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Strategie Pentru Tranziția De La Cărbune În Valea Jiului Analiza Principalelor Provocări Și Oportunități Din Valea Jiului
1/5/2020 Strategie pentru tranziția de la cărbune în Valea Jiului Analiza principalelor provocări și oportunități din Valea Jiului Material tradus după documentul PwC în limba engleză, prin grija Ministerului Fondurilor Europene Prefață Proiectul „Strategie pentru tranziția de la cărbune în Valea Jiului” este finanțat de Comisia Europeană prin Programul de Sprijin pentru Reforme Structurale (DG-REFORM) și implementat în colaborare cu PricewaterhouseCoopers în baza Contractului cu numărul SRSS/SC2019/119, încheiat între PricewaterhouseCoopers EU Services EESV și Programul de Sprijin pentru Reforme Structurale (DG REFORM – Clientul) al Comisiei Europene, semnat la data de 23 octombrie 2019, având drept Beneficiar Ministerul Fondurilor Europene (MFE). Raportul de față a fost întocmit de PricewaterhouseCoopers Management Consultants SRL (în cele ce urmează „PwC”). Acesta reprezintă al treilea livrabil și a fost redactat cu scopul de a prezenta provocările și oportunitățile actuale din Valea Jiului, care acoperă dimensiunile politice și administrative, economică, sociale și culturale, tehnologice și de mediu. În identificarea și fundamentarea provocărilor și oportunităților, au fost utilizate surse publice de informații, precum și informații obținute în interviurile realizate de PwC cu părțile interesate în perioada ianuarie-februarie 2020 în Valea Jiului. Sursele de date și de informații sunt indicate atât sub grafice, scheme și tabele, cât și în notele de subsol. Informațiile utilizate au fost considerate corecte și de încredere, și nu au fost verificate separat de noi. Orice persoană care nu este destinatarul acestui raport sau care nu a semnat și returnat către PricewaterhouseCoopers Management Consultants SRL o scrisoare de acceptare a termenilor PwC privind furnizarea de informații („Release Letter”) nu este autorizată să aibă acces la acest raport. -
Climatic Implications of Cirque Distribution in the Romanian Carpathians: Palaeowind Directions During Glacial Periods
JOURNAL OF QUATERNARY SCIENCE (2010) Copyright ß 2010 John Wiley & Sons, Ltd. Published online in Wiley InterScience (www.interscience.wiley.com) DOI: 10.1002/jqs.1363 Climatic implications of cirque distribution in the Romanian Carpathians: palaeowind directions during glacial periods MARCEL MIˆNDRESCU,1 IAN S. EVANS2* and NICHOLAS J. COX2 1 Department of Geography, University of Suceava, Suceava, Romania 2 Department of Geography, Durham University, Durham, UK Mıˆndrescu, M., Evans, I. S. and Cox, N. J. Climatic implications of cirque distribution in the Romanian Carpathians: palaeowind directions during glacial periods. J. Quaternary Sci., (2010). ISSN 0267-8179. Received 10 May 2009; Revised 23 October 2009; Accepted 2 November 2009 ABSTRACT: The many glacial cirques in the mountains of Romania indicate the distribution of former glacier sources, related to former climates as well as to topography. In the Transylvanian Alps (Southern Carpathians) cirque floors rise eastward at 0.714 m kmÀ1, and cirque aspects tend ENE, confirming the importance of winds from some westerly direction. There is a contrast between two neighbouring ranges: the Fa˘ga˘ras¸, where the favoured aspect of cirques is ENE, and the Iezer, where the tendency is stronger and to NNE. This can be explained by the Iezer Mountains being sheltered by the Fa˘ga˘ras¸, which implies precipitation-bearing winds from north of west at times of mountain glaciation. Palaeoglaciation levels also suggest winds from north of west, which is consistent with aeolian evidence from Pleistocene dunes, yardangs and loess features in the plains of Hungary and south- western Romania. In northern Romania (including Ukrainian Maramures¸) the influence of west winds was important, but sufficient only to give a northeastward tendency in cirque aspects. -
Uricani Monografie Turistică
Uricani Monografie turistică URICANI 2021 Cuprins 1. Considerații generale …………………………………………..…pag. 3 1.1. Prezentarea cadrului de analiză .................................................................. pag.4 Scurt istoric ............................................................................................................... pag. 9 Generalități .............................................................................................................. pag. 13 Căile de acces .......................................................................................................... pag. 15 Infrastructura edilitară .......................................................................................... pag. 17 Cadrul natural ........................................................................................................ pag. 22 Cadrul socio – economic ....................................................................................... pag. 28 Probleme de mediu și factori de risc .................................................................... pag. 34 2. Analiza potențialului turistic ………………………….………. pag. 43 2.1. Turism montan pedestru ……………………………………………….. pag. 43 2.1.1. Munții Retezat ………………………………………………......pag. 43 2.1.2. Munții Vâlcan …………………………………………………. pag. 46 2.1.3. Munții Tulișa …………………………………………..……… pag. 49 2.1.4. Munții Retezatul Mic sau Calcaros …………………………… pag. 51 2.2. Trasee turistice montane ……………………………………………….. pag. 52 2.3. Silvoterapia …………………………………………………………….. ..pag. 62 2.4. Fitoterapia locală -
Geosciences in the 21 Century______
GEOSCIENCES IN THE 21st CENTURY Symposium dedicated to the 80th anniversary of professor Emil Constantinescu EXTENDED ABSTRACTS EDITORS Antoneta Seghedi, Gheorghe Ilinca, Victor Mocanu GeoEcoMar Bucharest, 2019 Organizatori: Sponsorul volumului: GEOSCIENCES IN THE 21ST CENTURY Symposium dedicated to the 80th anniversary of Professor Emil Constantinescu EXTENDED ABSTRACTS EDITORS Antoneta Seghedi, Gheorghe Ilinca, Victor Mocanu GeoEcoMar Bucharest 2019 NATIONAL INSTITUTE OF MARINE GEOLOGY AND GEOECOLOGY – GeoEcoMar – ROMANIA 23-25 Dimitrie Onciul St. 024053 Bucharest Tel./Fax: +40-021-252 30 39 Contact: [email protected] Descrierea CIP a Bibliotecii Naţionale a României Geosciences in the 21st century / editors: Antoneta Seghedi, Victor Mocanu, Gheorghe Ilinca. - Bucureşti : GeoEcoMar, 2019 Conţine bibliografie ISBN 978-606-94742-7-3 I. Seghedi, Antoneta (ed.) II. Mocanu, Victor (ed.) III. Ilinca, Gheorghe (ed.) 55 Cover: Nicoleta Aniţăi © GeoEcoMar 2019 Printed in Romania CONTENTS Foreword..................................................................................................................................................7 Nicolae Anastasiu The energy mix – the key to performance in the 21st century................................................................8 Alexandru Andrăşanu Geoconservation as a new discipline within Geosciences………………………………………………………………….10 Eliza Anton, Mihaela-Carmen Melinte-Dobrinescu Biostratigraphy of the Istria Basin (Nw Black Sea Shelf) based on calcareous nannofossils……………….14 Laurenţiu -
Uricani Monografie Turistică
Uricani Monografie turistică URICANI 2019 Cuprins 1. Considerații generale …………………………………………..…pag. 3 1.1. Prezentarea cadrului de analiză .................................................................. pag.4 1.2. Scurt istoric .................................................................................................. pag. 9 1.3. Generalități ................................................................................................. pag. 13 1.4. Căile de acces ............................................................................................. pag. 15 1.5. Infrastructura edilitară .............................................................................. pag. 17 1.6. Cadrul natural ........................................................................................... pag. 22 1.7. Cadrul socio – economic ........................................................................... pag. 28 1.8. Probleme de mediu și factori de risc ......................................................... pag. 34 2. Analiza potențialului turistic ………………………….………. pag. 43 2.1. Turism montan pedestru ……………………………………………….. pag. 43 2.1.1. Munții Retezat ………………………………………………......pag. 43 2.1.2. Munții Vâlcan …………………………………………………. pag. 46 2.1.3. Munții Tulișa …………………………………………..……… pag. 49 2.1.4. Munții Retezatul Mic sau Calcaros …………………………… pag. 51 2.2. Trasee turistice montane ……………………………………………….. pag. 52 2.3. Cicloturism ……………………………………………………………… pag. 62 2.4. Apele ………………………………………………………………...…… pag. 68 2.5. Cascadele ……………………………………………………………..…. -
FIELD TRIP 1 – Duration 3 Days
FIELD TRIP 1 – duration 3 days. Transportation: bus Tuesday August 26, 2014 - Thursday August 28, 2014 IGCP609 Field trip on Cretaceous cyclic sedimentation in the Eastern Carpathians. Lower Cretaceous Urgonian/platform facies, Lower Cretaceous black shales Deep-water sections with Cretaceous cyclic CORBs Degree of difficulty and weather: low, most of the stops are beside or near roads, although a couple of short (less than 1 km) hikes will be involved. Sturdy footwear is recommended. First day 26th of August Bucharest-Focsani-Lepsa Outcrops displaying Lower Cretaceous black shales, followed by Albian up to Coniacian red shales will be examined in the Putna Valley Basin (Marginal Fold Nappe, Vrancea Halfwindow). Albian black shales and red shales at Lepsa Turonian red shales in Putna Valley Overnight in Lepsa Second day 27th of August Lepsa-Covasna-Cernatu-Brasov-Bran-Dambovicioara Covasna Valley: mid Cretaceous black shales and red shales; mid-Cretaceous anoxic events; Upper Cretaceous red variegated marlstones (Outer Moldavides, Tarcau Nappe). Mid Cretaceous red shales Upper Cretaceous red marlstones Cernatu Valley: Albian turbidites, followed by Upper Albian dark grey shales and uppermost Albian-lowermost Cenomanian red shales, including OAE1d. Visit of the medieval Braşov town. Braşov known as Kronstadt in German óor Brass in Hungarian is the 7th largest city in Romania. The town is located almost in the centre of Romania (176 km from Bucharest), being surrounded by the Carpathian Mountains. The city provides a mix of wonderful mountain scenery in the nearby Poiana Braşov (a renown winter resort) and medieval history with German influences in the old town. Small outcrops of Urgonian rocks could be seen in the town. -
Descrierea Din Punct De Vedere Hidrografic a Bazinului Văii Jiului 7 1.1
CUPRINS pag. Introducere 5 Capitolul 1: Descrierea din punct de vedere hidrografic a bazinului Văii Jiului 7 1.1. Integrarea în mediu 7 1.1.1. Calitatea factorilor de mediu 7 1.1.2. Gradul de poluare 7 1.1.3. Riscuri 8 1.1.4. Obiectivele de mediu 8 1.1.5. Obiectivele de mediu pentru apele de suprafaţă 9 1.2. Descrierea generală a zonei riverane 10 1.2.1. Relieful şi solurile 10 1.3. Geologia şi hidrologia 11 1.3.1. Geologia 11 1.3.2. Hidrologia 12 1.4. Caracteristici climatice 12 Capitolul 2: Prezentarea situaţiei privind calitatea apelor de suprafaţă din partea vestică a Văii Jiului, înainte de restructurarea industriei miniere 15 2.1. Caracteristicile reţelei hidrografice în partea de vest a Văii Jiului 15 2.1.1. Studiul calităţii apelor de suprafaţă în cursurile de apă din zona Jiu Vest izvor 15 2.2. Studiul calităţii apelor de suprafaţă în cursurile de apă din zona Aninoasa 22 Capitolul 3: Caracterizarea economică a zonei vestice a bazinului Valea Jiului 28 3.1. Organizarea administrativă 28 3.1.1. Oraşul Aninoasa 28 3.1.2. Oraşul Vulcan 29 3.1.3. Oraşul Lupeni 31 3.1.4. Oraşul Uricani 35 Capitolul 4: Surse de poluare semnificative şi evoluţia calităţii apei în contextul restructurări industriei miniere în partea vestică a Văii Jiului 41 4.1. Surse difuze de poluare în partea vestică a Văii Jiului 41 4.1.1. Metode existente de evaluare a surselor difuze 41 4.1.2.Categoriile principale de surse difuze de poluare 41 4.1.3. -
ANEXĂ Datele De Identificare Ale Bunurilor Imobile Aflate În
ANEXĂ Datele de identificare ale bunurilor imobile aflate în domeniul public al statului şi în administrarea Administraţiei Naţionale „Apele Române” prin Administrația Bazinală de Apă Jiu, instituție publică aflată în coordonarea Ministerului Apelor și Pădurilor, prevăzute în Anexa nr. 12 la H.G. nr. 1705/2006 pentru aprobarea inventarului centralizat al bunurilor din domeniul public al statului, a căror valoare de inventar se actualizează ca urmare a reevaluării Ministerul Apelor şi 1.Ordonator principal de credite (Ministere sau autoritati 36904099 Pădurilor administratiei publice centrale) Administraţia Naţională 2.Ordonator secundar de credite RO 24326056 „Apele Române” 3. Ordonator tertiar de credite 4.Regii autonome si companii/societati nationale aflate sub autoritatea ordonatorului principal de credite, institute nationale de cercetare- dezvoltare care functioneaza in baza O.G. nr.57/2002 aprobata prin Legea nr.324/2003 cu modificarile ulterioare, si dupa caz, societati comerciale cu capital majoritar de stat care au in administrare bunuri din patrimoniu public de stat Valoare de Nr. Nr. Cod de Denumire Descriere tehnică Adresa inventar crt M.F.P clasific. actualizată (LEI) Nr.foraje=200;Suprafațã Țara: România; Județ: DOLJ; -; -; Nr: -; 1 63977 8.03.11 foraje DA Jiu 208,846 ocupată de foraje= mp;CF= ; DA Jiu Nr.foraje=53 ;Suprafață Țara: România; Judet: MEHEDINȚI; - ; - 2 63978 8.03.11 foraje DA Jiu 33,501 ocupată de foraje= mp;CF= ; ; Nr: -; DA Jiu Nr.foraje=26 ;Suprafață Țara: România; Județ: GORJ; -; -; Nr: -; 3 63979 8.03.11 foraje DA Jiu 57,547 ocupată de foraje= mp;CF= ; DA Jiu Valoare de Nr. Nr. Cod de Denumire Descriere tehnică Adresa inventar crt M.F.P clasific. -
Water Quality Survey of Streams from Retezat Mountains (Romania)
JOURNAL OF ENVIRONMENTAL GEOGRAPHY Journal of Environmental Geography 9 (3–4), 27–32. DOI: 10.1515/jengeo-2016-0009 ISSN: 2060-467X WATER QUALITY SURVEY OF STREAMS FROM RETEZAT MOUNTAINS (ROMANIA) Mihai-Cosmin Pascariu1,2, Tiberiu Tulucan3,4, Mircea Niculescu5, Iuliana Sebarchievici2, Mariana Nela Ștefănuț2* 1”Vasile Goldiş” Western University of Arad, Faculty of Pharmacy, 86 Liviu Rebreanu, RO-310414, Arad, Romania 2National Institute of Research & Development for Electrochemistry and Condensed Matter – INCEMC Timișoara, 144 Dr. Aurel Păunescu-Podeanu, RO-300569, Timișoara, Romania 3”Vasile Goldiș” Western University of Arad, Izoi-Moneasa Center of Ecological Monitoring, 94 Revoluției Blvd., RO-310025, Arad, Romania 4Romanian Society of Geography, Arad subsidiary, 2B Vasile Conta, RO-310422, Arad, Romania 5University Politehnica Timișoara, Faculty of Industrial Chemistry and Environmental Engineering, 6 Vasile Pârvan Blvd., RO- 300223, Timișoara, Romania *Corresponding author, e-mail: [email protected] Research article, received 3 July 2016, accepted 14 November 2016 Abstract The Retezat Mountains, located in the Southern Carpathians, are one of the highest massifs in Romania and home of the Retezat National Park, which possesses an important biological value. This study aimed at the investigation of water quality in creeks of the Southern Retezat (Piule-Iorgovanul Mountains) in order to provide information on pollutants of both natural and anthropogenic origin, which could pose a threat for the human health. Heavy metal and other inorganic ion contents of samples were analyzed with on-site and laboratory measurements to estimate water quality. The samples were investigated using microwave plasma - atomic emission spectrometry to quantify specific elements, namely aluminium, cadmium, cobalt, chromium, copper, iron, magnesium, manganese, molybdenum, nickel, lead and zinc. -
Limnological Changes in South Carpathian Glacial Lakes
This manuscript is contextually identical with the following published paper: Tóth M, Buczkó K, Specziár A, Heiri O, Braun M, Hubay K, Czakó D, Magyari EK (2018) Limnological changes in South Carpathian glacier-formed lakes (Retezat Mountains, Romania) during the Late Glacial and the Holocene: A synthesis. Quaternary International, 477, pp. 138-152. The original published PDF available in this website: https://www.sciencedirect.com/science/article/pii/S1040618216308321?via%3Dihub Limnological changes in South Carpathian glacier-formed lakes (Retezat Mountains, Romania) during the Late Glacial and the Holocene: a synthesis Mónika Tóth1,2*, Krisztina Buczkó3, András Specziár1, Oliver Heiri2, Mihály Braun4, Katalin Hubay4, Dániel Czakó5, Enikő K. Magyari6 1 MTA Centre for Ecological Research, Balaton Limnological Institute, Klebelsberg Kuno 3, H-8237 Tihany, Hungary 2 Institute of Plant Sciences and Oeschger Centre for Climate Change Research, University of Bern, Altenbergrain 21, CH-3013 Bern, Switzerland 3 Department of Botany, Hungarian Natural History Museum, P.O. Box 222, H-1476 Budapest, Hungary 4 Herteleni Laboratory of Environmental Studies, Institute for Nuclear Research of the HAS, Bem tér 18/C, H-4026 Debrecen, Hungary 5School of Earth Sciences and Geography, Kingston University, Penrhyn road, Kingston Upon Thames, Surrey, KT1 2EE, UK 6 MTA-MTM-ELTE Research Group for Paleontology, Pázmány Péter stny 1/C, H-1117 Budapest, Hungary *Correspondent author: Mónika Tóth; MTA Centre for Ecological Research, Balaton Limnological Institute, Klebelsberg Kuno 3, H-8237 Tihany, Hungary; E-mail: [email protected] Abstract Remains of aquatic biota preserved in mountain lake sediments provide an excellent tool to study lake ecosystem responses to past climate change. -
Territorial Concentration of the Poor People in the Petroşani Depression
The Annals of Valahia University of Târgovişte, Geographical Series, Tome 10 / 2010 __________________________________________________________________________________________________ TERRITORIAL CONCENTRATION OF THE POOR PEOPLE IN THE PETROŞANI DEPRESSION Andra COSTACHE1 1Valahia University of Târgovişte Abstract: The paper analyses the features of the deprived urban areas from Petroşani Depression, characterized by the residential concentration of the poor people, but also by poor living conditions, households with limited access to utilities and low acces to urban services. These areas have been identified following field surveys applied in the six towns of the studied region. Key words: Petroşani Depression, poverty, deprived urban areas 1. Dimensions of poverty in the Petroşani Depression. In the Petroşani Depression, the level of poverty is a direct consequence of the regions’ evolution in the last 50 years and of the economic restructuring. These factors have had an impact on the structure of active and inactive population and influenced the income sources and the income level, which are the main prerequisites of poverty. Compared to the national average for urban areas, in the cities of Petroşani Depression the income from wages, from self-employed activities or from goods saling (other than agricultural products) have a lower weight. On the other hand, there are higher than the national urban averages the value of social transfers and the amount of services that are covered by certain discounts provided by employers (in this case the National Pit Coal Company) – Table 1. This reflects the dependence of incomes on the welfare system and on the coal-extracting activities (the revenues of 14.3% of households rely solely on wages, social benefits or social transfers from CNH - Negulescu et al., 2004). -
Forest Stands from Accumulation and Natural Lakes Slopes from the Southern Carpathians
https://doi.org/10.15551/pesd2020141016 PESD, VOL. 14, no. 1, 2020 FOREST STANDS FROM ACCUMULATION AND NATURAL LAKES SLOPES FROM THE SOUTHERN CARPATHIANS Dincă Lucian1, Voichița Timiș-Gânsac2, Breabăn Iuliana Gabriela3 Keywords: lakes, forests, exposition, field inclination, forest soils. Abstract. The Southern Carpathians are situated in the central part of Romania, between Prahova Valley and the Danube, being the highest and most massive mountains from the Romanian Carpahtians. The relief and vegetation are similar to the Alps. These mountains conserve the most representative glaciar relief from Romania, with cuaternar glaciar tracks. Some of its peaks, namely Moldoveanu, Negoiu, Parângul Mare and Peleaga exceed 2500 m. From its total 217.889 ha occupied by forests with water protection functions, the forests located on lake slopes occupy 9.746 ha, namely 5%. The forests from this area are composed of spruce (Picea abies L.H. Karst) and beech (Fagus sylvatica L.), accompanied by other species such as birch (Alnus glutinosa, L., Gaertn.) and pine (Pinus sp.). From the point of view of the field’s orography, these forests are located on lands with an middle inclination on all exposition categories, but predominantly on the North-East, one at an average altitude of 1050 m. From the point of view of site conditions, the characteristic flora type is Asperula-Dentaria, while the main soils are dystric cambisol and eutric cambisol. 1. Introduction The Southern Carpathians are situated within Prahova Valley in the east, and Timiş-Cerna valleys in the west, Getic Subcarpathians and Mehedinți Plateau in the south and Transylvania’s basin in the north.