A safe storage of radioactive waste in repositories is an important task to protect humans and the environment from radio- and chemotoxicity. Long-term safety assessments predict the behavior of potential environmental contaminants like the actinides plutonium, uranium, or neptunium, in the near and far field of repositories. For such safety assessments, it is necessary to know the migration behavior of the contaminants in the environment, which is mainly dependent on the aquatic speciation, the solubility product of relevant solid phases, and the retardation due to sorption on surrounding minerals. Thus, an investigation of sorption processes of contaminants onto different minerals as well as the derivation of mineral specific surface complexation model (SCM) parameters is of great importance. Feldspar and mica are widely distributed in nature. They occur as components of granite, which is considered as a potential host rock for a repository in Germany, and in numerous other rocks, and thus also in the far field of nearly all repositories. However, their sorption behavior with actinides has only been scarcely investigated until now. In order to better characterize these systems and subsequently to integrate these minerals into the long-term safety assessments, this work focuses on the investigation of the sorption behavior of U(VI), Np(V), and Nd(III) as analogue for An(III) onto the minerals orthoclase and muscovite, representing feldspars and mica, respectively. All investigations were performed under conditions relevant to the far field of a repository. In addition to the extensive characterization of the minerals, batch sorption experiments, spectroscopic investigations, and surface complexation modeling were performed to elucidate the uptake and speciation of actinides on the mineral surfaces. In addition, the influence of microorganisms naturally occurring on the mineral surfaces and the effect of Ca2+ on U(VI) uptake on the minerals was studied. The obtained sorption curves exhibit a similar characteristic for orthoclase and muscovite. As expected Nd(III) shows the highest amount of sorption followed by U(VI) and finally Np(V). With spectroscopic investigations of the aquatic U(VI) solution in presence of Ca2+, the Ca2UO2(CO3)3 complex could be identified. Furthermore, with spectroscopic methods the U(VI) surface species onto orthoclase could be characterized, of which a novel uranium-carbonate surface species was observed. Based on the results of batch experiments and spectroscopic methods new SCM parameters for the sorption of U(VI), Np(V), and Nd(III) onto orthoclase and for Np(V) and Nd(III) onto muscovite could be derived. SCM parameters for U(VI) sorption onto muscovite confirmed earlier investigations. The obtained SCM parameters increase the amount of data available for sorption processes onto feldspar and mica. With this the relevance of feldspars for the sorption of actinides and lanthanides could be shown. Thus, this work contributes to a better understanding of interactions of actinides and lanthanides, in particular U(VI), Np(V), and Nd(III), with mineral phases ubiquitous in the environment. This in turn adds confidence to long-term safety assessments essential for the protection of humans and the environment from the hazards of radioactive waste.

Clay formations are investigated worldwide as potential host rock for the deep geological disposal of high-level radioactive waste (HLW). Usually bentonite is preferred as the buffer and backfill material in the disposal system. In the disposal of HLW, heat emission is one of the most important issues as it can generate a series of complex thermo-hydro-mechanical (THM) processes in the surrounding materials and thus change the material properties. In the context of safety assessment, it is important to understand the thermally induced THM interactions and the associated change in material properties. In this work, the thermally induced coupled THM behaviours in the clay host rock and in the bentonite buffer as well as the corresponding coupling effects among the relevant material properties are numerically analysed. A coupled non-isothermal Richards flow mechanical model and a non-isothermal multiphase flow model were developed based on the scientific computer codes OpenGeoSys (OGS). Heat transfer in the porous media is governed by thermal conduction and advective flow of the pore fluids. Within the hydraulic processes, evaporation, vapour diffusion, and the unsaturated flow field are considered. Darcy’s law is used to describe the advective flux of gas and liquid phases. The relative permeability of each phase is considered. The elastic deformation process is modelled by the generalized Hooke’s law complemented with additional strain caused by swelling/shrinkage behaviour and by temperature change. In this study, special attention has been paid to the analysis of the thermally induced changes in material properties. The strong mechanical and hydraulic anisotropic properties of clay rock are described by a transversely isotropic mechanical model and by a transversely isotropic permeability tensor, respectively. The thermal anisotropy is described by adoption of the bedding-orientation-dependent thermal conductivity. The dependency of the thermal conductivity on the degree of water saturation, the dependency of the thermal effects on the water retention behaviour, and the dependency of the effects of the pore pressure variation on the permeability and the anisotropic swelling/shrinkage behaviour have been intensively analysed and the corresponding numerical models to consider those coupling effects have been developed. The developed numerical model has been applied to simulate the laboratory and in situ heating experiments on the bentonite and clay rock at different scales. Firstly the laboratory heating experiment on Callovo-Oxfordian Clay (COX) and the laboratory long-term heating and hydration experiment on MX80 pellets were simulated. Based on the knowledge from the numerical analysis of the laboratory experiments, a 1:2 scale in situ heating experiment of an integrated system of the bentonite engineered barrier system (EBS) in the Opalinus Clay host rock was simulated. All the relevant operation phases were considered in the modelling. Besides, the modelling was extended to 50 years after the heat shut-down with the aim of predicting the long-term behaviours. Additionally, variation calculations were carried out to investigate the effects of the storage capacity of the Opalinus Clay on the thermally induced hydraulic response. In the long-term modelling, the effects of different saturated water permeabilities of buffer material on the resaturation process were analysed. Based on the current researches and model developments, the observed THM behaviours of the bentonite buffer and the clay rock, that is, the measured evolution of temperature, pore pressure, humidity, swelling pressure, and so on in the laboratory and in situ experiments can be reproduced and interpreted well. It is proved that by using both a non-isothermal multiphase flow model and a non-isothermal Richards flow model combined with the corresponding thermal and mechanical models, the major THM behaviours can be captured. It is validated that the developed model is able to simulate the relevant coupled THM behaviours of clayey material under the well-defined laboratory conditions as well as under the complex natural disposal conditions.

Uran kann sowohl durch geogene als auch anthropogene Vorgänge in die Umwelt gelangen. Dazu zählen natürliche Uranerzvorkommen und deren Leaching sowie die Auswaschung von Uran aus den Hinterlassenschaften des ehemaligen Uranerzbergbaus. Die Aufklärung des Verhaltens von Uran in der Geo- und Biosphäre ist für eine Risikoabschätzung des Migrationsverhaltens von Radionukliden in der Umwelt notwendig. Algen sind in der Natur weit verbreitet und die wichtigste Organismengruppe in den aquatischen Lebensräumen. Durch ihre ubiquitäre Verbreitung in der Natur ist ihr Einfluss auf das Migrationsverhalten von Uran in der Umwelt von grundlegendem Interesse z.B. um effektive und wirtschaftliche Remediationsstrategien für Wässer zu entwickeln. Außerdem stehen Algen am Beginn der Nahrungskette und spielen eine wirtschaftlich relevante Rolle als Nahrung beziehungsweise Nahrungsergänzungsmittel. Die Möglichkeit des Transfers von algengebundenem Uran entlang der Nahrungskette könnte eine ernsthafte Gesundheitsgefahr für den Menschen darstellen. Das Ziel dieser Arbeit war die quantitative und strukturelle Charakterisierung der Wechselwirkung zwischen Uran(VI) und der Grünalge Chlorella vulgaris im umweltrelevanten Konzentrations- und pH-Wertbereich unter besonderer Berücksichtigung der Stoffwechselaktivität. Die in dieser Arbeit erzielten Ergebnisse der Sorptionsexperimente zeigen deutlich den maßgeblichen Einfluss des Stoffwechselstatus von Chlorella auf die Wechselwirkung mit Uran. So kann in Gegenwart von umweltrelevanten Urankonzentrationen eine Remobilisierung von zuvor passiv gebundenem Uran durch die stoffwechselaktiven Algen erfolgen. Die in Abhängigkeit von der Stoffwechselaktivität, der Urankonzentration und dem pH-Wert mit den Algenzellen gebildeten Uran(VI)-Komplexe wurden strukturell mit Hilfe der spektroskopischen Methoden TRLF-, EXAFS- und ATR-FTIR-Spektroskopie charakterisiert. Mittels TEM konnte Uran in Form von 30-70 nm großen nadelförmigen Ablagerungen in der Zellwand der lebende Algenzellen nachgewiesen werden. Die in dieser Arbeit erhaltenen Ergebnisse leisten einen wichtigen Beitrag zur Vorhersage des Migrationsverhaltens von Uran unter umweltrelevanten Bedingungen und der radiologischen Risikobewertung von geogen und anthropogen auftretendem Uran. / Uranium could be released into the environment from geogenic deposits and from former mining and milling areas by weathering and anthropogenic activities. The elucidation of uranium behavior in geo- and biosphere is necessary for a reliable risk assessment of radionuclide migration in the environment. Algae are widespread in nature and the most important group of organisms in the aquatic habitat. Because of their ubiquitous occurrence in nature the influence of algae on the migration process of uranium in the environment is of fundamental interest e.g. for the development of effective and economical remediation strategies for contaminated waters. Besides, algae are standing at the beginning of the food chain and play an economically relevant role as food and food additive. Therefore the transfer of algae-bound uranium along the food chain could arise to a serious threat to human health. Aim of this work was the quantitative and structural characterization of the interaction between U(VI) and the green alga Chlorella vulgaris in environmental relevant concentration and pH range with special emphasis on metabolic activity. The obtained findings of the sorption experiments in this study demonstrate clearly, the interactions with uranium are heavily influenced by the status of the investigated Chlorella cells. So in presence of environmentally relevant uranium concentrations a remobilization of algal-bound uranium by metabolically active algae occurred. The U(VI)-algae-complexes formed in dependence of cell activity, uranium concentration and pH value were structural characterized by TRLF, EXAFS and ATR-FTIR spectroscopy. With the help of TEM under the given experimental conditions uranium was detected in form of 30-70 nm needle-like deposites in the cell wall of living algae. The obtained results of this study contribute to the prediction of the migration behavior of uranium under environmental conditions, the radiological risk assessment of geogenic and anthropogenic appearing uranium and a reliable estimation of the accumulation of uranium in the food chain.