En France, les anciennes mines d'uranium et leurs eaux d'exhaure font l'objet d’une surveillance environnementale dû à la présence de stériles miniers qui peuvent modifier la chimie des eaux en augmentant leur concentration en uranium. Afin de pouvoir rejeter des eaux dans le milieu naturel dont les concentrations en U(VI) soient conformes aux normes, des stations de traitement ont été mises en place. Cependant, une future règlementation diminuera drastiquement la limite autorisée de rejet en uranium impliquant une révision des méthodes d'élimination de celui-ci. L'adsorption aqueuse est une méthode efficace et peu couteuse. Les matériaux à mésoporosité ordonnée présentent des propriétés d'adsorption intéressantes à cause de leurs propriétés texturales et leurs possibles fonctionnalisations. Plusieurs familles de matériaux mésoporeux (silices fonctionnalisées ou non, carbones, oxyde de magnésium) ont été synthétisées, caractérisées et utilisées pour adsorber U(VI). Des études en batch et en dynamique ont été réalisées à partir de solutions reconstituées et d'eaux d'exhaure issues du site de Bellezane (87) sur les différents matériaux choisis, et les mécanismes d'adsorption ont été étudiés en fonction de la spéciation aqueuse de l'uranium et de la présence d'ions compétiteurs. Les résultats ont montré que la SBA-15 greffée avec des fonctions aminopropyles, présentait les meilleures capacités d'adsorption à pH 6. Il a été montré que l'U(VI) s'adsorbait par formation de complexe de sphère interne dans la mésoporosité du matériau, et que la présence de complexes entre l'U(VI) et les carbonates dissous diminuait significativement la capacité d'adsorption du matériau en U(VI). / In France, former uranium mines and their draining effluents are kept under environmental monitoring due to the presence of mine tailings which can modify the chemistry of surface waters and increase their uranium concentration. In order to decrease the U(VI) concentration to the one set by the standards, water treatment facilities are used. However, an incoming regulation will drastically decrease the allowed U(VI) concentration in the released water, implying the changing of the current U(VI) removal methods. Aqueous adsorption is known to be an efficient and non expensive method. Ordered mesoporous materials have interesting adsorption properties due to their textural properties and their ability to be functionalized. Different types of mesoporous materials (functionalized or non functionalized silica, carbon, magnesium oxide) were synthesized, characterized, and experimented as U(VI) adsorbents. Studies made in batch and dynamic modes were achieved from reconstituted solutions and mine-water from the Bellezane's site (87), on the different materials, and adsorption mechanisms were studied in function of the aqueous uranium speciation and the presence of competitive ions. Results show that aminopropyl grafted SBA-15 displays the best adsorption capacities at pH 6. It is also shown that U(VI) adsorption proceeds through the formation of inner-sphere complex inside of the mesoporosity of the material, and that the presence of complexes involving U(VI) and dissolved carbonates significantly decrease the adsorption capacity of the material toward U(VI).

Ce travail vise à comprendre et quantifier le comportement de U(VI) dans les argilites du Callovo-Oxfordien(COₓ), prévues pour accueillir les déchets nucléaires de haute activité en France. L’effet de la température sur ce comportement est particulièrement étudié. La première partie du travail s'est concentrée sur les propriétés thermodynamiques des complexes ternaires Ca-U(VI)-CO₃ qui contrôlent la spéciation de U(VI) en solution. Ces dernières ont été mesurées par une méthode de compétition en présence d’une résine sous pCO₂ et pH contrôlés. Les résultats indiquent que la température ne favorise pas la formation de CaUO₂(CO₃)₃²⁻ (log₁₀ βº₁₁₃ = 27,3 ± 0,3 ; ΔrHº = -27,4 ± 8 kJ/mol) et n'affecte pas la formation de Ca₂UO₂(CO₃)₃(aq)(log₁₀ βº₂₁₃ = 29,7 ± 0,3 ; ΔrHº = 0 ± 2 kJ/mol). Une approche « bottom-up » avec le modèle « 2SPNE SC /CE » publié dans la littérature a été suivie pour décrire les phénomènes de sorption, en considérant que la fraction argileuse du COₓ (Illite et I/S) gouverne la sorption de U(VI). Ce modèle a été appliqué avec succès pour reproduire une multitude de données expérimentales obtenues avec l'illite, la fraction argileuse du COₓ et les argilites du COₓ en fonction de paramètres clés (pH, pCO₂, [U(VI)], [Ca]) à 20 °C. Le phénomène de rétention dans les conditions in-situ est principalement régi par la sorption des complexes U(VI)-carbonate et une nouvelle constante d´équilibre de réaction de complexation de surface est proposée pour l'illite. Une augmentation de la température à 80 °C conduit à une augmentation de la rétention de U(VI) sur le COₓ. Cette augmentation est accompagnée d'un changement de pCO₂et de pH. Le modèle de rétention testé à 20 °C combiné avec les paramètres thermodynamiques décrivant le comportement de U(VI) en solution expliquent cette augmentation sans pour autant obtenir un accord satisfaisant avec l’expérience. Le modèle est amélioré en intégrant des valeurs de ΔrHº obtenues pour les réactions de complexation de surface à partir du système U(VI)/illite. / The aim of this study was to understand and quantify the behaviour of U(VI) on the Callovo-Oxfordian(COx) clay which is envisioned to host high-level radioactive waste in France. The temperature effect up to 80°C on this behaviour was particularly studied. The first part of the work focussed on the thermodynamic properties of the calcium uranyl carbonate aqueous complexes which govern U(VI) speciation in solution. They were measured indirectly by sorption-based methodologies under controlled pCO₂ and pH. The results indicate that the temperature does not favour the formation of CaUO₂(CO₃)₃²⁻ (log₁₀ βº₁₁₃ = 27,3 ± 0,3 ; ΔrHº = -27,4 ± 8 kJ/mol) and does not affect the formation of Ca₂UO₂(CO₃)₃(aq)(log₁₀ βº₂₁₃ = 29,7 ± 0,3 ; ΔrHº = 0 ± 2 kJ/mol). A bottom-up approach with the published “2SPNE SC/CE”model was used for describing the sorption processes, with the assumption that the clay fraction of the COx (Illite, andI/S) governs U(VI) sorption.The model was successfully applied to reproduce a wealth of experimental data obtained with illite, the COₓ clay fractionand the COₓ clay rock as a function of key parameters (pH, pCO2, [U(VI)], [Ca]) at 20 °C. The sorption on COₓ conditions is mainly governed by the sorption of U(VI)-CO3 complexes and a new sorption constant is proposed for illite. An increase in temperature to 80 °C leads to an in-crease of U(VI) retention on COx. This increase is ac-companiedby a change of both pCO₂ and pH. The sorption model developed at 20 °C, together with the thermodynamic parameters describing U(VI) speciation in solution, can explain this increase but without obtaining a good agreement with the experiment. The model is improved by considering ΔrHº values for sur-face complexation reactions obtained for the U(VI))/illite system.

Uranium contaminations of the subsurface in the vicinity of nuclear materials processing sites pose a health risk as the uranyl ion in its oxidized state, U(VI), is highly mobile in aquifers. Current remediation strategies such as pump and treat or excavation are invasive and expensive to implement on a large scale. In situ bioremediation represents an alternative strategy that uses the ability of local microbial communities to immobilize contaminants and is actively studied for uranium remediation. The immobilization of U(VI) in groundwater is achieved either by bioreduction to solid uraninite (U(IV)), adsorption to the soil matrix, or non-reductive precipitation of uranium phosphate minerals through the activity of bacterial phosphatases. Bioreduction has been widely studied for remediation of the saturated zone, as anaerobic conditions typically prevail in these environments. This process is only efficient at circumneutral pH, however, and the end product uraninite is unstable under aerobic conditions or in the presence of manganese oxides, nitrite, or even freshly formed iron oxides. Although non-reductive biomineralization of uranium catalyzed by bacterial phosphatase activity successfully removes uranium from the vadose zone, further studies are needed to assess the ability of microbial communities to hydrolyze organophosphate compounds in the saturated zone where oxygen is often depleted and uranium bioreduction may be significant. To investigate this process under anaerobic conditions, low pH soil samples from a uranium contaminated site at the Oak Ridge Field Research Center were incubated anaerobically in flow through reactors in the presence of exogenic organophosphate compounds to stimulate the natural microbial communities in the original soil matrix. Aqueous uranium was injected continuously in the reactors to determine the fraction of uranium removed during these incubations. The reactors amended with organophosphate produced inorganic phosphate in the effluent, suggesting that bacterial phosphatase activity can be stimulated even in anaerobic environments at low pH. Removal of U(VI) in a control amended with organophosphate over a short time period was similar compared to reactors amended with organophosphate for long times suggesting that adsorption may also play a role in U(VI) immobilization. A sequential extraction technique was optimized to differentiate the fraction of uranium loosely adsorbed and the fraction of uranium precipitated as phosphate minerals and batch adsorption experiments were performed to obtain thermodynamic parameters that could be used to predict the fraction of U(VI) adsorbed onto the soil matrix. Results indicated that 100% uranium adsorption was favorable from pH 5 to 10 (without the presence of phosphate), and that most of the solid phase uranium was extracted in the step defined for the strongly adsorbed/uranium phosphate mineral in both long and short-term amended reactors. Overall, these results demonstrate that the biomineralization of uranium phosphate minerals is a viable bioremediation strategy in both the vadose and saturated zones of aquifers at both low and high pH, provided an organophosphate source is available.

Clays are considered as potential host rocks and backfill material for deep geological repositories for radioactive waste. Therefore, profound understanding of radionuclide retention processes at clay mineral surfaces is essential for a long-term safety assessment. This understanding has already been generated in the past for simple chemical systems, in which experiments are easy to conduct and interpretation is straightforward. However, there is still a lack of molecular process understanding when considering complex natural systems (low radionuclide concentrations, high ionic strength, high pH values, multi-mineral solid phases, complex solution composition). This thesis aims to close some of these knowledge gaps, focusing on U(VI) and Np(VI) sorption on clays at (hyper)alkaline conditions. pH values between 10 and 13 can prevail in the near-field of a radioactive waste repository as a result of the degradation of concrete, which is part of the geo-engineered barrier. Existing studies on radionuclide sorption on clays do not exceed pH 10. Therefore, within this work, a comprehensive investigation in the pH range 8-13 was conducted. This included the quantification of radionuclide retention in batch sorption experiments as well as spectroscopic investigations to generate understanding about the underlying retention mechanisms on a molecular level. Beside the pH, additional focus was on the influence of dissolved carbonate and calcium on radionuclide sorption at (hyper)alkaline conditions. Next to two small chapters dealing with the stability and surface charge of Ca-bentonite at (hyper)alkaline conditions (chapter 4.1) and the influence of ISA on U(VI) sorption at high pH values (chapter 4.3), the thesis can be subdivided in two major parts. The first part (chapter 4.2) is a detailed investigation of U(VI) sorption on Ca-bentonite at (hyper)alkaline conditions in mixed electrolyte solutions. Batch sorption experiments were conducted, varying a number of experimental parameters (sorption time, S/L ratio, U(VI) concentration, pH value, carbonate concentration) and assessing their effect on U(VI) sorption. In order to be able to explain the observed sorption behavior, next to U(VI) solubility tests, spectroscopic techniques were applied. The aqueous speciation of U(VI) was investigated with TRLFS, while its surface speciation was probed with ATR FT-IR, site-selective TRLFS, EXAFS and CTR/RAXR. Since the results of this chapter indicated a great importance of the presence of calcium (see below), the second major part of the thesis (chapter 4.4) was dedicated to a careful evaluation of the influence of calcium on An(VI) sorption on clay minerals at (hyper)alkaline conditions. This encompasses the sorption of Ca(II) on Ca-bentonite and its effect on the bentonite surface charge. Furthermore, U(VI) batch sorption experiments with Na-montmorillonite, synthetic kaolinite and muscovite were conducted in 0.1 M NaCl as well as in 0.1 M NaCl + 0.02 M CaCl2 at pH 8-13, in order to quantify the influence of calcium on U(VI) sorption on supposedly Ca-free mineral phases. Site-selective TRLFS was applied with the aim to observe U(VI) sorption species involving calcium. Finally, complementary sorption experiments Np(VI) on muscovite were performed in order to check whether its sorption behavior is analogous to U(VI) under the given conditions. Batch sorption experiments demonstrate that U(VI) retention on Ca-bentonite can be very effective at pH > 10, even in the presence of carbonate and despite the prevalence of anionic aqueous species. Above a certain pH, depending on the concentration of carbonate in solution, carbonate does not play a role in the aqueous U(VI) speciation anymore due to the predominance of hydrolysis. TRLFS measurements revealed a clear correlation between sorption behavior and aqueous U(VI) speciation, showing that retention reaches a maximum at pH 10-12, where UO2(OH)3− is the predominant aqueous species. This raised the question whether the strong retention can be achieved by adsorption of an anionic species to the negatively charged mineral surface or rather by precipitation of uranates. By in situ ATR FT-IR and CTR/RAXR experiments the formation of U(VI) precipitates on the mineral surface was observed at U(VI) concentrations of 2×10-5 M and 5×10-5 M, respectively. However, solubility tests at sub-micromolar U(VI) concentrations, which were also applied in the batch sorption experiments, showed that the observed complete U(VI) removal at pH 10-12 cannot be attributed to precipitation of (earth) alkali-uranates from the solution. In order to unambiguously distinguish between surface precipitation and surface complexation, direct spectroscopic investigations of the U(VI) complexes on the Ca-bentonite surface were performed with site-selective TRLFS and EXAFS. The occurrence of luminescence line-narrowing and the frequency of the total symmetric stretch vibration obtained from the site-selective TRLFS emission spectra, indicate the presence of two U(VI) surface complexes. Also EXAFS spectroscopy confirmed the presence of two independent U(VI) sorption species on Ca-bentonite at pH 8-13. With increasing pH, the nature of the retained U(VI) complexes shifts from bidentate inner-sphere surface complexes with an overall equatorial coordination of five adsorbed on aluminol or silanol edge sites to surface complexes with a 4-fold equatorial coordination, resembling the aqueous species UO2(OH)42−. For the first time, a 4-fold coordination in the equatorial plane of U(VI) was univocally proven with the help of a multiple-scattering feature originating from the strong symmetry of the complexes, and without the need for error-prone shell fitting. The lack of scattering paths from the substrate and the comparatively high value for the total symmetric stretch vibration indicate that the high-pH-component is an outer-sphere complex. Concerning the character of the second sorption species at very high pH it was hypothesized that the anionic uranyl hydroxide complexes are mediated to the surface by calcium cations. It was found that calcium sorbs strongly on Ca-bentonite between pH 8 and 13. Also zeta potential measurements showed a partial compensation of the strongly negative surface charge of Ca-bentonite due to adsorption of calcium. U(VI) sorption on kaolinite and muscovite was strongly reduced in the absence of calcium at pH > 10. An increased retention upon addition of calcium proved the sorption enhancing effect of calcium at pH 10-12. Site-selective TRLFS allowed the spectroscopic observation and identification of calcium-induced U(VI) sorption complexes on muscovite. The obtained spectra correspond to the outer-sphere species found on Ca-bentonite. Combining the findings from batch sorption, zeta potential, TRLFS and EXAFS suggests that calcium adsorbs to the mineral surface in the first place, displaying locally positively charged sites which enable an electrostatically driven attachment of anionic uranyl hydroxides. The same effect could also be demonstrated for Np(VI) sorption on muscovite, which was also strongly enhanced in the presence of calcium at pH 9-12. ISA leads to a mobilization of U(VI) at (hyper)alkaline conditions only when present in very high excess of U(VI). A reduction of sorption on Ca-bentonite and the formation of aqueous U(VI)-ISA complexes, detected with TRLFS, occurred at an U:ISA ratio of 1:100,000. Such conditions are not likely to be found in deep geological repository environments. Based on these findings it can be concluded that under certain alkaline repository conditions, where precipitation does not occur (due to very low concentrations or kinetic restraints), U(VI) and Np(VI) are still effectively retained in argillaceous minerals and rocks by adsorption despite the anionic character of prevailing aqueous species. Repulsive forces between the actinide species and the mineral surfaces are overcome by mediating Ca2+. This finding is of great relevance, as also the migration of very small amounts of uranium or neptunium out of waste repositories could lead to a hazardous accumulation in the long term. The achieved knowledge gain concerning radionuclide retention at environmental conditions helps to take the next step towards realistic long-term safety assessment of nuclear waste repositories.

Teil A: Es wurde gezeigt, dass das Transportverhalten von Uran in der Umwelt und an den ehemaligen Uranabbaustätten stark von der Anwesenheit und Aktivität natürlich vorkommender Mikroorganismen abhängt. Die Untersuchungen zeigten, dass die Isolate eine hohe Toleranz gegenüber Uran aufweisen und in der Lage sind, relativ hohe Mengen an Uran zu immobilisieren und aus der umgebenden Lösung zu entfernen. Durch anaerobe Versuche konnte gezeigt werden, dass die mikrobielle Reduktion von Uran(VI) allein durch die Zugabe von 10 mM Glycerin bei zukünftigen Anwendungen als in situ Biosanierungsapplikationen genutzt werden könnte. Die Ergebnisse dieser Arbeit konnten die Wechselwirkungsmechanismen zwischen natürlich vorkommenden Mikroorganismen und Uran im Detail beschreiben und neue Zusammenhänge zwischen aktivem und inaktivem Stoffwechsel der Mikroorganismen zeigen. Zusammenfassend können diese einen wertvollen Beitrag zur Entwicklung von Biosanierungsansätzen für die Behandlung von Radionuklid-kontaminierten Standorten aus der ehemaligen Bergbauindustrie leisten. Teil B: Im Speichel dominiert neben einem kleinen Bindungsanteil an dem Enzym alpha-Amylase die Komplexierung mit anorganischen Liganden, im Magen dominiert aufgrund des sauren pH-Wertes das Eu- bzw. Cm-Aquo-Ion, und im Darm dominiert neben anorganischen Komplexen die Bindung der Metallionen an das Glycoprotein Mucin. Die starke Komplexfähigkeit von Mucin gegenüber dreiwertigen f-Elementen könnte die Absorption dieser im menschlichen Körper unterdrücken und deren Exkretion fördern. Die Ergebnisse dieser Arbeit geben neue Einblicke in das biochemische Verhalten dreiwertiger f-Elemente und können zudem zur Einschätzung von Gesundheitsrisiken nach der Inkorporation von Radionukliden und der Entwicklung von Dekontaminationstherapien beitragen.

Characterising the geochemistry and speciation of major contaminant radionuclides is crucial in order to understand their behaviour and migration in complex environmental systems. Organic complexing agents used in nuclear decontamination have been found to enhance migration of radionuclides at contaminated sites; however, the mechanisms of the interactions in complex environments are poorly understood. In this work, radionuclide speciation and sorption behaviour were investigated in order to identify interactions between four key radionuclides with different oxidation states (Cs(I) and Sr(II) as important fission products; Th(IV) and U(VI) as representative actinides), three anthropogenic organic complexing agents with different denticities (EDTA, NTA and picolinic acid as common co-contaminants), and natural sand (as simple environmental solid phase). A UV spectrophotometric and an IC method were developed to monitor the behaviour of EDTA, NTA and picolinic acid in the later experiments. The optimised methods were simple, applied widely-available instrumentation and achieved the necessary analytical figures of merit to allow a compound specific determination over variable background levels of DOC and in the presence of natural cations, anions and radionuclides. The effect of the ligands on the solubility of the radionuclides was studied using a natural sand matrix and pure silica for comparison of anions, cations and organic carbon. In the silica system, the presence of EDTA, NTA and, to a lesser extent, picolinic acid, showed a clear net effect of increasing Th and U solubility. Conversely, in the sand system, the sorption of Th and U was kinetically controlled and radionuclide complexation by the ligands enhanced the rate of sorption, by a mechanism identified as metal exchange with matrix metals. Experiments in which excess EDTA, NTA and picolinic acid (40 – 100 fold excess) were pre-equilibrated with Th and U prior to contact with the sand, to allow a greater degree of radionuclide complex formation, resulted in enhanced rates of sorption. This confirmed that the radionuclide complexes interacted with the sand surface more readily than uncomplexed Th or U. Overall this shows that Th and U mobility would be lowered in this natural sand by the presence of organic co-contaminants. In contrast, the complexation of Sr with the complexing agents was rapid and the effect of the ligands was observed as a net increase on Sr solubility (EDTA, picolinic acid) or sorption (NTA). As expected, Cs did not interact with the ligands, and showed rapid sorption kinetics. Finally, ESI-MS was used to study competitive interactions in the aqueous Th-Mn-ligand ternary system. Quantification presented a challenge, however, the careful approach taken to determine the signal correction allowed the competitive interactions between Mn and Th for EDTA to be studied semi-quantitatively. In an EDTA limited system, Th displaced Mn from the EDTA complex, even in the presence of a higher Mn concentration, which was consistent with the higher stability constant of the Th-EDTA complex.

Les gisements d’U de type discordance sont associés à des circulations de saumures chlorurées acides et caractérisés par des tonnages et concentrations exceptionnels ce qui amènent à s’interroger sur les processus de transport et de dépôt de l’U contribuant à leur genèse. Cette thèse est donc dédiée à des études expérimentales de la spéciation de l’U6+ et sa précipitation en UO2 par réduction en U4+ en condition hydrothermale. Concernant le transport de l’U, l’étude de la spéciation de l’U6+ dans ces fluides chlorurés (T ≤ 350°C) est réalisée par spectroscopie Raman et XAS. Les résultats montrant la coexistence de plusieurs complexes d’uranyle chlorurés UO2Cln2-n (n=0-5) dont certaines constantes de complexation sont proposées. Ainsi, la complexation de l’uranyle par les chlorures explique la forte capacité de transport en U6+ par les saumures chlorurées acides, condition nécessaire à la formation de gisements de fort tonnage. Pour le dépôt de l’U, les cinétiques de réduction de l’U6+ en U4+ par H2, CH4, Fe2+ et C-graphite sont mesurées et paramétrées en fonction de la température, de la chlorinité, du pH et de la concentration en réducteur. H2, CH4 et le C-graphite sont être très efficaces, contrairement au Fe2+. Le caractère mobile des gaz réducteurs explique en partie les minéralisations massives et focalisées observées dans ces gisements. Enfin des coefficients de partage UO2/fluide d’éléments en traces, dont certaines ETR, sont mesurés, ouvrant de nouvelles perspectives quant à (i) la compréhension de la signature des ETR caractéristiques de chaque type de gisement d’U, et (ii) la composition des fluides à l’origine des minéralisations uranifères / Circulations of acidic chloride brines are associated with unconformity-related uranium (URU) deposits. The spectacular high grade combined with the large tonnage of these deposits is at the origin of the key questions concerning the geological processes responsible for U transport and precipitation. The aim of this work is to performed experimental studies of U6+ speciation and its reduction to U4+ subsequently precipitation to UO2 under hydrothermal condition. About U transport, the study of U6+ speciation in acidic brines at high temperature is performed by Raman spectroscopy and XAS, showing the coexistence of several uranyl chloride complexes UO2Cln2-n (n=0-5). From this study, complexation constants are proposed. The strong capability of chloride to complex uranyl is at the origin of the transport of U6+ at high concentration in acidic chloride brines. Concerning U precipitation, the reactivity of four potential reductants under conditions relevant for URU deposits genesis is investigated: H2, CH4, Fe2+ and the C-graphite. The kinetics of reduction reaction is measured as a function of temperature, salinity, pH and concentration of reductant. H2, CH4, and the C-graphite are very efficient while Fe2+ is not able to reduce U6+ in same conditions. These mobile and efficient gaseous reductant could be at the origin of the extremely focus and massive character of ore in URU deposits. Finally, first partition coefficients UO2/fluid of trace elements are obtained. This last part opens-up new perspectives on (i) REE signatures interpretation for a given type of U deposit (ii) and reconstruction of mineralizing fluids composition