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Features of cutans complex in Albeluvisols of the Ukrainian Precarpathians

Features of cutans complex in Albeluvisols of the ...

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dc.contributor.author Nikorych, V. pl
dc.contributor.author Szymański, Wojciech [SAP13003405] pl
dc.contributor.author Skiba, Stefan [SAP11013048] pl
dc.contributor.author Kryzhanivskiy, O. pl
dc.date.accessioned 2016-08-09T13:09:46Z
dc.date.available 2016-08-09T13:09:46Z
dc.date.issued 2012 pl
dc.identifier.issn 1684-9094 pl
dc.identifier.uri http://ruj.uj.edu.pl/xmlui/handle/item/29465
dc.language eng pl
dc.rights Dodaję tylko opis bibliograficzny *
dc.rights.uri *
dc.title Features of cutans complex in Albeluvisols of the Ukrainian Precarpathians pl
dc.type JournalArticle pl
dc.description.physical 40-51 pl
dc.description.additional Bibliogr. s. 50-51 pl
dc.identifier.weblink http://www.ussj.cv.ua/2012_t13_3-4/Nikorych.pdf pl
dc.abstract.en Cutans occurring in Albeluvisols of the Precarpathians in the Ukraine were studied. The morphology of the cutans and their components were described. The obtained results show that the studied cutans are composed mainly of colloidal clay. Clay cutans in the studied soils are characterized by smooth surface, microlamination, and clear optical orientation of clay domains. It was found that the microlamination of the clay cutans is a result of cyclic material deposition due to translocation of colloids (i.e. eluviation-illuviation). Complex layered cutans containing layers of pure clay, microlaminated clay and silt were also found. It was shown that the colour of clay cutans depends on their composition. Domination of brown, dark brown and rusty-brown cutans indicates that clay minerals and Fe-oxides are main component of such microstructures. Several morphotypes of cutans were determined: sandy-silty, clay, humus-clay, humus-silty-clay, silty-clay, and iron-clay. Most of the identified morphotypes of cutans are a result of mobilization, translocation, and accumulation of colloids within the studied soil profiles. Based on the cutans complex it was concluded that the genesis of the studied soils is related to illimerization (lessivage) and gley-eluvial processes. pl
dc.subject.en cutans pl
dc.subject.en gley-eluvial process pl
dc.subject.en illimerization (lessivage) pl
dc.subject.en Albeluvisols pl
dc.subject.en Precarpathians pl
dc.description.volume 13 pl
dc.description.number 3-4 pl
dc.identifier.eissn 2310-4341 pl
dc.title.journal Ґрунтознавство = Ġruntoznavstvo = Soil Science pl
dc.language.container ukr pl
dc.date.accession 2015-03-10 pl
dc.affiliation Wydział Biologii i Nauk o Ziemi : Instytut Geografii i Gospodarki Przestrzennej pl
dc.subtype Article pl
dc.rights.original OTHER; otwarte czasopismo; ostateczna wersja wydawcy; w momencie opublikowania; 0; pl


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