Recent Advances In Actinide Science
836
Recent Advances In Actinide Science
836Hardcover
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Product Details
| ISBN-13: | 9780854046782 |
|---|---|
| Publisher: | RSC |
| Publication date: | 08/08/2006 |
| Series: | Special Publications , #305 |
| Pages: | 836 |
| Product dimensions: | 6.15(w) x 9.20(h) x (d) |
About the Author
R Alvarez:
Over eight years of research in environmental geochemistry including more than two years of postdoctoral research experience at The University of Manchester, UK studying analytical environmental separations of actinides in support of the Geoffrey Schofield Laboratories at BNFL, Sellafield. Currently undertaking research on the environmental biogeochemistry of depleted uranium.
PhD obtained in the area of analytical environmental geochemistry.
One year industrial experience at Australia’s National Medical Cyclotron facility at ANSTO, Sydney, producing radiopharmaceuticals.
Author of five refereed publications and two technical reports.
N D Bryan:
Following Ph.D. 5 years postdoctoral experience researching the colloidal properties of humic substances, their interaction with metal ions, particularly radionuclides, and their effects upon the transportation of pollutants in the environment.
In 1999, appointed as lecturer in Radiochemistry in the Centre for Radiochemistry Research, School of Chemistry, University of Manchester.
I May:
4 Years experience working for BNFL at Sellafield as a Research Associate on actinide chemistry of relevance to nuclear fuel reprocessing
Since 1999 employed as a Lecturer in the Centre for Radiochemistry Research, School of Chemistry, University of Manchester
Over 60 publications and numerous technical reports on actinide coordination chemistry and related subject areas.
Read an Excerpt
Recent Advances in Actinide Science
By Iain May, Rebeca Alvares, Nicholas Bryan
The Royal Society of Chemistry
Copyright © 2006 The Royal Society of ChemistryAll rights reserved.
ISBN: 978-0-85404-678-2
CHAPTER 1
Analysis, the Environment and Biotransformations
T. Ohnuki
Advanced Science Research Center, Japan Atomic Energy Research Institute, 2-4 Shirakata, Tokai, Ibaraki, 319-1195 Japan
1 INTRODUCTION
The presence of actinides in nuclear reactors and radioactive wastes is a major environmental concern, due to their long radioactive half-lives, their high energy radiation emissions, and their chemical toxicity. In order to estimate the potential impact of actinides on human beings, the mobility of actinides has been examined in terms of its interactions with soils and subsoils composed of abiotic and biotic components, principally minerals and bacteria. Among the biotic components, some microorganisms have cells whose surfaces sorb actinides. The high capacity of microbial surfaces to bind actinides may affect the migration of actinides in the environment. However, we have only limited knowledge of the role of microorganisms in the migration of actinides in the environment.
The interaction of actinides with microorganisms involves (i) adsorption, (ii) oxidation/reduction, (iii) degradation of actinide-organic component complexes and (iv) mineralization (Fig. 1). The interaction of actinides with microorganisms results in changes in their chemical state (biotransformation). The microbiology research group of JAERI is conducting basic scientific research on microbial interactions with actinides. Fundamental research on microbial transformations of actinides involves elucidating the mechanisms of dissolution and precipitation of various chemical forms, such as ions, oxides, and organic and inorganic complexes of actinides by aerobic or anaerobic microorganisms under relevant microbial process conditions. In the present report, recent findings from the heavy elements microbiology research group of JAERI are summarized.
2 ADSORPTION OF Pu(VI) AND U(VI) BY LICHEN AND YEAST
Lichens are symbiotic organisms consisting of fungal (mycobiont) and photosynthetic (photobiont) components, the latter of which may be a green alga or cyanobacterium. Lichens occur worldwide and on account of their dominance in certain terrestrial ecosystems (especially arctic/Antarctic tundra regions), play a major role in plant ecology and the cycling of some elements, such as C, N and P, and radionuclides. The ability of lichens to accumulate metals has led to their use in monitoring Pu fall-out from accidents, e.g. from Chernobyl and nuclear weapons tests. The concentration of Pu in reindeer lichen (Cladonia subgen. Cladina) has been studied, because Cladonia species form the first link of the lichen-reindeer-man subarctic food chain. These findings suggest that lichen affects the long-term migration of Pu in the environment. However, the accumulation mechanisms have not yet been identified.
Actinides can exist in different oxidation states of III, IV, V and VI in solution, and their chemical behaviour depends on the oxidation state. Actinides (V) and (VI) are more mobile than actinides (III) and (IV) in groundwater. Ohnuki et al. have studied the uptake of plutonium (VI) and uranium (VI) by lichen biomass of foliose lichen Parmotrema tinctorum to elucidate the migration behaviour of Pu and U in the terrestrial environment.
In accumulation experiments, discs 1 cm diam., weighing ca 9 mg cut from the outer margin of Parmotrema tinctorum (Nyl.) Hale were exposed to a Pu (VI) or U (VI) solution of 4.0x10-4 mol L-1 for 96 h at pH 3, 4 and 5. The oxidation states of Pu and U in the solutions were determined by UV/VIS absorption spectroscopy. The oxidation states of Pu and U accumulated by P. tinctorum were determined by UV/VIS absorption spectroscopy on extracts from the Pu/U-accumulated samples with 50% H3PO4 solutions.
Plutonium and uranium uptake by P. tinctorum after 96 h incubation averaged 0.040 and 0.055 g gdry-1, respectively. SEM observations showed that the accumulated Pu is evenly distributed on the upper and lower surfaces of P. tinctorum. On the contrary, U(VI) was accumulated in medullary layers as well as both cortexes (Fig. 2). Interestingly, U in the region of the algal layer was below the detection limit. UV/VIS absorption spectroscopy demonstrated that a fraction of Pu(VI) in the solution was reduced to Pu(V), and the accumulated Pu on the surface was reduced to Pu(IV). Meanwhile, U(VI) maintained the oxidation state of VI in the solution and on the lichen.
Plutonium (VI) was reduced to Pu(V) in the exudates solution, in which P. tinctorum was immersed in a 0.01 M NaCl solution for 96 h and then P. tinctorum was removed. These results indicate that the exudates reduce Pu from VI to V in solution. Melanin can act as an electron donor. Approximately 5% Pu(VI) was reduced to Pu(IV) in the solution containing the exudates within 480 h contact. This reduction was caused by the exudates of organic substances released from P. tinctorum. Metabolites other than melanin may have a similar potential to melanin to be electron donors. These findings suggest that the organic substances on the cortical cortex directly transfer electrons from their functional groups to the sorbed Pu(VI) and Pu(V) to Pu(IV). This direct electron transfer is one of the possible mechanisms for the reduction of Pu(VI) and Pu(V). Since the solubility of Pu(IV) hydroxides is very low, reduced Pu(VI) does not penetrate to medullary layers, but is probably precipitated as Pu(IV) hydroxides on the cortical lichen surface.
Similar adsorption experiments have been carried out to examine the interactions of U(VI) and Pu(VI) with Saccharomyces cerevisiae and thereby elucidate the accumulation mechanism of actinides(VI) by microorganisms. In the accumulation experiments, precultured S. cerevisiae was exposed to 4x10-4 M U(VI) or Pu(VI) in 0.01 M NaCl solution with an initial pH between 3 and 5. Concentrations and oxidation states of U and Pu in the solutions were measured at predetermined intervals. Oxidation states of the sorbed Pu and U were determined by UV/VIS spectrometry and XANES, respectively.
Time courses of sorption of Pu(VI) and U(VI) by the yeast cells (Fig. 3) showed abrupt decreases in solution fraction with time after exposure to the yeast. Interestingly, the accumulation rate of Pu was higher than that of U. More than 90% of Pu and U were accumulated by the yeast under experimental conditions. These results indicated that the cell surfaces of the yeast also have high affinities for Pu and U.
Only one peak around 570 nm (Pu(V)) was distinguished in the UV/VIS spectrum of the Pu solution at 2 h after the exposure (Fig. 4a). No peak around 831 nm (Pu(VI) appeared. No peak for Pu was distinguished in the UV/VIS spectrum of the Pu solution at 24 h. These results indicated that the oxidation state of Pu in the solution changed from VI to V within 2 h. A sharp peak appeared around 831 nm, and small peaks around 642 and 667 nm (Pu(IV)) were distinguished in the UV/VIS spectrum of the extract from the Pu-accumulated S. cerevisiae at 2 h after the exposure (Fig. 4b). Peak intensity around 642 and 667 nm increased with the exposure time; by contrast, peak intensity around 831 nm decreased. It is known that Pu(V) in the acid solution changes its oxidation state to IV and VI by disproportionation, i.e.,
2Pu(V)O2+ + 4H+ = Pu(VI)O22+ + Pu4+ + 2H2O
Thus, the oxidation state of Pu was V at 2 h, and changed to IV with increasing time.
These results showed that Pu was highly accumulated in microorganisms after their exposure to it. Even though the oxidation state of Pu kept at VI in the solution without microorganisms, it changed from VI to V in solution after exposure to microorganisms, probably by released exudates. Direct electron transfer from functional groups of organic substances to the sorbed Pu(VI) and Pu(V) is one of the possible mechanisms for the reduction of Pu(VI) and Pu(V). The Pu(VI) reduction occurs by a two step reaction from VI to IV through V, and differs from that of U(VI), where no reduction occurred.
3 ADSORPTION OF Ln(III) AND An(III) ON CELL SURFACES OF MICROORGANISMS
Various microbial species have different cell-surface characteristics. Chrorella vulgaris is an autotrophic unicellular alga having cellulose as cell-wall components. Bacillus subtilis is a Gram-positive bacterium whose cell surface is composed of peptidoglycan and teicoic acid. Pseudomonas fluorescens is a Gram-negative bacterium. Its cell wall is more complex in both chemical and structural terms than that of a Gram-positive bacterium, and its external outer membrane is composed of protein, phospholipid and lipopolysaccharide. Halomonas sp., Halomonas salinarum and Halomonas halobium are halophic bacteria having highly hydrophobic cell surfaces. The association of Eu(III) and Cm(III) with these microorganisms was studied to elucidate the effects of cell surface structure on adsorption.
Ozaki et al. have studied the kinetics of Eu(III) and Cm(III) sorption by various kinds of bacteria at pH 3-5. The amounts of organic carbon exuded from C. vulgaris, Halomonas sp. and H. halobium were determined by measurements of the dissolved organic carbon (DOC). The kinetics of the adsorption of Eu(III) and Cm(III) on the cell surfaces of C. vulgaris indicated that adsorption reached a maximum in a very short time, and then decreased with increasing time. This decrease reflects the presence of exuded organic carbon, which desorbed Eu(III) and Cm(III) from the cell surfaces. A similar tendency was observed for Halomonas sp. at pH 5 and H. halobium at pH 4. These imply that exudates from bacteria enhance the mobility of actinides and lanthanides.
The kinetics of Eu(III) and Cm(III) sorption showed no significant difference between Eu(III) and Cm(III) for C. vulgaris, B. subtilis, P. fluorescens, and H. halobium. However, a difference in the sorption kinetics of Eu(III) and Cm(III) by Halomonas sp. was observed. Higher amounts of Cm(III) than Eu(III) were accumulated at 20 min after exposure to Halomonas sp., suggesting a difference in the affinity of Eu(III) and Cm(III) to the functional groups of its cell surfaces. A slight higher fraction of Cm(III) was accumulated by H. halobium than Eu(III). These results suggest that halophilic bacteria have different sorption sites for actinides from non-halophilic bacteria.
4 EFFECTS OF METABOLITES ON THE SORPTION ACTINIDES
As mentioned above, exudates from microorganisms reduce the sorption of Eu(III) by bacteria. Naturally occurring chelating substances also have the potential to reduce the sorption of actinides and lanthanides by forming complexes in the environment. Siderophores, produced by microorganisms, access insoluble cations and form complexes, not only with Fe but also with actinides, causing their solubility to increase. Yoshida et al.' have studied the effects of desferrioxamine (DFO) B on the sorption of trivalent and tetravalent lanthanides and actinides by soil bacteria of P. fluorescens and B. subtilis.
The sorption density of Pu(IV) and Th(IV) on bacterial cells, and Fe(III) and Eu(III) on P. fluorescens in the presence of DFO (Fig. 5) indicated that sorption of Pu(IV) on P. fluorescens increased from 3 to 19 µM g-1 with a decrease of pH from 7.3 to 3.0, while sorption of Pu(IV) on B. subtilis and Fe(III) on P. fluorescens was smaller than 3 µM g-1 at about pH 3-8. Sorption of Th(IV) on P. fluorescens increased from 21 to 42 µM g-1 with a decrease of pH from 7.5 to 4.0, and sorption of Th(IV) on B. subtilis increased from 3 to 31 µM g-1 with a decrease of pH from 7.8 to 3.3. On the contrary, adsorption of DFO on both species was negligible at 3 hours after contact of the 1:1 Th(IV)-DFO complex with P. fluorescens or B. subtilis cells at pH 5.5. No DFO was sorbed on P. fluorescens cells from Eu(III)-DFO complexes. These results indicate that Th(IV)-, Pu(IV)- and Eu(III)-dissociate by contact with cells, after which the metals are sorbed.
Stability constants of the metal-DFO complexes decrease in the order of Pu(IV) (log K = 30.8) > Fe(III) (log K = 30.6) > Th(IV) (log K = 26.6) > Eu(III) (log K = 15). Adsorption density of Eu(III), Th(IV), and Pu(IV) on P. fluorescens cells decreased in the order Eu(III) > Th(IV) > Pu(IV), which corresponds to the increasing order of the stability constant of the DFO complexes. Adsorption of hydrated Eu(III) on P. fluorescens cells does not change significantly at pH 3 - 8, indicating that the affinity of P. fluorescens cell surfaces with metal ions is not changed significantly at these pHs. These facts indicate that pH dependence of adsorption density of metal ions on cells is dominated by the stability of the metal-DFO complexes.
Yoshida et al. investigated the influence of DFO on the sorption behavior of 11 rare-earth elements (REEs), La, Ce, Pr, Nd, Sm Eu, Gd, Tb, Dy, Ho, and Er on P. fluorescens cells at neutral pH. Pseudomonas fluorescens cell suspensions (1.3 g (dry wt.) L-1) in the suspensions were incubated for 30 minutes in 10 ml of 0.1 M Tris-HCl solutions containing 1.0 mg L-1 of each REE (La, 7.20 µM; Ce, 7.14 µM; Pr, 7.10 µM; Nd, 6.93 µM; Sm, 6.65 µM; Eu, 6.58 µM; Gd, 6.36 µM; Tb, 6.29 µM; Dy, 6.15 µM; Ho, 6.06 µM; Er, 5.98 µM) and 0.5 mM DFO in air at room temperature. The oxidation state of Ce was determined by X-ray absorption near edge structure (XANES) spectroscopy in fluorescence mode at the BL27B line at the High Energy Accelerator Research Organization (Tsukuba, Japan).
In the presence of DFO, the percent fraction of REEs in the solution after exposure to P. fluorescens cells (Fig. 6) showed a tendency to increase with increasing atomic number, except for Ce. The adsorption of Ce was significantly lower than those of the neighbouring REEs, La and Pr. On the contrary, no Ce anomaly in the sorption was distinguished in the solution with hydroxylammonium. XANES analysis of Ce in the Ce-DFO complex showed that Ce was in the tetravalent state. Adding hydroxylammonium reduced the tetravalent Ce in the complex to its trivalent form and erased the Ce anomaly (Fig. 6). These results show that DFO can oxidize Ce(III) to Ce(IV). Cyclic voltammetry revealed that the redox potential of the Ce(IV)/Ce(III) couple in the DFO complex was much lower than the standard redox potential, and that the stability of Ce(IV)-DFO is much higher than that of Ce(III)-DFO. These findings suggest that the observed Ce anomaly is due to the oxidation of the Ce(III)-DFO complex to the more stable Ce(IV)-DFO complex, and that naturally occurring organic ligands can contribute to this Ce anomaly in the natural environment.
5 SORPTION OF U(VI) BY THE MIXTURES OF MICROORGANISM AND CLAY
Soils and subsoils are composed of abiotic and biotic components, principally minerals and bacteria. It is therefore important to elucidate the role of microorganisms on the accumulation of actinides in such mixtures. Ohnuki et al. assessed the accumulation of uranium (VI) by a bacterium, Bacillus subtilis, suspended in a slurry of kaolinite clay, to elucidate the role of microbes on the mobility of U(VI). Various mixtures of bacteria and the koalinite were exposed to solutions of 8x10-6 M and 4x10-4 M-U(VI) in 0.01 M NaCl at pH 4.7. After 48 h, the mixtures were separated from the solutions by centrifugation, and treated with a 1 M CH3COOK for 24 h to determine the associations of U within the mixture. The mixture exposed to 4x10-4 M U was analyzed by a transmission electron microscope (TEM) equipped with EDS.
The accumulation of U by the mixture increased with an increase in the amount of B. subtilis cells present at both U concentrations. Treatment of kaolinite with CH3COOK removed approximately 80% of the associated uranium. However, in the presence of B. subtilis the amount of U removed was much less. TEM-EDS analysis confirmed that most of the U removed from solution was associated with B. subtilis. XANES analysis of the oxidation state of uranium associated with B. subtilis, kaolinite, and with the mixture containing both revealed that it was present as U(VI). These results suggest that the bacteria have a higher affinity for U than the kaolinite clay mineral under the experimental conditions tested, and that they can immobilize significant amounts of uranium.
CHAPTER 2MICROBIAL TRANSFORMATIONS OF ACTINIDES IN TRANSURANIC- AND MIXED-WASTES: IMPLICATIONS FOR RADIOACTIVE-WASTE DISPOSAL
A.J. Francis
Environmental Sciences Department Brookhaven National Laboratory, Upton, New York 11973, USA
1 INTRODUCTION
The presence of actinides (U, Np, Pu, Am), organic- (cellulose, plastics, rubber, chelating agents) and inorganic- (nitrate and sulfate) compounds in transuranic (TRU) and mixed wastes are a major concern, because of their potential for migration from the waste repositories and contamination of the environment. The primary causes of this disquiet are the toxicity of the actinide elements and the long half-lives of their isotopes. The radionuclides may be present in TRU wastes in various forms, such as elemental, oxide, co-precipitates, ionic, inorganic-, and organic-complexes, and also as naturally occurring minerals, depending on the process and waste stream.
The actinides existing in various oxidation states that are the ones of concern are III (Am, Pu, U), IV (Pu, U), V (Np, Pu), and VI (Pu, U). Significant aerobic- and anaerobic-microbial activity is expected to occur in the waste because of the presence of electron donors and acceptors. The actinides initially may be present as soluble- or insoluble-forms but, after disposal, may be converted from one to the other by microorganisms. The direct enzymatic or indirect non-enzymatic actions of microbes could alter the speciation, solubility, and sorption properties of the actinides, thereby increasing or decreasing their concentrations in solution. Dissolution of radionuclides reflects changes in the Eh and pH of the local environment caused by the microorganisms, by their production of CO2, or of extra cellular metabolic products, such as organic acids, and sequestering agents such as siderophores. Immobilization or precipitation of radionuclides is due to changes in the Eh of the environment, enzymatic reductive precipitation (reduction from a higher to lower oxidation state), biosorption, bioaccumulation, biotransformation of radionuclide-organic and -inorganic complexes, and bioprecipitation. Free-living bacteria suspended in the groundwater fall within the colloidal size range and may have a strong radionuclide sorbing capacity, giving them the potential to transport radionuclides in the subsurface. Further, gases generated from the biodegradation of TRU wastes, thereby pressurizing the containment areas, with subsequent reduction in the volume of the waste and subsidence in the repository. Microbial corrosion of the waste canisters also is a major concern.
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Excerpted from Recent Advances in Actinide Science by Iain May, Rebeca Alvares, Nicholas Bryan. Copyright © 2006 The Royal Society of Chemistry. Excerpted by permission of The Royal Society of Chemistry.
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