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Soil properties in sessile oak forests (Quercetum montanum typicum Čer. et Jov. 1953) in the area of Fruška Gora

dc.creatorKnežević, Milan
dc.creatorBabić, Violeta
dc.creatorGalić, Zoran
dc.creatorKošanin, Olivera
dc.date.accessioned2024-12-20T12:14:50Z
dc.date.available2024-12-20T12:14:50Z
dc.date.issued2011
dc.identifier.issn0353-4537
dc.identifier.urihttps://omorika.sfb.bg.ac.rs/handle/123456789/374
dc.description.abstractU radu su prikazani rezultati proučavanja zemljišta obrazovanih na peščarima u šumama hrasta kitnjaka (Quercetum montanum typicum Čer. et Jov. 1953) na području Fruške Gore. Na stalnim oglednim površinama osnovanim u gazdinskim jedinicama 'Čortanovačka šuma-Hopovo-Velika Remeta' i 'Beočin-Manastir-Katanske Livade-Osovlje', na području NP 'Fruška Gora', u cilju praćenja uticaja režima svetlosti na razvoj podmlatka hrasta kitnjaka u datim ekološkim uslovima, na osnovu morfogenetskih karakteristika zemljišta i analitičkih vrednosti proučenih osobina zemljišta, a prema klasifikaciji zemljišta Škorića i sar. (1985) definisana su dva tipa zemljišta: kiselo smeđe zemljište (distrični kambisol) i ilimerizovano zemljište (luvisol). Kiselo smeđe zemljište pripada formi srednje dubokog, a ilimerizovano formi dubokog zemljišta.sr
dc.description.abstractThe soils formed on sandstones in sessile oak forests (Quercetum montanum typicum Čer. et Jov. 1953) were researched in the area of Fruška Gora. On permanent sample plots established in management units 'Čortanovačka Forest-Hopovo-Velika Remeta' and 'Beočin-Manastir-Katanske Livade-Osovlje', in the are of NP 'Fruška Gora', aiming at the monitoring of the effect of light regime on the development of sessile oak progeny in the given environmental conditions, based on the morphogenetic characteristics of the soil and analytic values of the soil properties, and based on the soil classification by Škorić et al. (1985), the following two soil types were defined: acid brown soil (dystric cambisol), and illimerised soil (luvisol). Acid brown soil belongs to the form of medium deep soils, and illimerised soil is classified as deep soil.en
dc.publisherUniverzitet u Beogradu - Šumarski fakultet, Beograd
dc.relationinfo:eu-repo/grantAgreement/MESTD/Technological Development (TD or TR)/31041/RS//
dc.rightsopenAccess
dc.rights.urihttps://creativecommons.org/licenses/by/4.0/
dc.sourceGlasnik Šumarskog fakulteta
dc.subjectpeščarsr
dc.subjectluvisolsr
dc.subjecthrast kitnjaksr
dc.subjectFruška Gorasr
dc.subjectdistrični kambisolsr
dc.subjectsessile oaken
dc.subjectsandstoneen
dc.subjectluvisolen
dc.subjectFruška Goraen
dc.subjectdystric cambisolen
dc.titleOsobine zemljišta u šumama hrasta kitnjaka (Quercetum montanum typicum čer. et Jov. 1953) na području Fruške Goresr
dc.titleSoil properties in sessile oak forests (Quercetum montanum typicum Čer. et Jov. 1953) in the area of Fruška Goraen
dc.typearticle
dc.rights.licenseBY
dc.citation.epage108
dc.citation.issue104
dc.citation.other(104): 97-108
dc.citation.spage97
dc.identifier.doi10.2298/GSF1104097K
dc.identifier.fulltextomorika.sfb.bg.ac.rs/bitstream/id/629/371.pdf
dc.identifier.rcubconv_349
dc.type.versionpublishedVersion


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