Actinide thermodynamics department
Research
The department of “Thermodynamics of Actinides” is hosting a significant part of the analytical backbone of the institutes, e.g. mass spectrometry, atomic emission spectrometry, elemental analyses, powder diffraction, vibrational and nuclear magnetic resonance spectroscopy. This allows us to work on several steps in the thermodynamics value chain.
From a chemical point of view, the focus is set on heavy metal contaminants, namely long-lived radionuclides. The derivation of parameters describing hydrolysis, aqueous complexation, surface reactions or solubilities are combined with structural investigations to validate the species set forming reactions, enabling mechanistic models. Such parameters are fed into respective databases after verification. Gaps still remaining can be closed by applying different estimation methods, from mineral analogies to Linear Free Energy Relationships.
Combined with field data (mineralogical composition, porosity, pH, redox potential, ionic strength, temperature, or CO2 partial pressure), geochemical speciation patterns and radionuclide retardation can then be computed for complex systems on different scales. To name just a few, we worked on cementitious barriers with organic additives, with real-world crystalline samples or with Chornobyl soils. There, also, geostatistics helps to map the heterogeneities observed, and sensitivity / uncertainty analysis not only increases confidence in computational results but supports also the identification of critical parameters and submodels.
Quite recently, these approaches were complemented by machine learning methods, this will eventually lead to digital twins for nuclear waste repositories. Eventually, this shall bridge the distance between atomistic investigations and the large-scale prognostics required e.g. in performance assessment covering distances of several km over up to one million years.
The actual major research topics of our department can be summarized as follows:
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Spectroscopic characterization of heavy metal species in aqueous solutions and at mineral surfaces.
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(Radio)chemical analyses of contaminant elements as well as matrix compounds down to the ultratracer level.
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Set-up of thermodynamic data bases for prospective deep nuclear waste repositories.
Latest publication
Reactive transport modelling of neptunium migration in Opalinus Clay
Hennig, T.; Stockmann, M.; Joseph, C.; Brendler, V.; Reich, T.; Sayahi, M.; Kühn, M.
Abstract
One-dimensional simulations of Np diffusion through Opalinus Clay (OPA) were conducted. The experimental data were based on two laboratory diffusion experiments. Both experiments used the same setup for two different drill core samples and exhibited differences in the measured Np concentration profiles. Previous studies showed that the Fe(II)-bearing mineral phases in the OPA lead to a partial reduction of the initially used Np(V) to Np(IV). Diffusion and sorption were the governing processes. For the simulation of diffusive transport, both experimentally determined effective diffusion coefficients (single-component) and a species-specific multi-component (MC) diffusion approach were used. Sorption processes were integrated in the reactive transport simulations using surface complexation models for Np(V) and Np(IV) on illite and montmorillonite. Three scenarios were simulated that increased in terms of their geochemical process complexity. Scenario 1 only considered surface complexation of Np(V) on various illite quantities. Redox reactions via pyrite dissolution and oxidation together with surface complexation of Np(IV) and Np(V) on illite and montmorillonite were added to the system in scenario 2. In scenario 3, redox reactions were simulated via Fe associated with the clay minerals. Clay mineral quantity had only a minor effect on the Np distribution in the cores. Instead, the Np(IV)/Np(V) ratio was essential for the migration lengths. The ratio was controlled by the inherent redox potential of the core sample. Consequently, the difference between the experiments could not be attributed to variations in the clay mineral composition of the used core samples, but rather to differences in the initially inherent redox conditions and accessibility of Fe. The simulation results showed that measurements of core mineralogy, composition of boundary solutions as well as determination of Np oxidation states along the concentration profile are essential to capture the entire geochemical picture of future laboratory investigations of redox-active radionuclides.
Keywords: Multi-component diffusion; Sorption; Redox potential; Iron; Illite; Montmorillonite; Pyrite; Np(IV); Np(V)
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Applied Clay Science 289(2026), 108253
DOI: 10.1016/j.clay.2026.108253
Permalink: https://www.hzdr.de/publications/Publ-43357
Team
Head | |||||
| Name | Bld./Office | +49 351 260 | |||
|---|---|---|---|---|---|
| Prof. Dr. Vinzenz Brendler | 801/P250 | 2430 | v.brendler@hzdr.de | ||
Employees | |||||
| Name | Bld./Office | +49 351 260 | |||
| Dr. Frank Bok | 801/P202 | 3551 | f.bok@hzdr.de | ||
| Rodrigo Castro Biondo | r.castro-biondo | ||||
| Alexandra Duckstein | 801/P153 | 2774 | a.duckstein | ||
| Dr. Stephan Hilpmann | 801/P318 | 2759 | s.hilpmann | ||
| Dr. Jerome Kretzschmar | 801/P207 | 3136 | j.kretzschmar | ||
| Dr. Elmar Plischke | e.plischke | ||||
| Dr. Solveig Pospiech | 801/P205 | 2128 | s.pospiech | ||
| Dr. Anke Richter | 801/P202 | 2426 | anke.richter | ||
| Raj Sarkar | 801/P103 | 2720 | r.sarkar | ||
| Dr. Katja Schmeide | 801/P208 | 2436 2513 | k.schmeide | ||
| Salim Shams Aldin Azzam | 801/P103 | 2720 | s.shams | ||
| Susanne Zechel | 801/P352 | 3328 | s.zechel | ||
Other employees | |||||
| Name | Bld./Office | +49 351 260 | |||
| Liya Tomy | F100/431 | 4438 | l.tomy | ||
Analytics
Head | |||||
| Name | Bld./Office | +49 351 260 | |||
|---|---|---|---|---|---|
| Dr. Harald Foerstendorf | 801/P251 | 3664 2504 | h.foerstendorf | ||
Employees | |||||
| Name | Bld./Office | +49 351 260 | |||
| Sabrina Beutner | 801/P203 | 2429 2528 | s.beutner | ||
| Tim Gitzel | 801/P316 | 2025 2517 | t.gitzel | ||
| Dominik Goldbach | 801/P203 | 3198 | d.goldbach | ||
| Karsten Heim | 801/P201 | 2434 2504 | k.heim | ||
| Sylvia Schöne | 850/102.1 | 2526 3198 | s.schoene@hzdr.de, s.guertler | ||

