DOCSLIB.ORG

State of Play on CO2 Geological Storage in 28 European Countries

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
State of Play on CO2 Geological Storage in 28 European Countries State of play on CO2 geological storage in 28 European countries • June 2013 • CGS Europe CO2GeoNet FP7 Pan-European Coordination The European Network of Excellence Action on CO2 Geological Storage on the Geological Storage of CO2 This report was prepared in the framework of the FP7 EU-funded "Pan-European Coordination Action on CO2 Geological Storage (CGS Europe; Project no.: 256725)" as Deliverable D2.10 by the CGS Europe partners under the coordination of Heike Rütters (Bundesanstalt für Geowissenschaften und Rohstoffe - BGR). This report should be cited in literature as follows: Rütters, H. and the CGS Europe partners (2013) - State of play on CO2 geological storage in 28 European countries. CGS Europe report No. D2.10, June 2013, 89 p. CGS Europe 256725: D2.10 – State of Play on CO2 Geological Storage in Europe TABLE OF CONTENTS 1. Introduction 1 2. Storage options, potentials and capacities in Europe 3 3. Research activities related to CO2 geological storage in CGS Europe countries 6 4. Research topics related to CO2 storage addressed by CGS Europe partners 8 5. National research funding in CGS Europe countries 11 6. Research activities on a regional and European level 17 7. Current pilot, demonstration and test sites in CGS Europe countries 21 8. State of transposition of the EU Directive on the geological storage of carbon dioxide in CGS Europe countries 23 9. Summary and Conclusions 25 10. References 28 ANNEX: Summarising the state of play on CO2 geological storage in the CGS Europe countries (as of July 31st 2012) - country-specific information provided by CGS Europe partners: Austria; Belgium; Bulgaria; Czech Republic; Croatia; Denmark; Estonia; Finland; France; Germany; Greece; Hungary; Ireland; Italy; Latvia; Lithuania; The Netherlands; Norway; Poland; Portugal; Romania; Serbia; Slovakia; Slovenia; Spain; Sweden; Turkey; United Kingdom 31 CGS Europe 256725: D2.10 – State of Play on CO2 Geological Storage in Europe LIST OF FIGURES Fig. 1: Extent of sedimentary basins (in grey: Fugro Tellus (FT), 2008; in shaded green: GeoCapacity (GC), 2009) and potential hydrocarbon fields for CO2 storage in Europe (GeoCapacity, 2009). 3 Fig. 2: Extent of sedimentary basins (in grey: Fugro Tellus (FT), 2008; in shaded green: GeoCapacity (GC), 2009) and potential coal fields for CO2 storage in Europe (GeoCapacity, 2009). 4 Fig. 3: Research hot spots in CGS Europe countries (as of July 31st 2012). 6 Fig. 4: Share of universities out of the total number of research entities involved in CO2 storage- related research in CGS Europe countries as of July 31st 2012 [weighted count as % of the weighted total count]. 7 st Fig. 5: Funding sources for research related to CO2 storage in CGS Europe countries (as of July 31 2012). 11 Fig. 6: National research funding by different Ministries/Departments of CGS Europe countries (as of July 31st 2012). 11 Fig. 7: Current demonstration, pilot and test sites for CO2 storage in CGS Europe countries (as of July 31st 2012). 21 Fig. 8: Status of the transposition of EU Directive on the geological storage of CO2 in CGS Europe countries, Malta and Cyprus at national and European Commission (EC) levels by the end of 2012. 23 st Fig. 9: Assessment of CGS Europe countries‟ achievements regarding CO2 storage (as of August 31 2012) as a function of national annual CO2 emissions in 2009. 26 st Fig. 10: Assessment of CGS Europe countries‟ achievements regarding CO2 storage (as of August 31 2012) as a function of national annual CO2 emissions per capita in 2009. 27 LIST OF TABLES Tab. 1: Institutions of CGS Europe. 2 Tab. 2: FP7-ENERGY collaborative projects – calls and topics. 18 Tab. 3: Weighting criteria for the overall assessment of achievements regarding CO2 storage in the CGS Europe countries. 25 Tab. 4: Classification of the CGS Europe countries according to their overall achievements regarding st CO2 storage (as of August 31 2012). 25 CGS Europe 256725: D2.10 – State of Play on CO2 Geological Storage in Europe 1 Introduction The “Pan-European coordination action on CO2 Geological Storage (CGS Europe)” (www.cgseurope.net) started in November 2010 and is funded within the 7th Framework Programme of the European Community for three years. In CGS Europe, the established expert networks CO2GeoNet Association (www.co2geonet.com), CO2NET EAST (co2neteast.energnet.com) and ENeRG (www.energnet.eu) are joining forces and pooling their expertise to build a credible, independent, and representative pan- European scientific body of expertise on CO2 geological storage. CGS Europe provides an independent platform and reference source where national, European and international experts, institutes and regulators are able to - access the most up-to-date results of CO2-storage-related studies, - share experiences and good practises, - discuss the implementation of regulations, - identify research needs to face upcoming challenges, and - build new projects. Partners of CGS Europe comprise members of the CO2GeoNet Association and 22 other participants covering most of Europe with 24 EU Member States as well as Croatia, Norway, Serbia and Turkey (Tab. 1). The objectives of CGS Europe are, among others, to support the implementation of the European Directive on the geological storage of CO2 and other regulatory regimes and to facilitate the large-scale demonstration and industrial deployment of CCS. In addition, CGS Europe is contributing to reducing the gap between the „forerunner‟ countries, where CCS activities have been started or planned, and the „follower‟ countries where these actions are not yet happening. As one of CGS Europe‟s activities, information was collated about the state of play on CO2 geological storage in the 28 countries covered by CGS Europe. The following topics have been addressed: i) research activities and national funding opportunities for research on CO2 storage; ii) current pilot, demo and test sites in the CGS Europe countries; iii) state of transposition of the EU Directive on the geological storage of CO2; iv) public awareness in the CGS Europe countries. The current state of play on CO2 geological storage in the CGS Europe countries is summarised in this report. More detailed country-specific information is provided in Annex I. In this report, a brief overview of the CO2 storage options, potentials and capacities in Europe is provided in Chapter 2. Structure and organisation of research funding related to CO2 storage on a national level are outlined in Chapters 3 and 5 of the current report. Research topics addressed by the CGS Europe partners and other research institutions in the CGS Europe countries are introduced in Chapter 4, followed by a summary of current pilot, demo and test sites (Chapter 7) and an overview of the current state of transposition of the EU Directive on the geological storage of CO2 in the CGS Europe countries (Chapter 8). Information on a national level is complemented by an overview of ongoing EU-funded research projects related to CO2 storage (www.cordis.eu) and a summary of activities of the European Energy Research Alliance (www.eera-set.eu) in Chapter 6. This report reflects the state of play in Europe as of July 31st 2012 unless indicated otherwise. 1 CGS Europe 256725: D2.10 – State of Play on CO2 Geological Storage in Europe Tab. 1: Institutions of CGS Europe. Short name Name Country GBA Geologische Bundesanstalt Austria RBINS-GSB Institut Royal Des Sciences Naturelles De Belgique Belgium SU Sofiiski Universitet Sveti Kliment Ohridski Bulgaria UNIZG-RGNF University of Zagreb, Croatia Faculty of Mining, Geology and Petroleum Engineering CzGS Ceska Geologicka Sluzba Czech Republic GEUS Geological Survey of Denmark and Iceland Denmark TTUGI Tallinna Tehnikaulikool Estonia GTK Geologian Tutkimuskeskus Finland BRGM Bureau De Recherches Geologiques Et Minieres France IFPEN IFP Energie Nouvelles France BGR Bundesanstalt für Geowissenschaften und Rohstoffe Germany EKBAA-IGME Ethniko Kentro Viosimis Kai Aeiforou Anaptyxis Greece IMFGI Magyar Földtani és Geofizikai Intezet Hungary (former ELGI) GSI Department of Communications, Energy and Natural resources – Ireland Geological Survey of Ireland OGS Istituto Nazionale di Oceanografia e di Geofisica Sperimentale Italy URS Università di Roma “La Sapienza” Italy LEGMC Latvijas Vides, Geologijas Un Meteorologijas Centrs SIA Latvia GTC Gamtos tyrimų centras Lithuania TNO TNO – Netherlands Organisation for Applied Science The Netherlands NIVA Norwegian Institute for Water Research Norway IRIS International Research Institute of Stavanger Norway SINTEF SINTEF Petroleum Research Norway PGI-NRI Panstwowy Institut Geologiczny - Panstwowy Institut Badawczy Poland LNEG Laboratorio Nacional de Energia e Geologia I.P. Portugal GEOECOMAR Institutul National De Cercetare-Dezvoltare Pentru Geologie Si Romania Geoecologie Marina - GEOECOMAR AGES Association of Geophysicists and Environmentalists of Serbia Serbia SGUDS Statny Geologicky Ustav Dionyza Stura Slovakia GEO-INZ Geoinzeniring, druzba za geoloski inzeniring d.o.o. Slovenia S-IGME Instituto Geológico Y Minero De España Spain SGU Sveriges geologiska undersökning Sweden METU-PAL Middle East Technical University - Petroleum Research Centre Turkey BGS British Geological Survey United Kingdom IMPERIAL Imperial College Consultants Ltd. United Kingdom HWU Institute of Petroleum Engineering, Heriott-Watt University United Kingdom 2 CGS Europe 256725: D2.10 – State of Play on CO2 Geological Storage in Europe 2 Storage options, potentials and capacities in Europe For the geological storage
Load more

Recommended publications
  • Thessaloniki
    Thessaloniki Photo: joaoa Byzantine churches, Roman constructions, Muslim buildings, modern architecture, intensive nightlife and stunning beaches - this is the essence of Thessaloniki. Being the second largest city in Greece, Thessaloniki combines more than 2,300 years of history with every facility and excitement that a modern European city can offer a visitor. Tilemahos Top 5 The White Tower The White Tower is a widely known symbol of the city and a point of reference for locals and visitors. It stands next to the s... Ladadika Quarter The area from Koudouriotou to Diamanti streets and from Hiou to Lemnou streets is known as Ladadika. Here you can find many ba... Aristotelous Square Photo: Tilemahos This is the most impressive square in Thessaloniki. It features buildings with great architecture inspired by European and col... Saint Dimitrios Church The church of the patron saint of the town is a must see in Thessaloniki. The first church of Saint Dimitrios was built in 313... Galerius Arch (Kamara) In addition to The Rotonda, this is one of the two most characteristic monuments in town. Galerius arch is situated near the e... Photo: Dave Proffer Updated 15 July 2014 Destination: Thessaloniki Publishing date: 2014-07-15 THE CITY ArrivalGuides goes ArrivalTV! Photo: Tilemahos Thessaloniki is the capital of the region Central Macedonia and it was rst established in 316 BC by Kassandros and named after his wife, Thessalonike, half-sister of Alexander the Great. The name Thessaloniki means "Thessalian Victory". It was the second most important city of the Byzantine Empire, next to Constantinople. Thessaloniki is a town with rich history and an exciting present.
    [Show full text]
  • Morphological and Sedimentological Characteristics of a Cuspate Foreland (Mytikas Epanomi, East Thessaloniki City, Greece)
    Morphological and sedimentological characteristics of a cuspate foreland (Mytikas Epanomi, east Thessaloniki city, Greece) S.G.Kirkou1,2, K.Almpanakis3, K.Vouvalidis3, P.Tsourlos2, G.Vargemezis 2 1Laboratory of Geophysical-Satellite Remote Sensing & Archaeo-environment, Institute for Mediterranean Studies, Foundation for Research & Technology-Hellas (F.O.R.T.H.), Rethymno, Crete 2Department of Geophysics, School of Geology, Aristotle University of Thessaloniki, sgkirkou@geo.auth.gr 3Department of Physical Geography and Environment, School of Geology, Aristotle University of Thessaloniki ABSTRACT Cuspate foreland is a geographical feature developed in a long shore drift or lakeshores. It is formed in a downwind area of an island or a coast, or at the end of a river where the conditions are appropriate by the incremental progress of sand and gravels in a triangle shape. The formation of the shape depends on the wave refraction and the deposition of sediments at the two sides of the triangle. Some cuspate forelands are flushed with floras which emigrated from the main land and they consist of many geomorphological features, like the lagoon and different types of dunes. Such kinds of ecosystems are sensitive to the human’s activity and nature. The subject of this research was the geological history and geomorphological characteristics of such a cuspate foreland. To this purpose, electric resistivity tomography (ERT) method was employed to map the vertical sequence of sediments in such an environment. The research was focused on a specific cuspate foreland at ‘Mytikas’ in Epanomi, close to Thessaloniki. The main purpose of the work was to map the surface sediments as well as the stratigraphy in depth and to record all the features that are developed on it and which contributed to the forming of this ecosystem.
    [Show full text]
  • Heteroptera: Belostomatidae) in Greece
    Ecologica Montenegrina 41: 56-61 (2021) This journal is available online at: www.biotaxa.org/em http://dx.doi.org/10.37828/em.2021.41.8 Further distributional records of Lethocerus patruelis (Stål, 1854) (Heteroptera: Belostomatidae) in Greece LEONIDAS-ROMANOS DAVRANOGLOU1 & IOANNIS KARAOUZAS2* 1 Department of Zoology, University of Oxford, OX1 3SZ, UK. E-mail: lrdreduvius@yahoo.gr 2Institute of Marine Biological Resources and Inland Waters, Hellenic Centre for Marine Research, Anavyssos, 19013, Attica, Greece. * Corresponding author: E-mail: ikarz@hcmr.gr Received 24 March 2021 │ Accepted by V. Pešić: 6 April 2021 │ Published online 11 April 2021. Abstract Although the Indo-Eastern Mediterranean giant water bug Lethocerus patruelis (Stål, 1854) is Europe’s largest hemipteran and aquatic insect, its distribution in Greece has remained poorly understood. Only a handful of records exists from the Ionian Islands, Macedonia, Thrace, and isolated observations in Preveza (Epirus), Achaia (north-western Peloponnese) and the islands of Rhodes and Thasos. Using records from personal observations, biomonitoring data, online arthropod identification groups and museum collections, we expand the distribution knowledge of this species to Aetolia-Acarnania, Thessaly, southern Peloponnese, Samothraki, North Sporades and the Cyclades. We also include a large number of new localities in areas within its previously known range. Key words: Lethocerinae; Nepomorpha; true bugs; aquatic insects; social networks; biogeography. Introduction Belostomatidae are the most charismatic of the true water bugs (Nepomorpha), due to their large size (up to 120 mm) and their voracious predatory habits, feeding on a wide range of invertebrates, fish, turtles, and even birds (Matheson 1907; Ribeiro et al.
    [Show full text]
  • GOVERNMENT GAZETTE Series B- 5922/31.12.2018
    69941 GREEK GOVERNMENT GAZETTE Series B- 5922/31.12.2018 TRUE COPY 69941 OF THE ORIGINAL DOCUMENT Greek Government Gazette December 31st 2018 SERIES B Issue No. 5922 Β' 464/19-4-2010). DECISIONS 9. The provisions of ministerial decision “Natural Gas Dec. No 1314/2018 Licensing Regulation” ref. no. 178065 (Government Gazette Β' 3430/17.08.2018, hereinafter referred to as For the granting of a Natural Gas Distribution “Licensing Regulation”). License to the company under the trade name 10. The Tariffs Regulation for the Main Distribution “Gas Distribution Company Thessaloniki- Activity of distribution networks in Attica, Thessaloniki, Thessaly S.A.” and the distinctive title “EDA Thessaly and other Greece (Government Gazette Β' THESS”. 3067/26.09.2016) (hereinafter referred to as “Tariffs Regulation”). THE REGULATORY AUTHORITY FOR ENERGY 11. The RAE's Decision No 346/2016 on the Approval Taking into consideration the following: of the Tariff for the Charge of the Main Natural Gas 1. The provisions of Law 4001/2011 “For the Distribution Activity on Thessaloniki distribution network operation of the Energy Markets of Electricity and (Government Gazette Β' 3490/31.10.2016). Natural Gas, for Research, Production and transmission 12. The RAE's Decision No 347/2016 on the Approval networks of Hydrocarbons and other arrangements” of the Tariff for the Charge of the Main Natural Gas (Government Gazette A’179/22.08.2011), as amended Distribution Activity on Thessaly distribution network and in force (hereinafter referred to as “the Law”), and (Government Gazette Β'3537/03.11.2016). especially articles 13 and 80C thereof.
    [Show full text]
  • New VERYMACEDONIA Pdf Guide
    CENTRAL CENTRAL ΜΑCEDONIA the trip of your life ΜΑCEDONIA the trip of your life CAΝ YOU MISS CAΝ THIS? YOU MISS THIS? #can_you_miss_this REGION OF CENTRAL MACEDONIA ISBN: 978-618-84070-0-8 ΤΗΕSSALΟΝΙΚΙ • SERRES • ΙΜΑΤΗΙΑ • PELLA • PIERIA • HALKIDIKI • KILKIS ΕΣ. ΑΥΤΙ ΕΞΩΦΥΛΛΟ ΟΠΙΣΘΟΦΥΛΛΟ ΕΣ. ΑΥΤΙ ΜΕ ΚΟΛΛΗΜΑ ΘΕΣΗ ΓΙΑ ΧΑΡΤΗ European emergency MUSEUMS PELLA KTEL Bus Station of Litochoro KTEL Bus Station Thermal Baths of Sidirokastro number: 112 Archaeological Museum HOSPITALS - HEALTH CENTERS 23520 81271 of Thessaloniki 23230 22422 of Polygyros General Hospital of Edessa Urban KTEL of Katerini 2310 595432 Thermal Baths of Agkistro 23710 22148 23813 50100 23510 37600, 23510 46800 KTEL Bus Station of Veria 23230 41296, 23230 41420 HALKIDIKI Folkloric Museum of Arnea General Hospital of Giannitsa Taxi Station of Katerini 23310 22342 Ski Center Lailia HOSPITALS - HEALTH CENTERS 6944 321933 23823 50200 23510 21222, 23510 31222 KTEL Bus Station of Naoussa 23210 58783, 6941 598880 General Hospital of Polygyros Folkloric Museum of Afytos Health Center of Krya Vrissi Port Authority/ C’ Section 23320 22223 Serres Motorway Station 23413 51400 23740 91239 23823 51100 of Skala, Katerini KTEL Bus Station of Alexandria 23210 52592 Health Center of N. Moudania USEFUL Folkloric Museum of Nikiti Health Center of Aridea 23510 61209 23330 23312 Mountain Shelter EOS Nigrita 23733 50000 23750 81410 23843 50000 Port Authority/ D’ Section Taxi Station of Veria 23210 62400 Health Center of Kassandria PHONE Anthropological Museum Health Center of Arnissa of Platamonas 23310 62555 EOS of Serres 23743 50000 of Petralona 23813 51000 23520 41366 Taxi Station of Naoussa 23210 53790 Health Center of N.
    [Show full text]
  • About Thessaloniki
    INFORMATION ON THESSALONIKI Thessaloniki is one of the oldest cities in Europe and the second largest city in Greece. It was founded in 315 B.C. by Cassander, King of Macedonia and was named after his wife Thessaloniki, sister of Alexander the Great. Today Thessaloniki is considered to be one of the most important trade and communication centers in the Mediterranean. This is evident from its financial and commercial activities as well as its geographical position and its infrastructure. As a historic city Thessaloniki is well – known from its White Tower dating from the middle of the 15th century in its present form. Thessaloniki presents a series of monuments from Roman and Byzantine times. It is known for its museums, Archaeological and Byzantine as well as for its Art, Historical and War museums and Galleries. Also, it is known for its Churches, particularly the church of Agia Sophia and the church of Aghios Dimitrios, the patron Saint of the city. Thessaloniki’s infrastructure, which includes the Universities campus, the International trade, its port and airport as well as its road rail network, increases the city’s reputation; it is also famous for its entertainment, attractions, gastronomy, shopping and even more. A place that becomes a vacation resort for many citizens of Thessaloniki especially in the summer and only 45 minutes away is Chalkidiki. Chalkidiki is a beautiful place, which combines the sea with the mountain. Today, Chalkidiki is a summer resort for the people of Thessaloniki. It is really a gifted place due to its natural resources, its crystal waters and also the graphical as well as traditional villages.
    [Show full text]
  • Granular Aquifer System of West Chalkidiki Area, Region of Central Macedonia, Northern Greece
    Bulletin of the Geological Society of Greece Vol. 50, 2016 GRANULAR AQUIFER SYSTEM OF WEST CHALKIDIKI AREA, REGION OF CENTRAL MACEDONIA, NORTHERN GREECE Veranis N. Nimfopoulos M. Christidis C. Chrysafi A. https://doi.org/10.12681/bgsg.11806 Copyright © 2017 N. Veranis, M. Nimfopoulos, C. Christidis, A. Chrysafi To cite this article: Veranis, N., Nimfopoulos, M., Christidis, C., & Chrysafi, A. (2016). GRANULAR AQUIFER SYSTEM OF WEST CHALKIDIKI AREA, REGION OF CENTRAL MACEDONIA, NORTHERN GREECE. Bulletin of the Geological Society of Greece, 50(2), 1016-1026. doi:https://doi.org/10.12681/bgsg.11806 http://epublishing.ekt.gr | e-Publisher: EKT | Downloaded at 07/10/2020 09:11:15 | Δελτίο της Ελληνικής Γεωλογικής Εταιρίας, τόμος L, σελ. 1016-1026 Bulletin of the Geological Society of Greece, vol. L, p. 1016-1026 Πρακτικά 14ου Διεθνούς Συνεδρίου, Θεσσαλονίκη, Μάιος 2016 Proceedings of the 14th International Congress, Thessaloniki, May 2016 GRANULAR AQUIFER SYSTEM OF WEST CHALKIDIKI AREA, REGION OF CENTRAL MACEDONIA, NORTHERN GREECE Veranis N.1, Nimfopoulos M.2, Christidis C.3 and Chrysafi A.4 1Hydrogeologist, 39 Perraivou st., 543 52, Thessaloniki, Greece, nikosveranis@gmail.com 2Environmental Geochemist, IGME, 1 Fragon street, 546 26 Thessaloniki, mnimfo@thes.igme.gr 3MSc Geologist, christidisc@hotmail.com 4MSc Geologist, alexchrysafi@hotmail.com Abstract The granular aquifer system of the western Chalkidiki peninsula covers an area of 667 Km2 occupying Neogene and Quaternary sediments. The present study deals with the hydrogeological and hydrogeochemical characterization of the granular aquifer system for the purposes of efficient utilization and management of groundwater resources. It is a multilayered formation, composed of unconsolidated to semi-consolidated sands, gravels, conglomerates, sandstones and marly limestones with intercalated impermeable to semi-permeable beds of clays, marls or mixed with pebbles and sands.
    [Show full text]
  • Hydrogeological Regime and Groundwater Occurence in the Anthemountas River Basin, Northern Greece
    Bulletin of the Geological Society of Greece, vol. XLVII 2013 Δελτίο της Ελληνικής Γεωλογικής Εταιρίας, τομ. XLVII , 2013 Proceedings of the 13th International Congress, Chania, Sept. Πρακτικά 13ου Διεθνούς Συνεδρίου, Χανιά, Σεπτ. 2013 2013 HYDROGEOLOGICAL REGIME AND GROUNDWATER OCCURENCE IN THE ANTHEMOUNTAS RIVER BASIN, NORTHERN GREECE Kazakis N.1, Voudouris K.1, Vargemezis G.2 and Pavlou A.1 1Laboratory of Engineering Geology & Hydrogeology, Department of Geology, Aristolte University of Thessaloniki, Greece. 2Laboratory of Applied Geophysics Department of Geology Aristotle University of Thessaloniki, Greece. Abstract The Anthemountas river basin is located in northern Greece and covers an area of 374 km2. The mountainous part of the basin consists of ophiolitic, crystalline and carbonate rocks, whereas the lowlands comprise Neogene and Quaternary sedi- ments. Porous aquifers are developed in neogene and quaternary deposits of con- fined and/or unconfined conditions. Karstic aquifers are developed in the carbonate rocks and there are aquifers in the Mesozoic and Palaeozoic fissured rocks. The wa- ter demands of the basin are mainly met by the exploitation of the porous aquifers through a large number of boreholes (more than 1000). The aquifers of fissured rocks discharge through cold springs without significant flow rate. Thermal hot springs are recorded across the Anthemountas fault discharging a mixture of geo- thermal fluids and cold water from the karst aquifer. According to their hydrogeo- logical and lithological characteristics, porous aquifers can be divided into the sub- systems of Galatista and Galarinos in the eastern part of the Anthemountas basin, Vasilika-Risio-Thermi and Tagardes-Trilofos in the western part and Peraia-Agia Triada and AUTh farm-Makedonia airport in the coastal area.
    [Show full text]
  • GONIDA Address(Es) P.O
    Europass Curriculum Vitae Personal information First name(s) / Surname(s) Sofia-Eleftheria GONIDA Address(es) P.O. Box: 4510, GR-575 00 Epanomi, Greece Telephone(s) +30 2310997309 (office) Fax(es) +30 2310997332 E-mail gonida@psy.auth.gr Nationality Hellenic Date of birth August 18, 1966 Gender Female Work experience Dates Since April 15, 2019 Occupation or position held Professor of Educational Psychology and Human Development / Vice Chair of the School of Psychology Main activities and responsibilities Teaching, research, administrative duties Name and address of employer Same as below Dates August 30, 2011 – April 14 2019 Occupation or position held Associate Professor of Educational Psychology and Human Development Main activities and responsibilities Teaching, research, administrative duties Name and address of employer Department of Developmental and School Psychology, School of Psychology, Faculty of Philosophy, Aristotle University of Thessaloniki, GR- 541 24 Thessaloniki, Greece. Dates August 30, 2006 – August 25, 2011 Occupation or position held Assistant Professor of Educational Psychology and Human Development Main activities and responsibilities Teaching, research, administrative duties Name and address of employer Department of Developmental and School Psychology, School of Psychology, Faculty of Philosophy, Aristotle University of Thessaloniki, GR- 541 24 Thessaloniki, Greece. Dates June 14, 2001 - August 30, 2006 Occupation or position held Lecturer Main activities and responsibilities Teaching and research Name and address
    [Show full text]
  • Exploration History and Hydrocarbon Potential of Greece
    IENE workshop 26-27April 2012 ExplorationExploration historyhistory andand HydrocarbonHydrocarbon PotentialPotential ofof GreeceGreece G. Zafiropoulos Exploration Manager Hellenic Petroleum S.A. Exploration and Production of Hydrocarbons 1 Topics Historical background • Exploration before 1975 • Exploration from1975 to 2000 • 1st International Exploration Round 1997-2002 Petroleum system in Greece Review by area • Epirus-Aitoloakarnania • NW Peloponessos • Grevena basin • W. Thrace, Orestiada & Evros Delta • Crete, Messara basin & Libyan sea • Ionian sea and Ionian islands • Thessaloniki basin - Epanomi area -Thermaikos gulf • North Aegean sea - Thracian sea • Hellenic Trench - Mediterranean Ridge Conclusions 2 HistoricalHistorical backgroundbackground 3 Greek Sedimentary Basins Eastern Greece: Exploration of the neogene basins Western Greece: Exploration in the overthrusted zone of the external Hellenides and on the foreland. 4 Exploration activity before 1975 • Concessions were awarded to various, some majors, Oil Companies (ESSO, TEXACO, BP, Oceanic etc) • Acquisition of about 12,200 Km of seismic lines • 68 well were drilled with TD varying from a few meters to 4,573m • Discovery of the Prinos oil field and the South Kavala gas field. • Significant hydrocarbon shows in many wells (Aitoliko, Zakynthos, Thermaikos etc) • Some of the of the findings of the deep wells contributed to the overall knowledge of the stratigraphy and the tectonics of Greece 5 Exploration by DEP/DEP-EKY/HELPE (1/3) • 6 fully owned and operated seismic crews (3 dynamite, 2 Vibroseis, 1 shallow water telemetric) as well as subcontractors for offshore or onshore seismic acquisition. • Gravity/magnetic crew. • Integrated center for processing and interpretation of seismic data. • Drilling ring (capacity for drilling down to 4.000 m). • 2 Geological laboratories for evaluation of the results while drilling.
    [Show full text]
  • The Importance of Incorporating Denitrification in The
    applied sciences Article The Importance of Incorporating Denitrification in the Assessment of Groundwater Vulnerability Gianluigi Busico 1,2 , Nerantzis Kazakis 2,* , Nicolò Colombani 3 , Khabat Khosravi 4, Konstantinos Voudouris 2 and Micòl Mastrocicco 1 1 Department of Environmental, Biological and Pharmaceutical Sciences and Technologies, University of Campania “Luigi Vanvitelli”, Via Vivaldi 43, 81100 Caserta, Italy; gianluigi.busico@unicampania.it (G.B.); micol.mastrocicco@unicampania.it (M.M.) 2 Department of Geology, Lab. of Engineering Geology & Hydrogeology, Aristotle University of Thessaloniki, 54124 Thessaloniki, Greece; kvoudour@geo.auth.gr 3 Department of Materials, Environmental Sciences and Urban Planning “SIMAU”, Polytechnic University of Marche, via Brecce Bianche 12, 60131 Ancona, Italy; n.colombani@univpm.it 4 School of Engineering, University of Guelph, ON N1G 2W1, Canada; kkhosrav@uoguelph.ca * Correspondence: kazakis@geo.auth.gr; Tel.: +306942411653 Received: 27 February 2020; Accepted: 26 March 2020; Published: 28 March 2020 Abstract: Human activities are deeply connected with groundwater reservoirs, so protecting them from pollution has become a priority in many regions of the world. Nitrate is considered the main groundwater pollutant since it is directly linked to many human activities. Agricultural activities and domestic wastewater have been identified as the main sources of nitrate in groundwater. Nevertheless, there are some natural processes that can mitigate nitrate pollution. Together with dilution processes,
    [Show full text]
  • State of Play Analyses for Thessaloniki, Greece
    State of play analyses for Thessaloniki, Greece Contents Socio-economic characterization of the region ................................................................ 2 Hydrological data .................................................................................................................... 20 Regulatory and institutional framework ......................................................................... 23 Legal framework ...................................................................................................................... 25 Applicable regulations ........................................................................................................... 1 Administrative requirements ................................................................................................ 6 Monitoring and control requirements .................................................................................. 7 Identification of key actors .............................................................................................. 14 Existing situation of wastewater treatment and agriculture .......................................... 23 Characterization of wastewater treatment sector: ................................................................ 23 Characterization of agricultural sector: .................................................................................. 27 Existing related initiatives ................................................................................................ 38 Discussions
    [Show full text]