Oil Pollution in the Black and Caspian Seas
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Cleanseanet Surveillance of Sea-Based Oil Spills by Radar Satellite Images Bachelor of Science Thesis in Shipping and Marine Technology
CleanSeaNet Surveillance of sea-based oil spills by radar satellite images Bachelor of Science Thesis in Shipping and Marine Technology ANA PAULA ROBALO DA SILVA RODRIGUES Department of Shipping and Marine Technology Bachelor’s Degree in Nautical Science CHALMERS University of Technology Gothenburg, Sweden 2009 Diploma Thesis SK-09/26 ii REPORT NO. SK-09/26 CleanSeaNet Surveillance of sea-based oil spills by satellite radar images ANA PAULA ROBALO DA SILVA RODRIGUES Department of Shipping and Marine Technology CHALMERS UNIVERSITY OF TECHNOLOGY Gothenburg, Sweden 2009 iii CleanSeaNet Surveillance of sea-based oil spills by satellite radar images ANA PAULA ROBALO DA SILVA RODRIGUES © ANA PAULA ROBALO DA SILVA RODRIGUES, 2009 Technical report no. SK-09/26 Department of Shipping and Marine Technology Chalmers University of Technology SE-412 96 Gothenburg Sweden Telephone + 46 (0)31-772 1000 Figure 1 (cover): Oil spill off the north-west coast of Spain (© European Space Agency / EMSA 2007) This image, taken by ENVISAT-ASAR on 1 June 2007 off the coast north-west Spain, shows 2 large oil spills. The 1st one, in the bottom right of the image has very distinct linear dark features with sharp edges and uniform backscattered signal area with a potential polluter vessel connected to it (visible as a bright white spot). The 2nd one, in the left top corner, has diffuse shape but high contrast typical of a spill that has been discharged several hours ago (source: EMSA 2009a). Printed by Chalmers Reproservice Gothenburg, Sweden 2009 iv Preface This report constitutes my Bachelor of Science thes is for Nautical Studies at Chalmers University of Technology in Gothenburg, S wed en. -
1 EMSA's Pollution Response & Detection Services
EMSA’s Pollution Response & Detection Services PAJ Oil Spill Symposium 2008 1 Bernd Bluhm Head of Unit Pollution Response European Maritime Safety Agency (EMSA) Background Post-Erika (2002: EMSA established) Post-Prestige (2004: new tasks include pollution response) 2 Agency of the European Community • Own legal identity • No legislative role • Technical and operational support 1 EMSA provides operational support • A European network of oil recovery vessels • Setting up a network of chemical experts for responding to HNS spills 3 • A satellite monitoring and surveillance service • EMSA experts service to second the MS and the EC during the marine pollution response operations Major European Oil Spills >10,000 Tonnes Year Name of the Vessel Tonnes spilled Countries affected 1989 KHARK 5 80,000 Portugal/Morocco 1989 ARAGON 25,000 Portugal 1990 SEA SPIRIT 10,000 Spain/Morocco 1991 HAVEN 144,000 Italy 4 1992 AEGEAN SEA 73,500 Spain 1993 BRAER 84,000 United Kingdom 1994 NASSIA 33,000 Turkey 1994 NEW WORLD 11,000 Portugal 1996 SEA EMPRESS 72,360 United Kingdom 1999 ERIKA 19,800 France 2002 PRESTIGE 63,000 Spain 2 Large oil spills in European waters Spills >700 tonnes 5 Spills >10,000 tonnes Recent major incidents in Europe 6 Erika Dec.1999; 20,000 tons HFO spilled Prestige Nov. 2002; 63,000 tons HFO spilled 3 Oil Pollution Response Equipment 7 Different Methods for Mechanical Recovery Network of Stand-by Oil Recovery Vessels Concept: • Vessel carries out normal commercial service • Request from Member State for assistance • Short notice transformation -
Sensors, Features, and Machine Learning for Oil Spill Detection and Monitoring: a Review
remote sensing Review Sensors, Features, and Machine Learning for Oil Spill Detection and Monitoring: A Review Rami Al-Ruzouq 1,2,* , Mohamed Barakat A. Gibril 2,3 , Abdallah Shanableh 1,2, Abubakir Kais 1, Osman Hamed 4 , Saeed Al-Mansoori 5 and Mohamad Ali Khalil 2 1 Civil and Environmental Engineering Department, University of Sharjah, Sharjah 27272, UAE; [email protected] (A.S.); [email protected] (A.K.) 2 GIS & Remote Sensing Center, Research Institute of Sciences and Engineering, University of Sharjah, Sharjah 27272, UAE; [email protected] (M.B.A.G.); [email protected] (M.A.K.) 3 Department of Civil Engineering, Faculty of Engineering, Universiti Putra Malaysia, Serdang 43400, Malaysia 4 Faculty of Science and Engineering, University of Wolverhampton, Wolverhampton WV1 1LY, UK; [email protected] 5 Applications Development and Analysis Section (ADAS), Mohammed Bin Rashid Space Centre (MBRSC), Dubai 211833, UAE; [email protected] * Correspondence: [email protected]; Tel.: +971-6-505-0953 Received: 2 September 2020; Accepted: 7 October 2020; Published: 13 October 2020 Abstract: Remote sensing technologies and machine learning (ML) algorithms play an increasingly important role in accurate detection and monitoring of oil spill slicks, assisting scientists in forecasting their trajectories, developing clean-up plans, taking timely and urgent actions, and applying effective treatments to contain and alleviate adverse effects. Review and analysis of different sources of remotely sensed data and various components of ML classification systems for oil spill detection and monitoring are presented in this study. More than 100 publications in the field of oil spill remote sensing, published in the past 10 years, are reviewed in this paper. -
Cleanseanet 1
17ème journée d’information du Cedre: La Détection des Pollutions accidentelles et des Rejets Illicites Paris, 20 Mars 2012 CleanSeaNet 1 Marc Journel Unit C3 Satellite Based Monitoring Services CleanSeaNet • The European satellite oil pollution and vessel detection and monitoring system • Linked into national/regional response chain strengthening operational pollution surveillance and response for deliberate and accidental spills. 2 Legal basis • Directive 2005/35/EC* of 7 September 2005 on ship-source pollution and on the introduction of penalties, including criminal penalties, for pollution offences Article 10 Accompanying measures 2. In accordance with its tasks as defined in Regulation (EC) No 1406/2002, the European Maritime Safety Agency shall: 3 (a) work with the Member States in developing technical solutions and providing technical assistance in relation to the implementation of this Directive, in actions such as tracing discharges by satellite monitoring and surveillance; (b) assist the Commission in the implementation of this Directive, including, if appropriate, by means of visits to the Member States, in accordance with Article 3 of Regulation (EC) No 1406/2002. * as amended by Directive 2009/123/EC of 21 October 2009 Operational use of CleanSeaNet Routine monitoring of all European waters looking for illegal discharges : •Detection of possible spills •Detection of vessels •Identification of polluters by combining CleanSeaNet and Vessel traffic information available through SafeSeaNet 4 Supporting enforcement actions by the -
Tetrapod Localities from the Triassic of the SE of European Russia
Earth-Science Reviews 60 (2002) 1–66 www.elsevier.com/locate/earscirev Tetrapod localities from the Triassic of the SE of European Russia Valentin P. Tverdokhlebova, Galina I. Tverdokhlebovaa, Mikhail V. Surkova,b, Michael J. Bentonb,* a Geological Institute of Saratov State University, Ulitsa Moskovskaya, 161, Saratov 410075, Russia b Department of Earth Sciences, University of Bristol, Bristol, BS8 1RJ, UK Received 5 November 2001; accepted 22 March 2002 Abstract Fossil tetrapods (amphibians and reptiles) have been discovered at 206 localities in the Lower and Middle Triassic of the southern Urals area of European Russia. The first sites were found in the 1940s, and subsequent surveys, from the 1960s to the present day, have revealed many more. Broad-scale stratigraphic schemes have been published, but full documentation of the rich tetrapod faunas has not been presented before. The area of richest deposits covers some 900,000 km2 of territory between Samara on the River Volga in the NW, and Orenburg and Sakmara in the SW. Continental sedimentary deposits, consisting of mudstones, siltstones, sandstones, and conglomerates deposited by rivers flowing off the Ural Mountain chain, span much of the Lower and Middle Triassic (Induan, Olenekian, Anisian, Ladinian). The succession is divided into seven successive svitas, or assemblages: Kopanskaya (Induan), Staritskaya, Kzylsaiskaya, Gostevskaya, and Petropavlovskaya (all Olenekian), Donguz (Anisian), and Bukobay (Ladinian). This succession, comprising up to 3.5 km of fluvial and lacustrine sediments, documents major climatic changes. At the beginning of the Early Triassic, arid-zone facies were widely developed, aeolian, piedmont and proluvium. These were replaced by fluvial facies, with some features indicating aridity. -
Geochemical and Lu-Hf Isotope (LA-ICP-MS
Arch & Anthropol Open Acc Archaeology Copyright& Anthropology: © Kuznetsov NB CRIMSON PUBLISHERS C Wings to the Research Open Access ISSN: 2577-1949 Research Article Geochemical and Lu-Hf Isotope Systematic of Detrital Zircons from the Ordovician Sandstones of the Sol-Iletsk Arch (Russia, Northern Caspian, Borehole Ordovician-2) Kuznetsov NB 1,2,3,4*, Belousova EA4, Romanyuk TV2,3,4 1Geological Institute, Russian Academy of Sciences, Russia 2Schmidt Institute of Physics of the Earth, Russian Academy of Science, Russia 3Gubkin Russian State University of Oil and Gas, National Research University, Russia 4Australian Research Council Centre of Excellence for Core to Crust Fluid Systems/GEMOC, Macquarie University, Australia *Corresponding author: Kuznetsov NB, Geological Institute, Russian Academy of Sciences, Gubkin Russian State University of Oil and Gas, Russia Submission: July 02, 2018; Published: September 20, 2018 Abstract The Sol-Iletsk arch is located at the south eastern edge of the East European platform (EEP), where EEP adjoins with the Southern Urals. The results of the integrated (U-Pb age, Lu-Hf isotopic system and trace-elements) study of detrital zircons (dZr) from the Ordovician sandstones (within Sol-Iletsk arch) reached by borehole Ordovician-2 are presented. The primary sources of Early Precambrian dZr were most likely the crystalline complexes of the Late Proterozoic Volgo-Sarmatian and Taratash orogens and Archean Volga-Uralia basement. However, for numerous dZr with ages younger 1.65Ga, it is not possible presently to unambiguously identify primary sources. Crystalline complexes with such ages are absolutely atypical for the south-eastern part of the EEP, but they occurred within parts EEP very remote from Sol-Iletsk arch and beyond EEP. -
Ages of Detrital Zircons (U/Pb, LA-ICP-MS) from the Latest
Precambrian Research 244 (2014) 288–305 Contents lists available at ScienceDirect Precambrian Research jo urnal homepage: www.elsevier.com/locate/precamres Ages of detrital zircons (U/Pb, LA-ICP-MS) from the Latest Neoproterozoic–Middle Cambrian(?) Asha Group and Early Devonian Takaty Formation, the Southwestern Urals: A test of an Australia-Baltica connection within Rodinia a,∗ b c Nikolay B. Kuznetsov , Joseph G. Meert , Tatiana V. Romanyuk a Geological Institute, Russian Academy of Sciences, Pyzhevsky Lane, 7, Moscow 119017, Russia b Department of Geological Sciences, University of Florida, 355 Williamson Hall, Gainesville, FL 32611, USA c Schmidt Institute of Physics of the Earth, Russian Academy of Sciences, B. Gruzinskaya ul. 10, Moscow 123810, Russia a r t i c l e i n f o a b s t r a c t Article history: A study of U-Pb ages on detrital zircons derived from sedimentary sequences in the western flank of Received 5 February 2013 Urals (para-autochthonous or autochthonous with Baltica) was undertaken in order to ascertain/test Received in revised form source models and paleogeography of the region in the Neoproterozoic. Samples were collected from the 16 September 2013 Ediacaran-Cambrian(?) age Asha Group (Basu and Kukkarauk Formations) and the Early Devonian-aged Accepted 18 September 2013 Takaty Formation. Available online 19 October 2013 Ages of detrital zircons within the Basu Formation fall within the interval 2900–700 Ma; from the Kukkarauk Formation from 3200 to 620 Ma. Ages of detrital zircons from the Devonian age Takaty For- Keywords: Australia mation are confined to the Paleoproterozoic and Archean (3050–1850 Ma). -
UNEP(DEPI)/MED IG.22/28 Page 245 Decision IG.22/4 Regional Strategy
UNEP(DEPI)/MED IG.22/28 Page 245 Decision IG.22/4 Regional Strategy for Prevention of and Response to Marine Pollution from Ships (2016-2021) The 19th Meeting of the Contracting Parties to the Convention for the Protection of the Marine Environment and the Coastal Region of the Mediterranean, herein after referred to as the Barcelona Convention, Recalling the Protocol concerning Cooperation in Preventing Pollution from Ships and, in Cases of Emergency, Combating Pollution of the Mediterranean Sea, hereinafter referred to as the “2002 Prevention and Emergency Protocol”, and in particular article 18 providing for the formulation and adoption “of strategies, action plans and programmes for its implementation”; Recalling also the Regional Strategy for Prevention of and Response to Marine Pollution from Ships (2005-2015), hereinafter referred to as “the Regional Strategy (2005-2015)”, adopted by COP 14 (Portorož, Slovenia, 2005); Noting the progress achieved and the challenges faced in the implementation of the Regional Strategy (2005-2015) and the possible areas of improvements; Based on Decision IG.21/17 of COP 18 (Istanbul, Turkey, December 2013) on the Programme of Work and Budget 2014-2015 mandating the revision and update of the Regional Strategy (2005- 2015); Further recalling that the mandate of the Regional Marine Pollution Emergency Response Centre for the Mediterranean Sea (REMPEC), adopted by the 16th Meeting of the Contracting Parties in Marrakesh (Morocco) in 2009, is to assist the Contracting Parties in meeting their obligations under the 2002 Prevention and Emergency Protocol and in implementing related strategies; 1. Adopts the Regional Strategy for Prevention of and Response to Marine Pollution from Ships (2016-2021), hereinafter referred to as “the Regional Strategy (2016-2021)”, contained in the Annex to this Decision; 2. -
20020011.Pdf
Color profile: Generic CMYK printer profile Composite Default screen 1144 PERSPECTIVE Geological and evolutionary underpinnings for the success of Ponto-Caspian species invasions in the Baltic Sea and North American Great Lakes David F. Reid and Marina I. Orlova1 Abstract: Between 1985 and 2000, ~70% of new species that invaded the North American Great Lakes were endemic to the Ponto-Caspian (Caspian, Azov, and Black seas) basins of eastern Europe. Sixteen Ponto-Caspian species were also established in the Baltic Sea as of 2000. Many Ponto-Caspian endemic species are characterized by wide environmental tolerances and high phenotypic variability. Ponto-Caspian fauna evolved over millions of years in a series of large lakes and seas with widely varying salinities and water levels and alternating periods of isolation and open connections between the Caspian Sea and Black Sea depressions and between these basins and the Mediterranean Basin and the World Ocean. These conditions probably resulted in selection of Ponto-Caspian endemic species for the broad environmental tolerances and euryhalinity many exhibit. Both the Baltic Sea and the Great Lakes are geologi- cally young and present much lower levels of endemism. The high tolerance of Ponto-Caspian fauna to varying environmental conditions, their ability to survive exposure to a range of salinities, and the similarity in environmental conditions available in the Baltic Sea and Great Lakes probably contribute to the invasion success of these species. Human activities have dramatically increased the opportunities for transport and introduction and have played a cata- lytic role. Résumé : Entre 1985 et 2000, environ 70 % des espèces qui ont envahi pour la première fois les Grands-Lacs d’Amérique du Nord étaient endémiques aux bassins versants de la région pontocaspienne de l’Europe de l’Est, soit ceux de la mer Caspienne, de la mer d’Azov et de la mer Noire. -
Subsidence History and Basin-Fill Evolution in the South Caspian
Downloaded from http://sp.lyellcollection.org/ by guest on September 26, 2021 Subsidence history and basin-fill evolution in the South Caspian Basin from geophysical mapping, flexural backstripping, forward lithospheric modelling and gravity modelling N. A. ABDULLAYEV1,2*, F. KADIROV1 & I. S. GULIYEV1 1Institute of Geology, Azerbaijan National Academy of Sciences, H. Javid Avenue, 29A, Baku AZ1143, Azerbaijan 2BP Caspian Ltd, Xazar Centre, Port Baku, 153 Neftchilyar Avenue, Baku AZ1010 *Corresponding author (e-mail: [email protected]) Abstract: This study summarizes the subsidence history and aspects of the geodynamic evolution of the South Caspian Basin based on the integration of geophysical observations, and subsidence and gravity modelling on selected two-dimensional (2D) profiles. This analysis implies the pres- ence of an attenuated ‘oceanic-type’ crust in the northern portion of the South Caspian Basin, demonstrates characteristics of basin subsidence on variable crustal types and describes sedi- ment-fill evolution in several different parts of the basin. Modelling conducted in this study shows that the observed pattern of subsidence and sedimentation in the South Caspian Basin can be explained by a process of thermal subsidence following Jurassic rifting and further enhanced subsidence that resulted from sediment-induced loading in the Late Tertiary, especially after a large-scale base-level fall after 6 Ma.Variation in crustal type is reflected in differences observed in the degree of subsidence and sediment fill in the overlying stratigraphy. The western part of the South Caspian Basin has subsided differently to the eastern part because of this difference in crustal type. This is also confirmed by gravity modelling, which shows that the South Caspian Basin crustal density is compatible with an oceanic composition in the western part of the South Caspian Basin: the crust in the eastern part of the basin, however, is thicker. -
Eunaseis: a Seismic Model for Moho and Crustal Structure in Europe, Greenland, and the North Atlantic Region
EUNAseis a seismic model for Moho and crustal structure in Europe, Greenland, and the North Atlantic region Artemieva, Irina; Thybo, Hans Published in: Tectonophysics DOI: 10.1016/j.tecto.2013.08.004 Publication date: 2013 Document version Publisher's PDF, also known as Version of record Citation for published version (APA): Artemieva, I., & Thybo, H. (2013). EUNAseis: a seismic model for Moho and crustal structure in Europe, Greenland, and the North Atlantic region. Tectonophysics, 609, 97-153. https://doi.org/10.1016/j.tecto.2013.08.004 Download date: 04. Oct. 2021 Tectonophysics 609 (2013) 97–153 Contents lists available at ScienceDirect Tectonophysics journal homepage: www.elsevier.com/locate/tecto Review Article EUNAseis: A seismic model for Moho and crustal structure in Europe, Greenland, and the North Atlantic region☆ Irina M. Artemieva ⁎, Hans Thybo IGN, University of Copenhagen, Denmark article info abstract Article history: We present a new digital crustal model for Moho depth and crustal structure in Europe, Greenland, Iceland, Received 27 November 2012 Svalbard, European Arctic shelf, and the North Atlantic Ocean (72W–62E, 30N–84N). Our compilation is based Received in revised form 18 July 2013 on digitization of original seismic profiles and Receiver Functions from ca. 650 publications which provides a Accepted 4 August 2013 dense regional data coverage. Exclusion of non-seismic data allows application of the database to potential Available online 15 August 2013 field modeling. EUNAseis model includes Vp velocity and thickness of five crustal layers, including the sedimen- tary cover, and Pn velocity. For each parameter we discuss uncertainties associated with theoretical limitations, Keywords: Moho regional data quality, and interpolation. -
A Seismic Model for Moho and Crustal Structure in Europe, Greenland, and the North Atlantic Region☆
Tectonophysics 609 (2013) 97–153 Contents lists available at ScienceDirect Tectonophysics journal homepage: www.elsevier.com/locate/tecto Review Article EUNAseis: A seismic model for Moho and crustal structure in Europe, Greenland, and the North Atlantic region☆ Irina M. Artemieva ⁎, Hans Thybo IGN, University of Copenhagen, Denmark article info abstract Article history: We present a new digital crustal model for Moho depth and crustal structure in Europe, Greenland, Iceland, Received 27 November 2012 Svalbard, European Arctic shelf, and the North Atlantic Ocean (72W–62E, 30N–84N). Our compilation is based Received in revised form 18 July 2013 on digitization of original seismic profiles and Receiver Functions from ca. 650 publications which provides a Accepted 4 August 2013 dense regional data coverage. Exclusion of non-seismic data allows application of the database to potential Available online 15 August 2013 field modeling. EUNAseis model includes Vp velocity and thickness of five crustal layers, including the sedimen- tary cover, and Pn velocity. For each parameter we discuss uncertainties associated with theoretical limitations, Keywords: Moho regional data quality, and interpolation. Crustal thickness By analyzing regional trends in crustal structure and links to tectonic evolution illustrated by a new tectonic map, Crystalline crust we conclude that: (1) Each tectonic setting shows significant variation in depth to Moho and crustal structure, Sedimentary cover essentially controlled by the age of latest tectono-thermal processes; (2) Published global averages of crustal pa- Pn velocity rameters are outside of observed ranges for any tectonic setting in Europe; (3) Variation of Vp with depth in the Crustal evolution sedimentary cover does not follow commonly accepted trends; (4) The thickness ratio between upper-middle (Vp b 6.8 km/s) and lower (Vp N 6.8 km/s) crystalline crust is indicative of crustal origin: oceanic, transitional, platform, or extended crust; (5) Continental rifting generally thins the upper-middle crust significantly without changing Vp.