{"?xml":{"@version":"1.0"},"edm:RDF":{"@xmlns:dc":"http://purl.org/dc/elements/1.1/","@xmlns:edm":"http://www.europeana.eu/schemas/edm/","@xmlns:wgs84_pos":"http://www.w3.org/2003/01/geo/wgs84_pos","@xmlns:foaf":"http://xmlns.com/foaf/0.1/","@xmlns:rdaGr2":"http://rdvocab.info/ElementsGr2","@xmlns:oai":"http://www.openarchives.org/OAI/2.0/","@xmlns:owl":"http://www.w3.org/2002/07/owl#","@xmlns:rdf":"http://www.w3.org/1999/02/22-rdf-syntax-ns#","@xmlns:ore":"http://www.openarchives.org/ore/terms/","@xmlns:skos":"http://www.w3.org/2004/02/skos/core#","@xmlns:dcterms":"http://purl.org/dc/terms/","edm:WebResource":[{"@rdf:about":"http://www.dlib.si/stream/URN:NBN:SI:doc-5G5V44UD/5328b721-cb8b-4d23-a463-284b695c2ba0/PDF","dcterms:extent":"4304 KB"},{"@rdf:about":"http://www.dlib.si/stream/URN:NBN:SI:doc-5G5V44UD/889ef9cd-9b92-4fb2-a005-a2843fd846e1/TEXT","dcterms:extent":"0 KB"}],"edm:TimeSpan":{"@rdf:about":"1985-2025","edm:begin":{"@xml:lang":"en","#text":"1985"},"edm:end":{"@xml:lang":"en","#text":"2025"}},"edm:ProvidedCHO":{"@rdf:about":"URN:NBN:SI:doc-5G5V44UD","dcterms:isPartOf":[{"@rdf:resource":"https://www.dlib.si/details/URN:NBN:SI:spr-U694A0TC"},{"@xml:lang":"sl","#text":"Dela - Oddelek za geografijo Filozofske fakultete v Ljubljani"}],"dcterms:issued":"2020","dc:creator":"Grlj, Aleš","dc:format":[{"@xml:lang":"sl","#text":"številka:53"},{"@xml:lang":"sl","#text":"str. 5-22"}],"dc:identifier":["ISSN:0354-0596","DOI:10.4312/dela.53.5-22","COBISSID_HOST:43649283","URN:URN:NBN:SI:doc-5G5V44UD"],"dc:language":"sl","dc:publisher":{"@xml:lang":"sl","#text":"Znanstvena založba Filozofske fakultete"},"dc:subject":[{"@xml:lang":"sl","#text":"fizična geografija"},{"@xml:lang":"sl","#text":"geografski informacijski sistemi"},{"@xml:lang":"sl","#text":"geomorfologija"},{"@xml:lang":"en","#text":"geomorphology"},{"@xml:lang":"sl","#text":"GIS"},{"@xml:lang":"en","#text":"karst depressions"},{"@xml:lang":"en","#text":"karst forms"},{"@xml:lang":"en","#text":"karstology"},{"@xml:lang":"sl","#text":"krasoslovje"},{"@xml:lang":"sl","#text":"kraške kotanje"},{"@xml:lang":"sl","#text":"kraške oblike"},{"@xml:lang":"en","#text":"physical geography"},{"@xml:lang":"en","#text":"Slovenia"},{"@xml:lang":"sl","#text":"Slovenija"}],"dcterms:temporal":{"@rdf:resource":"1985-2025"},"dc:title":{"@xml:lang":"sl","#text":"Omejevanje kraških kotanj z analizo polrezov|"},"dc:description":[{"@xml:lang":"sl","#text":"The development of remote sensing methods, computers and spatial data processing software has also affected the field of geomorphology. All three allow for faster analysis of larger amounts of data, but not more accurate. The reason for this is the poor mathematical definition of some geomorphological forms. The research focuses on the delimitation of karst depressions. For this purpose, we have developed a new approach that analyzes its half-sections when determining the edge of a depression and also effectively detects the edges of depressions on slopes. The method allows obtaining more accurate morphographic and morphometric data on depressions. The method was developed and tested on five depressions of the Podgrajsko podolje (SW Slovenia), and the results were compared with the results of a method that uses hydrological modeling to delimit the depressions. We observe a significant improvement in the results obtained with the new method"},{"@xml:lang":"sl","#text":"Razvoj metod daljinskega zaznavanja, računalnikov in programske opreme za obdelavo prostorskih podatkov se je dotaknil tudi področja geomorfologije. Vse troje omogoča hitrejšo analizo večjih količin podatkov, ne pa tudi natančnejše. Vzrok za to je slaba matematična defi niranost nekaterih geomorfoloških oblik. V raziskavi se osredotočamo na omejevanje kraških kotanj. Za ta namen smo razvili nov pristop, ki pri določanju roba kotanje analizira njene polreze ter učinkovito zaznava tudi robove kotanj na pobočjih. Metoda omogoča pridobivanje natančnejših morfografskih in morfometričnih podatkov o kotanjah. Metodo smo razvili in preizkusili na petih kotanjah Podgrajskega podolja (JZ Slovenija) ter rezultate primerjali z rezultati metode, ki za omejevanje kotanj uporablja hidrološko modeliranje. Opažamo bistveno izboljšanje rezultatov pri omejevanju z novo metodo"}],"edm:type":"TEXT","dc:type":[{"@xml:lang":"sl","#text":"znanstveno časopisje"},{"@xml:lang":"en","#text":"journals"},{"@rdf:resource":"http://www.wikidata.org/entity/Q361785"}]},"ore:Aggregation":{"@rdf:about":"http://www.dlib.si/?URN=URN:NBN:SI:doc-5G5V44UD","edm:aggregatedCHO":{"@rdf:resource":"URN:NBN:SI:doc-5G5V44UD"},"edm:isShownBy":{"@rdf:resource":"http://www.dlib.si/stream/URN:NBN:SI:doc-5G5V44UD/5328b721-cb8b-4d23-a463-284b695c2ba0/PDF"},"edm:rights":{"@rdf:resource":"http://creativecommons.org/licenses/by-sa/4.0/"},"edm:provider":"Slovenian National E-content Aggregator","edm:intermediateProvider":{"@xml:lang":"en","#text":"National and University Library of Slovenia"},"edm:dataProvider":{"@xml:lang":"sl","#text":"Univerza v Ljubljani, Filozofska fakulteta"},"edm:object":{"@rdf:resource":"http://www.dlib.si/streamdb/URN:NBN:SI:doc-5G5V44UD/maxi/edm"},"edm:isShownAt":{"@rdf:resource":"http://www.dlib.si/details/URN:NBN:SI:doc-5G5V44UD"}}}}