{"?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-XN9TEZ1K/194e7246-a0d8-4b74-8abc-1f2f2dcd4f43/HTML","dcterms:extent":"96 KB"},{"@rdf:about":"http://www.dlib.si/stream/URN:NBN:SI:doc-XN9TEZ1K/38970af0-c0e8-47a2-b8f5-f4a99b57ebeb/PDF","dcterms:extent":"566 KB"},{"@rdf:about":"http://www.dlib.si/stream/URN:NBN:SI:doc-XN9TEZ1K/e4055eb9-a9b5-4a5f-ac76-a21470f4a108/TEXT","dcterms:extent":"67 KB"}],"edm:TimeSpan":{"@rdf:about":"1952-2002","edm:begin":{"@xml:lang":"en","#text":"1952"},"edm:end":{"@xml:lang":"en","#text":"2002"}},"edm:ProvidedCHO":{"@rdf:about":"URN:NBN:SI:doc-XN9TEZ1K","dcterms:isPartOf":[{"@rdf:resource":"https://www.dlib.si/details/URN:NBN:SI:spr-TPZVJGGM"},{"@xml:lang":"sl","#text":"Geografski zbornik"}],"dcterms:issued":"2001","dc:creator":["Hrvatin, Mauro","Hrvatin, Mojca"],"dc:format":[{"@xml:lang":"sl","#text":"27 strani"},{"@xml:lang":"sl","#text":"številka:41"},{"@xml:lang":"sl","#text":"str. 91-117"}],"dc:identifier":["ISSN:0373-4498","ISSN:1581-6613","COBISSID:19326509","URN:URN:NBN:SI:doc-XN9TEZ1K"],"dc:language":"en","dc:publisher":{"@xml:lang":"sl","#text":"Znanstvenoraziskovalni center SAZU, Geografski inštitut"},"dc:subject":[{"@xml:lang":"sl","#text":"Dinarski kras"},{"@xml:lang":"sl","#text":"Dobrepolje"},{"@xml:lang":"en","#text":"Dobrepolje Municipality"},{"@xml:lang":"sl","#text":"kras (geologija)"},{"@xml:lang":"sl","#text":"kraška polja"},{"@xml:lang":"sl","#text":"pokrajinska ekologija"},{"@xml:lang":"en","#text":"regional geography"},{"@xml:lang":"sl","#text":"regionalna geografija"},{"@xml:lang":"sl","#text":"Struge"},{"@rdf:resource":"http://www.wikidata.org/entity/Q817121"}],"dcterms:temporal":{"@rdf:resource":"1952-2002"},"dc:title":{"@xml:lang":"sl","#text":"Ecological landscape units of the Dobrepolje-Struge karst| Naravne enote Dobrepoljsko-Struškega krasa|"},"dc:description":[{"@xml:lang":"sl","#text":"Dobrepoljsko-Struško polje pada med tipična kraška polja Dinarskega krasa Slovenije. Močno razpotegnjeno v dinarski smeri lezi v globoki kotanji med Malo goro in Suho krajino. Dno Dobrepoljsko-Struškega polja, kraški ravnik v okolici Ponikev ter okoliška pobočja Male gore, Suhe krajine in Čušperške planote oblikujejo pokrajino, ki smo jo po osrednji reliefni enoti poimenovali Dobrepoljsko-Struški kras. Med naravnimi prvinami, ki sooblikujejo Dobrepoljsko-Struški kras, smo kot najbolj pomembne izpostavili kamnine, relief, prsti in rastje. Naravne prvine so med seboj tesno povezane in medsebojno odvisne. Najbolj tipične in najpomembnejše kombinacije posameznih kategorij naravnih prvin tvorijo naravne enote. Te smo poskušali ugotoviti s prekrivanjem posameznih vsebinskih slojev v okviru geografskega informacijskega sistema. Od 648 teoretično možnih kombinacij kategorij naravnih prvin, se jih dejansko pojavlja 19. Na temelju kriterijev tipičnosti in pomembnosti smo ugotovljene kombinacije kategorij združili v šest naravnih enot"},{"@xml:lang":"sl","#text":"The Dobrepolje-Struge polje is a typical karst polje of Slovenia's Dinaric karst region. Distinctly prolonged in the direction of the Dinaric Alps, it lies in a deep trough between the Mala gora and Suha krajina plateaus. The bottom of the Dobrepolje-Struge polje, the karst corrosion plain around Ponikve, and the neighbouring hillslopes of Mala gora, Suha krajina, and the Čušperk plateau comprise the Dobrepolje-Struge karst, so named after its central relief unit. Among the natural elements that form the Dobrepolje-Struge karst, rock, relief, soil, and vegetation were found to be of greatest importance. The natural elements of the Dobrepolje-Struge karst are closely connected and interdependent. The most typical and most significant combination of natural elements form ecological landscape units. We determined these units by overlapping content layers of rock, relief, soil and vegetation employing the Geographical Information System"}],"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-XN9TEZ1K","edm:aggregatedCHO":{"@rdf:resource":"URN:NBN:SI:doc-XN9TEZ1K"},"edm:isShownBy":{"@rdf:resource":"http://www.dlib.si/stream/URN:NBN:SI:doc-XN9TEZ1K/38970af0-c0e8-47a2-b8f5-f4a99b57ebeb/PDF"},"edm:rights":{"@rdf:resource":"http://rightsstatements.org/vocab/InC/1.0/"},"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":"ZRC SAZU, Geografski inštitut Antona Melika"},"edm:object":{"@rdf:resource":"http://www.dlib.si/streamdb/URN:NBN:SI:doc-XN9TEZ1K/maxi/edm"},"edm:isShownAt":{"@rdf:resource":"http://www.dlib.si/details/URN:NBN:SI:doc-XN9TEZ1K"}}}}