Geography of the Ob-Irtysh River Basin and River Shipping
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Ob' River Discharge from TOPEX/Poseidon Satellite Altimetry
Ob’ river discharge from TOPEX/Poseidon satellite altimetry (1992–2002) A. Kouraev, E. A. Zakharova, O. Samain, N. Mognard-Campbell, A. Cazenave To cite this version: A. Kouraev, E. A. Zakharova, O. Samain, N. Mognard-Campbell, A. Cazenave. Ob’ river discharge from TOPEX/Poseidon satellite altimetry (1992–2002). Remote Sensing of Environment, Elsevier, 2004, 93 (1-2), pp.238-245. 10.1016/j.rse.2004.07.007. hal-00280276 HAL Id: hal-00280276 https://hal.archives-ouvertes.fr/hal-00280276 Submitted on 6 Apr 2020 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. Distributed under a Creative Commons Attribution| 4.0 International License Ob’ river discharge from TOPEX/Poseidon satellite altimetry (1992–2002) Alexei V. Kouraeva,b,*, Elena A. Zakharovab, Olivier Samainc, Nelly M. Mognarda, Anny Cazenavea aLaboratoire d’Etudes en Ge´ophysique et Oce´anographie Spatiales (LEGOS), Toulouse, France bState Oceanography Institute, St. Petersburg Branch, St. Petersburg, Russia cMe´te´o-France, CNRM, Toulouse, France The paper discusses an application of the TOPEX/Poseidon (T/P) altimetry data to estimate the discharge of one of the largest Arctic rivers—the Ob’ river. We first discuss the methodology to select and retrieve the altimeter water levels during the various phases of the hydrological regime. -
Economic and Social Council
UNITED E NATIONS Economic and Social Distr. Council GENERAL ECE/TRANS/SC.2/2006/2/Add.1 13 October 2006 ENGLISH Original: RUSSIAN ENGLISH AND RUSSIAN ONLY ECONOMIC COMMISSION FOR EUROPE INLAND TRANSPORT COMMITTEE Working Party on Rail Transport Sixtieth session Geneva, 15-17 November 2006 Agenda item 3 (b) Euro-Asian transport corridors* Transmitted by the Committee of the Organization for Cooperation between Railways (OSJD) 1. The programme of work of the Organization for Cooperation between Railways (OSJD) for 2005-2010 calls for the development within the Organization of comprehensive plans for the improvement of transport and the development of OSJD transport corridors (hereinafter, Comprehensive Plan). The Comprehensive Plans for OSJD Corridors Nos. 1, 9 and 11 were completed in 2006 and endorsed by the thirty-fourth session of the OSJD Ministerial Meeting, held in Sofia in June 2006. 2. Of the three corridors, Corridor No. 1 has the greatest capacity and is the best equipped. Its overall length, including branch lines, is 24,800 kilometres. The most important branch lines are in Kazakhstan, China and Mongolia. * The ECE Transport Division has submitted the present document after the official document deadline due to resource constraints. GE.06-25845 (E) 141106 151106 ECE/TRANS/SC.2/2006/2/Add.1 page 2 3. Corridor No. 1 passes through 11 countries, namely Poland, Latvia, Lithuania, Estonia, Belarus, the Russian Federation, Kazakhstan, Uzbekistan, China, Mongolia and the Democratic People’s Republic of Korea. 4. The main route of the corridor is: Kunowice-Warszawa-Brest-Minsk-Moskva- Nizhny Novgorod-Sverdlovsk (Ekaterinburg)-Omsk-Novosibirsk-Krasnoyarsk-Irkutsk - Nakhodka/Vanino/Khasan. -
Selected Works of Chokan Valikhanov Selected Works of Chokan Valikhanov
SELECTED WORKS OF CHOKAN VALIKHANOV CHOKAN OF WORKS SELECTED SELECTED WORKS OF CHOKAN VALIKHANOV Pioneering Ethnographer and Historian of the Great Steppe When Chokan Valikhanov died of tuberculosis in 1865, aged only 29, the Russian academician Nikolai Veselovsky described his short life as ‘a meteor flashing across the field of oriental studies’. Set against his remarkable output of official reports, articles and research into the history, culture and ethnology of Central Asia, and more important, his Kazakh people, it remains an entirely appropriate accolade. Born in 1835 into a wealthy and powerful Kazakh clan, he was one of the first ‘people of the steppe’ to receive a Russian education and military training. Soon after graduating from Siberian Cadet Corps at Omsk, he was taking part in reconnaissance missions deep into regions of Central Asia that had seldom been visited by outsiders. His famous mission to Kashgar in Chinese Turkestan, which began in June 1858 and lasted for more than a year, saw him in disguise as a Tashkent mer- chant, risking his life to gather vital information not just on current events, but also on the ethnic make-up, geography, flora and fauna of this unknown region. Journeys to Kuldzha, to Issyk-Kol and to other remote and unmapped places quickly established his reputation, even though he al- ways remained inorodets – an outsider to the Russian establishment. Nonetheless, he was elected to membership of the Imperial Russian Geographical Society and spent time in St Petersburg, where he was given a private audience by the Tsar. Wherever he went he made his mark, striking up strong and lasting friendships with the likes of the great Russian explorer and geographer Pyotr Petrovich Semyonov-Tian-Shansky and the writer Fyodor Dostoyevsky. -
The Security of the Caspian Sea Region
4. The Caspian Sea: threats to its biological resources and environmental security Igor Zonn I. Introduction The Caspian Sea is the world’s largest inland sea. Physiographically it is unique. It is the most productive body of water in the world1 and the only one that preserves the geno-fund of the sturgeon, the source of almost all the black caviar produced. About 10 million people live around the Caspian Sea and the occupations of many of them are connected with the sea, and first of all with fishing. By virtue of its oil and gas potential the Caspian has a place among the major world centres of hydrocarbon production. The rivers of the largest water catchment area in the world discharge into it from the industrial and production regions of the littoral states. This fact accounts for the periodic fluctuations of the sea level and for the nature and scale of pollution of the sea. As for the water body itself, there has always been a conflict between the use of its principal natural resources—biological resources (fishing of valuable fish species, first and foremost the sturgeon)—and the exploitation of hydrocarbons (the development of shelf and offshore oil and gas fields). This conflict has become especially acute since the breakup of the Soviet Union, as a result of which the legal status of the Caspian Sea changed, regulation of the exploitation of the sea’s resources has broken down, and the geopolitical interests of five different states conflict. These interests are those connected with military and political security, with shipping, with the exploitation of biological and mineral resources, and with environmental security. -
THE NATURAL RADIOACTIVITY of the BIOSPHERE (Prirodnaya Radioaktivnost' Iosfery)
XA04N2887 INIS-XA-N--259 L.A. Pertsov TRANSLATED FROM RUSSIAN Published for the U.S. Atomic Energy Commission and the National Science Foundation, Washington, D.C. by the Israel Program for Scientific Translations L. A. PERTSOV THE NATURAL RADIOACTIVITY OF THE BIOSPHERE (Prirodnaya Radioaktivnost' iosfery) Atomizdat NMoskva 1964 Translated from Russian Israel Program for Scientific Translations Jerusalem 1967 18 02 AEC-tr- 6714 Published Pursuant to an Agreement with THE U. S. ATOMIC ENERGY COMMISSION and THE NATIONAL SCIENCE FOUNDATION, WASHINGTON, D. C. Copyright (D 1967 Israel Program for scientific Translations Ltd. IPST Cat. No. 1802 Translated and Edited by IPST Staff Printed in Jerusalem by S. Monison Available from the U.S. DEPARTMENT OF COMMERCE Clearinghouse for Federal Scientific and Technical Information Springfield, Va. 22151 VI/ Table of Contents Introduction .1..................... Bibliography ...................................... 5 Chapter 1. GENESIS OF THE NATURAL RADIOACTIVITY OF THE BIOSPHERE ......................... 6 § Some historical problems...................... 6 § 2. Formation of natural radioactive isotopes of the earth ..... 7 §3. Radioactive isotope creation by cosmic radiation. ....... 11 §4. Distribution of radioactive isotopes in the earth ........ 12 § 5. The spread of radioactive isotopes over the earth's surface. ................................. 16 § 6. The cycle of natural radioactive isotopes in the biosphere. ................................ 18 Bibliography ................ .................. 22 Chapter 2. PHYSICAL AND BIOCHEMICAL PROPERTIES OF NATURAL RADIOACTIVE ISOTOPES. ........... 24 § 1. The contribution of individual radioactive isotopes to the total radioactivity of the biosphere. ............... 24 § 2. Properties of radioactive isotopes not belonging to radio- active families . ............ I............ 27 § 3. Properties of radioactive isotopes of the radioactive families. ................................ 38 § 4. Properties of radioactive isotopes of rare-earth elements . -
Dr. Nikitin A.I., Dr. Kryshev I.I
1 Research & Production Association “Typhoon” of Roshydromet, Obninsk, Russia Results of Radioecological Monitoring of the Irtysh-Ob’ River System and Opportunity of Use in Monitoring and Radioecological Assessment of Marine/Freshwater Systems Contaminated in Japan after NPP Fukushima Accident ISTC Projects 2558 and 3547 Dr. Nikitin A.I., Dr. Kryshev I.I. Tokyo, 3-4 February 2012 Ob-Irtysh river system: 2 Location of nuclear industry facilities Mayak Production Association Siberian Chemical Combine 3 Main topic of presentation Radioecological monitoring and development of a database on radioactive contamination of: • Techa-Iset-Tobol-Irtysh-Ob rivers, in the areas influenced by discharges from the Mayak Production Association (project 2558) • Tom and Ob rivers, in the areas influenced by discharges from the Siberian Chemical Combine (SCC) (project 3547) 4 Methodological approach for field studies: combining boat radioecological surveys of the whole river system with regular water sampling in one of the critical regions throughout the hydrological cycle, with measurement of man-made radionuclides (137Cs, 90Sr , Pu isotopes and tritium) ISTC project 2558 r e v i r h s Main region for round-the-year y t r P o i n t N o . 3 I monitoring: I r t y s h r i v e r , 6 k m T o b o l s k d o w n s t r e a m f r o m c o n f l u e n c e Confluence of the “contaminated” river w i t h T o b o l r i v e r P o i n t N o . -
Genetic Effects of Sable (Martes Zibellina L.) Reintroduction in Western Siberia
See discussions, stats, and author profiles for this publication at: https://www.researchgate.net/publication/323725844 Genetic Effects of Sable (Martes zibellina L.) Reintroduction in Western Siberia Article in Russian Journal of Genetics · March 2018 DOI: 10.1134/S1022795418030079 CITATIONS READS 5 73 3 authors: Vladimir G. Monakhov Makar Modorov Russian Academy of Sciences Russian Academy of Sciences 178 PUBLICATIONS 435 CITATIONS 32 PUBLICATIONS 87 CITATIONS SEE PROFILE SEE PROFILE Maryana Ranyuk Russian Academy of Sciences 30 PUBLICATIONS 70 CITATIONS SEE PROFILE Some of the authors of this publication are also working on these related projects: Genetic consequences of sable introductions on Western and Eastern Siberia View project Genrikh Monakhov Publications View project All content following this page was uploaded by Maryana Ranyuk on 13 March 2018. The user has requested enhancement of the downloaded file. ISSN 1022-7954, Russian Journal of Genetics, 2018, Vol. 54, No. 3, pp. 358–362. © Pleiades Publishing, Inc., 2018. Original Russian Text © V.G. Monakhov, M.V. Modorov, M.N. Ranyuk, 2018, published in Genetika, 2018, Vol. 54, No. 3, pp. 361–365. SHORT COMMUNICATIONS Genetic Effects of Sable (Martes zibellina L.) Reintroduction in Western Siberia V. G. Monakhov, M. V. Modorov, and M. N. Ranyuk* Institute of Plant and Animal Ecology, Ural Branch, Russian Academy of Sciences, Yekaterinburg, 620144 Russia *e-mail: [email protected] Received February 1, 2017; in final form, July 10, 2017 Abstract⎯In the middle of the 20th century, massive introductions of sables were performed to recover the area of this valuable fur species. In this work, genetic variation of a naturalized sable population from the Vakh River basin (Nizhnevartovskiy district, Khanty-Mansi Autonomous Okrug) was investigated. -
Water Resources Lifeblood of the Region
Water Resources Lifeblood of the Region 68 Central Asia Atlas of Natural Resources ater has long been the fundamental helped the region flourish; on the other, water, concern of Central Asia’s air, land, and biodiversity have been degraded. peoples. Few parts of the region are naturally water endowed, In this chapter, major river basins, inland seas, Wand it is unevenly distributed geographically. lakes, and reservoirs of Central Asia are presented. This scarcity has caused people to adapt in both The substantial economic and ecological benefits positive and negative ways. Vast power projects they provide are described, along with the threats and irrigation schemes have diverted most of facing them—and consequently the threats the water flow, transforming terrain, ecology, facing the economies and ecology of the country and even climate. On the one hand, powerful themselves—as a result of human activities. electrical grids and rich agricultural areas have The Amu Darya River in Karakalpakstan, Uzbekistan, with a canal (left) taking water to irrigate cotton fields.Upper right: Irrigation lifeline, Dostyk main canal in Makktaaral Rayon in South Kasakhstan Oblast, Kazakhstan. Lower right: The Charyn River in the Balkhash Lake basin, Kazakhstan. Water Resources 69 55°0'E 75°0'E 70 1:10 000 000 Central AsiaAtlas ofNaturalResources Major River Basins in Central Asia 200100 0 200 N Kilometers RUSSIAN FEDERATION 50°0'N Irty sh im 50°0'N Ish ASTANA N ura a b m Lake Zaisan E U r a KAZAKHSTAN l u s y r a S Lake Balkhash PEOPLE’S REPUBLIC Ili OF CHINA Chui Aral Sea National capital 1 International boundary S y r D a r Rivers and canals y a River basins Lake Caspian Sea BISHKEK Issyk-Kul Amu Darya UZBEKISTAN Balkhash-Alakol 40°0'N ryn KYRGYZ Na Ob-Irtysh TASHKENT REPUBLIC Syr Darya 40°0'N Ural 1 Chui-Talas AZERBAIJAN 2 Zarafshan TURKMENISTAN 2 Boundaries are not necessarily authoritative. -
Second Report Submitted by the Russian Federation Pursuant to The
ACFC/SR/II(2005)003 SECOND REPORT SUBMITTED BY THE RUSSIAN FEDERATION PURSUANT TO ARTICLE 25, PARAGRAPH 2 OF THE FRAMEWORK CONVENTION FOR THE PROTECTION OF NATIONAL MINORITIES (Received on 26 April 2005) MINISTRY OF REGIONAL DEVELOPMENT OF THE RUSSIAN FEDERATION REPORT OF THE RUSSIAN FEDERATION ON THE IMPLEMENTATION OF PROVISIONS OF THE FRAMEWORK CONVENTION FOR THE PROTECTION OF NATIONAL MINORITIES Report of the Russian Federation on the progress of the second cycle of monitoring in accordance with Article 25 of the Framework Convention for the Protection of National Minorities MOSCOW, 2005 2 Table of contents PREAMBLE ..............................................................................................................................4 1. Introduction........................................................................................................................4 2. The legislation of the Russian Federation for the protection of national minorities rights5 3. Major lines of implementation of the law of the Russian Federation and the Framework Convention for the Protection of National Minorities .............................................................15 3.1. National territorial subdivisions...................................................................................15 3.2 Public associations – national cultural autonomies and national public organizations17 3.3 National minorities in the system of federal government............................................18 3.4 Development of Ethnic Communities’ National -
List of Grain Elevators in Which Grain Will Be Deposited for Subsequent Shipment to China
List of grain elevators in which grain will be deposited for subsequent shipment to China Contact Infromation (phone № Name of elevators Location num. / email) Zabaykalsky Krai Rapeseed 1 ООО «Zabaykalagro» Zabaykalsku krai, Borzya, ul. Matrosova, 2 8-914-120-29-18 2 OOO «Zolotoy Kolosok» Zabaykalsky Krai, Nerchinsk, ul. Octyabrskaya, 128 30242-44948 3 OOO «Priargunskye prostory» Zabaykalsky Krai, Priargunsk ul. Urozhaynaya, 6 (924) 457-30-27 Zabaykalsky Krai, Priargunsky district, village Starotsuruhaytuy, Pertizan 89145160238, 89644638969, 4 LLS "PION" Shestakovich str., 3 [email protected] LLC "ZABAYKALSKYI 89144350888, 5 Zabaykalskyi krai, Chita city, Chkalova street, 149/1 AGROHOLDING" [email protected] Individual entrepreneur head of peasant 6 Zabaykalskyi krai, Chita city, st. Juravleva/home 74, apartment 88 89243877133, [email protected] farming Kalashnikov Uriy Sergeevich 89242727249, 89144700140, 7 OOO "ZABAYKALAGRO" Zabaykalsky krai, Chita city, Chkalova street, 147A, building 15 [email protected] Zabaykalsky krai, Priargunsky district, Staroturukhaitui village, 89245040356, 8 IP GKFH "Mungalov V.A." Tehnicheskaia street, house 4 [email protected] Corn 1 ООО «Zabaykalagro» Zabaykalsku krai, Borzya, ul. Matrosova, 2 8-914-120-29-18 2 OOO «Zolotoy Kolosok» Zabaykalsky Krai, Nerchinsk, ul. Octyabrskaya, 128 30242-44948 3 OOO «Priargunskye prostory» Zabaykalsky Krai, Priargunsk ul. Urozhaynaya, 6 (924) 457-30-27 Individual entrepreneur head of peasant 4 Zabaykalskyi krai, Chita city, st. Juravleva/home 74, apartment 88 89243877133, [email protected] farming Kalashnikov Uriy Sergeevich Rice 1 ООО «Zabaykalagro» Zabaykalsku krai, Borzya, ul. Matrosova, 2 8-914-120-29-18 2 OOO «Zolotoy Kolosok» Zabaykalsky Krai, Nerchinsk, ul. Octyabrskaya, 128 30242-44948 3 OOO «Priargunskye prostory» Zabaykalsky Krai, Priargunsk ul. -
Ethnic and Cultural Mosaic in Western Baraba During the Late Bronze to Iron Age Transition (14Th–8Th Centuries Bc)*
ARCHAEOLOGY, ETHNOLOGY & ANTHROPOLOGY OF EURASIA Archaeology Ethnology & Anthropology of Eurasia 42/4 (2014) 54–63 E-mail: [email protected] 54 THE METAL AGES AND MEDIEVAL PERIOD V.I. Molodin Novosibirsk State University, Pirogova 2, Novosibirsk, 630090, Russia Institute of Archaeology and Ethnography, Siberian Branch, Russian Academy of Sciences, Pr. Akademika Lavrentieva 17, Novosibirsk, 630090, Russia E-mail: [email protected] ETHNIC AND CULTURAL MOSAIC IN WESTERN BARABA DURING THE LATE BRONZE TO IRON AGE TRANSITION (14TH–8TH CENTURIES BC)* In the Late Bronze Age, a group of cultures dominated by that of the Irmen had appeared in the forest-steppe area located on the right bank of the Irtysh River basin. Different parts of this region were inhabited by populations from the Irmen, Suzgun, and Pakhomovskaya cultures as well as those related to the Relief-Band Ware culture. The degree of their interaction appears to have varied. Evidence suggests that the intensive development of this group occurred during the subsequent transitional period, which spanned from the Bronze to the Iron Age. Populations that inhabited the north, west and south-west regions migrated into this area to establish large and forti¿ ed trading posts. Keywords: Late Bronze Age, Bronze/Iron Age transition, Irtysh River basin, Western Siberia. Introduction (Polosmak, 1987), and Early and High Middle Ages (Elagin, Molodin, 1991; Baraba..., 1988), as well as the The Ob-Irtysh forest-steppe area, referred to as the Late Middle Ages and the Modern Period (Molodin, Baraba forest-steppe, is thought to have been developed Sobolev, Soloviev, 1990). by Man as far back as the Late Pleistocene. -
Siberia, the Wandering Northern Terrane, and Its Changing Geography Through the Palaeozoic ⁎ L
Earth-Science Reviews 82 (2007) 29–74 www.elsevier.com/locate/earscirev Siberia, the wandering northern terrane, and its changing geography through the Palaeozoic ⁎ L. Robin M. Cocks a, , Trond H. Torsvik b,c,d a Department of Palaeontology, The Natural History Museum, Cromwell Road, London SW7 5BD, UK b Center for Geodynamics, Geological Survey of Norway, Leiv Eirikssons vei 39, Trondheim, N-7401, Norway c Institute for Petroleum Technology and Applied Geophysics, Norwegian University of Science and Technology, N-7491 NTNU, Norway d School of Geosciences, Private Bag 3, University of the Witwatersrand, WITS, 2050, South Africa Received 27 March 2006; accepted 5 February 2007 Available online 15 February 2007 Abstract The old terrane of Siberia occupied a very substantial area in the centre of today's political Siberia and also adjacent areas of Mongolia, eastern Kazakhstan, and northwestern China. Siberia's location within the Early Neoproterozoic Rodinia Superterrane is contentious (since few if any reliable palaeomagnetic data exist between about 1.0 Ga and 540 Ma), but Siberia probably became independent during the breakup of Rodinia soon after 800 Ma and continued to be so until very near the end of the Palaeozoic, when it became an integral part of the Pangea Supercontinent. The boundaries of the cratonic core of the Siberian Terrane (including the Patom area) are briefly described, together with summaries of some of the geologically complex surrounding areas, and it is concluded that all of the Palaeozoic underlying the West Siberian