<?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-01NYH1QI/65cf5891-9449-4df1-b541-a95fe0fe084f/HTML"><dcterms:extent>57 KB</dcterms:extent></edm:WebResource><edm:WebResource rdf:about="http://www.dlib.si/stream/URN:NBN:SI:DOC-01NYH1QI/74c51afe-93c3-4344-9dfd-53c985051dc4/PDF"><dcterms:extent>1680 KB</dcterms:extent></edm:WebResource><edm:WebResource rdf:about="http://www.dlib.si/stream/URN:NBN:SI:DOC-01NYH1QI/4671c4cc-f1e6-4c33-be33-a3dba7a753ca/TEXT"><dcterms:extent>30 KB</dcterms:extent></edm:WebResource><edm:TimeSpan rdf:about="2000-2024"><edm:begin xml:lang="en">2000</edm:begin><edm:end xml:lang="en">2024</edm:end></edm:TimeSpan><edm:ProvidedCHO rdf:about="URN:NBN:SI:DOC-01NYH1QI"><dcterms:isPartOf rdf:resource="https://www.dlib.si/details/urn:nbn:si:spr-fzwbu7gu" /><dcterms:issued>2001</dcterms:issued><dc:creator>Balagurunathan, Yoganand</dc:creator><dc:creator>Bilinski, Halka</dc:creator><dc:creator>Dougherty, Edward R.</dc:creator><dc:creator>Frančišković-Bilinski, Stanislav</dc:creator><dc:creator>Vdovć, Neda</dc:creator><dc:format xml:lang="sl">13 strani</dc:format><dc:format xml:lang="sl">številka:2</dc:format><dc:format xml:lang="sl">letnik:20</dc:format><dc:format xml:lang="sl">str. 87-99</dc:format><dc:identifier>ISSN:1580-3139</dc:identifier><dc:identifier>COBISSID:16031961</dc:identifier><dc:identifier>URN:URN:NBN:SI:doc-01NYH1QI</dc:identifier><dc:language>en</dc:language><dc:publisher xml:lang="sl">Društvo za stereologijo in kvantitativno analizo slike, Medicinska fakulteta</dc:publisher><dcterms:isPartOf xml:lang="sl">Image analysis and stereology</dcterms:isPartOf><dc:subject xml:lang="sl">Delec, velikost</dc:subject><dc:subject xml:lang="en">Geologic Sediments</dc:subject><dc:subject xml:lang="sl">geologija</dc:subject><dc:subject xml:lang="en">geology</dc:subject><dc:subject xml:lang="sl">Geološki sedimenti</dc:subject><dc:subject xml:lang="sl">granule</dc:subject><dc:subject xml:lang="en">Image Processing, Computer-Assisted</dc:subject><dc:subject xml:lang="sl">morfologija</dc:subject><dc:subject xml:lang="en">Particle Size</dc:subject><dc:subject xml:lang="en">Random Allocation</dc:subject><dc:subject xml:lang="sl">razporeditev</dc:subject><dc:subject xml:lang="sl">sedimenti</dc:subject><dc:subject xml:lang="sl">Slika, obdelava z računalnikom</dc:subject><dc:subject xml:lang="sl">Slučajnost, razporeditev</dc:subject><dc:subject rdf:resource="http://www.wikidata.org/entity/Q82480" /><dcterms:temporal rdf:resource="2000-2024" /><dc:title xml:lang="sl">Morphological granulometric analysis of sediment images|</dc:title><dc:description xml:lang="sl">Sediments are routinely analyzed in terms of the sizing characteristics of thegrains of which they are composed. Via sieving methods, the grains are separated and a weight-based size distribution constructed. Various moment parameters are computed from the size distribution and these serve as sedimentcharacteristics. This paper examines the feasibility of a fully electronic granularity analysis using digital image processing. The study usesa random model of three-dimensional grains in conjunction with the morphological method of granulometric size distributions. The random model is constructed to simulate sand, silt, and clay particle distributions. Owing to the impossibility of perfectly sifting small grains so that they do not touch,the model is used in both disjoint and non-disjoint modes, and watershedsegmentation is applied in the non-disjoint model. The image-based granulometric size distributions are transformed so that they take into account the necessity to view sediment fractions at different magnifications and in different frames. Gray-scale granulometric moments are then computed using both ordinary and reconstructive granulometries. The resulting moments are then compared to moments found from real grains in seven different sediments using standard weight-based size distributions</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-01NYH1QI"><edm:aggregatedCHO rdf:resource="URN:NBN:SI:DOC-01NYH1QI" /><edm:isShownBy rdf:resource="http://www.dlib.si/stream/URN:NBN:SI:DOC-01NYH1QI/74c51afe-93c3-4344-9dfd-53c985051dc4/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">Društvo za stereologijo in kvantitativno analizo slike</edm:dataProvider><edm:object rdf:resource="http://www.dlib.si/streamdb/URN:NBN:SI:DOC-01NYH1QI/maxi/edm" /><edm:isShownAt rdf:resource="http://www.dlib.si/details/URN:NBN:SI:DOC-01NYH1QI" /></ore:Aggregation></rdf:RDF>