The ThermoGIS methodology `calculate_doublet_performance_stochastic` assumes that we know the net-to-gross, porosity and depth of the aquifer perfectly and simulates a range of values only over permeability, thickness (and thus; transmissivity).
This is because transmissivity is usually the most important aquifer property when determining performance and for the ThermoGIS project we make country-wide maps with simulations of 1km x 1km for the Netherlands; this means choices have to be made when selecting what properties to sample over.
However, if conducting a local study you may well want to also incorporate statistical sampling across other reservoir properties, it is relatively easy (and insightful) to use pythermogis to generate samples and make your own stochastic framework.