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Investigation of the interaction of Greek dolomitic marble with metal aqueous solutions using rutherford backscattering and X-ray photoelectron spectroscopy

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dc.contributor.author Godelitsas, A en
dc.contributor.author Kokkoris, M en
dc.contributor.author Misaelides, P en
dc.date.accessioned 2014-03-01T02:44:44Z
dc.date.available 2014-03-01T02:44:44Z
dc.date.issued 2007 en
dc.identifier.issn 0236-5731 en
dc.identifier.uri https://dspace.lib.ntua.gr/xmlui/handle/123456789/31945
dc.subject Aqueous Solution en
dc.subject X Ray Photoelectron Spectroscopy en
dc.subject.classification Chemistry, Analytical en
dc.subject.classification Chemistry, Inorganic & Nuclear en
dc.subject.classification Nuclear Science & Technology en
dc.subject.other cadmium en
dc.subject.other carbonic acid en
dc.subject.other chromium en
dc.subject.other cobalt en
dc.subject.other lead en
dc.subject.other aqueous solution en
dc.subject.other conference paper en
dc.subject.other Greece en
dc.subject.other infrared radiation en
dc.subject.other molecular interaction en
dc.subject.other precipitation en
dc.subject.other solid state en
dc.subject.other surface property en
dc.subject.other X ray diffraction en
dc.subject.other X ray photoelectron spectroscopy en
dc.title Investigation of the interaction of Greek dolomitic marble with metal aqueous solutions using rutherford backscattering and X-ray photoelectron spectroscopy en
heal.type conferenceItem en
heal.identifier.primary 10.1007/s10967-007-0526-1 en
heal.identifier.secondary http://dx.doi.org/10.1007/s10967-007-0526-1 en
heal.language English en
heal.publicationDate 2007 en
heal.abstract The interaction of Greek dolomitic marble (from Thassos island, northern Greece) with Co2+, Cd2+, Pb2+ and Cr 3+ containing aqueous solutions was studied by characterizing the surface of the solid experimental samples, using a combination of spectroscopic, microscopic, and diffraction techniques (RBS, XPS, SEM-EDS, FT-IR, powder-XRD). The obtained results indicated a considerable Cd2+ and Co 2+ sorption on the dissolved surface of the carbonate substrate, whereas, under the same experimental conditions, the Pb2+ and Cr 3+ interaction is more intense leading to extended overgrowth of crystalline Pb2+ carbonates and massive surface precipitation of amorphous Cr3+ hydroxide/oxyhydroxide. © 2007 Akadémiai Kiadó. en
heal.publisher SPRINGER en
heal.journalName Journal of Radioanalytical and Nuclear Chemistry en
dc.identifier.doi 10.1007/s10967-007-0526-1 en
dc.identifier.isi ISI:000245360100027 en
dc.identifier.volume 272 en
dc.identifier.issue 2 en
dc.identifier.spage 339 en
dc.identifier.epage 344 en


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