Joan Serra-Ventura , Guillem Sabaté-Herrero , Anna Rigol , Miquel Vidal
{"title":"Chemical analogues and probabilistic functions to derive distribution coefficients of radium in soils","authors":"Joan Serra-Ventura , Guillem Sabaté-Herrero , Anna Rigol , Miquel Vidal","doi":"10.1016/j.jenvrad.2025.107769","DOIUrl":null,"url":null,"abstract":"<div><div>The existing data gaps in the sorption and desorption parameters of naturally occurring radionuclides (e.g., radium (Ra)) challenge the use of radioecological risk assessment models. We present two alternatives for deriving Ra distribution coefficients (K<sub>d</sub> (Ra)) in soils when the physicochemical information on the solid and liquid phases involved is too scarce to apply parametric prediction models: the deduction of sorption parameters from those of chemical analogues (such as Ba and Sr) and the proposal of best estimate K<sub>d</sub> (Ra) values deduced from probabilistic distribution functions of data grouped according to relevant factors affecting K<sub>d</sub> (Ra) variability. Regarding the use of chemical analogues, partial least squares regression analysis and univariate linear correlations revealed that Ba and Ra sorption in soils was governed by the same soil properties (K<sub>d</sub> (Ca + Mg) and Mn<sub>am</sub>), related to exchangeable sites on the soil surface. The derivation of K<sub>d</sub> (Ra) values from K<sub>d</sub> (Ba) and also K<sub>d</sub> (Sr) is feasible by applying suitable correction factors. Furthermore, several K<sub>d</sub> (Ra) best estimates were derived from the distribution functions of K<sub>d</sub> (Ra) datasets obtained from own and literature data. Statistical differences were noticed for the sorption and desorption datasets (the latter significantly affected by data from native Ra), leading to the proposal of distinct K<sub>d</sub> (Ra) values (870 and 2760 L kg<sup>−1</sup>, respectively) for uptake and remobilisation scenarios. Regarding the desorption data, diverse K<sub>d</sub> (Ra) best estimates were suggested for acidic (1540 L kg<sup>−1</sup>) and alkaline (6440 L kg<sup>-1</sup>) soils. For the sorption data, statistically different K<sub>d</sub> (Ra) best estimates were suggested according to pH (100 and 1240 L kg<sup>−1</sup> for pH < 4.5 and pH ≥ 7, respectively) and water-soluble Ca + Mg content, allowing for the selection of the most appropriate best estimate values for use in risk assessment models depending on the available information.</div></div>","PeriodicalId":15667,"journal":{"name":"Journal of environmental radioactivity","volume":"289 ","pages":"Article 107769"},"PeriodicalIF":2.1000,"publicationDate":"2025-07-31","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Journal of environmental radioactivity","FirstCategoryId":"93","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S0265931X25001560","RegionNum":3,"RegionCategory":"环境科学与生态学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q3","JCRName":"ENVIRONMENTAL SCIENCES","Score":null,"Total":0}
引用次数: 0
Abstract
The existing data gaps in the sorption and desorption parameters of naturally occurring radionuclides (e.g., radium (Ra)) challenge the use of radioecological risk assessment models. We present two alternatives for deriving Ra distribution coefficients (Kd (Ra)) in soils when the physicochemical information on the solid and liquid phases involved is too scarce to apply parametric prediction models: the deduction of sorption parameters from those of chemical analogues (such as Ba and Sr) and the proposal of best estimate Kd (Ra) values deduced from probabilistic distribution functions of data grouped according to relevant factors affecting Kd (Ra) variability. Regarding the use of chemical analogues, partial least squares regression analysis and univariate linear correlations revealed that Ba and Ra sorption in soils was governed by the same soil properties (Kd (Ca + Mg) and Mnam), related to exchangeable sites on the soil surface. The derivation of Kd (Ra) values from Kd (Ba) and also Kd (Sr) is feasible by applying suitable correction factors. Furthermore, several Kd (Ra) best estimates were derived from the distribution functions of Kd (Ra) datasets obtained from own and literature data. Statistical differences were noticed for the sorption and desorption datasets (the latter significantly affected by data from native Ra), leading to the proposal of distinct Kd (Ra) values (870 and 2760 L kg−1, respectively) for uptake and remobilisation scenarios. Regarding the desorption data, diverse Kd (Ra) best estimates were suggested for acidic (1540 L kg−1) and alkaline (6440 L kg-1) soils. For the sorption data, statistically different Kd (Ra) best estimates were suggested according to pH (100 and 1240 L kg−1 for pH < 4.5 and pH ≥ 7, respectively) and water-soluble Ca + Mg content, allowing for the selection of the most appropriate best estimate values for use in risk assessment models depending on the available information.
期刊介绍:
The Journal of Environmental Radioactivity provides a coherent international forum for publication of original research or review papers on any aspect of the occurrence of radioactivity in natural systems.
Relevant subject areas range from applications of environmental radionuclides as mechanistic or timescale tracers of natural processes to assessments of the radioecological or radiological effects of ambient radioactivity. Papers deal with naturally occurring nuclides or with those created and released by man through nuclear weapons manufacture and testing, energy production, fuel-cycle technology, etc. Reports on radioactivity in the oceans, sediments, rivers, lakes, groundwaters, soils, atmosphere and all divisions of the biosphere are welcomed, but these should not simply be of a monitoring nature unless the data are particularly innovative.