One example as pointed out by @maximilian-gelbrecht is the soil_characteristic_fractions method here.
Other examples might include the temperature-energy closure methods (energy_to_temperature and temperature_to_energy), diffusive_heat_flux, and the soil stratigraphy and hydraulics methods which should ideally have a formal interface defined.
One example as pointed out by @maximilian-gelbrecht is the
soil_characteristic_fractionsmethod here.Other examples might include the temperature-energy closure methods (
energy_to_temperatureandtemperature_to_energy),diffusive_heat_flux, and the soil stratigraphy and hydraulics methods which should ideally have a formal interface defined.