Mixing und compartment models dienen zur Rekonstruktion von Wasserflüssen aus chemischen und Isotopendaten. MCM ist ein inverses Multi-End-Member Kompartmentmodell zur Systemanalyse.

The geohydrological model provides a basin-oriented approach to the recharge of alluvial aquifers and to their management. It fills a gap between hydrological modeling of surface hydrology, runoff production, concentration and groundwater flow and management. The alluvial aquifer is subdivided into compartments and the contributing sub-basins for each compartment are identified. The model describes and calculates indirect recharge, groundwater flow processes into, within, through and from the alluvial aquifer and handles water abstractions.

A library of hydrological methods and processes implemented in R and Python encompassing quantitative and qualitative hydrology (water quality).

A library of isotope and tracer methods programmed in R and Python.