Geografski oris občine Loški Potok:
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| Format: | Buch |
| Sprache: | Slovenian |
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Ljubljana
Znanstvena založba Filozofske fakultete
2022
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| Ausgabe: | Prva izdaja |
| Schriftenreihe: | GeograFF
25 |
| Schlagworte: | |
| Online-Zugang: | Inhaltsverzeichnis Abstract Register // Gemischte Register |
| Beschreibung: | Auflage 200 |
| Beschreibung: | 244 Seiten Illustrationen, Diagramme, Karten 24 cm |
| ISBN: | 9789610605591 |
Internformat
MARC
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| 245 | 1 | 0 | |a Geografski oris občine Loški Potok |c Matej Ogrin (ur.) |
| 250 | |a Prva izdaja | ||
| 264 | 1 | |a Ljubljana |b Znanstvena založba Filozofske fakultete |c 2022 | |
| 300 | |a 244 Seiten |b Illustrationen, Diagramme, Karten |c 24 cm | ||
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| 338 | |b nc |2 rdacarrier | ||
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| 856 | 4 | 2 | |m Digitalisierung BSB München 19 - ADAM Catalogue Enrichment |q application/pdf |u http://bvbr.bib-bvb.de:8991/F?func=service&doc_library=BVB01&local_base=BVB01&doc_number=034310840&sequence=000001&line_number=0001&func_code=DB_RECORDS&service_type=MEDIA |3 Inhaltsverzeichnis |
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| 856 | 4 | 2 | |m Digitalisierung BSB München 19 - ADAM Catalogue Enrichment |q application/pdf |u http://bvbr.bib-bvb.de:8991/F?func=service&doc_library=BVB01&local_base=BVB01&doc_number=034310840&sequence=000005&line_number=0003&func_code=DB_RECORDS&service_type=MEDIA |3 Register // Gemischte Register |
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Datensatz im Suchindex
| _version_ | 1804185346668232704 |
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| adam_text | GeograFF 25 KAZALO Predgovor........................................................................................................................... 9 Uvod....................................................................................................................................11 Uroš Stepišnik I Geomorfološke značilnosti......................................................................................... 13 l.l Fizičnogeografske značilnostiLoškega Potoka............................................................... 13 1.2 Geomorfološke značilnosti.......................................................................................... 16 1.3 Sklepne geomorfološke ugotovitve............................................................................. 20 Darko Ogrin, Matej Ogrin, Miroslav Vysoudil 2 Splošno in lokalno podnebje..................................................................................... 23 2.1 Splošne podnebne poteze...........................................................................................23 2.1.1 Padavinski postaji Hrib-Loški Potok in Trava................................................... 26 2.1.2 Opis temperaturnih razmer glede na meritve amaterske meteorološke postaje Hrib-Loški Potok in primerjava s postajama Nova vas na Blokah in Babno Polje......................................................... 28 2.2 Nekatere lokalne podnebne značilnosti....................................................................... 33 2.2.1 Lokalne razlike v
osončenosti.......................................................................... 35 2.3 Toplotni odziv površja v Loškem Potoku..................................................................... 36 2.3.1 Primerjava toplotnih razmer površja med dnevom in nočjo........................... 36 2.3.2 Primerjava toplotnih razmer površja ob radiacijskem in advekcijskem vremenu......................................................................... 38 2.4 Vpliv izoblikovanosti in pokrovnosti površja na temperaturo zraka........................... 39 2.4.1 Zniževanje temperature zraka z višino............................................................. 39 2.4.2 Temperaturni obrat v konkavnih oblikahLoškega Potoka................................. 42 2.4.3 Zimske razmere................................................................................................ 43 2.4.4 Poletne razmere............................................................................................... 45 2.4.5 Maršrutne meritve minimalnih temperatur obradiacijskem vremenu............. 47 2.4.6 Topoklimatska karta...................................................................................... 48 Tajan Trobec 3 Hidrogeografske značilnosti........................................................................................ 57 3.1 Naravnogeografski dejavniki odtoka......................................................................... 57 3.2 Površinske tekoče vode.............................................................................................57 5
Geografski oris občine Loški Potok ■ 3.3 Podzemne vode in podzemne vodne povezave............................................................... 59 3.4 Odtočne značilnosti, pretoki in poplave........................................................................... 60 3.5 Bogastvo preostalih vodnih virov in vodooskrba............................................................ 67 3.6 Pritiski na vodne vire in kakovost voda............................................................................ 73 Blaž Repe 4 Prsti in rastlinstvo.................................................................................................. 85 4.1 Preučevanje prsti in rastlinstva v občini Loški Potok.....................................................85 4.2 Nekatere splošne značilnosti prsti in rastlinstva .......................................................... 88 4.3 Pedoskevence na trdih sedimentnih silikatnih kamninah v dolini reke Čabranke (lito- in toposekvenca)....................................................................................................... 90 4.3.1 Morfološke značilnosti podrobno preučenih prsti..............................................94 4.4 Primer lito- in toposekvence........................................................................................... 101 4.5 Tujerodne invazivne rastlinske vrste................................................................................ 108 Urška Pajnič, Andrej Gaspari 5 Arheološka najdišča Loškega Potoka in vpetost prostora v širšo regionalno podobo dinarskokraške pokrajine med prazgodovino in
srednjim vekom............................................................................................ 113 5.1 Pregled raziskav................................................................................................................. 113 5.2 Pregled najdišč po obdobjih............................................................................................. 116 5.3 Pogled naprej......................................................................................................................121 Vlado Mohar 6 Začetki Loškega Potoka..................................................................................... 125 6.1 Nekaj najstarejših navedb dogajanja na območju današnjega Loškega Potoka.........125 6.2 Nastanek imena................................................................................................................. 128 6.3 Od kod so prišli prvi naseljenci?...................................................................................... 129 6.4 Gospodarska slika leta 1573............................................................................................ 132 6.5 Gospodarska slika leta 1621........................................................................................... 136 6.6 Življenje v Loškem Potoku vztraja še danes................................................................. 137 6.7 Razlaga izrazov................................................................................................................... 141 Vera Smole 7 Loškopotoški govor - naglas, glasoslovje in
besedila...................................... 145 7.1 Kraj in ljudje....................................................................................................................... 145 7.2 Projekt ŠIPK...................................................................................................................... 146 7.3 Umestitev govora............................................................................................................... 147 6
GeograFF 25 7.3.1 Zgodovina dolenjskega narečja....................................................................... 147 7.3.2 Sedanje stanje dolenjskega narečja................................................................. 148 7.4 Fonološki opis govora................................................................................................ 150 7.5 Besedila....................................................................................................................166 7.5.1 Informatorji, snemalci in čas posnetkov......................................................... 166 7.6 Na kratko o potoškem govoru.................................................................................. 175 Blanka Bartol 8 Potoška krajina včeraj, danes, jutri?................................................................... 177 8.1 Potoška krajina in njena zgradba................................................................................ 177 8.2 Zgodovinski razvoj krajine....................................................................................... 178 8.3 Krajinske značilnosti.................................................................................................. (81 8.4 Krajinski vzorci......................................................................................................... 183 8.5 Izjemna krajina Retje.................................................................................................. 185 8.6 Spremembe v krajini................................................................................................... 188
8.6.1 Spremembe krajinena območju Retij ............................................................ 191 8.7 Kakšna naj bo prihodnost?......................................................................................... 191 Kristina Glojek,Asta Gregorič, Griša Močnik, Luka Drinovec, Honey Dawn C.Alas, Andrea Cuesta - Mosquera, Kay Weinhold, Maik Merkel, Thomas Müller, Martina Ristorini, Dominik van Pinxteren, Hartmut Herrmann, Alfred Wiedensohler, Matej Ogrin 9 Onesnaženost zraka z delci in s črnim ogljikom.............................................. 195 9.1 Koncentracije delcev PMo in črnega ogljika (BC)...................................................... 196 9.2 Viri črnega ogljika (BC) in časovno spreminjanje koncentracij................................. 198 9.4 . Prostorsko spreminjanje koncentracij PM2.S glede na stabilnost ozračja............ 200 9.5 Loški Potok je pokazatelj kakovosti zraka dolin, kraških polj in drugih kotanj hribovitih območij.........................................................................201 Nina Krašovec, Klara Cevka,Tadeja Babič, Matej Ogrin, Kristina Glojek 10 Študija ranljivosti okolja................................................................................... 207 10.1 Ranljivost okolja....................................................................................................... 207 10.2 Pokrajinskoekološka členitev in tipizacija................................................................ 208 10.3 Pokrajinskoekološka regionalizacija.........................................................................
209 10.4 Ocena nosilnih sposobnosti okolja.......................................................................... 210 10.5 Ocena dosežene stopnje obremenitve okolja......................................................... 213 10.6 Ocena ranljivosti okolja Loškega Potoka................................................................. 216 10.7 Razvoj in skrb za občutljivo kraško pokrajino......................................................... 218 7
Geografski oris občine Loški Potok I 11 Sklepne misli....................................................................................................... 221 Summary.................................................................................................................. 225 Seznam slik.................................................................................................................................. 229 Seznam preglednic...................................................................................................................... 234 Stvarno kazalo..............................................................................................................................237 Avtorji........................................................................................................................................... 239 8
GeograFF 25 I Summary The archaeological picture of Loški Potok, even if fragmentary, points to the settle ment of this area in the first centuries of the first millennium BC. However, research ers allow for the possibility of an even older human presence in this area. We do not know exactly when today s settlement of Loški Potok was established, but mentions indicate as early as the end of the 15th century AD .The strategic location of Tabor Hill has been proven for centuries, as the inhabitants of Loški Potok used this place around 1500 as their first fortress, where they defended themselves and their liveli hood from bandits, and later an anti-Turkish camp was established there. What drove people to the forested karst landscape, far from the wide plains and rolling hills? Was it the forests or the agrarian overpopulation elsewhere? Difficult natural conditions and a dangerous location due to exposure toTurkish invasions and other bandits hin dered the smooth development of the Loški Potok and Draga Valley. Today we can not imagine that the traditional cultural landscape, perhaps most typically reflected in the view from Tabor to Retje, reflects the centuries-long struggle of the people of Loški Potok and Draga Valley not only with nature, but also with various conquerors of the region. The long, continuous presence of people on the territory of Loški Potok and Draga Valley has led to the development of special linguistic features, which are not uni form. In the villages of Mali Log, Retje, Hrib, Šegova vas, Srednja vas and Travnik, one of the local dialects of the
tonemic Dolenjska dialect (southern) of western type is spoken, while in the villages of Lazeč, Podpreska, Draga, Srednja vas pri Dragi, Stari and Novi Kot and Trava, the non-tonemic Kostel dialect is already spoken, and both belong to the Dolenjska dialect group. The surface of the Loški Potok and Draga Valley landscape is now interpreted as a typical karst surface, which is also reshaped by forms of fluvial material transfer. In the elongated lowland that runs through the western part of the area, there are two typi cal karst fields: Retje and Travnik. According to the morphodynamic characteristics, the Retje field is defined as an occasional lake field and the Travnik field as an over flowing karst field. Occasional flooding also indicates land use and limits settlement of areas with regular flooding. Both fields are also distinct frost hollows and the set tlements of Retje and Travnik are among the coldest settlements in Slovenia, along side Babno Polje, Rakitna or the settlements on the plateau of Bloke. Although the inhabitants of Loški Potok have always been farmers, the climate is not particularly favourable for them, and in the past was even more unfavourable. The short grow ing season with frequent cold spells, which can bring frost from August to June, has given rise in folk tradition to the saying that winter in Loški Potok lasts nine months and then it is cold for three months. Loški Potok and Draga Valley are relatively humid areas of Slovenia, especially in the higher parts of the region. Lower temperatures and reduced evaporation also con tribute to
humidification, but the actual availability of water on the predominantly 225
Geografski oris občine Loški Potok I karstified surface is severely limited. Surface runoff is reduced due to the large forest cover that is a hallmark of the area. Nevertheless, the area has a higher than aver age runoff coefficient, reaching values between 60 and 70% of precipitation, which is above the Slovenian average (Frantar, 2008). With a relatively high level of precipitation the region is thus wet, but due to the geological karst structure the water is more difficult to access, and the self-purify ing power of the water is also limited. The extreme south-eastern part of the mu nicipality of Loški Potok, which does not belong to the Loški Potok - Draga Valley region, stands out from this framework. Here is the headwaters of the Čabranka river, practically the only part of the Loški Potok municipality with fluvial relief and the most water-rich river course. The source of the Čabranka is a karst spring, but the water-resistant geological base enables its surface drainage towards Osilnica, where it flows into the Kolpa River. In addition to geomorphological and hydrological features, the geological struc ture also determines the pedogenetic processes, of which the following are pre dominant in Loški Potok and Draga Valley : Humus accumulation, slow weathering of the hard carbonate parent rock and rather modest formation of fine soil parti cles. As a result, young soil stages are predominant, which are shallow, have a low clay content and high reaction (the pH fluctuates around the neutral value). Due to the carbonate parent rock, the saturation with bases is
high. These factors, pro cesses and general characteristics were also confirmed by field research at 48 sites. Accordingly, in the Loški Potok municipality Rendzina is predominant, appearing on up to 64% of the area, followed by brown Chromic Cambisolsoils with 33%. A modest proportion of Dystric Brown soils occur in the extreme south, and in some places Eutric Brown soils occur in the bottom of the elongated lowland. The agrar ian settlement of Loški Potok and the Draga Valley is also reflected in a very special cultural landscape, which occupies a special place among Slovenian landscapes. The landscape features in the municipality of Loški Potok are shaped by natural or culturally determined landscape elements and patterns. In some cases, the natu ral morphology carries built accents such as churches and chapels, such as Tabor hill with two churches and a cemetery, and the church in Draga with linden trees, which stands on a hill in front of the village in a place visible from both Podpreska and Srednja vas near Draga. Other landscape elements are individual trees or groups of trees on farmland, usually lime trees, which often mark crosses, chapels, and churches, or other types of fruit or forest trees along roads; orchards; shrub vegetation; patches of forest on steeper parts of depressions; stone walls along some field paths, puddles or ponds; springs; rocks on farmland; streambeds of permanent and occasional streams, etc. A study of the vulnerability of the municipality of Loški Potok showed a moderate impact of human activities. In most geo-ecological units air and
water quality as sessments reach a state of low pollution, due to the low density of settlements and population. The situation is different in the settlements in the karst fields of Retje and Travnik. Due to the lower self-cleaning capacity of the atmosphere in the two depres sions, even a small number of households in winter causes air pollution with black carbon (BC) and particulate matter comparable to that of larger cities in valleys and 226
GeograFF 25 basins. The measurements also show that particulate air pollution in smaller popu lated hollows in rural areas can be much higher than is generally assumed. At the time of the temperature inversions, the inhabitants of the bottom of both karst fields are most exposed to high concentrations of BC and PM particles. The measured concentrations of the pollutants in question during the winter temperature inver sions are of great concern, as in the evenings they reach the level of the most pol luted areas in the world, such as the city of Delhi in India (Apte et al., 2011 ; Goel et al., 2015; WHO, 2016). How should this area develop in the future? Although it is a sensitive karst area with limited carrying capacity, for the preservation of the traditional cultural landscape, its functions and structure, depopulation of the area and aging are also problematic processes. In addition, environmental changes due to climate change will shape the Dinaric regions, which include Loški Potok and Dragarska dolina, in the coming dec ades. The traditional and recognized cultural landscape of Loški Potok and Dragarska dolina must find a place in the municipal development plans for the coming decades. The municipality should continue the transition to renewable energy sources (biomass, wind energy), support the maintenance of quality forests and wood process ing, strengthen local entrepreneurship, including forms of rural tourism, and mitigate the effects of transport-related remoteness by accelerating digitalization. 227
GeograFF 25 Stvarno kazalo A advekcijski (alohtoni) tip vremena 34, 36,38,40 Alisol 97,99 amonij 75-76,78 analiza lidarskih posnetkov 113,115, 120,185 Ängströmov eksponent 198 Anton Skubic 126-127,132 arheološka topografija 113,115,121, 178 B Blate 64-65,74 Blošček 19,70,177-178,190 bukovi gozdovi 88-91,93,97 C CAI 113,115,118-120 Cambisol 96,104,226 cerkev 9,115,117,120,126-127,145, 169,178,180-182,184,186-188, 191,222 Claustra Alpinum luliarium 113,121, 125 Claustra Alpium luliarum 113,121,125 č Čabranka 14,23,36,39-47,50,52, 57-65,67,74-77,79,85,90-92, 100-102,104,113,116,120,126, 180,209-210,212-213,215-216, 218,222,226 čistilna naprava 59,73,76,214 črni og ljik (BC) 11,195-201,215,222 D dediščina 12,70-71,114,146,182,187, 192 delci 9,11,88,90,99,101 -103,195198,201-202,215,222 delci PM 195-198,200-202,215,222 depopulacija 218,223 destruktivni geomorfni procesi 211,213 dinarska pregrada 24 dinarski jelovo bukovi gozdovi 88 distrične rjave prsti 88,91,99-100,103, 222 dolek 67 dolenjska narečna skupina 147,221, 225 dolenjsko narečje 147-149,153,175, 221,225 dolomit 14-18,21,75,85,91 -92,94,99, 104,210 Dragarsko podolje 13-14,19-20, 209-210,212,214-216 drevesa 40,51,128,133,181 -182,222 E ekološko stanje 74 ekosistemske storitve 218,223 energija Sončevega obsevanja 34-35, 39,48 enoletna suholetnica 109 erozijski jarek 14,16-18,21,92 estavela 20 F fizikalne lastnosti prsti 94-98 fizikalno-kemijski parametri 78 fluviokras 13-14,16-18,21,66 fluviokraški relief 14,21 fluviokrašo površje 13,16 fonološki opis govora 150 fosfati 75-76,78 Frančišek Kramer 126 G GIS študije 120
Glažuta 12,14,68,79,114,120-121, 180,209-210,212,215-216,218 237
Geografski oris občine Loški Potok • Glažutarsko podolje 13-14,20 Gleysol 98,105 glinovec 92,98 globina prsti 85,87,89,94-101,103 Goteniška gora 13-14,20,23,36,39,50, 57, 60,68, 74-75,209-210,212,215, 216 gozdna združba bukve in spomladanske torilnice 88 gozdne združbe 87-91,93 gozdni ekosistem 219 Gradišče 115,117,119,125,187 greznica 73,76 grumbla 182-183,185,190,222 H horizont 25,36,85,88-89,94-99, 101-102,118 hranila 76,103,106 Hrib 9,11 -13,25-33,36,51 -52,57,59, 72-73, 76, 79,93,103,109,114-115, 117,136-137,145,147,167,178180,182-184,186-189,200-201, 214,221,225 hrvatarstvo 137,140 huba 130-131,134-139,141 hudourniški potok 57,67,93 I identiteta 70,148,178,191 -192 indeks kakovosti zraka 198,200-202 individualna kurišča 214,218 interaktivni spletni slovar 146 Iso Cluster Unsupervised Classification 209 izhlapevanje 36,57,66,221 izprane prsti, luvisol 91,99-100,102-103 izvir 16,20,58-60,64,67-70, 72, 74-76, 78-79,91,98,11,3, 128,182,184, 222 izvor naglasa 151,153,175 izvor samoglasnikov 153 izvor soglasnikov 163 J Janez Andrej Turjaški 127 japonski dresnik, dresniki 108-110 238 Jernej Pečnik 114,117,125,178 jezera hladnega zraka 50,52,201, 213 jezikovna dediščina 146 K kakovost vode 73-75 kakovost zraka 11-12,28,42,195-198, 200-202,214-215,218 kal 68-72,75,78-79,182,222 kambične prsti, kambisoli 91,96-97, 99-100,102-103,106 kamnita orodja 116 kanalizacija 73-74,76,214 kapnica 68,70,73 karbonatna matična podlaga 57-58, 75-76,85,88,100,103-104,211, 222 kemične lastnosti prsti 94-99,101-102, 214 kemijsko stanje 74-75 keramika 114-118,120,125 kloridi 75-76,78 Kolačnik 117
kopasta vzpetina 13,16,19 kopasti hrbet 14,16 kopasti kras 13,18-20,209-210, 212-216,221 krajevni govor 147-149,175,221 krajina 12,177-178,180-192,222 kraško polje 13,15-16,19-21,28-29, 52,93,183-188,190-191,196,201, 209,212-217,221-222 kraško polje Travnik 13,15-16,20 kulturna pokrajina Loškega Potoka 218-219,221,223 kurilne naprave 202 L Laßerbach 128,134 Lenart Sigesdorf 126 Leptosol 91,94-95,99-102,104 ljudsko izročilo 146,221 lokalna identiteta 148 lokalno podnebje 33-34,42 loškopotoški govor 145-146 loškopotoški slovar 146
GeograFF 25 M mala hidroelektrarna 58-59 Malenščica 57-59,61 -64,72,75,78,180 Marjan Slabe 114,117,125 Martolozi 131 meljevec 57,59,222 meritve onesnaženosti zraka 196 mesečni pretočni režim 61-62,64,66, 55 Mežnarjev potok 20,43,58,68,75-76, 78,179-180,212 minimalne (najnižje) temperature 29-30,33,37-39,42-47,50-51,93 mlin 58-59,137-139 morfologija 181,185,222 morfološke značilnosti prsti 94-99,101 mrazišče 23,29,43-44,46-47,188,221 N nadmorska višina 16,20,23,25,28,31, 33,39-41,43,45,57,59,68,75,85, 87,89,91 -92,101 -102,145,177, 209-210 najmanjši pretok 61-62,64-65 največji pretok 61-62,64-65 naklon pobočja 17,99,100-101 narečna besedila 147,149-150 narečni govor 145-146 nasičenost s kisikom 76 nenadzorovana klasifikacija 208-209 nepopolno zgorevanje ogljičnih goriv 195 nitriti 75-76,78 O občasno ojezerjeno polje 20-21,27, 184-185,221 ocena dosežene stopnje obremenitve okolja 213-216 ocena nosilnih sposobnosti okolja 210-213 ocena regeneracijskih in nevtralizacijskih sposobnosti 207 octovec 108-109 Od volkodlaka do Klepca 126 odtočni količnik 57,221 odtok 57,61 -62,64-66,102,221 ogrevanje gospodinjstev na les 106, 196,199,201-202,215 okoljska nosilna zmogljivost 207,218 onesnažen zrak 9,42,195-196,201 202,214-218,222 osamelec 177,181-182,184,222 osončenost 25,35-36,50 P padavine 24-27,51-52,57,59,66-67, 73,75,91-93,100,221 parcela 115,141,180,183-184,186, 190-191 pedosekvenca 90-91,99-101,103-106 pelinolistna žvrklja, ambrozija 108-109 pHvode 76 plitvi kras 19-20 podeželje 196,202,222 podnebje nižjega gorskega sveta 23 podzemna bifurkacija 59,65,75 podzemna voda
16,19-20,57,59-60, 64-66,74-75,212 podzemne povezave 16,59-60,74 pogled 31,92,105,121,152,186,188, 190-191,196,221 pokrajinotvorna sestavina 207-208, 212-217 pokrajinskoekološka enota 207, 209-210,212,222 pokrajinskoekološka regionalizacija 209 pokrajinskoekološka tipizacija 208 pokrajinskoekološki tip 207-209,211 pokrajinskoekološko členitev 207-208, 210 pokriti kras 16-17 polovnik 135 ponikalnica 58,64,67 ponikva 18 popis rastlinstva 86-87 poplave 60-61,66-67,128-129,186, 188,212-213,217,221 porečje 16,59-60,64 posamična najdba 113,116,119,121 poselitev 21,67-68,71,73-74,115-117, 120-121,125,177-178,184-186, 188,191,213-215,218,221-222 Potočanska dolina 11,13 239
Geografski oris občine Loški Potok | povesmo 135-136 povodje 59 povprečni pretok 61-62,64 pozna antika 119-121 pozna bronasta doba 116-117 prelivno kraško polje 20-21,221 prevodnost vode 75-78 profil 39-41,47,87-88,94-98,101-102 prostor 113,115,117,119,121,125128,133,177-178,183-185,188189,191 -192,207,213,218,222 protiturški tabor 126,145,221 Pungert 79,91,115,120-121,180 R raba 13,21,33-35,48,58,73,85,88-89, 93,102-105,145,156,177,180,183, 185-186,188,191,209-210,213214,219,221 Račna gora 13-15,18-20,23,50,113, 117,119-120,184 radiacijski (avtohtoni) tip vremena 33, 36-40,42-43,45,47,50,52 Rakitnica 16,59-60,64-65,74-75 ranker 91,99,103 ranljivost 208,216,218,222 ranljivost okolja 207,209,216-218 rastlinstvo, rastlinski pokrov 85-88, 90-91,93,98,104-105,210 razvodje 59-60 razvodnica 59,63,66 rečna mreža 58,51,74,93,100 rečni pretočni količnik 62-64 regionalno ozadje 198,202 rendzine 88-89,91,99,212,222,226 Retje 9,12-14,16,19-21,23-25,27, 29,36-38,43,52,66,73,76-77,79, 103,106,109,115-117,125-126, 128,130,135-137,145,147,152, 167,178,180-181,183-184-185, 187-188,190,196-202,209-210, 212,214-216,218,221,225-226 Rettiach 134-136 rimska cesta 125 Rinža 16,59-60,64-65,74-75 rjave pokarbonatne prsti 88-89,91,210, 212,222 240 S samočistilna sposobnost 74-75,77,208, 212-213 samočistilne sposobnosti voda 75,77, 217,222 samočistilne sposobnosti zraka 213 silikatne kamnine 88,90-93,100,103 simbol 177,186 skupine govorov v dolenjskem narečju 149 skupna ocena obremenjenosti prsti 214 skupna ocena ranljivosti 216,218 snežna odeja 25-27,39,43,66,93 snovna kulturna dediščina 146
sondiranje 85,87 specifični odtok 61-62,64-66 srednji vek 113,120-121,178,186 starejša železna doba 117 stopnja obremenitve okolja 207, 213-216 stopnja obremenjenosti reliefa 213 stopnja obremenjenosti voda 214,218 sulična ost 118,120-121 Svetovna zdravstvena organizacija 200 š Senik 120,136 Študentski inovativni projekti za družbeno korist (ŠIPK) 146-147, 149-150,166 Tabor 9,12-13,19,28,42-44,46-47, 114-115,117-118,121,125-126, 145,152,177-182,184,186-188, 190,196-198,201,215,221 -222, 225-226 temperatura vode 75 temperaturna inverzija 31,93,195-198, 200-202,213,215,218 temperaturni obrat 23,39,42-43,45, 47-48,50 terensko proučevanje 222 termalno snemanje 34-37,52 tonemski naglas 147-148,175 topoklima 33-34,38,52 topoklimatska karta 48-49
GeograFF 25 trajanje Sončevega obsevanja 34-35, 42,52 transkripcija posnetkov 166 Travnik 13-16,19-21,28-29,35-36, 58-64,66,73,103,109-110,115, 120,126,129,136-137,145,147, 167,178-180,184,189,209-210, 212-216,218,221,225-226 trdota vode 75-77 tujerodne invazivne rastlinske vrste 108-109 zgodovina dolenjskega narečja 147149 zgorevanje biomase 196,198-200,218 zlata rozga 109 Zörrer 119 Ž žaga 58-59,106-107,137,140,180 živica 182-186,190,222 U urbar 129-141,178 uvala 13-14,16,18-21,42,59,66-67, 73,76,128,196,221 uvala Retje 19-20,59,66-67,73,76, 128,196 V Veliki Obrh 16,59,64-65,74-75 vertikalni temperaturni gradient 39 višina (količina) padavin 26-27,51,57, 66,91-92,100 višina snežne odeje 25-27 vodna bilanca 57 vododržna podlaga 69,222 vodomerna postaja 60-66 vodostaj 20,61 vodovarstveno območje 73-74,76 vodovod 68,72-74 vodozbirno zaledje 60-66 Votla stena 119,121 vročinski stres 219 vršaj 14,18,21 vršni (terminalni) poganjki 40-41 vrtača 16,18,20,35-36,42,57,182, 186,191,222 vsebnost kisika 75-76 vzorec 26,67,73,75-76,100,177-178, 181,183-184,186-187,189-190, 222 WRB 86,104-105 Z zbirka starih fotografij 146 zbirke starih predmetov 146 241
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GeograFF 25 KAZALO Predgovor. 9 Uvod.11 Uroš Stepišnik I Geomorfološke značilnosti. 13 l.l Fizičnogeografske značilnostiLoškega Potoka. 13 1.2 Geomorfološke značilnosti. 16 1.3 Sklepne geomorfološke ugotovitve. 20 Darko Ogrin, Matej Ogrin, Miroslav Vysoudil 2 Splošno in lokalno podnebje. 23 2.1 Splošne podnebne poteze.23 2.1.1 Padavinski postaji Hrib-Loški Potok in Trava. 26 2.1.2 Opis temperaturnih razmer glede na meritve amaterske meteorološke postaje Hrib-Loški Potok in primerjava s postajama Nova vas na Blokah in Babno Polje. 28 2.2 Nekatere lokalne podnebne značilnosti. 33 2.2.1 Lokalne razlike v
osončenosti. 35 2.3 Toplotni odziv površja v Loškem Potoku. 36 2.3.1 Primerjava toplotnih razmer površja med dnevom in nočjo. 36 2.3.2 Primerjava toplotnih razmer površja ob radiacijskem in advekcijskem vremenu. 38 2.4 Vpliv izoblikovanosti in pokrovnosti površja na temperaturo zraka. 39 2.4.1 Zniževanje temperature zraka z višino. 39 2.4.2 Temperaturni obrat v konkavnih oblikahLoškega Potoka. 42 2.4.3 Zimske razmere. 43 2.4.4 Poletne razmere. 45 2.4.5 Maršrutne meritve minimalnih temperatur obradiacijskem vremenu. 47 2.4.6 Topoklimatska karta. 48 Tajan Trobec 3 Hidrogeografske značilnosti. 57 3.1 Naravnogeografski dejavniki odtoka. 57 3.2 Površinske tekoče vode.57 5
Geografski oris občine Loški Potok ■ 3.3 Podzemne vode in podzemne vodne povezave. 59 3.4 Odtočne značilnosti, pretoki in poplave. 60 3.5 Bogastvo preostalih vodnih virov in vodooskrba. 67 3.6 Pritiski na vodne vire in kakovost voda. 73 Blaž Repe 4 Prsti in rastlinstvo. 85 4.1 Preučevanje prsti in rastlinstva v občini Loški Potok.85 4.2 Nekatere splošne značilnosti prsti in rastlinstva . 88 4.3 Pedoskevence na trdih sedimentnih silikatnih kamninah v dolini reke Čabranke (lito- in toposekvenca). 90 4.3.1 Morfološke značilnosti podrobno preučenih prsti.94 4.4 Primer lito- in toposekvence. 101 4.5 Tujerodne invazivne rastlinske vrste. 108 Urška Pajnič, Andrej Gaspari 5 Arheološka najdišča Loškega Potoka in vpetost prostora v širšo regionalno podobo dinarskokraške pokrajine med prazgodovino in
srednjim vekom. 113 5.1 Pregled raziskav. 113 5.2 Pregled najdišč po obdobjih. 116 5.3 Pogled naprej.121 Vlado Mohar 6 Začetki Loškega Potoka. 125 6.1 Nekaj najstarejših navedb dogajanja na območju današnjega Loškega Potoka.125 6.2 Nastanek imena. 128 6.3 Od kod so prišli prvi naseljenci?. 129 6.4 Gospodarska slika leta 1573. 132 6.5 Gospodarska slika leta 1621. 136 6.6 Življenje v Loškem Potoku vztraja še danes. 137 6.7 Razlaga izrazov. 141 Vera Smole 7 Loškopotoški govor - naglas, glasoslovje in
besedila. 145 7.1 Kraj in ljudje. 145 7.2 Projekt ŠIPK. 146 7.3 Umestitev govora. 147 6
GeograFF 25 7.3.1 Zgodovina dolenjskega narečja. 147 7.3.2 Sedanje stanje dolenjskega narečja. 148 7.4 Fonološki opis govora. 150 7.5 Besedila.166 7.5.1 Informatorji, snemalci in čas posnetkov. 166 7.6 Na kratko o potoškem govoru. 175 Blanka Bartol 8 Potoška krajina včeraj, danes, jutri?. 177 8.1 Potoška krajina in njena zgradba. 177 8.2 Zgodovinski razvoj krajine. 178 8.3 Krajinske značilnosti. (81 8.4 Krajinski vzorci. 183 8.5 Izjemna krajina Retje. 185 8.6 Spremembe v krajini. 188
8.6.1 Spremembe krajinena območju Retij . 191 8.7 Kakšna naj bo prihodnost?. 191 Kristina Glojek,Asta Gregorič, Griša Močnik, Luka Drinovec, Honey Dawn C.Alas, Andrea Cuesta - Mosquera, Kay Weinhold, Maik Merkel, Thomas Müller, Martina Ristorini, Dominik van Pinxteren, Hartmut Herrmann, Alfred Wiedensohler, Matej Ogrin 9 Onesnaženost zraka z delci in s črnim ogljikom. 195 9.1 Koncentracije delcev PMo in črnega ogljika (BC). 196 9.2 Viri črnega ogljika (BC) in časovno spreminjanje koncentracij. 198 9.4 . Prostorsko spreminjanje koncentracij PM2.S glede na stabilnost ozračja. 200 9.5 Loški Potok je pokazatelj kakovosti zraka dolin, kraških polj in drugih kotanj hribovitih območij.201 Nina Krašovec, Klara Cevka,Tadeja Babič, Matej Ogrin, Kristina Glojek 10 Študija ranljivosti okolja. 207 10.1 Ranljivost okolja. 207 10.2 Pokrajinskoekološka členitev in tipizacija. 208 10.3 Pokrajinskoekološka regionalizacija.
209 10.4 Ocena nosilnih sposobnosti okolja. 210 10.5 Ocena dosežene stopnje obremenitve okolja. 213 10.6 Ocena ranljivosti okolja Loškega Potoka. 216 10.7 Razvoj in skrb za občutljivo kraško pokrajino. 218 7
Geografski oris občine Loški Potok I 11 Sklepne misli. 221 Summary. 225 Seznam slik. 229 Seznam preglednic. 234 Stvarno kazalo.237 Avtorji. 239 8
GeograFF 25 I Summary The archaeological picture of Loški Potok, even if fragmentary, points to the settle ment of this area in the first centuries of the first millennium BC. However, research ers allow for the possibility of an even older human presence in this area. We do not know exactly when today's settlement of Loški Potok was established, but mentions indicate as early as the end of the 15th century AD .The strategic location of Tabor Hill has been proven for centuries, as the inhabitants of Loški Potok used this place around 1500 as their first fortress, where they defended themselves and their liveli hood from bandits, and later an anti-Turkish camp was established there. What drove people to the forested karst landscape, far from the wide plains and rolling hills? Was it the forests or the agrarian overpopulation elsewhere? Difficult natural conditions and a dangerous location due to exposure toTurkish invasions and other bandits hin dered the smooth development of the Loški Potok and Draga Valley. Today we can not imagine that the traditional cultural landscape, perhaps most typically reflected in the view from Tabor to Retje, reflects the centuries-long struggle of the people of Loški Potok and Draga Valley not only with nature, but also with various conquerors of the region. The long, continuous presence of people on the territory of Loški Potok and Draga Valley has led to the development of special linguistic features, which are not uni form. In the villages of Mali Log, Retje, Hrib, Šegova vas, Srednja vas and Travnik, one of the local dialects of the
tonemic Dolenjska dialect (southern) of western type is spoken, while in the villages of Lazeč, Podpreska, Draga, Srednja vas pri Dragi, Stari and Novi Kot and Trava, the non-tonemic Kostel dialect is already spoken, and both belong to the Dolenjska dialect group. The surface of the Loški Potok and Draga Valley landscape is now interpreted as a typical karst surface, which is also reshaped by forms of fluvial material transfer. In the elongated lowland that runs through the western part of the area, there are two typi cal karst fields: Retje and Travnik. According to the morphodynamic characteristics, the Retje field is defined as an occasional lake field and the Travnik field as an over flowing karst field. Occasional flooding also indicates land use and limits settlement of areas with regular flooding. Both fields are also distinct frost hollows and the set tlements of Retje and Travnik are among the coldest settlements in Slovenia, along side Babno Polje, Rakitna or the settlements on the plateau of Bloke. Although the inhabitants of Loški Potok have always been farmers, the climate is not particularly favourable for them, and in the past was even more unfavourable. The short grow ing season with frequent cold spells, which can bring frost from August to June, has given rise in folk tradition to the saying that winter in Loški Potok lasts nine months and then it is cold for three months. Loški Potok and Draga Valley are relatively humid areas of Slovenia, especially in the higher parts of the region. Lower temperatures and reduced evaporation also con tribute to
humidification, but the actual availability of water on the predominantly 225
Geografski oris občine Loški Potok I karstified surface is severely limited. Surface runoff is reduced due to the large forest cover that is a hallmark of the area. Nevertheless, the area has a higher than aver age runoff coefficient, reaching values between 60 and 70% of precipitation, which is above the Slovenian average (Frantar, 2008). With a relatively high level of precipitation the region is thus wet, but due to the geological karst structure the water is more difficult to access, and the self-purify ing power of the water is also limited. The extreme south-eastern part of the mu nicipality of Loški Potok, which does not belong to the Loški Potok - Draga Valley region, stands out from this framework. Here is the headwaters of the Čabranka river, practically the only part of the Loški Potok municipality with fluvial relief and the most water-rich river course. The source of the Čabranka is a karst spring, but the water-resistant geological base enables its surface drainage towards Osilnica, where it flows into the Kolpa River. In addition to geomorphological and hydrological features, the geological struc ture also determines the pedogenetic processes, of which the following are pre dominant in Loški Potok and Draga Valley : Humus accumulation, slow weathering of the hard carbonate parent rock and rather modest formation of fine soil parti cles. As a result, young soil stages are predominant, which are shallow, have a low clay content and high reaction (the pH fluctuates around the neutral value). Due to the carbonate parent rock, the saturation with bases is
high. These factors, pro cesses and general characteristics were also confirmed by field research at 48 sites. Accordingly, in the Loški Potok municipality Rendzina is predominant, appearing on up to 64% of the area, followed by brown Chromic Cambisolsoils with 33%. A modest proportion of Dystric Brown soils occur in the extreme south, and in some places Eutric Brown soils occur in the bottom of the elongated lowland. The agrar ian settlement of Loški Potok and the Draga Valley is also reflected in a very special cultural landscape, which occupies a special place among Slovenian landscapes. The landscape features in the municipality of Loški Potok are shaped by natural or culturally determined landscape elements and patterns. In some cases, the natu ral morphology carries built accents such as churches and chapels, such as Tabor hill with two churches and a cemetery, and the church in Draga with linden trees, which stands on a hill in front of the village in a place visible from both Podpreska and Srednja vas near Draga. Other landscape elements are individual trees or groups of trees on farmland, usually lime trees, which often mark crosses, chapels, and churches, or other types of fruit or forest trees along roads; orchards; shrub vegetation; patches of forest on steeper parts of depressions; stone walls along some field paths, puddles or ponds; springs; rocks on farmland; streambeds of permanent and occasional streams, etc. A study of the vulnerability of the municipality of Loški Potok showed a moderate impact of human activities. In most geo-ecological units air and
water quality as sessments reach a state of low pollution, due to the low density of settlements and population. The situation is different in the settlements in the karst fields of Retje and Travnik. Due to the lower self-cleaning capacity of the atmosphere in the two depres sions, even a small number of households in winter causes air pollution with black carbon (BC) and particulate matter comparable to that of larger cities in valleys and 226
GeograFF 25 basins. The measurements also show that particulate air pollution in smaller popu lated hollows in rural areas can be much higher than is generally assumed. At the time of the temperature inversions, the inhabitants of the bottom of both karst fields are most exposed to high concentrations of BC and PM particles. The measured concentrations of the pollutants in question during the winter temperature inver sions are of great concern, as in the evenings they reach the level of the most pol luted areas in the world, such as the city of Delhi in India (Apte et al., 2011 ; Goel et al., 2015; WHO, 2016). How should this area develop in the future? Although it is a sensitive karst area with limited carrying capacity, for the preservation of the traditional cultural landscape, its functions and structure, depopulation of the area and aging are also problematic processes. In addition, environmental changes due to climate change will shape the Dinaric regions, which include Loški Potok and Dragarska dolina, in the coming dec ades. The traditional and recognized cultural landscape of Loški Potok and Dragarska dolina must find a place in the municipal development plans for the coming decades. The municipality should continue the transition to renewable energy sources (biomass, wind energy), support the maintenance of quality forests and wood process ing, strengthen local entrepreneurship, including forms of rural tourism, and mitigate the effects of transport-related remoteness by accelerating digitalization. 227
GeograFF 25 Stvarno kazalo A advekcijski (alohtoni) tip vremena 34, 36,38,40 Alisol 97,99 amonij 75-76,78 analiza lidarskih posnetkov 113,115, 120,185 Ängströmov eksponent 198 Anton Skubic 126-127,132 arheološka topografija 113,115,121, 178 B Blate 64-65,74 Blošček 19,70,177-178,190 bukovi gozdovi 88-91,93,97 C CAI 113,115,118-120 Cambisol 96,104,226 cerkev 9,115,117,120,126-127,145, 169,178,180-182,184,186-188, 191,222 Claustra Alpinum luliarium 113,121, 125 Claustra Alpium luliarum 113,121,125 č Čabranka 14,23,36,39-47,50,52, 57-65,67,74-77,79,85,90-92, 100-102,104,113,116,120,126, 180,209-210,212-213,215-216, 218,222,226 čistilna naprava 59,73,76,214 črni og ljik (BC) 11,195-201,215,222 D dediščina 12,70-71,114,146,182,187, 192 delci 9,11,88,90,99,101 -103,195198,201-202,215,222 delci PM 195-198,200-202,215,222 depopulacija 218,223 destruktivni geomorfni procesi 211,213 dinarska pregrada 24 dinarski jelovo bukovi gozdovi 88 distrične rjave prsti 88,91,99-100,103, 222 dolek 67 dolenjska narečna skupina 147,221, 225 dolenjsko narečje 147-149,153,175, 221,225 dolomit 14-18,21,75,85,91 -92,94,99, 104,210 Dragarsko podolje 13-14,19-20, 209-210,212,214-216 drevesa 40,51,128,133,181 -182,222 E ekološko stanje 74 ekosistemske storitve 218,223 energija Sončevega obsevanja 34-35, 39,48 enoletna suholetnica 109 erozijski jarek 14,16-18,21,92 estavela 20 F fizikalne lastnosti prsti 94-98 fizikalno-kemijski parametri 78 fluviokras 13-14,16-18,21,66 fluviokraški relief 14,21 fluviokrašo površje 13,16 fonološki opis govora 150 fosfati 75-76,78 Frančišek Kramer 126 G GIS študije 120
Glažuta 12,14,68,79,114,120-121, 180,209-210,212,215-216,218 237
Geografski oris občine Loški Potok • Glažutarsko podolje 13-14,20 Gleysol 98,105 glinovec 92,98 globina prsti 85,87,89,94-101,103 Goteniška gora 13-14,20,23,36,39,50, 57, 60,68, 74-75,209-210,212,215, 216 gozdna združba bukve in spomladanske torilnice 88 gozdne združbe 87-91,93 gozdni ekosistem 219 Gradišče 115,117,119,125,187 greznica 73,76 grumbla 182-183,185,190,222 H horizont 25,36,85,88-89,94-99, 101-102,118 hranila 76,103,106 Hrib 9,11 -13,25-33,36,51 -52,57,59, 72-73, 76, 79,93,103,109,114-115, 117,136-137,145,147,167,178180,182-184,186-189,200-201, 214,221,225 hrvatarstvo 137,140 huba 130-131,134-139,141 hudourniški potok 57,67,93 I identiteta 70,148,178,191 -192 indeks kakovosti zraka 198,200-202 individualna kurišča 214,218 interaktivni spletni slovar 146 Iso Cluster Unsupervised Classification 209 izhlapevanje 36,57,66,221 izprane prsti, luvisol 91,99-100,102-103 izvir 16,20,58-60,64,67-70, 72, 74-76, 78-79,91,98,11,3, 128,182,184, 222 izvor naglasa 151,153,175 izvor samoglasnikov 153 izvor soglasnikov 163 J Janez Andrej Turjaški 127 japonski dresnik, dresniki 108-110 238 Jernej Pečnik 114,117,125,178 jezera hladnega zraka 50,52,201, 213 jezikovna dediščina 146 K kakovost vode 73-75 kakovost zraka 11-12,28,42,195-198, 200-202,214-215,218 kal 68-72,75,78-79,182,222 kambične prsti, kambisoli 91,96-97, 99-100,102-103,106 kamnita orodja 116 kanalizacija 73-74,76,214 kapnica 68,70,73 karbonatna matična podlaga 57-58, 75-76,85,88,100,103-104,211, 222 kemične lastnosti prsti 94-99,101-102, 214 kemijsko stanje 74-75 keramika 114-118,120,125 kloridi 75-76,78 Kolačnik 117
kopasta vzpetina 13,16,19 kopasti hrbet 14,16 kopasti kras 13,18-20,209-210, 212-216,221 krajevni govor 147-149,175,221 krajina 12,177-178,180-192,222 kraško polje 13,15-16,19-21,28-29, 52,93,183-188,190-191,196,201, 209,212-217,221-222 kraško polje Travnik 13,15-16,20 kulturna pokrajina Loškega Potoka 218-219,221,223 kurilne naprave 202 L Laßerbach 128,134 Lenart Sigesdorf 126 Leptosol 91,94-95,99-102,104 ljudsko izročilo 146,221 lokalna identiteta 148 lokalno podnebje 33-34,42 loškopotoški govor 145-146 loškopotoški slovar 146
GeograFF 25 M mala hidroelektrarna 58-59 Malenščica 57-59,61 -64,72,75,78,180 Marjan Slabe 114,117,125 Martolozi 131 meljevec 57,59,222 meritve onesnaženosti zraka 196 mesečni pretočni režim 61-62,64,66, 55 Mežnarjev potok 20,43,58,68,75-76, 78,179-180,212 minimalne (najnižje) temperature 29-30,33,37-39,42-47,50-51,93 mlin 58-59,137-139 morfologija 181,185,222 morfološke značilnosti prsti 94-99,101 mrazišče 23,29,43-44,46-47,188,221 N nadmorska višina 16,20,23,25,28,31, 33,39-41,43,45,57,59,68,75,85, 87,89,91 -92,101 -102,145,177, 209-210 najmanjši pretok 61-62,64-65 največji pretok 61-62,64-65 naklon pobočja 17,99,100-101 narečna besedila 147,149-150 narečni govor 145-146 nasičenost s kisikom 76 nenadzorovana klasifikacija 208-209 nepopolno zgorevanje ogljičnih goriv 195 nitriti 75-76,78 O občasno ojezerjeno polje 20-21,27, 184-185,221 ocena dosežene stopnje obremenitve okolja 213-216 ocena nosilnih sposobnosti okolja 210-213 ocena regeneracijskih in nevtralizacijskih sposobnosti 207 octovec 108-109 Od volkodlaka do Klepca 126 odtočni količnik 57,221 odtok 57,61 -62,64-66,102,221 ogrevanje gospodinjstev na les 106, 196,199,201-202,215 okoljska nosilna zmogljivost 207,218 onesnažen zrak 9,42,195-196,201 202,214-218,222 osamelec 177,181-182,184,222 osončenost 25,35-36,50 P padavine 24-27,51-52,57,59,66-67, 73,75,91-93,100,221 parcela 115,141,180,183-184,186, 190-191 pedosekvenca 90-91,99-101,103-106 pelinolistna žvrklja, ambrozija 108-109 pHvode 76 plitvi kras 19-20 podeželje 196,202,222 podnebje nižjega gorskega sveta 23 podzemna bifurkacija 59,65,75 podzemna voda
16,19-20,57,59-60, 64-66,74-75,212 podzemne povezave 16,59-60,74 pogled 31,92,105,121,152,186,188, 190-191,196,221 pokrajinotvorna sestavina 207-208, 212-217 pokrajinskoekološka enota 207, 209-210,212,222 pokrajinskoekološka regionalizacija 209 pokrajinskoekološka tipizacija 208 pokrajinskoekološki tip 207-209,211 pokrajinskoekološko členitev 207-208, 210 pokriti kras 16-17 polovnik 135 ponikalnica 58,64,67 ponikva 18 popis rastlinstva 86-87 poplave 60-61,66-67,128-129,186, 188,212-213,217,221 porečje 16,59-60,64 posamična najdba 113,116,119,121 poselitev 21,67-68,71,73-74,115-117, 120-121,125,177-178,184-186, 188,191,213-215,218,221-222 Potočanska dolina 11,13 239
Geografski oris občine Loški Potok | povesmo 135-136 povodje 59 povprečni pretok 61-62,64 pozna antika 119-121 pozna bronasta doba 116-117 prelivno kraško polje 20-21,221 prevodnost vode 75-78 profil 39-41,47,87-88,94-98,101-102 prostor 113,115,117,119,121,125128,133,177-178,183-185,188189,191 -192,207,213,218,222 protiturški tabor 126,145,221 Pungert 79,91,115,120-121,180 R raba 13,21,33-35,48,58,73,85,88-89, 93,102-105,145,156,177,180,183, 185-186,188,191,209-210,213214,219,221 Račna gora 13-15,18-20,23,50,113, 117,119-120,184 radiacijski (avtohtoni) tip vremena 33, 36-40,42-43,45,47,50,52 Rakitnica 16,59-60,64-65,74-75 ranker 91,99,103 ranljivost 208,216,218,222 ranljivost okolja 207,209,216-218 rastlinstvo, rastlinski pokrov 85-88, 90-91,93,98,104-105,210 razvodje 59-60 razvodnica 59,63,66 rečna mreža 58,51,74,93,100 rečni pretočni količnik 62-64 regionalno ozadje 198,202 rendzine 88-89,91,99,212,222,226 Retje 9,12-14,16,19-21,23-25,27, 29,36-38,43,52,66,73,76-77,79, 103,106,109,115-117,125-126, 128,130,135-137,145,147,152, 167,178,180-181,183-184-185, 187-188,190,196-202,209-210, 212,214-216,218,221,225-226 Rettiach 134-136 rimska cesta 125 Rinža 16,59-60,64-65,74-75 rjave pokarbonatne prsti 88-89,91,210, 212,222 240 S samočistilna sposobnost 74-75,77,208, 212-213 samočistilne sposobnosti voda 75,77, 217,222 samočistilne sposobnosti zraka 213 silikatne kamnine 88,90-93,100,103 simbol 177,186 skupine govorov v dolenjskem narečju 149 skupna ocena obremenjenosti prsti 214 skupna ocena ranljivosti 216,218 snežna odeja 25-27,39,43,66,93 snovna kulturna dediščina 146
sondiranje 85,87 specifični odtok 61-62,64-66 srednji vek 113,120-121,178,186 starejša železna doba 117 stopnja obremenitve okolja 207, 213-216 stopnja obremenjenosti reliefa 213 stopnja obremenjenosti voda 214,218 sulična ost 118,120-121 Svetovna zdravstvena organizacija 200 š Senik 120,136 Študentski inovativni projekti za družbeno korist (ŠIPK) 146-147, 149-150,166 Tabor 9,12-13,19,28,42-44,46-47, 114-115,117-118,121,125-126, 145,152,177-182,184,186-188, 190,196-198,201,215,221 -222, 225-226 temperatura vode 75 temperaturna inverzija 31,93,195-198, 200-202,213,215,218 temperaturni obrat 23,39,42-43,45, 47-48,50 terensko proučevanje 222 termalno snemanje 34-37,52 tonemski naglas 147-148,175 topoklima 33-34,38,52 topoklimatska karta 48-49
GeograFF 25 trajanje Sončevega obsevanja 34-35, 42,52 transkripcija posnetkov 166 Travnik 13-16,19-21,28-29,35-36, 58-64,66,73,103,109-110,115, 120,126,129,136-137,145,147, 167,178-180,184,189,209-210, 212-216,218,221,225-226 trdota vode 75-77 tujerodne invazivne rastlinske vrste 108-109 zgodovina dolenjskega narečja 147149 zgorevanje biomase 196,198-200,218 zlata rozga 109 Zörrer 119 Ž žaga 58-59,106-107,137,140,180 živica 182-186,190,222 U urbar 129-141,178 uvala 13-14,16,18-21,42,59,66-67, 73,76,128,196,221 uvala Retje 19-20,59,66-67,73,76, 128,196 V Veliki Obrh 16,59,64-65,74-75 vertikalni temperaturni gradient 39 višina (količina) padavin 26-27,51,57, 66,91-92,100 višina snežne odeje 25-27 vodna bilanca 57 vododržna podlaga 69,222 vodomerna postaja 60-66 vodostaj 20,61 vodovarstveno območje 73-74,76 vodovod 68,72-74 vodozbirno zaledje 60-66 Votla stena 119,121 vročinski stres 219 vršaj 14,18,21 vršni (terminalni) poganjki 40-41 vrtača 16,18,20,35-36,42,57,182, 186,191,222 vsebnost kisika 75-76 vzorec 26,67,73,75-76,100,177-178, 181,183-184,186-187,189-190, 222 WRB 86,104-105 Z zbirka starih fotografij 146 zbirke starih predmetov 146 241 |
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| geographic | Loški Potok / Geografija / Zborniki ssg Loški Potok (DE-588)1276249098 gnd |
| geographic_facet | Loški Potok / Geografija / Zborniki Loški Potok |
| id | DE-604.BV049048441 |
| illustrated | Illustrated |
| index_date | 2024-07-03T22:20:55Z |
| indexdate | 2024-07-10T09:53:47Z |
| institution | BVB |
| isbn | 9789610605591 |
| language | Slovenian |
| oai_aleph_id | oai:aleph.bib-bvb.de:BVB01-034310840 |
| oclc_num | 1403380509 |
| open_access_boolean | |
| owner | DE-12 |
| owner_facet | DE-12 |
| physical | 244 Seiten Illustrationen, Diagramme, Karten 24 cm |
| psigel | BSB_NED_20231012 |
| publishDate | 2022 |
| publishDateSearch | 2022 |
| publishDateSort | 2022 |
| publisher | Znanstvena založba Filozofske fakultete |
| record_format | marc |
| series | GeograFF |
| series2 | GeograFF |
| spelling | Geografski oris občine Loški Potok Matej Ogrin (ur.) Prva izdaja Ljubljana Znanstvena založba Filozofske fakultete 2022 244 Seiten Illustrationen, Diagramme, Karten 24 cm txt rdacontent n rdamedia nc rdacarrier GeograFF 25 Auflage 200 občine / Slovenija / regionalna geografija Regionale Geografie (DE-588)4131549-2 gnd rswk-swf Loški Potok / Geografija / Zborniki ssg Loški Potok (DE-588)1276249098 gnd rswk-swf Loški Potok (DE-588)1276249098 g Regionale Geografie (DE-588)4131549-2 s DE-604 Ogrin, Matej 1975- (DE-588)1258218127 edt Erscheint auch als Online-Ausgabe, PDF 978-961-06-0558-4 GeograFF 25 (DE-604)BV036521490 25 Digitalisierung BSB München 19 - ADAM Catalogue Enrichment application/pdf http://bvbr.bib-bvb.de:8991/F?func=service&doc_library=BVB01&local_base=BVB01&doc_number=034310840&sequence=000001&line_number=0001&func_code=DB_RECORDS&service_type=MEDIA Inhaltsverzeichnis Digitalisierung BSB München 19 - ADAM Catalogue Enrichment application/pdf http://bvbr.bib-bvb.de:8991/F?func=service&doc_library=BVB01&local_base=BVB01&doc_number=034310840&sequence=000003&line_number=0002&func_code=DB_RECORDS&service_type=MEDIA Abstract Digitalisierung BSB München 19 - ADAM Catalogue Enrichment application/pdf http://bvbr.bib-bvb.de:8991/F?func=service&doc_library=BVB01&local_base=BVB01&doc_number=034310840&sequence=000005&line_number=0003&func_code=DB_RECORDS&service_type=MEDIA Register // Gemischte Register |
| spellingShingle | Geografski oris občine Loški Potok GeograFF občine / Slovenija / regionalna geografija Regionale Geografie (DE-588)4131549-2 gnd |
| subject_GND | (DE-588)4131549-2 (DE-588)1276249098 |
| title | Geografski oris občine Loški Potok |
| title_auth | Geografski oris občine Loški Potok |
| title_exact_search | Geografski oris občine Loški Potok |
| title_exact_search_txtP | Geografski oris občine Loški Potok |
| title_full | Geografski oris občine Loški Potok Matej Ogrin (ur.) |
| title_fullStr | Geografski oris občine Loški Potok Matej Ogrin (ur.) |
| title_full_unstemmed | Geografski oris občine Loški Potok Matej Ogrin (ur.) |
| title_short | Geografski oris občine Loški Potok |
| title_sort | geografski oris obcine loski potok |
| topic | občine / Slovenija / regionalna geografija Regionale Geografie (DE-588)4131549-2 gnd |
| topic_facet | občine / Slovenija / regionalna geografija Regionale Geografie Loški Potok / Geografija / Zborniki Loški Potok |
| url | http://bvbr.bib-bvb.de:8991/F?func=service&doc_library=BVB01&local_base=BVB01&doc_number=034310840&sequence=000001&line_number=0001&func_code=DB_RECORDS&service_type=MEDIA http://bvbr.bib-bvb.de:8991/F?func=service&doc_library=BVB01&local_base=BVB01&doc_number=034310840&sequence=000003&line_number=0002&func_code=DB_RECORDS&service_type=MEDIA http://bvbr.bib-bvb.de:8991/F?func=service&doc_library=BVB01&local_base=BVB01&doc_number=034310840&sequence=000005&line_number=0003&func_code=DB_RECORDS&service_type=MEDIA |
| volume_link | (DE-604)BV036521490 |
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