Приказ основних података о документу

dc.creatorTomić, Zorica
dc.creatorMakreski, Petre
dc.creatorGajić, Boško
dc.date.accessioned2020-12-17T19:51:27Z
dc.date.available2020-12-17T19:51:27Z
dc.date.issued2010
dc.identifier.issn0377-0486
dc.identifier.urihttp://aspace.agrif.bg.ac.rs/handle/123456789/2329
dc.description.abstractRaman and IR spectroscopy were used for the characterization of several minerals in morphologically similar vertisol sequences from Kizevak (Serbia). It helped us to establish the surface layer transition going from calcic vertisols (containing gypsum and calcite) to calcimagnesic vertisols (containing aragonite, magnesium-calcite and dolomite) derived from peridotite and serpentinite. The observed band positions are found to be solely characteristic for each carbonate mineral and are used to discuss the main structural features of carbonates and sulfates present in the studied soil. It was found that the dolomite, calcite and aragonite concretions are present in the deepest layer of the soil, whereas the gypsum is found in the topsoil. The identification was confirmed of the carbonates having calcite and aragonite structure, and the representative from the sulfate group (gypsum) was confirmed by X-ray powder diffraction.en
dc.publisherWiley, Hoboken
dc.rightsrestrictedAccess
dc.sourceJournal of Raman Spectroscopy
dc.subjectsoilen
dc.subjectmineralsen
dc.subjectRaman spectroscopyen
dc.subjectIR spectroscopyen
dc.subjectX-ray powder diffraction (XRPD)en
dc.titleIdentification and spectra-structure determination of soil minerals: Raman study supported by IR spectroscopy and X-ray powder diffractionen
dc.typearticle
dc.rights.licenseARR
dc.citation.epage586
dc.citation.issue5
dc.citation.other41(5): 582-586
dc.citation.rankM21
dc.citation.spage582
dc.citation.volume41
dc.identifier.doi10.1002/jrs.2476
dc.identifier.scopus2-s2.0-77952937748
dc.identifier.wos000278338200016
dc.type.versionpublishedVersion


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Приказ основних података о документу