- Department:(Dept. 1) Ecohydrology and Biogeochemistry
Activation of persulfate by biochar and iron: role of biochar pyrolysis conditions and ash amendments
Summer temperatures, autumn winds, and thermal structure under the ice in arctic lakes of varying morphometry
Storage Dynamics and Groundwater–Surface Water Interactions in a Drought Sensitive Lowland Catchment: Process-Based Modelling as a Learning Tool
One-Hundred Fundamental, Open Questions to Integrate Methodological Approaches in Lake Ice Research
Microbial communities and fatty acid markers across acidification and eutrophication extremes in a river influenced by mining activities
Length Scales, Rates, and Variability of Mixing Downstream of River Confluences
The Unexploited Treasures of Hydrological Observations Beyond Streamflow for Catchment Modeling
Other hydrological data than streamflow have the potential to improve process consistency in hydrological modeling and consequently for predictions under change. The authors review how storage and flux variables are used for model evaluation and calibration; improving process representation.
Biogenic polyphosphate as relevant regulator of seasonal phosphate storage in surface sediments of stratified eutrophic lakes
Using nuclear magnetic resonance spectroscopy, the authors studied the polyphosphate seasonality in the topmost sediment layer of three stratified lakes with prolonged anoxic periods during summer stratification. Polyphosphate acted as a temporary phosphorus storage, formed at the beginning of the summer stratification under oxic conditions and released time delayed under anoxic conditions.
Environmental effects of the Kakhovka Dam destruction by warfare in Ukraine
Recent Developments and Emerging Challenges in Tracer-Aided Modeling
The authors reviewed recent advances and remaining challenges of tracer-aided modelling which offers insights into internal storages, water sources, flow pathways, mixing processes, and water ages, which cannot be derived from hydrometric data alone. Tracer data have the capability to falsify hydrological models and test hypotheses, and thus increase understanding of hydrological processes.