1998
DOI: 10.1016/s0925-8388(98)00059-0
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Lysimeter studies to investigate the leaching of 241Am from low level radioactive waste

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Cited by 6 publications
(2 citation statements)
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“…To place the obtained results in prespective, we performed a comprehensive literature search and found out that, to the best of our knowledge, only about 20 reports have evaluated leaching behavior of sequestered 241 Am (we used cerium in the current studies as a surrogate). Of the approximately 20 publications, only five of them reported the data associated with leaching kinetics of 241 Am. Despite none of these studies being performed on MOFs, the leaching rates for the other materials such as perovskites, , phosphate ceramics, and zeolites , are on the order of 10 –1 –10 –6 g m –2 ·day –1 , which are in line with the leaching rates presented in our manuscript for MOFs (∼10 –5 g m –2 ·day –1 ).…”
Section: Resultssupporting
confidence: 84%
“…To place the obtained results in prespective, we performed a comprehensive literature search and found out that, to the best of our knowledge, only about 20 reports have evaluated leaching behavior of sequestered 241 Am (we used cerium in the current studies as a surrogate). Of the approximately 20 publications, only five of them reported the data associated with leaching kinetics of 241 Am. Despite none of these studies being performed on MOFs, the leaching rates for the other materials such as perovskites, , phosphate ceramics, and zeolites , are on the order of 10 –1 –10 –6 g m –2 ·day –1 , which are in line with the leaching rates presented in our manuscript for MOFs (∼10 –5 g m –2 ·day –1 ).…”
Section: Resultssupporting
confidence: 84%
“…the top soil layer under the influence of plant roots) may increase 241 Am activity in leachate as a result of acidification and complexation by organic acids exudated by roots and soil microorganisms (Carlsen, 1989;Lu et al, 1998) as it has been demonstrated for heavy metals from mine tailings (Banks et al, 1994;Burckhard et al, 1995). If a great deal of research has been done to assess the distribution and total inventories of 241 Am in surface soils, few studies have tried to understand 241 Am mobility in these environments (Kelly et al, 1998;Bundt et al, 2000;Morris and Raiswell, 2002;Sokolik et al, 2003), even though such understanding stands as a crucial point for risk assessments. At present risk assessment models use a single parameter, the partition coefficient, to apportion contaminant concentrations between dissolved and solid phases (Carroll and Harms, 1999).…”
mentioning
confidence: 99%