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Modelling Flow of Subterranean Pivka River in Postojnska Jama, Slovenia Modeliranje Toka Podzemeljske Pivke V Postojnski Jami, Slovenija
COBISS: 1.02 Modelling floW of subterranean Pivka river in Postojnska jama, Slovenia Modeliranje toka podzemeljske Pivke V Postojnski jami, Slovenija Georg Kaufmann1, Franci Gabrovšek2 & Janez TURK3 Abstract UDC 556.32:551.44(497.471) Izvleček UDK 556.32:551.44(497.471) Georg Kaufmann, Franci Gabrovšek, Janez Turk: Modelling Georg Kaufmann, Franci Gabrovšek, Janez Turk: Modeliranje cave flow hydraulics in Postojnska jama, Slovenia toka podzemeljske Pivke v Postojnski jami, Slovenija The sub-surface flow path through the Postojnska jama cave Z avtomatskimi merilniki in registratorji podatkov smo sprem- system has been monitored with 7 stations distributed along ljali podzemni tok Pivke v Postojnski jami na sedmih točkah the flow path, monitoring stage and temperature.W e have used med ponorom in odtočnim sifonom v Pivki jami. Podatke the stage data to model flow through the cave system with the nivojev in pretoka smo obravnavali z modelom EPA SWMM, program package SWMM, simulating the active parts of Pos- s katerim smo simulirali tok v poenostavljeni geometriji ka- tojnska jama with simplified geometry. From the comparison nalov. S primerjavo med opazovanji in modelskimi rezultati of stage observations and predictions, we identified key sec- smo določili ključne odseke (podore, zožitve, sifone, obtoke), tions in the cave, which control the sub-surface flow, such as ki najbolj vplivajo na dinamiko toka podzemne Pivke. Glavne passage constrictions, sumps and by-passes. Using a formal parametre teh odsekov smo določili z inverzno metodo, ki te- inverse procedure, we determined the geometry of this key sec- melji na algoritmu soseske (Neighbourhood algorithm, NA) in tions by fitting predicted to observed stages, and we achieved a pri tem dobili odlično ujemanje med modelom in podatki. -
JULIAN ALPS TRIGLAV NATIONAL PARK 2The Julian Alps
1 JULIAN ALPS TRIGLAV NATIONAL PARK www.slovenia.info 2The Julian Alps The Julian Alps are the southeast- ernmost part of the Alpine arc and at the same time the mountain range that marks the border between Slo- venia and Italy. They are usually divided into the East- ern and Western Julian Alps. The East- ern Julian Alps, which make up approx- imately three-quarters of the range and cover an area of 1,542 km2, lie entirely on the Slovenian side of the border and are the largest and highest Alpine range in Slovenia. The highest peak is Triglav (2,864 metres), but there are more than 150 other peaks over 2,000 metres high. The emerald river Soča rises on one side of the Julian Alps, in the Primorska re- gion; the two headwaters of the river Sava – the Sava Dolinka and the Sava Bohinjka – rise on the other side, in the Gorenjska region. The Julian Alps – the kingdom of Zlatorog According to an ancient legend a white chamois with golden horns lived in the mountains. The people of the area named him Zlatorog, or “Goldhorn”. He guarded the treasures of nature. One day a greedy hunter set off into the mountains and, ignoring the warnings, tracked down Zlatorog and shot him. Blood ran from his wounds Chamois The Triglav rose and fell to the ground. Where it landed, a miraculous plant, the Triglav rose, sprang up. Zlatorog ate the flowers of this plant and its magical healing powers made him invulnerable. At the same time, however, he was saddened by the greed of human beings. -
TRIGLAV NATIONAL PARK (Slovenia)
Strasbourg, 6 January 2003 PE-S-DE (2002) 22 [diplome/docs/2003/de06e_03] English only Committee for the activities of the Council of Europe in the field of biological and landscape diversity (CO-DBP) Group of specialists – European Diploma of Protected Areas 20-21 January 2003 Room 2, Palais de l'Europe, Strasbourg TRIGLAV NATIONAL PARK (Slovenia) APPLICATION for the European Diploma of Protected Areas Document established by the Directorate of Culture and Cultural and Natural Heritage This document will not be distributed at the meeting. Please bring this copy. Ce document ne sera plus distribué en réunion. Prière de vous munir de cet exemplaire. PE-S-DE (2003) 22 - 2 - INFORMATION FORM FOR NEW APPLICATION FOR THE EUROPEAN DIPLOMA OF PROTECTED AREAS Council of Europe European Diploma Information form for Candidate Sites This form is also available on diskette Site code (to be given by the Council of Europe) 1. SITE IDENTIFICATION 1.1. SITE NAME Triglavski narodni park 1.2. COUNTRY Slovenija 1.3. DATE CANDIDATURE 1.4. SITE INFORMATION COMPILATION DATE Y Y Y Y M M D D - 3 - PE-S-DE (2003) 22 1.5. ADDRESSES: administrative authorities National authority Regional authority Local authority Name: Name: Name: Javni zavod Triglavski Address: Address: narodni park Address: Triglavski narodni park, Kidričeva 2, 4260 Bled, Slovenija Tel. +386 4 5780 200 ............. Tel.......................................... Tel. ......................................... Fax.+ 386 4 5780 201............. Fax. ........................................ Fax......................................... -
Isotopic Study of Karst Water
Jr-> n <'-' FKPOPT KO. IABA-R-2845-F TITLE Isotopic study of Karst water PIKAL RKPOPT FOR THE-'PERIOD I98I-O4-OI - 1984-05-31 AUTHOR(S) H. Leskovsek-Sefman INSTITUTE Institute "Jozef Stefan" Ljubljana Yugoslavia INTEPKATIONAL ATOMIC EMFFGY ACEKCY DATE January 1985 FINAL REPORT ON RESEARCH CONTRACT No. 2845/fcB ISOTOPIC STUDY OF KARST WATER J. Pezdic, H. Leskovsek-Sefman, T. Dolenec, J. Urbane April 1981 to December 1983 Ljubljana, 1984 univerza e. kardelja institut "jo2ef Stefan" Ijubljana, jugoslavija univerza o kardeljj institut"jo2ef Stefan" Ijubljanajugoslavija FINAL REPORT ON RESEARCH CONTRACT No. 2845/RB ISOTOPlC STUDY OF KARST WATER I J. Pezdic, H. Leskovsek-Sefman, T. Dolenec, J. Urbane I J.Stefan Institute, University E. Kardelj, Ljubljana, Yugoslavia I April 1981 to December 1983 1 1 I 1 I 1 i Ljubljana, 1984 I I CONTENTS INTRODUCTION GEOLOGICAL AND CLIMATIC CHARACTERISTICS 4 Precipitation 4 PLANINA CAVE 8 Streamlet 1 10 I Streamlet 6 and Tihi rov 16 1 CAVE CARBONATES 21 UUBLJANICA RIVER BASIN 27 I THE WATER CATCHMENT AREA OF Rlf ANA 32 i THE WATER CATCHMENT AREA OF IDRIJCA 38 CONCLUSIONS 42 i REFERENCES 46 I I 1 I I I Final Report on Research Contract No. 2845/RB - July, 1984 I ISOTOPIC STUDY OF KARST WATER I J. Pezdic, H. Leskovsek-Sefman, T. Dolenec, J. Urbane I J. Stefan Institute, University E. Kardelj, Ljubljana, Yugoslavia I Summary I Mass spectrometric investigations of the isotopic composition of some elements in water and in dissolved carbonates from the Slovenian Karst are presented. Additionally, the isotopic composition of oxygen and I carbon in cave carbonates is given. -
Contaminated Sites and Health
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Effects of the Vadose Zone On
COBISS 1.01 EFFECTS OF THE VADOSE ZONE ON GROUNDWATER FLOW AND SOLUTE TRANSPORT CHARACTERISTICS IN MOUNTAINOUS KARST AQUIFERS – THE CASE OF THE JAVORNIKI–SNEŽNIK MASSIF (SW SLOVENIA) VPLIVI NEZASIČENE CONE NA ZNAČILNOSTI TOKA PODZEMNE VODE IN PRENOSA TOPNIH SNOVI V GORSKIH KRAŠKIH VODONOSNIKIH - PRIMER JAVORNIŠKO - SNEŽNIŠKEGA MASIVA (JZ SLOVENIJA) Metka PETRIČ1, Janja KOGOVŠEK1 & Nataša RAVBAR1 Abstract UDC 556.34(497.471) Izvleček UDK 556.34(497.471) Metka Petrič, Janja Kogovšek & Nataša Ravbar: Effects of the Metka Petrič, Janja Kogovšek & Nataša Ravbar: Vplivi ne- vadose zone on groundwater flow and solute transport char- zasičene cone na značilnosti toka podzemne vode in prenosa acteristics in mountainous karst aquifers – the case of the Ja- topnih snovi v gorskih kraških vodonosnikih - primer Javor- vorniki–Snežnik massif (SW Slovenia) niško - Snežniškega masiva (JZ Slovenija) Tracer tests are rarely applied in mountainous karst aquifers due Sledilni poskusi sodijo med metode, ki neposredno prikazujejo to difficult or limited basic data acquisition, problems of access značilnosti toka podzemne vode. Zaradi oteženih ali omejenih and expected strong tailing effects in tracer breakthrough. They dostopov do osnovnih podatkov, zahtevnosti terenskega dela in are, however, a straightforward method for learning about the pričakovanega dolgotrajnega podaljšanja pojavljanja sledila se characteristics of underground water flow. The main aim of this sledilni poskusi v gorskih kraških vodonosnikih redko izvajajo. study was to better understand the processes of flow and storage Glavni namen te študije je bil boljše razumevanje procesov toka in the karst aquifer and its unsaturated (vadose) zone, which is in skladiščenja v kraškem vodonosniku in njegovi nezasičeni several hundreds of metres thick. -
Slovenia: the European Cycling Gem You’Ve Never Heard Of
Slovenia: The European Cycling Gem You’ve Never Heard Of Story and photos by Carolyn Bys and Tyler Robertson fter several years of working, living, and, most important,A cycling around Central Europe, we were excited to finally cross into the northern edge of the Balkan Peninsula and into Slovenia. And, when we arrived, we were smitten. Sitting at the geocultural crossroads between Eastern and Western Europe and the Balkans, Slovenia is a land of contrasts. Italian flavored in the west with a distinct Austrian influence in the north while retaining the veneer of its former identity as Yugoslavia make a unique experience. Almost endless miles of gravel roads carried us over high ridges and along deep valleys. Dozens of storybook villages captured our attention throughout the countryside. Castles and churches seemed to sprout from the hilltops like mushrooms after the rain. Not only did Slovenia have these varied cultural influences, the terrain was equally diverse. We could ride the best of Europe — wine country, the Alps, and the Story and photos by Mediterranean — in a cross-country jaunt of roughly 1,000 kilometers. After an all-too-brief visit on our Carolyn Bys and Tyler Robertson trip from Prague, Czech Republic, to Dubrovnik, Croatia, we resolved to 20 Miles return and discover some of the best A H T R I Grad Slovenian bike-touring routes. A U S U N G Crna Na Maribor Secrets of the East Slovenj Lendava A Kranjska Koroskem Gradec Our journey began in early June, Gorta Jeruzalem R Y with a four-day, 300-kilometer loop Lake Bled from Maribor, Slovenia’s second city, Kranj A along the eastern borders and through Tolmin I Y the hilly wine-growing regions of L Ljubljana N CROATIA Jeruzalem, Lendava, and Goricko. -
Pretoki Rek V 21. Stoletju V Sloveniji Rezultati Projekta Ocena Podnebnih Sprememb V Sloveniji Do Konca 21
Pretoki rek v 21. stoletju v Sloveniji Rezultati projekta Ocena podnebnih sprememb v Sloveniji do konca 21. stoletja dr. Mira Kobold Ljubljana, 12. november 2018 VSEBINA • Stanje voda v obdobju meritev – Medletna spremenljivost pretokov – Trendi pretokov – Sprememba pretočnih režimov • Ocena hidroloških razmer do konca 21. stoletja – Orodja in metode – Rezultati analiz za hidrološke kazalnike (male, srednje in velike pretoke) – Napajanje podzemne vode STANJE VODA V OBDOBJU MERITEV Medletna spremenljivost in trendi pretokov Sava, v. p. Litija 280 230 /s) 3 (m 180 Pretok 130 80 1895 1905 1915 1925 1935 1945 1955 1965 1975 1985 1995 2005 2015 srednji letni pretok STANJE VODA V OBDOBJU MERITEV Medletna spremenljivost in trendi pretokov Sava, v. p. Litija 280 230 /s) 3 (m 180 Pretok 130 80 1895 1905 1915 1925 1935 1945 1955 1965 1975 1985 1995 2005 2015 srednji letni pretok 10-letno drseče povprečje linearni trend STANJE VODA V OBDOBJU MERITEV milijon m3/leto Kazalec letne rečne bilance Slovenije 45 000 40 000 35 000 30 000 25 000 20 000 15 000 10 000 5 000 1961 1963 1965 1967 1969 1971 1973 1975 1977 1979 1981 1983 1985 1987 1989 1991 1993 1995 1997 1999 2001 2003 2005 2007 2009 2011 2013 2015 odtok dotok razlika (neto odtok) linearni trend neto odtoka Kazalci okolja v Sloveniji Upad trendne črte neto odtoka v obdobju http://kazalci.arso.gov.si/ 1961–2016 (56 let): 14 % (2,5 % / 10 let) STANJE VODA V OBDOBJU MERITEV Spremembe pretočnih režimov Sava Bohinjka - Sveti Janez Ljubljanica - Moste alpski snežno-dežni režim dinarski dežno-snežni režim 2,5 2,5 2,0 2,0 1,5 1,5 1,0 1,0 0,5 0,5 mesečni pretočni količnik pretočni mesečni 0,0 količnik pretočni mesečni 0,0 1 2 3 4 5 6 7 8 9 10 11 12 1 2 3 4 5 6 7 8 9 10 11 12 1961-1990 1981-2010 1961-1990 1981-2010 Ščavnica - Pristava panonski dežno-snežni režim 2,5 2,0 • Upad spomladanskega viška, 1,5 dvig jesenskega. -
Povratne Dobe Velikih in Malih Pretokov Za Merilna Mesta Državnega Hidrološkega Monitoringa Površinskih Voda
POVRATNE DOBE VELIKIH IN MALIH PRETOKOV ZA MERILNA MESTA DRŽAVNEGA HIDROLOŠKEGA MONITORINGA POVRŠINSKIH VODA Sektor za analize in prognoze površinskih voda Urad za hidrologijo in stanje okolje November 2013 Agencija Republike Slovenije za okolje POVRATNE DOBE VELIKIH IN MALIH PRETOKOV Ve čina hidroloških procesov v naravi se zgodi naklju čno, zato je uporaba verjetnostne teorije in matemati čne statistike v hidrologiji neizogibna za reševanje hidroloških problemov in za boljši opis hidroloških procesov. Verjetnost nastopa dolo čenega pojava predstavlja eno izmed najpomembnejših analiz hidroloških podatkov, kjer na podlagi predhodnih dogajanj napovedujemo dogodke v prihodnosti. Vsak napovedan dogodek (pretok) pa ima dolo čeno verjetnost nastopa. Zaradi enostavnosti in lažjega razumevanja v praksi verjetnost nastopa prikazujemo z njeno recipro čno vrednostjo, to je povratno dobo dogodka. Povratna doba je ocena časovnega intervala med dogodki. Pretok s povratno dobo 10 let je koli činska ocena pretoka, ki se v povpre čju pojavi enkrat na 10 let. Pomembno je poudariti, da je pojav dogodka slu čajen, saj se v kronološkem smislu dogodki ne pojavljajo vsakih 10 let, ampak pri čakujemo, da se bo dogodek pojavil 10- krat v 100 letih, ali v povpre čju vsakih 10 let. Povratne dobe smo izra čunali za najve čje letne pretoke (letne visokovodne konice – Qvk) in najmanjše male letne srednje dnevne pretoke (Qnp). Izra čun je narejen za lokacije merilnih mest državnega hidrološkega monitoringa površinskih voda z nizom podatkov vsaj 10 let (slika 1, preglednica 1). V izra čunih so upoštevana razpoložljiva obdobja podatkov do vklju čno leta 2010. Za ra čunanje povratnih dob smo uporabili Pearson III in Log Pearson III porazdelitveni funkciji, ki sta v hidrološki praksi najpogosteje uporabljeni metodi. -
Development of a New Biotic Index Based on Hyporheic Fauna for Water Quality Determination in Lotic Ecosystems
UNIVERSITY OF NOVA GORICA GRADUATE SCHOOL Uroš ŽIBRAT DEVELOPMENT OF A NEW BIOTIC INDEX BASED ON HYPORHEIC FAUNA FOR WATER QUALITY DETERMINATION IN LOTIC ECOSYSTEMS Dissertation Supervisor: prof. dr. Anton Brancelj Nova Gorica 2012 Ţibrat, U.: Development of a new biotic index based on hyporheic fauna for water quality determination in lotic ecosystems. PhD thesis. University of Nova Gorica, Graduate school, 2012 Auch dem Wasser darf es in Kanälen Nie am Laufe, nie an Reine fehlen. J. W. von Goethe II ABSTRACT We assess water quality and the status of water bodies with numerous variables, both abiotic and biotic. Up to date, few water quality assessment and ecoremediation measures took the surface water – groundwater ecotone (i.e. the hyporheic zone) into consideration. We developed a new index based on hyporheic copepod fauna. The copepod biodiversity in the hyporheic of 26 Slovenian rivers, belonging to all five river basins, was assessed, and 49 species, belonging to 6 families were found. Species accumulation curves and richness estimators indicated that our sampling effort was sufficient, all estimates pointed toward a richness of 50 species. Two biodiversity hotspots were identified, but one of them was found to have an uneven species distribution, indicating human-impacted sites. One species (Moraria radovnae) appears to be endemic. Differences in relative abundances of the most common species accounted for most of the differences between river basins. The hyporheic copepod community, combined with an accurate typology and diversity measures, and while considering the limitations of our model, can be used for water quality assessment. The obtained final model is most accurate in mid-range classes, while being inaccurate at extreme values. -
Phytosociological Analysis of Riverine Forests Along the Sava Bohinjka, Radovna, Učja and Slatenik Rivers in Northwestern Slovenia
PHYTOSOCIOLOGICAL ANALYSIS OF RIVERINE FORESTS ALONG THE SAVA BOHINJKA, RADOVNA, UČJA AND SLATENIK RIVERS IN NORTHWESTERN SLOVENIA FITOCENOLOŠKA ANALIZA LOGOV OB SAVI BOHINJKI, RADOVNI, UČJI IN SLATENIKU V SEVEROZAHODNI SLOVENIJI Igor DAKSKOBLER1,2 & Andrej ROZMAN2 ABSTRACT UDC 630*26(497.452):581.9 IZVLEČEK UDK 630*26(497.452):581.9 Phytosociological analysis of riverine forests along the Fitocenološka analiza logov ob Savi Bohinjki, Radovni, Sava Bohinjka, Radovna, Učja and Slatenik Rivers in Učji in Slateniku v severozahodni Sloveniji northwestern Slovenia Po standardni srednjeevropski metodi smo Applying the standard Central-European method we fitocenološko raziskali obrežne gozdove ob rekah Savi Boh- conducted a phytosociological study of riverine forests along injki, Radovni, Učji in potoku Slatenik v severozahodni the rivers Sava Bohinjka, Radovna, Učja and the Slatenik Sloveniji in jih primerjali s podobnimi logi v povodju Soče brook in northwestern Slovenia and compared them to sim- ter v sosednjih državah Hrvaški, Avstriji in Italiji. Na podla- ilar riverine forests in the Soča river basin and the neigh- gi te primerjave smo jih uvrstili v naslednje sintaksone: Sa- bouring countries of Croatia, Austria and Italy. Based on licetum eleagno-purpureae, Salicetum albae, Lamio or- this comparison they were classified into the following syn- valae-Salicetum eleagni (tudi v novo subasociacijo -cari- taxa: Salicetum eleagno-purpureae, Salicetum albae, cetosum eletae) in Lamio orvalae-Alnetum incanae (tudi Lamio orvalae-Salicetum eleagni (also in the new subas- v novi subasociaciji -fraxinetosum excelsioris in -rhamne- sociation -caricetosum eletae) and Lamio orvalae-Alne- tosum fallacis). Opisali smo sukcesivno nadomeščanje tum incanae (also in the new subassociation -fraxineto- (conacijo) združb ob Savi Bohinjki od inicialnih prodišč sum excelsioris and -rhamnetosum fallacis). -
63/2005, Uredbeni
PRILOGA 1: Seznam vodnih teles, imena in šifre, opis glede na uporabljena merila za njihovo dolo�itev in razvrstitev naravnih vodnih teles v tip Merila, uporabljena za dolo�itev vodnega telesa Zap. Šifra Povodje ali Površinska voda Ime vodnega telesa Vrsta Razvrstitev Tip Pomembna Presihanje Pomembna Pomembno št. pore�je v tip hidro - antropogena razli�no morfološka fizi�na stanje sprememba sprememba 1 SI1118VT Sava Radovna VT Radovna V 4SA x x x 2 SI111VT5 Sava Sava Dolinka VT Sava izvir – Hrušica V 4SA x x x 3 SI111VT7 Sava Sava Dolinka kMPVT zadrževalnik HE Moste kMPVT x 4 SI1128VT Sava Blejsko jezero VTJ Blejsko jezero J A2 x 5 SI112VT3 Sava Bohinjsko jezero VTJ Bohinjsko jezero J A1 x 6 SI112VT7 Sava Sava Bohinjka VT Sava Sveti Janez – Jezernica V 4SA x x 7 SI112VT9 Sava Sava Bohinjka VT Sava Jezernica – soto�je s Savo Dolinko V 4SA x x 8 SI114VT3 Sava Tržiška Bistrica VT Tržiška Bistrica povirje – soto�je z Lomš�ico V 4SMS x x 9 SI114VT9 Sava Tržiška Bistrica VT Tržiška Bistrica soto�je z Lomš�ico – V 4SA x x x Podbrezje 10 SI116VT5 Sava Kokra VT Kokra Jezersko – Preddvor V 4SA x x x 11 SI116VT7 Sava Kokra VT Kokra Preddvor – Kranj V 5SA x x x 12 SI121VT Sava Poljanska Sora VT Poljanska Sora V 4SS x x 13 SI122VT Sava Selška Sora VT Selška Sora V 4SS x x 14 SI123VT Sava Sora VT Sora V 5SS x x x 15 SI1324VT Sava Ra�a VT Ra�a z Radomljo V 4SS x x x 16 SI1326VT Sava Pšata VT Pšata V 5SA x x 17 SI132VT1 Sava Kamniška Bistrica VT Kamniška Bistrica povirje – Stahovica V 4SMA x x x 18 SI132VT5 Sava Kamniška Bistrica VT Kamniška Bistrica Stahovica – Študa V 5SA x x x 19 SI132VT7 Sava Kamniška Bistrica VT Kamniška Bistrica Študa – Dol V 5SA x x 20 SI14102VT Sava Cerkniš�ica VT Cerkniš�ica V 5SMA x x 21 SI141VT1 Sava Jezerski Obrh VT Jezerski Obrh V 5SMA x x 22 SI141VT2 Sava Cerkniško jezero VTJ Cerkniško jezero J JDP x x 23 SI143VT Sava Rak VT Rak V 5SA x x 1/7 Merila, uporabljena za dolo�itev vodnega telesa Zap.