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	<dc:title xml:lang="en-US">Application of the de Job method in the evaluation of the stoichiometry of uranyl phosphate complexes sorbed on bentonite</dc:title>
	<dc:creator>Grabias, Ewelina</dc:creator>
	<dc:creator>Gładysz-Płaska, Agnieszka</dc:creator>
	<dc:creator>Lipke, Agnieszka</dc:creator>
	<dc:creator>Pikus, Stanisław</dc:creator>
	<dc:creator>Majdan, Marek</dc:creator>
	<dc:subject xml:lang="en-US">Uranium</dc:subject>
	<dc:subject xml:lang="en-US">Bentonite</dc:subject>
	<dc:subject xml:lang="en-US">Phosphates</dc:subject>
	<dc:subject xml:lang="en-US">Job method</dc:subject>
	<dc:subject xml:lang="en-US">Sorption spectra</dc:subject>
	<dc:subject xml:lang="en-US">Uranyl phosphate complexes</dc:subject>
	<dc:description xml:lang="en-US">For the first time, the continuous variation method was applied for the evaluation of the stoichiometry of uranyl phosphate complexes sorbed on bentonite. Sorption of UO2(CH3COO)2⋅2H2O in the presence of Na2HPO4⋅7H2O from 0.001 mol/L solutions led to the appearance of maxima in the sorption peaks of U(VI) and P(V) ions at molar ratios of [U(VI)]/[P(V)]s = 1.4, 3.3, 3.6 and 1.2, 1.7. It is suggested, based on complementary XRD and XPS data, that the UO2HPO4 complex is located on aluminols (ºAl-OH) whereas the (UO2)3(PO4)2⋅4H2O complex is precipitated in the interlamellar space of bentonite. The participation of (UO2)3(OH)5+ and (UO2)4(OH)7+ species in the formation of U(VI) surface complexes is suggested, based on the deconvolution of sorption spectra of U(VI) on the bentonite in the presence of phosphates.</dc:description>
	<dc:publisher xml:lang="en-US">Atlanta Publishing House LLC</dc:publisher>
	<dc:date>2016-03-31</dc:date>
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	<dc:identifier>https://www.eurjchem.com/index.php/eurjchem/article/view/1348</dc:identifier>
	<dc:identifier>10.5155/eurjchem.7.1.42-48.1348</dc:identifier>
	<dc:source xml:lang="en-US">European Journal of Chemistry; Vol. 7 No. 1 (2016): March 2016; 42-48</dc:source>
	<dc:source>2153-2257</dc:source>
	<dc:source>2153-2249</dc:source>
	<dc:language>eng</dc:language>
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