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  4. Effects of low molecular weight organic acids on 137Cs release from contaminated soils
 
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Effects of low molecular weight organic acids on 137Cs release from contaminated soils

Journal
Applied Radiation and Isotopes
Journal Volume
69
Journal Issue
6
Start Page
844
End Page
851
Date Issued
2011-06
Author(s)
Po Neng Chiang  
Ming Kuang Wang
Pan Ming Huang
Jeng Jong Wang
DOI
10.1016/j.apradiso.2011.02.043
DOI
10.1016/j.apradiso.2011.02.043
URI
https://www.scopus.com/record/display.uri?eid=2-s2.0-79953039743&origin=resultslist
https://scholars.lib.ntu.edu.tw/handle/123456789/724394
Abstract
Radio pollutant removal is one of several priority restoration strategies for the environment. This study assessed the effect of low molecular weight organic acid on the lability and mechanisms for release of 137Cs from contaminated soils. The amount of 137Cs radioactivity released from contaminated soils reacting with 0.02M low molecular weight organic acids (LMWOAs) specifically acetic, succinic, oxalic, tartaric, and citric acid over 48h were 265, 370, 760, 850, and 1002Bqkg-1, respectively. The kinetic results indicate that 137Cs exhibits a two-step parabolic diffusion equation and a good linear relationship, indicating that the parabolic diffusion equation describes the data quite well, as shown by low p and high r2 values. The fast stage, which was found to occur within a short period of time (0.083-3h), corresponds to the interaction of LMWOAs with the surface of clay minerals; meanwhile, during the slow stage, which occurs over a much longer time period (3-24h), desorption primarily is attributed to inter-particle or intra-particle diffusion. After a fifth renewal of the LMWOAs, the total levels of 137Cs radioactivity released by acetic, succinic, oxalic, tartaric, and citric acid were equivalent to 390, 520, 3949, 2061, and 4422Bqkg-1 soil, respectively. H+ can protonate the hydroxyl groups and oxygen atoms at the broken edges or surfaces of the minerals, thereby weakening Fe-O and Al-O bonds. After protonation of H+, organic ligands can attack the OH and OH2 groups in the minerals easily, to form complexes with surface structure cations, such as Al and Fe. The amounts of 137Cs released from contaminated soil treated with LMWOAs were substantially increased, indicating that the LMWOAs excreted by the roots of plants play a critical role in 137Cs release.
Subjects
137Cs
Complexation
Low molecular weight organic acids (LMWOAs)
Parabolic diffusion
SDGs

[SDGs]SDG15

Type
journal article

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