. Mikhasek2 1 Samara State University of Economics, Samara, 141 Sovetskoi Armii Str. 443090, Russia 2Samara State Technical University, Academy of Architecture and Civil Engineering, Samara, 224, Molodogvardeyskaya Str. 443110, Russia Abstract. The article notes that natural-anthropogenic emergencies often arise with the co-occurrence of factors of both man-caused and natural origin of very rare recurrence. In order to avoid such situations, it is necessary to provide for special arrangements and technical measures. The authors analyzed the condi- tions for preventing flooding of the territory built up with residential multi-storey buildings and social infrastructure. The territory has low surface elevation marks and is surrounded by water bodies: the Volga and Samara Rivers, as well as the oxbow channel path. At the same time, practically along the entire border of the territory, there are infrastructure engineering facilities and lines (roads, dams) with surface elevations that are significantly higher than the existing elevations of the built-up area. The authors present the results of the survey of these facili- ties, on the basis of which recommendations for the reconstruction of their indi- vidual sections are developed. When justifying the minimum elevation of protec- tive lines, the parameters of a rise of water level in water bodies (at the times of discharge in the Samara River of rare recurrence) were taken into account. -
The Caspian-Volga-Baltic Invasion Corridor
E. Leppäkoski et al. (eds.), Invasive Aquatic Species of Europe, 399-411 © 2002 Kluwer Academic Publishers. Printed in the Netherlands THE CASPIAN-VOLGA-BALTIC INVASION CORRIDOR YURY V. SLYNKO1*, LIUDMILA G. KORNEVA1, IRINA K. RIVIER1, VLADIMIR G. PAPCHENKOV1, GRIGORY H. SCHERBINA1, MARINA I. ORLOVA2 & THOMAS W. THERRIAULT3 1Institute of Biology of Inland Waters, Russian Academy of Science, Borok, Russia 2Zoological Institute, Russian Academy of Science, St. Petersburg, Russia 3Great Lakes Institute for Environmental Research, University of Windsor, Windsor, Canada *Corresponding author [email protected] ABSTRACT The north-south transfer of species in the Volga River basin is not new, but the scale and nature of inva- sions changed along the Volga-Baltic corridor following transformation of the Volga River from a rive- rine environment to one of a series of cascading reservoirs. Southward penetration of northern species was facilitated by the formation of a cold-water hypolimnion in the Volga reservoirs. Following reservoir impoundment, 106 invasive species have been found in the Volga River basin, a process that occurred over two different time periods. The first period of invasions occurred between 1940 and 1970, and involved many northern species (77% of total species) moving downstream by passive dispersal. The second period of invasions is still on going and involves invasions by many Ponto-Caspian species (51% of total species) while new invasions by northern species has decreased substantially (7% of total spe- cies). The proportion of exotic species (i.e., invaders originating from basins not adjacent to the Volga basin) increased from 7% during the first period to 41% during the second period.