DOCSLIB.ORG

Izrada Karata Opasnosti I Izračun Šteta Na Slivu Rijeke Bednje

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
Izrada Karata Opasnosti I Izračun Šteta Na Slivu Rijeke Bednje IZRADA KARATA OPASNOSTI I IZRAČUN ŠTETA NA SLIVU RIJEKE BEDNJE Marin Paladin, dipl.ing.građ.a, Renata Vidaković Šutić, dipl.ing.građ.b, Boris Vrcelj, dipl.ing.geol.c, Vedrana Ričković, dipl.ing.građ.d a Institut za elektroprivredu i energetiku d.d. Zagreb, [email protected] b Institut za elektroprivredu i energetiku d.d. Zagreb, [email protected] c Institut za elektroprivredu i energetiku d.d. Zagreb, [email protected] d Institut za elektroprivredu i energetiku d.d. Zagreb, [email protected] SAŽETAK U ovom radu prikazana je analiza sliva rijeke Bednje kao područja s potencijalno značajnim poplavnim rizikom. Analiza je provedena u sklopu izrade studijske dokumentacije za pripremu projekata zaštite od poplava na slivu Bednje za sufinanciranje iz fondova Europske unije. Ciljevi studije su definiranje elemenata planova upravljanja rizicima od poplava na slivu Bednje te izrada studije izvodljivosti za pojedine projekte sadržane u optimalnom sustavu mjera upravljanja rizicima od poplava u svrhu ishođenja sufinanciranja iz EU fondova. U prvoj fazi provedena je detaljna analiza postojećeg stanja, uključujući hidrološko-hidrauličke analize i modeliranja te izradu karata opasnosti od poplava opisane u ovom radu. Prethodnim aktivnostima obuhvaćeni su pregled podloga, analiza postojeće studijske i projektne dokumentacije te obilazak terena. Analize su započele izradom hidroloških i meteoroloških podloga na temelju raspoloživih podatka službene mreže hidroloških i meteoroloških stanica DHMZ-a. Simulacija procesa oborina-otjecanje provedena je na hidrološkom modelu sliva (HEC-HMS) koristeći hidrološke i meteorološke podloge te topografske, hidrografske i pedološke značajke podslivova na koje je sliv rijeke Bednje u tu svrhu podijeljen. Hidrološki model je kalibriran i verificiran na temelju izmjerenih vodnih valova na hidrološkim stanicama. Uspoređeni su sintetski vodni valovi dobiveni statističkom obradom izmjerenih podataka s hidroloških stanica i teoretski valovi dobiveni hidrološkim modelom za odgovarajuće povratne periode. Nastavno je izrađen hidraulički, nestacionarni 2D numerički model sliva (MIKE 21) koji koristi dostupne prostorne podatke te sintetske vodne valove sa svakog podsliva koji su rezultat hidrološkog modela. Hidraulički model je također kalibriran i verificiran na temelju snimljenih vodnih valova i zabilježenih poplavnih događaja. Rezultat hidrauličkog modela su karte opasnosti od poplava, odnosno karte dubina i brzina vode na čitavom slivu za određene povratne periode. Na temelju karata dubina, računaju se potencijalne štete pomoću usvojene metodologije, odnosno alata (NACER) za izračun šteta na poplavljenim područjima. Iznesen je osvrt na kvalitetu i dostupnost podloga za uspostavljene modele, kao i osvrt na vrijednosti izračunate potencijalne štete na poplavljenom području. KLJUČNE RIJEČI: Sliv rijeke Bednje, Hidrološki model, 2D hidraulički model, Karte opasnosti od poplava, Potencijalne štete od poplava SUMMARY This paper presents an analysis of the Bednja river basin as a potentially significant flood risk area. The analysis was conducted in the scope of producing the documentation for the preparation of flood protection projects in the Bednja river basin for co-financing from EU funds. The objectives of the study are defining elements of the plans of flood risk management in the Bednja river basin and feasibility study for individual projects contained in an optimal system of measures of flood risk management for the purpose of obtaining co-financing from EU funds. The first phase contains detailed analysis of the current situation, including hydrological and hydraulic analyzes and modeling, together with the development of the flood hazard maps described in this paper. The preceding activities included are view of the baseline materials, an analysis of the existing study and project documents and a field trip. The analyses started with the development of hydrological and meteorological maps based on available data from the official network of hydrological and meteorological stations of the State Meteorological and Hydrological Service. The simulation of the rainfall-runoff process was carried out on the basin’s hydrological model (HEC-HMS) by utilization of hydrological and meteorological maps and topographic, hydrographical and pedological characteristics of the subbasins into which the Bednja river basin was divided for this purpose. The hydrological model was calibrated and verified according to the water waves measured at the hydrological stations. The synthetic water waves obtained by statistical processing of the data measured at the hydrological stations were compared with the theoretical water waves obtained through hydrological modelling for relevant return periods. Additionally, a hydraulic, non-stationary 2D numerical model (MIKE 21) of the basin was developed. This model uses available spatial data and synthetic water waves from each subbasin resulting from the hydrological model. The hydraulic model was also calibrated and verified based on the observed water waves and recorded flood events. The results of the hydraulic model were flood hazard maps, i.e. maps of water depths and velocities in the entire basin for relevant return periods. Potential damages were calculated on the basis of the depth maps with adopted methodology, i.e. and tools (NACER) for calculation of damage in flooded areas. The paper includes a review of quality and availability of baseline information for the established models and a review of values of the calculated potential damage in the flooded area. KEY WORDS: Bednja river basin, hydrological model, 2D hydrological model, flood hazard maps, potential flood damage 1. UVOD Pripremne analize za izradu Strategije upravljanja vodama (NN 91/08) su pokazale da je oko 15% kopnenog teritorija RH potencijalno ugroženo od poplava. Veći dio tog teritorija je zaštićen, ali s različitim razinama zaštite i sigurnosti. Zakon o vodama (NN 153/09, 63/11, 130/11, 56/13, 14/14) definira zaštitu od štetnog djelovanja voda i upravljanje rizicima. Prvi korak u upravljanju rizicima od poplava je izrada prethodne procjene rizika od poplava čiji je rezultat identifikacija područja s potencijalno značajnim poplavnim rizicima. Za ta područja potrebno je izraditi karte opasnosti od poplava, karte rizika od poplava i planove upravljanja rizicima od poplava. Neka od tih područja se nalaze u inundaciji rijeke Bednje i analizirat će se na razini sliva Bednje, a u nizinskom dijelu sliva Bednje u obzir će se uzeti i utjecaj rijeka Drave i Plitvice. U cilju smanjenja rizika od poplava na ugroženim područjima, kao što je sliv Bednje, potrebno je planirati i provoditi mjere upravljanja rizicima od poplava, uključujući preventivne mjere izgradnje, dogradnje ili rekonstrukcije sustava za zaštitu od poplava. U svrhu ishođenja sufinanciranja iz EU fondova za mjere upravljanja rizicima od poplava na slivu Bednje, Hrvatske vode su pokrenule aktivnosti na izradi studijske dokumentacije za pripremu EU projekata zaštite od poplava na ovom slivu. Ciljevi studije su definiranje elemenata planova upravljanja rizicima od poplava na slivu Bednje te izrada studije izvodljivosti za pojedine projekte sadržane u optimalnom sustavu mjera upravljanja rizicima od poplava u svrhu ishođenja sufinanciranja iz EU fondova. U prvoj fazi provedena je detaljna analiza postojećeg stanja, uključujući hidrološko- hidrauličke analize i modeliranja te izradu karata opasnosti od poplava opisane u ovom radu. 2. HIDROLOŠKI MODEL Na predmetnom području sliva Bednje, kao mjerodavne hidrološke stanice (h.s.) analizirane su hidrološke stanice Lepoglava, Željeznica, Ključ, Tuhovec i Ludbreg na Bednji (Slika 1). Nizovi protoka su određeni za pojedinu hidrološku stanicu na temelju vodostaja koji su izravno mjerena hidrološka veličina i krivulja protoka koje su definirane na temelju mjerenja protoka. Ovako izračunati protoci, kao i mjereni vodostaji, te definirane krivulje protoka nalaze se u Bazi hidroloških podataka (HIS-2000) DHMZ-a. Slika 1. Hidrološke stanice, digitalni model reljefa i podjela sliva Bednje za hidraulički model Proračun maksimalnih godišnjih protoka različitih povratnih perioda rijeka Bednje proveden je primjenom standardnih teorijskih funkcija raspodjele za pet hidroloških stanica: Lepoglava, Željeznica, Ključ, Tuhovec i Ludbreg. Analizom hidrograma (srednji dnevni podaci o protoku) zabilježenih vodnih valova, utvrđeno je da vodni valovi na rijeci Bednji u prosjeku traju 4 dana (h.s. Lepoglava) i 5 dana (h.s. Željeznica, Ključ, Tuhovec i Ludbreg), stoga su analizirani maksimalni godišnji volumeni vodnih valova (konstantne trajnosti 4, odnosno 5 dana). Sukladno trajanju vodnih valova vrijeme podizanja vodnog vala na hidrološkoj stanici Lepoglava je 24 sata, dok je na ostalim hidrološkim stanicama oko 30 sati. Za konstrukciju kompletnog sintetskog hidrograma direktnog otjecanja koristi se Goodrichev izraz, za čiju su se konstrukciju kao osnovni elementi koriste maksimalni protok Qmax, vrijeme podizanja tp i vremenska baza hidrograma tB. Na dijelu toka Bednje uzvodno od h.s. Lepoglava, kao i na pritocima Bednje ne postoje sustavna mjerenja i opažanja hidroloških veličina. Za hidrološki model važan je odabir mjerodavne meteorološke stanice (m.s.) na kojoj se mjere oborine. Iako su meteorološke stanice Varaždin i Krapina opremljene ombrografima i raspolažu podacima o kratkotrajnim oborinama, obje se nažalost nalaze izvan orografskog sliva Bednje. Za brdski dio sliva Bednje, kao mjerodavna, odabrana
Load more

Recommended publications
  • Review of Research on Plitvice Lakes, Croatia in the Fields of Meteorology, Climatology, Hydrology, Hydrogeochemistry and Physical Limnology
    GEOFIZIKA VOL. 35 2018 DOI: 10.15233/gfz.2018.35.9 Review paper Review of research on Plitvice Lakes, Croatia in the fields of meteorology, climatology, hydrology, hydrogeochemistry and physical limnology Zvjezdana Bencetić Klaić 1, Josip Rubinić 2 and Sanja Kapelj 3 1 Department of Geophysics, Faculty of Science, University of Zagreb 2 Faculty of Civil Engineering, University of Rijeka 3 Faculty of Geotehnical Engineering, University of Zagreb Received 16 April 2018, in final form 22 October 2018 In lakes, several physical, chemical, and biological processes occur simulta- neously, and these processes are interconnected. Therefore, the investigation of lakes requires a multidisciplinary approach that includes physics (including the physics of the atmosphere, i.e., meteorology), chemistry, geology, hydrogeology, hydrology and biology. Each of these disciplines addresses a lake from a different point of view. However, lake studies that primarily belong to one field, at least to some extent, report their findings in ways that are associated with other fields; this type of reporting is caused by the inherent interconnections between phe- nomena from different disciplines. Plitvice Lakes, Croatia, are composed of a unique cascading chain of karst lakes, and these lakes have been investigated by numerous authors. Here, we provide an overview of the studies of the Plitvice Lakes Area (PLA) that address meteorology, climatology, hydrology, hydrogeo- chemistry and physical limnology. Our aim is to synthesize the results from each of these disciplines and make them available to scientists from other related disciplines; thus, this review will facilitate further investigations of the PLA within the natural sciences. In addition, valuable results from early investiga- tions of Plitvice Lakes are generally unavailable to the broader scientific com- munity, and are written in Croatian.
    [Show full text]
  • Research Article
    Ecologica Montenegrina 44: 69-95 (2021) This journal is available online at: www.biotaxa.org/em http://dx.doi.org/10.37828/em.2021.44.10 Biodiversity, DNA barcoding data and ecological traits of caddisflies (Insecta, Trichoptera) in the catchment area of the Mediterranean karst River Cetina (Croatia) IVAN VUČKOVIĆ1*, MLADEN KUČINIĆ2**, ANĐELA ĆUKUŠIĆ3, MARIJANA VUKOVIĆ4, RENATA ĆUK5, SVJETLANA STANIĆ-KOŠTROMAN6, DARKO CERJANEC7 & MLADEN PLANTAK1 1Elektroprojekt d.d., Civil and Architectural Engineering Department, Section of Ecology, Alexandera von Humboldta 4, 10 000 Zagreb, Croatia. E-mails:[email protected]; [email protected] 2Department of Biology (Laboratory for Entomology), Faculty of Science, University of Zagreb, Rooseveltov trg 6, 10 000 Zagreb, Croatia. E-mail: [email protected] 3Ministry of Economy and Sustainable Development, Radnička cesta 80/7, 10000 Zagreb, Croatia. E-mail: [email protected] 4Croatian Natural History Museum, Demetrova 1, 10 000 Zagreb, Croatia. E-mail: [email protected] 5Hrvatske vode, Central Water Management Laboratory, Ulica grada Vukovara 220, 10 000 Zagreb, Croatia. E-mail:[email protected] 6Faculty of Science and Education, University of Mostar, Matice hrvatske bb, 88000 Mostar, Bosnia and Herzegovina. E-mail: [email protected] 7Primary School Barilović, Barilović 96, 47252 Barilović and Primary School Netretić, Netretić 1, 47271 E-mail: [email protected] *Corresponding author: [email protected] **Equally contributing author Received 2 June 2021 │ Accepted by V. Pešić: 19 July 2021 │ Published online 2 August 2021. Abstract The environmental and faunistic research conducted included defining the composition and distribution of caddisflies collected using ultraviolet (UV) light trap at 11 stations along the Cetina River, from the spring to the mouth, and also along its tributaries the Ruda River and the Grab River with two sampling stations each, and the Rumin River with one station.
    [Show full text]
  • ELABORAT Zaštite Okoliša [PDF]
    NOSITELJ ZAHVATA: VODOVOD KORENICA d.o.o. ELABORAT ZAŠTITE OKOLIŠA U POSTUPKU OCJENE O POTREBI PROCJENE UTJECAJA NA OKOLIŠ SUSTAVA ODVODNJE I PROČIŠĆAVANJA AGLOMERACIJE PLITVIČKA JEZERA studeni 2016. REVIZIJA D Institut IGH d.d. Regionalni centar Split Odjel za ekologiju Matice hrvatske 15, 21000 Split tel. + 385 21 558 681 fax. + 385 21 465 335 NOSITELJ ZAHVATA: VODOVOD KORENICA d.o.o. Trg Sv. Jurja 12, 53230 Korenica NAZIV ZAHVATA: SUSTAV ODVODNJE I PROČIŠĆAVANJA AGLOMERACIJE PLITVIČKA JEZERA VRSTA PROJEKTA: ELABORAT ZAŠTITE OKOLIŠA U POSTUPKU OCJENE O POTREBI PROCJENE UTJECAJA NA OKOLIŠ BROJ PROJEKTA: 85013644 VODITELJ STUDIJE: mr.sc. Anita Erdelez, dipl.ing.građ. DIREKTORICA RC SPLIT: Vedrana Tudor, MBA, dipl.ing.građ. MJESTO I DATUM: Split, studeni 2016. IZRAĐIVAČI: POGLAVLJE IZRAĐIVAČI Opis zahvata, vodna tijela, mr.sc. Anita Erdelez, dipl.ing.građ. klimatske promjene Opći dijelovi Elaborata Zajednička redakcija IGH Prostorno-planska Petar Matulić, dipl.ing.građ. dokumentacija IGH Prostorno-planska Domagoj Vranješ, mag.ing.prosp.arch., dokumentacija, krajobraz univ.spec.oecoing. Valerija Butorac, mag. geograf. Ivana Tomašević, mag.ing.prosp.arch. Vita projekt d.o.o. Geološke i hidrogeološke prof.dr.sc. Tatjana Vlahović, značajke, utjecaj na vode dipl.ing.geol. Samostalni vanjski suradnik Utjecaj na vode (kombinirani mr.sc. Zlatko Perović, dipl.ing.pom. pristup), zrak i buka IGH Priroda, šume i divljač Agata Kovačev, mag.oecol., mag.biol. et oecol.mar. IGH dr.sc. Gordan Lukač, dipl.ing.biol. prof.dr.sc. Vladimir Hršak, dipl.ing.biol. Hrvoje Čižmek, dipl.ing.biol. Samostalni vanjski suradnici SADRŽAJ: POGLAVLJE 1: OPIS ZAHVATA 1 1.1. OBVEZA IZRADE ELABORATA 1 1.2.
    [Show full text]
  • Pakoštane Municipality Pakoštane Pakoštane, Drage, Vrgada, Vrana
    pakoštane municipality pakoštane pakoštane, drage, vrgada, vrana PUBLISHER TB Općine Pakoštane FOR PUBLISHER Milivoj Kurtov REVIEWERS Danijela Vulin CONSULTANTS Marko Meštrov, Milivoj Kurtov, Danijela Vulin, Slavo Stojanov, Milivoj Barišić, Frane Vulin TEXT Lili Lokin, Igor Gluić, TB Pakoštane PHOTOGRAPHY Jakov Đinđić, Igor Gluić, Dinko Denona, Natural Park “Vrana lake”, Archives Pakoštane Archives INFOGRAFIKA GRAPHIC DESIGN Igor Gluić PRINTING AKD Zagreb YEAR 2014. TOURIST BOARD OF THE MUNICIPALITY OF PAKOŠTANE Municipality Pakoštane History When searching for the origin or the emergence of a city or settlement, researchers most often search for bare physical remains so the question of the nature of the occurrence of human dwellings spins within the closed circle of remains of stones from residential units, temples or walls. But long before the emergence of settlements, there was some type of shelter there, a cave and above all the tendency of individuals, as in with animal species, to stop precisely there and make a campsite. That is why towns, even before they became towns, were an area where people would come to. Some magnetic force would pull them to come precisely here and to return precisely here. And this force was stronger than bare existential interest. Let us return for a moment to those first people who have stopped at this place. What mound - ledge - cape - an island, freshwater / saltwater emitted so much force that the man of that time, after having walked perhaps dozens, perhaps hundreds of kilometres, stopped at this place and said to himself: This is it, this is where I will live! Starting from the Neolithic period, the word “home” and “mother” are woven into every segment of Neolithic life.
    [Show full text]
  • Full of Stories
    Tourist Information FullDon´t fill your oflife with days,stories fill your days with life. D. Fabijanić D. 9 1 2 8 7 3 4 3 1. ISTRIA. 6 Routes following the smallest towns in the world. 2. KVARNER. 12 Routes of fragrant rivieras and islands. 3. DALMATIA. ZADAR. 18 10 The routes of Croatian rulers. 4. DALMATIA. ŠIBENIK. 24 The routes of Croatian rulers. 5. DALMATIA. SPLIT. 30 Routes of ancient cultures. 6. DALMATIA. DUBROVNIK. 36 Croatia. Routes of old sea captains. 7. LIKA - KARLOVAC. 42 Routes following natural wonders. 8. CENTRAL CROATIA. 48 5 Trails of the fairies. 8. CENTRAL CROATIA. 54 The trails of subterranean secrets. 9. CITY OF ZAGREB. 60 6 A city tailored to the needs of man . 10. SLAVONIA. 64 Trails of the Pannonian Sea. 4 Welcome to Croatia! Unique in so many ways, Croatia’s Croatia’s fertile plains, where freshly- roots stem from ancient times and picked fruits are grown which you its great cultural wealth tells of a can taste, the castles, museums and turbulent history going back to the parks, river ports and family farms, Roman era and continuing through wineries, freshly-baked bread whose the Renaissance, the Baroque period aroma tempts one to try it over and the Ottoman conquests right and over again, are all part of the up to the present day, all of which is unexplored hinterland of Croatia, a exceptionally appealing to all who place of mystery and secrets, dream visit the country. If we then add the and reality, the Croatia of feelings rich cultural heritage, the amaz- and senses.
    [Show full text]
  • Hydrogeology of the SINKING ZONE of the KORANA RIVER
    COBISS: 1.02 HYdrogeologY of THE sinking zone of THE Korana River doWnstream of the Plitvice Lakes, Croatia Hidrogeologija ponornega območja REKE Korane dolvodno od Plitviških JEZER, Hrvaška Ranko Biondić1, Hrvoje Meaški1 & Božidar Biondić1 Abstract UDC 556.3(497.56) Izvleček UDK 556.3(497.56) Ranko Biondić, Hrvoje Meaški & Božidar Biondić: Hydroge- Ranko Biondić, Hrvoje Meaški & Božidar Biondić: Hidro- ology of the sinking zone of the Korana River downstream of geologija ponornega območja reke Korane dolvodno od the Plitvice Lakes, Croatia Plitviških jezer, Hrvaška Downstream of the Plitvice Lakes National Park, water that Dolvodno od Nacionalnega parka Plitviška jezera vode, ki pass through the water system of the lakes begins its flow as the tečejo skozi sistem jezer, oblikujejo reko Korano. Nekaj sto Korana River. A few hundred meters downstream of the source metrov pod to izvirno cono v času poletnih sušnih obdobij zone, during the summer dry periods, there are losses of water voda v strugi ponika in s časom povsem presahne. Ponorno in the riverbed resulting in its total drying. The sinking zone in cono gradijo zelo dobro prepustne karbonatne kamnine in šele that area is built of high permeable carbonate rocks and with po prehodu na manj prepustne dolomite približno 17 km nižje the appearance of less permeable dolomite rocks, about 17 km po strugi Korana postane stalna reka. V članku so obravnavane downstream, the Korana River becomes a permanent river. hidrogeološke razmere v coni ponikanja vode v strugi in odno- This paper focuses on the explanation of hydrogeological rela- si s sosednjim porečjem reke Une, pa tudi možnosti prestavitve tions in the zone where losses of water occur in the riverbed, vira oskrbe s pitno vodo iz jezera Kozjak (Plitviška jezera) na relationship to the neighbouring Una River catchment, as well novo lokacijo v ponorni coni reke Korane.
    [Show full text]
  • Croatian Eno-Gastronomy Don´T Fill Your Life with Days, Fill Your Days
    Free Croatian Eno-Gastronomy Full of flavours Don´t fill your life with days, fill your days with life. photo by ivo pervan ivo by photo discover your story at croatia.hr Introduction Croatia, Gastronomic Princess of the Mediterranean and Europe 4 The country of culinary diversity 10 Why enjoy Croatia? 12 Regions (Gastronomy, Health, About wine) List of regions 14 1_Istria 16 2_Kvarner 24 3_Lika_Karlovac 32 4_Dalmatia_Zadar 38 5_Dalmatia_Šibenik 44 6_Dalmatia_Split 50 7_Dalmatia_Dubrovnik 56 8_Slavonia 64 9_Central Croatia 72 10_Zagreb 78 About wine and special subjects About wine_Croatia – a small country for great wines 86 Olive oils_Benefits of olive oil 88 Water_Water is life 90 Ecological products 92 Information Basic information about Croatia 94 Offices of the Croatian National Tourist Board 95 c o n t e n t s Acknowledgements 96 4 c roatia, Gastronomic Princess of the Mediterranean Veljko Barbieri and Europe In the mid nineties, during the rescue excavations in Starograd- nonian influences, it condenses a soupy experience of goulash sko Polje (old town field) on the island of Hvar, grape and olive and stews with a special kaleidoscope of vegetables and spices, seeds were found in one of the funeral urns. Researchers specu- and of course wine, without which this unique dish can neither lated that this was a common residue of agricultural crops from be prepared nor enjoyed. The dish can be spiced during cooking the 4th or 3rd century BC as it was thought that both cultures or later adjusted to taste when already seated at the table, with were connected to the arrival of the Greeks and the establish- spices and wine such as Slavonian Traminac or Klikun, indige- ment of their colonies on the eastern coast.
    [Show full text]
  • Report from Testing the Dynamic Model to Assess Cumulative Effect of N(S)
    REPORT FROM PILOT ACTION – Report from testing the dynamic model to assess cumulative effect of N(S)WRM Croatia /Croatian Waters Final version Pilot catchment Bednja December 2019 1 TABLE OF CONTENT …………………………………………………………………………………………………. 1. APPLICATION OF THE HYDROLOGICAL MODEL (3) 1.1 Description of the catchment (3) 1.2. Watershed delineation (5) 1.3. Land cover, soils and HRU delineation (6) 1.4. Weather data (7) 1.5. Model calibration and validation (9) 2. APPLICATION OF THE HYDRAULIC MODEL (15) 2.1. Description of the river network (15) 2.2. Geometric data (DEM, cross-sections, boundary conditions) (16) 2.3. Description of the model structure (17) 2.4. Hydrologic data (18) 2.5. Hydraulic data (18) 2.6. Model calibration and validation (18) 3. MEASURES IN THE PILOT AREA (22) 4. DYNAMIC MODELING OUTPUTS (25) 5. CONCLUSIONS (28) 2 1. APPLICATION OF THE HYDROLOGICAL MODEL 1.1 Description of the catchment The Bednja River basin occupies 616 km² and can be divided into two topographically different parts: upland and lowland. The lowland part accounts for app. 30 % of the basin area and spreads along the Bednja course from its confluence with the Drava River up to its 55th km. The upland part spreads upstream of the village of Presečno in the length of app. 51 km of the river course and accounts for app. 70 % of the overall basin area (app. 477 km2). In the upland part there are app. 48 torrential basins with approximately 250 km of watercourses. The hydrographic network is much more developed in the upland than in the lowland part of the basin.
    [Show full text]
  • Šifra Naselja Naziv Naselja Općina (3) Općina (5) Naziv Općine 000019 ADA 614 06149 ŠODOLOVCI 000027 ADAMOVEC 1
    šifra naselja naziv naselja općina (3) općina (5) naziv općine 000019 ADA 614 06149 ŠODOLOVCI 000027 ADAMOVEC 133 01333 GRAD ZAGREB 000035 ADŽAMOVCI 372 03727 REŠETARI 000043 ALAGINCI 351 03514 POŽEGA 000051 ALAN 387 03875 SENJ 000060 BUKOVAČKI ANTUNOVAC 283 02836 NOVA BUKOVICA 000078 ANTUNOVAC 475 04758 VELIKA 000086 ALEKSINICA 130 01309 GOSPIĆ 000094 ALILOVCI 177 01775 KAPTOL 000108 ALJMAŠ 110 01104 ERDUT 000116 AMATOVCI 035 00353 BRESTOVAC 000124 ANDIGOLA 063 00639 ČAZMA 000132 ANDRAŠEVEC 311 03115 OROSLAVJE 000159 ANDRIJAŠEVCI 001 00019 ANDRIJAŠEVCI 000167 ANDRILOVEC 101 01015 DUGO SELO 000175 ANTENAL 291 02917 NOVIGRAD 000183 ANTIN 458 04588 TORDINCI 000191 ANTOLOVEC 227 02275 LEGRAD 000205 SVETI ANTON 273 02739 MOŠĆENIČKA DRAGA 000213 ANTONCI 138 01384 GROŽNJAN 000221 ANTONCI 348 03484 POREČ 000248 ANTUNOVAC 002 00027 ANTUNOVAC 000256 ANTUNOVAC 231 02313 LIPIK 000264 ANŽIĆI 497 04979 VIŠNJAN 000272 APATIJA 244 02445 LUDBREG 000299 APATOVEC 214 02143 KRIŽEVCI 000302 APŠEVCI 295 02950 NIJEMCI 000329 ARAPOVAC 400 04006 SLUNJ 000337 ARBANIJA 463 04634 TROGIR 000345 ARŽANO 050 00507 CISTA PROVO 000353 AŠIKOVCI 334 03344 PLETERNICA 000361 AUGUŠTANOVEC 544 05444 POKUPSKO 000388 BABIĆI 468 04685 UMAG 000396 BABIĆI 597 05975 KAŠTELIR - LABINCI 000400 BABINA GREDA 003 00035 BABINA GREDA 000418 BABINA RIJEKA 083 00833 DONJI KUKURUZARI 000426 BABINAC 161 01619 IVANSKA 000434 BABINAC 478 04782 VELIKA PISANICA 000442 BABINDUB 520 05207 ZADAR 000469 BABINEC 048 00485 CESTICA 000477 BABINO POLJE 268 02682 MLJET 000485 BRANIMIROVAC 205 02054 KOŠKA
    [Show full text]
  • Hydrology of Fractured Rocks; 1967
    LAKES IN THE CROATIAN LIMESTONE REGION Milivoj PETRIK SUMMARY A discussion is presented on the permanent natural accumulations of water on earth’s surface in the limestone region of Croatia. Such accumulations are divided into two groups: lakes proper, and small accumulations called “Oka”. The discussion covers all lakes of that region. They are: 1. the lake Vrana on the island of Cres, 2. the lake Jezero on the island of Krk, 3. the lakes of Plitvice, i.e. the 14 larger basins, 4.the lake Vrana at Biograd in Dalmatia, 5. the lakes along the river Krka, 6. six lakes in the environs of Imotski, in Dalmatia, 7. the lakes of BaCina, in Dalmatia. Because the smaller accumulations, often called “Oka”, are too numerous to be discussed in their totality, only a representative series of the more interesting ones are discussed, viz. those at Sv. Stjepan in Istria, at Rijeka, Slunj, Ogulin, in the region of the lower Krka river, at Imotski and those in the region of the lower Neretva rive?. The discussion includes-as far as they are at present known-data on geographic position, altitude, general morphology, geology and hydrology, genesis, quality of water, temperature, dissolved oxygen, free carbon dioxide, total, carbonate and non- carbonate hardness, alkalinity, calcium, magnesium and chloride, transparency and productivity. Seasonal stratification of water is also discussed. Finally, an attempt is made to arrive at the common characteristics of the lakes in that region. RESUME Les lacs de la region cnlcnire de Croatie Cette étude porte sur les accumulations naturelles permanentes d’eaux super- ficielles dans la région calcaire de Croatie.
    [Show full text]
  • Annotated Checklist of Croatian Riffle Beetles (Insecta: Coleoptera: Elmidae)
    Nat. Croat. Vol. 24(1), 2015 93 NAT. CROAT. VOL. 24 No 1 93–109 ZAGREB June 30, 2015 original scientific paper / izvorni znanstveni rad ANNOTATED CHECKLIST OF CROATIAN RIFFLE BEETLES (INSECTA: COLEOPTERA: ELMIDAE) Vlatka Mičetić Stanković1,3*, Manfred A. Jäch2 & Mladen Kučinić3 1 Croatian Natural History Museum, Demetrova 1, Zagreb 2 Naturhistorisches Museum Wien, Burgring 7, A – 1010 Wien, Austria 3 Department of Biology, Faculty of Science, Rooseveltov trg 6, 10 000 Zagreb, Croatia Mičetić Stanković, V., Jäch, M.A. & Kučinić, M.: Annotated checklist of Croatian riffle beetles (Insecta: Coleoptera: Elmidae). Nat. Croat., Vol. 24, No. 1, 93–109, 2015, Zagreb In this paper an annotated checklist of Croatian riffle beetles is presented. It is a result of a literature review, revision of museum collections, implementation of results from various environmental impact and baseline studies, as well as field investigations throughout Croatia from 2002–2013. Altogether 23 species in eight genera of Elmidae were identified. Five species are new for the Croatian fauna: Elmis rioloides (Kuwert 1890), Esolus angustatus (Müller 1821), E. pygmaeus (Müller 1806), Oulimnius tuberculatus (Müller 1806) and Stenelmis consobrina Dufour 1835. Furthermore, the occurrence of Elmis aenea (Müller 1806) in Croatia is confirmed. Keywords: Insecta, Coleoptera, Elmidae, riffle beetles, first records, freshwater, water beetles Mičetić Stanković, V., Jäch, M.A. & Kučinić, M.: Popis slapoljuba (Insecta: Coleoptera: Elmidae) Hrvatske s napomenama. Nat. Croat., Vol. 24, No. 1, 93–109, 2015, Zagreb U ovom je radu dat popis slapoljuba Hrvatske s napomenama o njihovoj biologiji i staništima u Hrvatskoj. Rezultat je pregleda literature, uvida u muzejske zbirke, implementacije rezultata stručnih studija i elaborata, kao i prikupljanja vodenih kornjaša tijekom raznih terenskih istraživanja duž Hr- vatske u razdoblju od 2002.
    [Show full text]
  • Report Title
    The Danube River Basin District Management Plan – Update 2015 ANNEX DRAFT December 2014 ICPDR / International Commission for the Protection of the Danube River / www.icpdr.org The Danube River Basin District Management Plan – Update 2015 ANNEX List of Annexes Annex 1: Competent Authorities and Weblinks to National RBM Plans in the DRBD Annex 2: Update on DRBD Surface Water Typology Annex 3: Status of Urban Waste Water Infrastructure Annex 4: Industrial Emission Inventories Annex 5: Future Infrastructure Projects Annex 6: Groundwater Annex 7: Inventory of Protected Areas Annex 8: Economic Analysis Annex 9: Progress in Urban Wastewater Treatment Sector Annex 10: Nitrates Vulnerable Zones in the DRBD Annex 11: Overview on agricultural measures Annex 12: Progress on measures addressing hydromorphological alterations ICPDR / International Commission for the Protection of the Danube River / www.icpdr.org Competent authorities and Weblinks to National RBM Plans in the DRB Annex 1 DRAFT DRBM Plan – Update 2015 ICPDR / International Commission for the Protection of the Danube River / www.icpdr.org DRAFT Danube River Basin District Management Plan – Update 2015 Austria Hungary Federal Ministry for Agriculture, Forestry, Environment Ministry of Interior and Water Management Jozsef Attila u. 2-4 Stubenring 1 H-1051 Budapest A-1012 Wien Web link: www.kormany.hu/hu/belugyminiszterium Web link: www.bmlfuw.gv.at Web link national RBM Plan: www.euvki.hu; Web link national RBM Plan: http://wisa.bmlfuw.gv.at www.vizeink.hu Bosnia and Herzegovina Moldova Ministry of Foreign Trade and Economic Relations Ministry of Ecology, Construction and Territorial Musala 9 Development BiH-71000 Sarajevo 9 Cosmonautilor St.
    [Show full text]