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Conţinutul şi formele chimice ale fierului în cernoziomurile stagnice gleice

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dc.contributor.author LEAH, Tamara
dc.date.accessioned 2023-11-08T11:50:15Z
dc.date.available 2023-11-08T11:50:15Z
dc.date.issued 2010
dc.identifier.citation LEAH, Tamara. Conţinutul şi formele chimice ale fierului în cernoziomurile stagnice gleice. In: Ştiinţa Agricolă. 2010, nr. 2, pp. 3-7. ISSN 1857-0003, eISSN 2587-3202. en_US
dc.identifier.issn 1857-0003
dc.identifier.issn 2587-3202
dc.identifier.uri http://repository.utm.md/handle/5014/24688
dc.description.abstract The paper presents data on total content and chemical forms of iron in stagnogleyic chernozems from Răut river basin in the central part of Moldova. Essential accumulation of free iron oxides is highlighted only in heavily gley horizons. The absolute majority of these compounds is presented in a crystalline form. It was shown that the genesis of stagnic chernozems is conditioned by gley compounds of Pliocene’s sedimentary rock where they were formed. The accumulation of Fe in gley horizons and particularities of humus in soils’ profile came into being as a result of a combination of contemporary and relict processes of soils’ formation. en_US
dc.language.iso ro en_US
dc.publisher Universitatea Agrară de Stat din Moldova en_US
dc.relation.ispartofseries Știința Agricolă;2010, N. 2
dc.rights Attribution-NonCommercial-NoDerivs 3.0 United States *
dc.rights.uri http://creativecommons.org/licenses/by-nc-nd/3.0/us/ *
dc.subject sol en_US
dc.subject chernoziom stagnic en_US
dc.subject compuși ai fierului en_US
dc.subject gleizare en_US
dc.subject soil en_US
dc.subject stagnic chernozem en_US
dc.subject iron compounds en_US
dc.subject gleyic process en_US
dc.title Conţinutul şi formele chimice ale fierului în cernoziomurile stagnice gleice en_US
dc.title.alternative The content and chemical forms of iron in stagnogleic chernozems en_US
dc.type Article en_US


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