<Record><identifier xmlns="http://purl.org/dc/elements/1.1/">URN:NBN:SI:DOC-8IKRH37H</identifier><date>2004</date><creator>Kogovšek, Janja</creator><relation>documents/doc/8/URN_NBN_SI_doc-8IKRH37H_001.pdf</relation><relation>documents/doc/8/URN_NBN_SI_doc-8IKRH37H_001.txt</relation><format format_type="type">article</format><format format_type="extent">Str. 15-21</format><identifier identifier_type="COBISSID_HOST">21906733</identifier><identifier identifier_type="URN">URN:NBN:SI:doc-8IKRH37H</identifier><language>slv</language><publisher publisher_location="Ljubljana">Fakulteta za gradbeništvo in geodezijo</publisher><source>Raziskave s področja geodezije in geofizike</source><rights>InC</rights><subject language_type_id="slv">hidrologija</subject><subject language_type_id="eng">hydrology</subject><subject language_type_id="eng">karst</subject><subject language_type_id="eng">karstology</subject><subject language_type_id="slv">kras</subject><subject language_type_id="slv">krasoslovje</subject><subject language_type_id="eng">percolation water</subject><subject language_type_id="slv">pretakanje podzemeljske vode</subject><subject language_type_id="eng">vadose zone</subject><subject language_type_id="slv">vadozna cona</subject><title>Značilnosti pretakanja padavin skozi vadozno cono Krasa</title></Record>