Deepwater-Ce Workpackage T3, Activity T3.5
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Danubian Lowland - Ground Water Mode
SK98K0043 Ministry of the Environment, Slovak Republic Commission of The European Communities DANUBIAN LOWLAND - GROUND WATER MODE PHARE PROJECT NO. PHARE/EC/WAT/1 The Old Danube Final Report Volume 1 Summary Report December 1995 Danish Hydraulic Institute, Denmark in association with DHV Consultants BV, The Netherlands TNO - Institute of Applied Geoscience, The Netherlands Water Quality Institute, Denmark I Kriiger, Denmark The Royal Veterinary and Agricultural University, Denmark Danish Hydraulic Institute Danubian Lowland - Ground Water Model Agern Alle 5, DK-2970 Harsholm, Denmark PHARE/EC/WAT/1 Telephone: +45 45 76 95 55 Final Report Telefax: +45 45 76 25 67 Telex: 37 402 dhicph dk Client Client's representative Ministry of the Environment, Programme Implementation F. Kelbel, Director, PIU Unit, Slovak Republic Project Project No Danubian Lowland - Ground Water Model 92-6828 Authors Date Jens Chr. Refsgaard, DHI December 1 995 Henrik R. Sarensen, DHI DHV-Consultants BV, NL TNO-lnstitute of Applied Geoscience, NL Water Quality Institute (VKI), DK 1. Kriiger Consultant AS, DK Approved by Royal Veterinary and Agricultural University, DK VUVH - Water Resources Research Institute, SK Jens Chr. Refsgaard VU2H - Research Institute of Irrigation, SK /J^0) ecL T eanvpSad e r GWC - Ground Water Consulting Ltd., SK Comenius University, SK t 1 Final Report an 0 Draft Final Report Revision Description By Checked App. Date Key words Classification Danube, integrated modelling, water resources management, • Open numerical modelling, model development, river and reservoir, ground water, unsaturated zone, agriculture, sediment • Internal transport, ground water quality, surface water quality, ecology, geographical information system, field Ix! Proprietary investigations, equipment. -
Seismic and Geological Conditions at the Bohunice Npp Site
XA9952599 SEISMIC AND GEOLOGICAL CONDITIONS AT THE BOHUNICE NPP SITE Emilia Juhasova, Dr., Ing., DrSc. Institute of Construction and Architecture, SAS Dubravska cesta 9, 842 20 Bratislava, SLOVAKIA ABSTRACT The paper brings basic information on geological and seismic characteristics of the site of NPP Jaslovske Bohunice, Slovakia. Western Carpathians and Trnava bay geological properties are briefly introduced. The most important macroseismic data and data obtained from field measurements are analysed. Main features of the expected strong seismic motion are discussed. The attention is devoted to local soil characteristics just under the site of NPP. 1. INTRODUCTION The NPP VI, V2, EBO is located in north-west part of Danubian basin - so called Trnava bay, that is nearly 10 km in south-east direction from the mountains of Small Carpathians and in west direction from the Vali river valley. The Trnava bay territory belongs to the best geologically investigated parts of Slovakia. Many deep boreholes were realised here, together with all supporting seismological investigations. This is connected with prospector works and also with construction of important structures as dams, plants, factories, etc. The mentioned territory of EBO was the subject of intensive geological and seismological investigations during the last decade, v The complex synthesising work of all those investigations was done in the closing document of Institute of the Earth Physics AS in Moscow and C-S Institutes [4]. Due to recommendations of [4] the measurements of the seismic activity of near field of NPP were realised by the help of the very sensitive seismic station network. Thanks to obtained data we have nowadays new useful information about the site behaviour and in this way we can do the additional analyses of the safety degree and the measure of upgrading of NPP structures and technologies. -
Potential and Central Forms of Tourism in 21 Regions of Slovakia
Potential and Central Forms of Tourism in 21 Regions of Slovakia Importance and development priorities of regions The following previews list short characteristics of individual regions in terms of their current state, development possibilities and specific needs. The previews include a list of the most important destinations in the individual regions, the infrastructure that needs to be completed and the anticipated environmental impacts on tourism in the region. These lists are not entirely comprehensive and only include the main elements that create the character of the region as a tourist destination. 1. Bratislava Region Category / relevance Medium-term perspective International Long-term perspective International Sub-region, specific Medium-term perspective - Small Carpathians sub-region (viniculture) location - Bratislava - Senec Long-term perspective - Strip along the right bank of the Danube Type of tourism Long-term incoming foreign tourism over 50%; intensive domestic tourism as well Stay tourism – short-term in incoming as well as in domestic tourism Long–stay waterside tourism only in the summer time; one-day visits – domestic as well as foreign tourism. Transit Forms of tourism - Sightseeing tourism - Business tourism - Summer waterside stays Activities with the - Discovering cultural heritage – Business tourism - Congress/conference tourism – highest long-term Visiting cultural and sport events – Stays/recreation near water – Water sports – Boat potential sports and water tourism - Cycle tourism Position on the Slovak Number -
Meeting Report
PROCEEDINGS of the 2nd Meeting on the Follow-up of the Joint Statement on Inland Navigation and Environmental Sustainability in the Danube River Basin Zagreb, March 9-10, 2010 INTRODUCTION Background The ICPDR (International Commission for the Protection of the Danube River), the ISRBC (International Sava River Basin Commission) and the DC (Danube Commission) have jointly launched the process to develop the Joint Statement (JS) on Guiding Principles on the Development of Inland Navigation and Environmental Protection in the Danube River Basin (Joint Statement) . After a year-long process preparing the document, and its adoption by the three river commissions in December 2007 and January 2008, the Joint Statement was publicly announced in March 2008. In accordance with the Joint Statement, the ICPDR, Danube Commission, and International Sava River Basin Commission, including relevant stakeholders, shall meet yearly to discuss specific navigational and environmental developments and to highlight good practices in river maintenance projects. The first meeting was held on January 29-30, 2009, in Budapest in the seat of the Danube Commission and on this meeting it was agreed that the second meeting will be held in 2010 in Zagreb. Organization and objectives The meeting was organized by ISRBC together with ICPDR on March 9-10, 2010, in Zagreb. The objectives of the meeting were to: • inform about progress on the implementation of the Joint Statement on Inland Navigation and Environmental Sustainability in the Danube River Basin, • discuss the further development and application of the Joint Statement and its implications (regular information exchange), • inform and discuss new facts and perspectives of European inland waterway transport, • inform and discuss the current state of legal and policy frameworks of integrated river basin management and environmental protection, • inform about the state of IWT projects in the Danube basin. -
D4 Ivanka North – Raca Announcement of Change
Highway D4 Bratislava Ivanka North - Rača TABLE OF CONTENTS I. DATA ON PROPOSER.................................................................................................................. 3 I.1. Name ...................................................................................................................................... 3 I.2. Identification Number .............................................................................................................. 3 I.3. Seat ......................................................................................................................................... 3 I.4. Contact Data of the Proposer's Authorised Representative ................................................... 3 I.5. Contact Data of the Person Authorised to Provide Relevant Information on the Proposed Works and Place of Consultations: ..................................................................................................... 3 II. NAME OF THE CHANGE TO THE PROPOSED WORKS ........................................................... 3 III. DATA OF CHANGE TO THE PROPOSED WORKS .................................................................... 3 III.1 Location of the Proposed Works ............................................................................................ 3 III.2 Description of the Technical and Technological Solution .......................................................... 4 III.3 Connection with other planned and performed activities in the territory concerned ............ 12 III.4 -
Discover Europe. Discover Centrope
centrope region centrope partners Austria • Federal Province of Burgenland [email protected] Brno • Federal Province of Lower Austria www.centrope.com • Federal Province and City of Vienna • City of Eisenstadt Jižní Morava • City of St.Pölten Czech Republic • South Moravian Region • City of Brno Trnava • Vysočina Region (observer) Niederösterreich Trnava Hungary Bratislava • Győr-Moson-Sopron County St. Pölten Wien Bratislava • Vas County • City of Győr • City of Sopron • City of Szombathely Eisenstadt Legal notice: Slovakia Published by the centrope agency on behalf Sopron Győr • Bratislava Self-Governing Region of the centrope capacity partnership. Győr-Moson-Sopron • Trnava Self-Governing Region • City of Bratislava Design&Layout: • City of Trnava www.TOPVISION.sk Burgenland Supported by funds of the European Pictures: Szombathely Union, CENTRAL EUROPE programme centrope agency Vas discover europe discover centrope discover europe discover centrope The Czech Republic, Hungary, Austria and Slovakia are four countries that make up the heart of Europe. A shared history has naturally brought them together in the Central European region - centrope, which is incredibly varied and full of contrasts. The beautiful natural environment in the region’s national parks is combined with a wealth of rivers, lakes and thermal springs, as well as vast, sun-kissed vineyards, orchards and fields of sunflowers. This natural environment allows for leisure activities and family outings. As you walk through the centrope region, the common history of the old noble families who left behind magnificent mansions and castles - now used as unique cultural centres - oozes out with every step. Culture comes alive in all the region’s cities. Throughout the year you will find a wide range of cultural events, modern art and folk traditions. -
Pišút, P.1 – Falťan, V.1 – Chovanec, P.1 – Petrovič, F.3
Horáčková et al.: Historical changes and vegetation development after intensive peat extraction in the lowland mires of Slovakia - 5025 - HISTORICAL CHANGES AND VEGETATION DEVELOPMENT AFTER INTENSIVE PEAT EXTRACTION IN THE LOWLAND MIRES OF SLOVAKIA HORÁČKOVÁ, Š.1,2* – PIŠÚT, P.1 – FALŤAN, V.1 – CHOVANEC, P.1 – PETROVIČ, F.3 1Department of Physical Geography and Geoecology, Faculty of Natural Sciences, Comenius University in Bratislava, Ilkovičova 6, 84215 Bratislava 4, Slovakia (e-mails: [email protected], [email protected], [email protected]) 2Geographical Institute, Slovak Academy of Sciences Štefánikova 49, 81473 Bratislava, Slovakia 3Department of Ecology and Environmental Sciences, Faculty of Natural Sciences, Constantine the Philosopher University in Nitra, Trieda A. Hlinku 1, 94974 Nitra, Slovakia (e-mail: [email protected]) *Corresponding author e-mail: [email protected] (Received 10th May 2018; accepted 5th Jul 2018) Abstract. Mires in the Danubian Lowland (Northern part of the Pannonian Basin) are typically overgrown with common alder (Alnus glutinosa). Similar stands at this location are unfortunately very rare, what is caused by continuous human intervention in landscape and its natural pattern from Early Holocene. Peatland degradation near Pusté Úľany village started in the mid - eighteenth century, what is supported by historical maps. In the previous century a huge peat extraction took place at this specific mire. Despite these anthropogenic changes, there are still some remnants of natural habitats present, mostly dependant on ground water level. Methodology includes historical map’s analysis, digital terrain model and vegetation cover mapping. Actual map of biotopes was completed for the current state of the vegetation cover acquaintance. -
Diagnosis of the Impact of the Gabčíkovo Water Project on Soil Water Regime in the Surroundings
DOI: 10.1515/ahr-2014-0012 Miroslava JARABICOVÁ et al. Acta horticulturae et regiotecturae 2/2014 Acta horticulturae et regiotecturae 2 Nitra, Slovaca Universitas Agriculturae Nitriae, 2014, p. 48–51 DIAGNOSIS OF THE IMPACT OF THE GABČÍKOVO WATER PROJECT ON SOIL WATER REGIME IN THE SURROUNDINGS Miroslava JARABICOVÁ, Mária PÁSZTOROVÁ, Justína VITKOVÁ, Peter MINARIČ* Slovak University of Technology in Bratislava, Slovak Republic Rye Island is a unique natural formation, which lies between the main flow of the Danube River and the Little Danube River and is the largest river island in Europe. It is located in the southwest of Slovakia and with its mild to slightly warm climate is one of the most fertile agricultural areas in Slovakia. The whole Rye Island is also our greatest reservoir of quality waters used for drinking purposes, where groundwaters of Rye Island are permanently supplied with water from the Danube River. It means that as water levels in the Danube River were unstable before the construction of the Gabčíkovo Water Project, also the groundwater level faced large fluctuations. Changes occurred after putting the Gabčíkovo Water Project into service, with a decrease in groundwater levels. Thereby, the conditions for agriculture have improved and drying of surrounding protected floodplain forests has stopped. Through the present contribution we decided to analyse the impact of Gabčíkovo on soil water regime in the area of Rye Island, and evaluate the course of groundwater level, precipitation and soil water storage over time. For the representative area we chose a forest ecosystem of Kráľovská Lúka and evaluated the period 1999 to 2009. -
Slovak Hydronymy in the European Context Juraj Hladký University of Trnava (Slovakia) [email protected]
ONOMÀSTICA 5 (2019): 137–156 | RECEPCIÓ 12.3.2019 | ACCEPTACIÓ 10.12.2019 Slovak hydronymy in the European context Juraj Hladký University of Trnava (Slovakia) [email protected] Abstract: Historical Slavic toponymy is the sole basis for understanding the development of Slavic macrodialects and the formation of Slavic languages, including Slovak. In this respect, hydronymic lexis contributes significantly to views on developments in vocabulary. The oldest hydronyms in Slovakia are probably of pre-Slavic (Quadi, Celtic or Roman) origin (for example, the Hron, the Váh, the Nitra rivers and others). The older pre-Slavic-Slovak hydronymy provides evidence of the differentiation of dialects in the earlier periods (until the 10th–12th century). The younger Slovak hydronymic inventory is supplemented by Slovak-adapted foreign hydronyms (mainly of German and Hungarian origin). They reflect the degree of historical inter-lingual contacts in the regions of Slovakia and complete the diachronous-synchronous view of Slovak lexis. The study describes the tradition and outlines the results of hydronomastic studies in Slovakia and the relatively comprehensive characterization of Slovak hydronymy undertaken by the Hydronymia Slovaciae project. In line with the methodology employed by the Hydronymia Europaea project, all documented hydronyms have been systematically processed in individual river basins, from the oldest to the most recent. The analysis of the complex corpus of both existing and extinct hydronyms, in addition to its recognised linguistic (lexical-semantic, structural-typological characteristics, motivation) goals, has served in the reconstruction of the original non-linguistic side of the proper names, their standardization and cartography, etc. Thanks to methodologically similar hydronomastic research in other Slavic countries, the results of the studies in Slovakia can be applied in a broader Slavic context. -
Metropolitan Region on the Danube Content
Metropolitan Region on the Danube Content Content ........................................................................................................................................................................... 1 Foreword ........................................................................................................................................................................ 2 About Slovakia ........................................................................................................................................................... 3 Bratislava Region ...................................................................................................................................................... 4 International Context ............................................................................................................................................ 5 Population .................................................................................................................................................................... 6 Transport and Accessibility ................................................................................................................................ 7 Economy ....................................................................................................................................................................... 9 Tourism and Culture ........................................................................................................................................... -
Precipitation Regime and Temporal Changes in the Central Danubian Lowland Region
Hindawi Publishing Corporation Advances in Meteorology Volume 2015, Article ID 715830, 12 pages http://dx.doi.org/10.1155/2015/715830 Research Article Precipitation Regime and Temporal Changes in the Central Danubian Lowland Region Dana Halmova,1 Pavla Pekarova,1 Juraj Olbrimek,2 Pavol Miklanek,1 and Jan Pekar3 1 Institute of Hydrology, Slovak Academy of Sciences, Racianska 75, 83102 Bratislava, Slovakia 2Faculty of Civil Engineering, Slovak University of Technology in Bratislava, Radlinskeho 11, 81368 Bratislava, Slovakia 3Department of Applied Mathematics and Statistics, Faculty of Mathematics, Physics and Informatics, Comenius University, 84248 Bratislava, Slovakia Correspondence should be addressed to Dana Halmova; [email protected] Received 11 April 2014; Revised 13 July 2014; Accepted 28 August 2014 Academic Editor: Francisco J. Tapiador Copyright © 2015 Dana Halmova et al. This is an open access article distributed under the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited. The aim of this paper is to investigate the statistical aspects of multiannual variability of precipitation at the Hurbanovo station, Slovakia, over 140 years (1872–2011). We compare the long-term variability of annual precipitation for Hurbanovo (Slovakia), Brno (Czech Republic), Vienna (Austria), and Mosonmagyarovar (Hungary) stations using autocorrelation and spectral analysis methods. From the long-term point of view, there is no consistent trend in the annual precipitation; only a multiannual variability has been detected. Consequently we identify changes in the distribution of annual maximum daily precipitation for Hurbanovo during different periods for winter-spring and summer-autumn seasons using histograms, empirical exceedance curves, and frequency curves of daily precipitation. -
Bratislava Region in a Nutshell
22 Veľké Plavecké 23 Leváre Podhradie 24 21 Malacky Kuchyňa 15 Častá Záhorská Ves 14 13 Dubová Angern Pernek 16 Podunajsko 12 Modra Part of the Danubian Lowland belonging to Bratislava Region consists Morava 11 of villages in the Senec district. Th is fl at agricultural landscape sur- 18 19 Pezinok 25 17 Borinka rounded by the Danube and its tributary the Little Danube with many Stupava Slovenský Mariánka Grob gravel pits creates favourable conditions for summer relaxation by the 20 10 Svätý Jur water and in the vicinity of bodies of water. Its centre is the town of Senec 7 26 Senec where you can fi nd a popular summer destination for locals and BRATISLAVA foreigners alike – Sunny Lakes, in addition to a water park with well- AT 5 28 ness. Th e rivers fl owing through the region and the bodies of water are 4 27 Devín 3 1 30 a suitable place for fi shing and water sports. Th e most visited European Malý Dunaj cycling route – EuroVelo 6 – leads along the bank of the Danube. Along 2 with the other cycling routes in the region, it is suitable for families 6 Miloslavov with children and recreational cyclists. Dunaj Legenda: 29 Camping Dunajská Castle, manor house Ferry 8 Lužná Places to visit: 26. Sunny Lakes Castle ruin HU Čunovo Cycling bridge 9 26. Aquapark Senec Religious monument Lookout tower 27. Oasis of the Siberian Tiger Traditional ceramics Airport 28. Open-Air Museum of Bee Keeping Mushroom 29. Courtyard of Artisanal Crafts Miloslavov Wine-growing area picking area 30.