<?xml version="1.0"?><rdf: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-B27G0OOB/f873ea6d-b1e7-4b87-82f4-3c1bc7836da4/HTML"><dcterms:extent>46 KB</dcterms:extent></edm:WebResource><edm:WebResource rdf:about="http://www.dlib.si/stream/URN:NBN:SI:DOC-B27G0OOB/7641299c-d05c-40bc-b377-8360d415a49a/PDF"><dcterms:extent>2024 KB</dcterms:extent></edm:WebResource><edm:WebResource rdf:about="http://www.dlib.si/stream/URN:NBN:SI:DOC-B27G0OOB/579e605c-1758-46f9-b6d8-3e3e3d6b67b0/TEXT"><dcterms:extent>43 KB</dcterms:extent></edm:WebResource><edm:TimeSpan rdf:about="1925-2025"><edm:begin xml:lang="en">1925</edm:begin><edm:end xml:lang="en">2025</edm:end></edm:TimeSpan><edm:ProvidedCHO rdf:about="URN:NBN:SI:DOC-B27G0OOB"><dcterms:isPartOf rdf:resource="https://www.dlib.si/details/URN:NBN:SI:spr-M6F5Y6SH" /><dcterms:issued>1998</dcterms:issued><dc:creator>Brečko Grubar, Valentina</dc:creator><dc:format xml:lang="sl">letnik:70</dc:format><dc:format xml:lang="sl">str. 27-43</dc:format><dc:identifier>ISSN:0350-3895</dc:identifier><dc:identifier>COBISSID:8416354</dc:identifier><dc:identifier>URN:URN:NBN:SI:doc-B27G0OOB</dc:identifier><dc:language>sl</dc:language><dc:publisher xml:lang="sl">Zveza geografskih društev Slovenije</dc:publisher><dcterms:isPartOf xml:lang="sl">Geografski vestnik</dcterms:isPartOf><dc:subject xml:lang="sl">hidrogeografija</dc:subject><dc:subject xml:lang="sl">Ljubljana</dc:subject><dc:subject xml:lang="en">Ljubljana Basin</dc:subject><dc:subject xml:lang="sl">Ljubljanska kotlina</dc:subject><dc:subject xml:lang="sl">oskrba z vodo</dc:subject><dc:subject xml:lang="sl">pitna voda</dc:subject><dc:subject xml:lang="sl">podtalnica</dc:subject><dc:subject xml:lang="sl">vodni viri</dc:subject><dcterms:temporal rdf:resource="1925-2025" /><dc:title xml:lang="sl">Pokrajinske značilnosti območij virov pitne vode v jugovzhodni Ljubljanski kotlini|</dc:title><dc:description xml:lang="sl">There are numerous water resources in the northeast i.e. southeast Ljubljana basin which differ significantly as to their dynamic reserves, mode of resupply, baseflow speed, depth and permeability of cover layer, and quality. By suitability of these water resources for drinking water supply they are divided to six groups. It is necessary to provide about 1.5m3/s of drinking water for the supply of Ljubljana, and in case of pollution it would be very hard to substitude for the groundwater of the Ljubljansko Polje. In the southeast Ljubljana basin, the aquifers in nonconsolidated sediments have the greatest dynamic reserves of drinking water. Selected for the assessment of landscape sensitivity were four of them: the Ljubljansko Polje and the Iška alluvial fan as the areas of current drinking-water resources, and the Sorško Polje and the Ljubljansko Barje as the areas of possible resources. It has been established through the evaluation of selected physicogeographical features of the environment with groundwater that the Ljubljansko Barje is water-ecologically least sensitive, next come the Ljubljansko Polje and the Sorško Polje, while the Iška alluvial fan is the most sensitive environment with groundwater</dc:description><dc:description xml:lang="sl">V jugovzhodni Ljubljanski kotlini je veliko vodnih virov, ki se po dinamični zalogi, načinu obnavljanja, hitrosti pretakanja, debelini in prepustnosti krovne plasti ter po kakovosti zelo razlikujejo. Razdelili smo jih v šest skupin podzemnih voda glede na primernost vodnega vira za oskrbo s pitno vodo. Za oskrbo Ljubljane je treba zagotoviti približno 1,5 m3/s pitne vode, zato bi ob onesnaženju podtalnico Ljubljanskega polja težko nadomestili. V jugovzhodni Ljubljanski kotlini imajo največjo dinamično zalogo pitne vode vodonosniki v nesprijetih sedimentih, izmed katerih smo za ocenjevanje pokrajinske občutljivosti izbrali štiri območja: Ljubljansko polje in vršaj Iške kot območji sedanjih virov pitne vode ter Sorško polje in Ljubljansko barje kot območji možnih virov pitne vode. Z vrednotenjem izbranih fizičnogeografskih lastnosti okolja s podtalnicami smo ugotovili, da je vodno ekološko najmanj občutljivo Ljubljansko barje, sledita Ljubljansko in Sorško polje, najbolj občutljivo pa je okolje s podtalnico na vršaju Iške</dc:description><edm:type>TEXT</edm:type><dc:type xml:lang="sl">znanstveno časopisje</dc:type><dc:type xml:lang="en">journals</dc:type><dc:type rdf:resource="http://www.wikidata.org/entity/Q361785" /></edm:ProvidedCHO><ore:Aggregation rdf:about="http://www.dlib.si/?URN=URN:NBN:SI:DOC-B27G0OOB"><edm:aggregatedCHO rdf:resource="URN:NBN:SI:DOC-B27G0OOB" /><edm:isShownBy rdf:resource="http://www.dlib.si/stream/URN:NBN:SI:DOC-B27G0OOB/7641299c-d05c-40bc-b377-8360d415a49a/PDF" /><edm:rights rdf:resource="http://rightsstatements.org/vocab/InC/1.0/" /><edm:provider>Slovenian National E-content Aggregator</edm:provider><edm:intermediateProvider xml:lang="en">National and University Library of Slovenia</edm:intermediateProvider><edm:dataProvider xml:lang="sl">Zveza geografov Slovenije</edm:dataProvider><edm:object rdf:resource="http://www.dlib.si/streamdb/URN:NBN:SI:DOC-B27G0OOB/maxi/edm" /><edm:isShownAt rdf:resource="http://www.dlib.si/details/URN:NBN:SI:DOC-B27G0OOB" /></ore:Aggregation></rdf:RDF>