{"?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-QP3CCLJC/ab31aca8-8cbc-43f6-ba7e-2c66a807a071/PDF","dcterms:extent":"778 KB"},{"@rdf:about":"http://www.dlib.si/stream/URN:NBN:SI:doc-QP3CCLJC/d0a4e144-061a-4e3a-9713-e776679cea30/TEXT","dcterms:extent":"0 KB"}],"edm:TimeSpan":{"@rdf:about":"2006-2025","edm:begin":{"@xml:lang":"en","#text":"2006"},"edm:end":{"@xml:lang":"en","#text":"2025"}},"edm:ProvidedCHO":{"@rdf:about":"URN:NBN:SI:doc-QP3CCLJC","dcterms:isPartOf":[{"@rdf:resource":"https://www.dlib.si/details/URN:NBN:SI:spr-8USLDTJD"},{"@xml:lang":"sl","#text":"Revija za geografijo"}],"dcterms:issued":"2020","dc:creator":["Davidović, Danijel","Ivajnšič, Danijel"],"dc:format":[{"@xml:lang":"sl","#text":"številka:1"},{"@xml:lang":"sl","#text":"letnik:15"},{"@xml:lang":"sl","#text":"str. 91-107"}],"dc:identifier":["ISSN:1854-665X","COBISSID_HOST:52460803","URN:URN:NBN:SI:doc-QP3CCLJC"],"dc:language":"sl","dc:publisher":{"@xml:lang":"sl","#text":"Univerza v Mariboru, Filozofska fakulteta"},"dc:subject":[{"@xml:lang":"sl","#text":"daljinsko zaznavanje"},{"@xml:lang":"sl","#text":"geografski informacijski sistemi"},{"@xml:lang":"en","#text":"geographic information system"},{"@xml:lang":"sl","#text":"indeks vlažnosti tal"},{"@xml:lang":"en","#text":"land surface temperature"},{"@xml:lang":"sl","#text":"Landsat"},{"@xml:lang":"en","#text":"normalized difference vegetation index"},{"@xml:lang":"sl","#text":"normiran diferencialni vegetacijski indeks"},{"@xml:lang":"en","#text":"remote sensing"},{"@xml:lang":"en","#text":"soil moisture index"},{"@xml:lang":"sl","#text":"temperatura površja"}],"dcterms:temporal":{"@rdf:resource":"2006-2025"},"dc:title":{"@xml:lang":"sl","#text":"Indeks vlažnosti tal Pomurja| primer uporabe podatkov satelita Landsat 8|"},"dc:description":[{"@xml:lang":"sl","#text":"This research demonstrates the methodological implementation of satellite imagery for evaluation of soil moisture in the case of Pomurje (Slovenia). The presented soil moisture index is a derivative of surface temperature and NDVI vegetation index, using spectral bands detected by optical and thermal sensor of the Landsat 8 satellite. The obtained values of the soil moisture index vary between 0 (low soil moisture) and 1 (high soil moisture). Furthermore, we observe the differences in soil moisture with regard to intensive or extensive agricultural land use. The calculated estimates of soil moisture in Pomurje reached values between 0.06-0.99, with statistically significant differences between higher values in forests and lower values in fields and other selected landuse categories. This approach to soil moisture assessment is useful for monitoring and planning agricultural and environmental activities at the landscape level and for evaluating the climate change impact on the humidity conditions in a given area"},{"@xml:lang":"sl","#text":"V prispevku obravnavamo uporabo metode računanja vlažnosti tal s satelitskimi podobami na primeru Pomurja. Predstavljen indeks vlažnosti tal je derivat temperature površja in vegetacijskega indeksa NDVI, pri tem so uporabljeni spektralni pasovi, zaznani z optičnim in termičnim senzorjem satelita Landsat 8. Dobljene vrednosti indeksa vlažnosti tal zavzemajo vrednosti med 0 (nizka vlažnost tal) in 1 (visoka vlažnost tal). V nadaljevanju preverjamo razlike v vlažnosti tal gleda na intenzivno ali bolj ekstenzivno kmetijsko rabo. Izračunane ocene vlažnosti tal v Pomurju se gibljejo med 0,06-0,99, pri tem se pojavljajo statistično signifikantne razlike med višjimi vrednostmi v gozdovih ter nižjimi vrednostmi na njivah in drugih izbranih zemljiških kategorijah. Tovrstni pristop k oceni vlažnosti tal je uporaben za monitoring in načrtovanje kmetijskih in okoljevarstvenih dejavnosti na regionalni ravni hkrati pa omogoča prognozo vpliva podnebnih sprememb na vlažnostne razmere v danem prostoru"}],"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-QP3CCLJC","edm:aggregatedCHO":{"@rdf:resource":"URN:NBN:SI:doc-QP3CCLJC"},"edm:isShownBy":{"@rdf:resource":"http://www.dlib.si/stream/URN:NBN:SI:doc-QP3CCLJC/ab31aca8-8cbc-43f6-ba7e-2c66a807a071/PDF"},"edm:rights":{"@rdf:resource":"http://creativecommons.org/licenses/by/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 Mariboru, Filozofska fakulteta"},"edm:object":{"@rdf:resource":"http://www.dlib.si/streamdb/URN:NBN:SI:doc-QP3CCLJC/maxi/edm"},"edm:isShownAt":{"@rdf:resource":"http://www.dlib.si/details/URN:NBN:SI:doc-QP3CCLJC"}}}}