Literature DB >> 23137032

Environmental speciation of actinides.

Kate Maher1, John R Bargar, Gordon E Brown.   

Abstract

Although minor in abundance in Earth's crust (U, 2-4 ppm; Th, 10-15 ppm) and in seawater (U, 0.003 ppm; Th, 0.0007 ppm), light actinides (Th, Pa, U, Np, Pu, Am, and Cm) are important environmental contaminants associated with anthropogenic activities such as the mining and milling of uranium ores, generation of nuclear energy, and storage of legacy waste resulting from the manufacturing and testing of nuclear weapons. In this review, we discuss the abundance, production, and environmental sources of naturally occurring and some man-made light actinides. As is the case with other environmental contaminants, the solubility, transport properties, bioavailability, and toxicity of actinides are dependent on their speciation (composition, oxidation state, molecular-level structure, and nature of the phase in which the contaminant element or molecule occurs). We review the aqueous speciation of U, Np, and Pu as a function of pH and Eh, their interaction with common inorganic and organic ligands in natural waters, and some of the common U-containing minerals. We also discuss the interaction of U, Np, Pu, and Am solution complexes with common Earth materials, including minerals, colloids, gels, natural organic matter (NOM), and microbial organisms, based on simplified model system studies. These surface interactions can inhibit (e.g., sorption to mineral surfaces, formation of insoluble biominerals) or enhance (e.g., colloid-facilitated transport) the dispersal of light actinides in the biosphere and in some cases (e.g., interaction with dissimilatory metal-reducing bacteria, NOM, or Mn- and Fe-containing minerals) can modify the oxidation states and, consequently, the behavior of redox-sensitive light actinides (U, Np, and Pu). Finally, we review the speciation of U and Pu, their chemical transformations, and cleanup histories at several U.S. Department of Energy field sites that have been used to mill U ores, produce fissile materials for reactors and weapons, and store high-level nuclear waste from both civilian and defense operations, including Hanford, WA; Rifle, CO; Oak Ridge, TN; Fernald, OH; Fry Canyon, UT; and Rocky Flats, CO.

Entities:  

Year:  2012        PMID: 23137032     DOI: 10.1021/ic301686d

Source DB:  PubMed          Journal:  Inorg Chem        ISSN: 0020-1669            Impact factor:   5.165


  27 in total

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4.  Cleanup and Complexity: Nuclear and Industrial Contamination at The Santa Susana Field Laboratory, California.

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5.  Marine anoxia and delayed Earth system recovery after the end-Permian extinction.

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6.  Diagenetic formation of uranium-silica polymers in lake sediments over 3,300 years.

Authors:  Pierre Lefebvre; Alkiviadis Gourgiotis; Arnaud Mangeret; Pierre Sabatier; Pierre Le Pape; Olivier Diez; Pascale Louvat; Nicolas Menguy; Pauline Merrot; Camille Baya; Mathilde Zebracki; Pascale Blanchart; Emmanuel Malet; Didier Jézéquel; Jean-Louis Reyss; John R Bargar; Jérôme Gaillardet; Charlotte Cazala; Guillaume Morin
Journal:  Proc Natl Acad Sci U S A       Date:  2021-01-26       Impact factor: 12.779

7.  Insights into transport velocity of colloid-associated plutonium relative to tritium in porous media.

Authors:  Jinchuan Xie; Jiachun Lu; Jianfeng Lin; Xiaohua Zhou; Qichu Xu; Mei Li; Jihong Zhang
Journal:  Sci Rep       Date:  2014-05-22       Impact factor: 4.379

8.  Speciation and Bioavailability Measurements of Environmental Plutonium Using Diffusion in Thin Films.

Authors:  Ruslan Cusnir; Philipp Steinmann; Marcus Christl; François Bochud; Pascal Froidevaux
Journal:  J Vis Exp       Date:  2015-11-09       Impact factor: 1.355

9.  Escherichia coli response to uranyl exposure at low pH and associated protein regulations.

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Review 10.  Oxyhydroxy Silicate Colloids: A New Type of Waterborne Actinide(IV) Colloids.

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Journal:  ChemistryOpen       Date:  2016-04-21       Impact factor: 2.911

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