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Major and trace elements distribution in Moldavian soils

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dc.contributor.author ZINICOVSCAIA, Inga
dc.contributor.author DULIU, O. G.
dc.contributor.author CULICOV, Otilia-Ana
dc.contributor.author FRONTASYEVA, Marina V.
dc.contributor.author STURZA, Rodica
dc.date.accessioned 2021-05-13T12:18:09Z
dc.date.available 2021-05-13T12:18:09Z
dc.date.issued 2018
dc.identifier.citation ZINICOVSCAIA, Inga, DULIU, O. G., CULICOV, Otilia-Ana. Major and trace elements distribution in Moldavian soils. In: Romanian Reports in Physics. 2018, V. 70, Art. N. 701. ISSN 12211451, 18418759. en_US
dc.identifier.uri http://www.rrp.infim.ro/2018_70_2.html
dc.identifier.uri http://repository.utm.md/handle/5014/14911
dc.description.abstract The content of seven major and 26 trace elements were investigated by Epithermal Neuron Activation Analysis in a set of 17 samples of soil collected at a depth of 20 to 40 cm from Romanesti and Cricova vineyards. All data were interpreted within the Upper Continental Crust and Average Soil models as well as in accordance with sanitary norms concerning soil contamination. It was evidenced that the mineral material is very close to the Upper Continental Crust with a certain degree of chemical weathering and a prolonged process of sorting and recycling, which sustains the hypothesis of a mature, well developed soil. The content of Cr, Mn, Co, Zn and As, proved that, with excepting As, the soil have no traces of anthropogenic contamination. The As content, according to existing data, can be regarded as a characteristic of Moldavian soils, not related to any industrial polluting process. en_US
dc.language.iso en en_US
dc.publisher Editura Academiei Romane en_US
dc.rights Attribution-NonCommercial-NoDerivs 3.0 United States *
dc.rights.uri http://creativecommons.org/licenses/by-nc-nd/3.0/us/ *
dc.subject chernozems en_US
dc.subject soils en_US
dc.subject Romanesti vineyards en_US
dc.subject Cricova vineyards en_US
dc.title Major and trace elements distribution in Moldavian soils en_US
dc.type Article en_US


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