1991
DOI: 10.1080/18811248.1991.9731350
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Evaluation of Migration of Cesium-137 Adsorbed on Fine Soil Particles through Natural Aerated Soil Layer

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Cited by 3 publications
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“…This is confirmed by sorption isotherms onto chalky soil and onto chalk doped with humic acids, which clearly highlights the part taken by humic substances for complexation and immobilization of U in the chalky soil. Nevertheless, these observations are of interest for further investigations on U migration in the subsurface since humic substances are also known to be easily mobilizable from soils, mobile in soils, and mobile in aquifers and can enhance U migration under colloidal form. ,,,,, In the first 120 cm of the soil profile, where the U content is typically above 10 ppm, the results of EXAFS and TRLFS speciation analysis and interpretations from sorption isotherms are in agreement. The TRLFS analysis indicates a double speciation of U onto carbonate minerals, revealing the presence of at least two complexes for adsorbed U, which change proportion with U loading with a slight rearrangement of oxygen equatorial coordination, consistent with previous interpretations from other authors. For low U loading on the calcite surface, a bidentate uranyl tricarbonate complex with a liebigite-type structure dominates the speciation.…”
Section: Discussionmentioning
confidence: 54%
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“…This is confirmed by sorption isotherms onto chalky soil and onto chalk doped with humic acids, which clearly highlights the part taken by humic substances for complexation and immobilization of U in the chalky soil. Nevertheless, these observations are of interest for further investigations on U migration in the subsurface since humic substances are also known to be easily mobilizable from soils, mobile in soils, and mobile in aquifers and can enhance U migration under colloidal form. ,,,,, In the first 120 cm of the soil profile, where the U content is typically above 10 ppm, the results of EXAFS and TRLFS speciation analysis and interpretations from sorption isotherms are in agreement. The TRLFS analysis indicates a double speciation of U onto carbonate minerals, revealing the presence of at least two complexes for adsorbed U, which change proportion with U loading with a slight rearrangement of oxygen equatorial coordination, consistent with previous interpretations from other authors. For low U loading on the calcite surface, a bidentate uranyl tricarbonate complex with a liebigite-type structure dominates the speciation.…”
Section: Discussionmentioning
confidence: 54%
“…Nevertheless, these observations are of interest for further investigations on U migration in the subsurface since humic substances are also known to be easily mobilizable from soils, mobile in soils, and mobile in aquifers and can enhance U migration under colloidal form. [36][37][38]42,43,72,123,124 3) In the first 120 cm of the soil profile, where the U content is typically above 10 ppm, the results of EXAFS and TRLFS speciation analysis and interpretations from sorption isotherms are in agreement. The TRLFS analysis indicates a double speciation of U onto carbonate minerals, revealing the presence of at least two complexes for adsorbed U, which change proportion with U loading with a slight rearrangement of oxygen equatorial coordination, consistent with previous interpretations from other authors.…”
Section: Discussionmentioning
confidence: 74%
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