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Mössbauer and X-ray fluorescence study of sediments from Samana Bay, Dominican Republic

dc.contributor.authorVillagran, M.
dc.contributor.authorSbriz, L.
dc.contributor.authorAlvarez, M.
dc.date.accessioned2023-12-04T02:38:11Z
dc.date.available2023-12-04T02:38:11Z
dc.date.issued1995-08
dc.identifier.citationVillagrán, M., Sbriz, L., y Alvarez, M. (1995). Mössbauer and X-ray fluorescence study of sediments from Samana Bay, Dominican Republic. Journal of Radioanalytical and Nuclear Chemistry, 200, 483-490.https://doi.org/10.1007/BF02162497en_US
dc.identifier.urihttps://repositorio.unphu.edu.do/handle/123456789/5412
dc.description.abstractThe chemical state of iron in sediments collected from Samana Bay has been determined by Mössbauer spectroscopy. The Mössbauer spectra were composed of two paramagnetic doulets, which correspond to high=spin ferric and ferrous components. Based on the Mössbauer spectra, the possible origin of the different types of sediments are discussed. The mercury contamination calculated from X-ray fluorescence results for some sediments is shown in a comparative formen_US
dc.language.isoenen_US
dc.publisherJournal of Radioanalytical and Nuclear Chemistryen_US
dc.rightsAttribution-NonCommercial-NoDerivatives 4.0 Internacional*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/4.0/*
dc.subjectBahía de Samana (República Dominicana)en_US
dc.subjectEspectroscopía de Mössbaueren_US
dc.subjectSedimentos geológicosen_US
dc.subjectSedimentos marinosen_US
dc.titleMössbauer and X-ray fluorescence study of sediments from Samana Bay, Dominican Republicen_US
dc.typeArticleen_US


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Attribution-NonCommercial-NoDerivatives 4.0 Internacional
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