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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.). -
Alexander P. Lisitsyn Liudmila L. Demina Editors the White Sea
The Handbook of Environmental Chemistry 82 Series Editors: Damià Barceló · Andrey G. Kostianoy Alexander P. Lisitsyn Liudmila L. Demina Editors Sedimentation Processes in the White Sea The White Sea Environment Part II The Handbook of Environmental Chemistry Founding Editor: Otto Hutzinger Editors-in-Chief: Damia Barcelo´ • Andrey G. Kostianoy Volume 82 Advisory Editors: Jacob de Boer, Philippe Garrigues, Ji-Dong Gu, Kevin C. Jones, Thomas P. Knepper, Alice Newton, Donald L. Sparks More information about this series at http://www.springer.com/series/698 Sedimentation Processes in the White Sea The White Sea Environment Part II Volume Editors: Alexander P. Lisitsyn Á Liudmila L. Demina With contributions by T. N. Alexсeeva Á D. F. Budko Á O. M. Dara Á L. L. Demina Á I. V. Dotsenko Á Y. A. Fedorov Á A. A. Klyuvitkin Á A. I. Kochenkova Á M. D. Kravchishina Á A. P. Lisitsyn Á I. A. Nemirovskaya Á Y. A. Novichkova Á A. N. Novigatsky Á A. E. Ovsepyan Á N. V. Politova Á Y. I. Polyakova Á A. E. Rybalko Á V. A. Savitskiy Á L. R. Semyonova Á V. P. Shevchenko Á M. Y. Tokarev Á A. Yu. Lein Á V. A. Zhuravlyov Á A. A. Zimovets Editors Alexander P. Lisitsyn Liudmila L. Demina Shirshov Inst. of Oceanology Shirshov Inst. of Oceanology Russian Academy of Sciences Russian Academy of Sciences Moscow, Russia Moscow, Russia ISSN 1867-979X ISSN 1616-864X (electronic) The Handbook of Environmental Chemistry ISBN 978-3-030-05110-5 ISBN 978-3-030-05111-2 (eBook) https://doi.org/10.1007/978-3-030-05111-2 Library of Congress Control Number: 2018964918 © Springer Nature Switzerland AG 2018 This work is subject to copyright. -
Chronicle of Trans – Arctic Passage
UDK 656.614.33(985)(045) Chronicle of Trans – Arctic passage © Vladimir P. Sokolov, the sea captain, the captain-inspector of administration of seaport «Arkhangelsk». Education - the navigator and the journalist, has ended faculty of journalism of the Leningrad University. Worked on sea courts. More than thirty years co-operate with newspapers of Arkhangelsk. Its articles were published in central press. A member of the Union of journalists of the Russian Federation, the winner of the award of the Arkhangelsk regional journalistic organization. Mobile phone +7-906-28288-96. Abstract Notes of sea captain Vladimir Sokolova we begin a heading «Arctic regions today». For the first time in history existence of Northern sea way during navigation by one icebreaking vessel «Michael Somov» are provided all polar stations. The author reflects on problems of development of Northern sea way. Key words: «Michael Somov», development, northern sea way, supply of polar stations. I must say that for "Mikhail Somov" I'm not a stranger at all. Ten years ago, it took the post of chief mate, was in the Barents and Kara seas, and participated in the landings on the island weather station. The same type of "Somov" diesel-electric ice-class specially built for navigation in ice. And there were a to the Arctic in the 70-80s at least a dozen "Amguema", "Navarino", "Vankarem", "Paul Ponomarev," "Captain Myshevsky ..." On one of them - "Gizhiga" - as a young man I began my work the Navigation. Over time, the entire series has been written down by age, or, as sailors say, "on the needles." Today on the Northern Sea Route of them had only one - the famous "Mikhail Somov". -
The Flora and Vegetation of Sosnovets Island, the White Sea
Memoranda Soc. Fauna Flora Fennica 95: 1–35. 2019 ISSN 0373-6873 (print) Helsinki 24 January 2019 ISSN 1796-9816 (online) The flora and vegetation of Sosnovets Island, the White Sea Mikhail N. Kozhin*, Ekaterina O. Golovina, Ekaterina I. Kopeina, Stanislav A. Kutenkov & Alexander N. Sennikov Kozhin, M. N., Department of Geobotany, Faculty of Biology, Moscow State University, Leninskye Gory 1–12, GSP–1, 119234 Moscow, Russia; & Avrorin Polar-Alpine Botanical Garden and Institute of Kola Scientific Centre of Russian Academy of Sciences, 184250 Kirovsk, Murmansk Region, Russia. E-mail: [email protected] (*Author for correspondence) Golovina, E. O., Laboratory of Vegetation Geography and Mapping, Komarov Botanical Institute of Russian Academy of Sciences, Prof. Popov str. 2, 197376 St. Petersburg, Russia. E-mail: [email protected] Kopeina, E. I., Avrorin Polar-Alpine Botanical Garden and Institute of Kola Scientific Centre of Russian Academy of Sciences, 184250 Kirovsk, Murmansk Region, Russia. E-mail: kopeina-e@ yandex.ru Kutenkov, S. A., Institute of Biology of Karelian Research Centre of the Russian Academy of Sciences, Pushkinskaya str. 11, 185910 Petrozavodsk, Karelia, Russia. E-mail: effort@krc. karelia.ru Sennikov, A.N., Botanical Museum, Finnish Museum of Natural History, P.O. Box 7, 00014 University of Helsinki, Finland; & Herbarium, Komarov Botanical Institute of Russian Academy of Sciences, Prof. Popov str. 2, 197376 St. Petersburg, Russia. E-mail: alexander.sennikov@ helsinki.fi The flora and vegetation of Sosnovets Island (White Sea Throat, Murmansk Region, Russia) has been studied and described in detail. This is a small island situated within the tundra zone, largely covered by a permafrost peatland with the presence of flarks, a palsa mire, and rock outcrops. -
Late Pleistocene History?
Tolokonka on the Severnaya Dvina - A Late Pleistocene history? Field study in the Arkhangelsk region (Архангельская область), northwest Russia Russia Expedition – a SciencePub Project 25th May – 2nd July 2007 written by Udo Müller (Universität Leipzig) to obtain a B.Sc. degree’s equivalent APEX Udo Müller (2007): Tolokonka on the Severnaya Dvina - A Late Pleistocene history? Table of contents Introduction 3 The Late Pleistocene in northwest Russia 6 The Tolokonka section 18 Profile log 21 Interpretation 34 Conclusions 39 Acknowledgements 41 Abbreviations 42 References 43 - 2 - Udo Müller (2007): Tolokonka on the Severnaya Dvina - A Late Pleistocene history? Introduction The Russian North has been subject to many different research expeditions over the last decade, most of them as an integral part of the QUEEN Programme (Quaternary Environment of the Eurasian North), in order to reconstruct the glacial events throughout the Quaternary and their relation to sea-level change and paleoclimate. Fig.1 shows the localities that have been investigated between 1995 and 2002 – river sections along the Severnaya Dvina and its tributaries, the Mezen River Basin, the coasts of the White Sea and the Barents Sea, as well as the Timan Ridge (KJÆR et al. 2006a). Fig. 1. The Arkhangelsk region in NW Russia. Dots mark localities investigated between 1995 and 2002 (KJÆR et al. 2006a). For orientation see frontpage. According to KJÆR et al. (2006a), the Arkhangelsk region represents a key area for the understanding of Late Pleistocene glaciation history, since it was overridden by all three major Eurasian ice sheets: the Scandinavian, the Barents Sea and the Kara Sea ice sheets. -
The White Sea Report
Kolarctic ENPI CBC - Kolarctic salmon project (KO197) – the White Sea Report Summary results from coastal salmon fisheries in the White Sea: timing and origin of salmon catches Sergey Prusov1, Gennadiy Ustyuzhinsky2, Vidar Wennevik3, Juha-Pekka Vähä4, Mikhail Ozerov4, Rogelio Diaz Fernandez4, Eero Niemelä5, Martin-A. Svenning6, Morten Falkegård6, Tiia Kalske7, Bente Christiansen7, Elena Samoylova1, Vladimir Chernov1, Alexander Potutkin1, Artem Tkachenko1 1Knipovich Polar Research Institute of Marine Fisheries and Oceanography (PINRO), Murmansk, Russia 2Knipovich Polar Research Institute of Marine Fisheries and Oceanography (PINRO), Archangelsk, Russia 3Institute of Marine Research (IMR), Tromsø, Norway 4University of Turku (UTU), Finland 5Finnish Game and Fisheries Research Institute (FGFRI), Teno River Research Station Utsjoki, Finland 6Norwegian Institute of Nature Research (NINA), Tromsø, Norway 7County Governor of Finnmark (FMFI), Vadsø, Norway Knipovich Polar Research Institute of Marine Fisheries and Oceanography (PINRO) The White Sea Report – 2014 Contents Abstract.................................................................................................................................... 3 Introduction……………………………………………………………………………………………………………………….. 4 Materials and methods……………………………………………………….…………………………………………….. 6 Study area………………………………………………………………………..…………………………………………..… 6 Adult fish sampling…………………………………………………………………………………………………………. 7 Fisheries regulations and data………………………………………………………………………………………… 11 Results and discussions………………………………………………………………….…………………………………. -
KAROL PIASECKI Szczecin the WHITE SEA POMORYE and ITS
Studia Maritima, vol. XXII (2009) ISSN 0137-3587 KAROL PIASECKI Szczecin THE WHITE SEA POMORYE AND ITS INHABITANTS 1. The White Sea Pomorye owes its name to a group of Slavic settlers1 living mainly on the so-called Pomor Coast, i.e. a fragment of the White Sea coast be- tween the River Kem and Onega (Fig. 1). The present name of the White Sea became widespread at the beginning of the 17th century. Before that, the Slavic inhabitants of its coasts used a name Студеное Море, which means the Cold Sea, whereas on western maps, since the times of the reissue in 1568 of Claudius Ptole- my’s Geography, it appeared as Sinus Grandvicus (Granvicus, Grandvich). The name was taken from Norwegian sailors, for whom initially it probably meant the Western end of the Murmansk Coast.2 1 The term Pomors appeared for the first time in written sources in 1526, when: Поморцы с моря Океана из Кондолакской гyбы лросили вмесmе с лоплянамва yсmройства церкви. It functions quite commonly in the 16th century, both as a name of the inhabitants of the Pomor Coast, as well in the function of a proper name – I. Ul’janov: Strana Pomorja, 1984. From the second half of the 17th century, mainly because of Vasiliy Tatishchev, the author of the monumental Russian History, Pomorye was understood in three meanings: as 1) a territory of the White Sea coast from the Onega to the Kem, 2) the territory of the whole White Sea Coast, 3) the territory of the whole Russian North, including the provinces of Archangelsk, Vologda and Olonets. -
ISSN 2221-2698 Arkhangelsk, Russia DOI 10.17238/Issn2221-2698.2017
ISSN 2221-2698 Arkhangelsk, Russia DOI 10.17238/issn2221-2698.2017.28 Arctic and North. 2017. No. 28 2 ISSN 2221-2698 Arctic and North. 2017. No. 28 CC BY-SA © Northern (Arctic) Federal University named after M.V. Lomonosov, 2017 © Editorial board of electronic scientific journal “Arctic and North”, 2017 The journal “Arctic and North” (“Arktika i Sever”) is registered at Roskomnadzor as an in- ternet periodical issued in Russian and English, Registration certificate El № FS77-42809, Novem- ber 26, 2010; at the system of the Russian Science Citation Index (RSCI), license contract № 96- 04/2011R, April 12, 2011; Scientific Electronic Library "Сyberleninka" (2016); In the catalogs of in- ternational databases: Directory of Open Access Journals — DOAJ (2013); Global Serials Directory Ulrichsweb, USA (2013); NSD, Norway (2015); InfoBase Index, India (2015); ERIH PLUS, Norway (2016); MIAR, Spain (2016); OAJI (2017). The Journal is issued not less than 4 times per year. The Founder — Northern (Arctic) Federal University named after M.V. Lomonosov, Ar- khangelsk, Russia. Editor-in-Chief — Elena V. Kudryashova, D. Phil., Professor, Rector of Northern (Arctic) Federal University named after M.V. Lomonosov. All journal issues are available free of charge (CC BY-SA) in Russian and English at the webpage of the journal. Rules and regulations on submission, peer reviews, publication and the Declaration of Ethics are available at: http://narfu.ru/en/research/journals/ann/requirements.php The journal is devoted to the scientific articles focused on the Arctic and the North relevant for the following professional degrees (codes as indicated in the Russian scientific qualification in- dex): 03.00.00 Biology (including ecology; biological resources); 07.00.00 History and archaeology; 08.00.00 Economics; 22.00.00 Social science; 23.00.00 Political science; 24.00.00 Culturology; 25.00.00 Geoscience (including climatology; geography). -
133 INUNDATIONS in the DELTA of the NORTHERN DVINA RIVER Dmitry Magritsky*1, Serafima Lebedeva*, Vadim Polonsky**, Elena Skripn
Society and Natural Disaster UDC: 626.81/.85„2007” DOI: 10.2298/IJGI1303133M INUNDATIONS IN THE DELTA OF THE NORTHERN DVINA RIVER Dmitry Magritsky*1, Serafima Lebedeva*, Vadim Polonsky**, Elena Skripnik*** *Lomonosov Moscow State University, Faculty of Geography, Moscow, Russian Federation, **State Oceanographic Institute, Moscow, Russian Federation, ***Arkhangelsk CHMS, Arkhangelsk, Russian Federation Received 13 September 2013; reviewed 10 September 2013; accepted 01 October 2013 Abstract: This paper provides information about the types, factors and features of ice dam and storm surge inundations in the Northern Dvina River delta, new methods and results of their research, changing the situation with inundations for a long time-period. This article contains data on current structure and regime of the Northern Dvina delta, changes of hydrological factors in XX-XXI centuries Key words: delta, inundations, ice dams, surges Introduction River deltas, as well as seashores, have not only geographical and economic advantages, but also are exposed to a number of natural hazards and processes. They represent a real or potential threat to the population, economic activities and artificial objects. Among all the natural disasters of different origin inundations form the largest socio-economic and environmental damages. Northern Dvina River delta is not an exception. The first information about the severe floods in the delta dates back to XVII-XVIII centuries. However, despite the long history of the studying the factors and characteristics of inundations in the delta, and applied measures of fight against them, the inundations in the delta occur periodically and cause large damage to the population and economy of the delta. Structure and natural conditions of the delta of the Northern Dvina River The Northern Dvina River flows into the Dvina Bay of the White Sea (Figure 1). -
1. Geographic Location and Demographic Situation
1. Geographic location and demographic situation The city of Arkhangelsk where our meeting is taking place is the administrative center of the Arkhangelsk Oblast. The Arkhangelsk Oblast is located in the north-west of Russia (picture 1) and is washed by the water of three Arctic seas: the White Sea, the Barents Sea and the Kara Sea. The White Sea within the territory of the Arkhangelsk Oblast includes the Onega Bay, the Dvina Bay, and the Mezen Bay with the basins of main surface water bodies – the Northern Dvina, the Onega, and the Mezen rivers. Picture 1. Position of the Arkhangelsk Oblast on the map of Russia Favorable location and proximity to the White Sea contributed to establishment of Arkhangelsk – the first in Russia sea harbor and a center for trade with the Western European states. Arkhangelsk is a large historical, industrial, scientific and cultural center in the North-West of Russia. The following industrial sectors are concentrated here: timber, wood chemical, pulp-and-paper, fishing and fish processing, mechanical engineering. The city of Arkhangelsk is located on the banks of the Northern Dvina River and on the islands of its estuary (picture 2). The city is divided into 8 administrative districts. Total area of the city is 294.4 km2, the number of population as for January 1, 2009 is 348.3 thousand people. The construction of Arkhangelsk was mainly based on the location of large industrial and transportation facilities. As a result the city is stretched from the North to the South for more than 30 km, and from the West to the East – for 20 km. -
The Beluga Whale (Delphinapterus Leucas) Catches in the White, Barents, and Western Kara Seas from 1930 Based on Original Sources
Russian J. Theriol. 18(1): 20–32 © RUSSIAN JOURNAL OF THERIOLOGY, 2019 The beluga whale (Delphinapterus leucas) catches in the White, Barents, and western Kara seas from 1930 based on original sources Yaroslava I. Alekseeva, Olga V. Shpak* & Svyatoslav S. Gorbunov ABSTRACT: The work is based on an analysis of archival documents containing quantitative information on harvests of beluga whales in the White, Barents, and western Kara seas from 1930. Also, information is provided on the possible places where the documents containing data of beluga whaling could still be preserved. The probable causes of the reduction in catches and abundance of beluga whales in the coastal waters of the study areas, observed from the late 1960s, are discussed. How to cite this article: Alekseeva Y.I., Shpak O.V., Gorbunov S.S. 2019. The beluga whale (Delphinapterus leucas) catches in the White, Barents, and western Kara seas from 1930 based on original sources //Russian J. Theriol. Vol.18. No.1. P.20–32. doi: 10.15298/rusjtheriol.18.1.03. KEY WORDS: beluga whale, Delphinapterus leucas, commercial harvest, White Sea, Barents Sea, Kara Sea, archival documents. Yaroslava I. Alekseeva [[email protected]], K.A. Timiryazev State Biological Museum, Malaya Gruzinskaya 15, Moscow 123242, Russia; Olga V. Shpak [[email protected]], A.N. Severtsov Institute of Ecology and Evolution RAS, Leninsky prospect 33, Moscow 119071, Russia; Svyatoslav S. Gorbunov [[email protected]], independent researcher, Moscow, Russia. Документальные данные об уловах белухи (Delphinapterus leucas) в Белом, Баренцевом морях и западной части Карского моря с 1930 г. Я.И. Алексеева, О.В. -
6544-2013 72Dpi.Pdf (2.986Mb)
Statlig program for forurensningsovervåking Rapportnr. 1146/2013 Tilførselsprogrammet 2012 TA Overvåking av tilførsler og miljøtilstand i 3042 2013 Barentshavet og Lofotenområdet Utført av Norsk institutt for vannforskning RAPPORT Hovedkontor Sørlandsavdelingen Østlandsavdelingen Vestlandsavdelingen NIVA Midt-Norge Gaustadalléen 21 Jon Lilletuns vei 3 Sandvikaveien 41 Thormøhlensgate 53 D Pirsenteret, Havnegata 9 0349 Oslo 4879 Grimstad 2312 Ottestad 5006 Bergen Postboks 1266 Telefon (47) 22 18 51 00 Telefon (47) 22 18 51 00 Telefon (47) 22 18 51 00 Telefon (47) 22 18 51 00 7462 Trondheim Telefax (47) 22 18 52 00 Telefax (47) 37 04 45 13 Telefax (47) 62 57 66 53 Telefax (47) 55 31 22 14 Telefon (47) 22 18 51 00 Internett: www.niva.no Telefax (47) 73 54 63 87 Tittel Løpenr. (for bestilling) 10.06.2013 Tilførselsprogrammet 2012. Overvåking av tilførsler og 6544-2013 Sider miljøtilstand i Barentshavet og Lofotenområdet. Prosjektnr. 149 12309, 13309 Forfatter(e) Fagområde Distribusjon Norman W. Green1), Morten Skogen2), Wenche Aas3), Mikhail Iosjpe4), Marine miljøgifter Fri Amund Måge5), Knut Breivik3), Evgeniy Yakushev1), Tore Høgåsen1), 3) 1) 1) Sabine Eckhardt , Anne Birgitta Ledang , Pierre Francois Jaccard , Geografisk område Trykket 1) 6) 5) Andre Staalstrøm , Pål Erik Isachsen , Sylvia Frantzen Barentshavet NIVA 1) Norsk institutt for vannforskning (NIVA) 2) Havforskningsinstituttet (IMR) 3) Norsk institutt for luftforskning (NILU) 4) Statens strålevern (NRPA) 5) Nasjonalt institutt for ernærings- og sjømatforskning (NIFES) 5) Meteorologisk Institutt (met.no) Oppdragsgiver(e) Oppdragsreferanse Klima- og forurensningsdirektoratet (Klif) TA 3042/2013 SPFO 1146/2013 Sammendrag Denne rapporten beskriver beregninger av tilførsel av olje, miljøgifter og radioaktive stoffer fra åtte kilder til fire regioner i Lofotenområdet og den norske delen av Barentshavet.