From a beaker to a province

Via automatic adaptation of the internal coordinate system to the particular model dimensions SPRING always calculates with high precision, independent of scale and without intervention.


Microscale:
Simulation of the Saltpool Experiment [OSWALD 1999]
  • Transient, density dependent 3D flow and transport model
  • Model area 0,25 cm²
  • 71 vertical layers, partly converging
  • Ca. 155.000 nodes


Large scale:
Groundwater model Saarland
  • Territory of Saarland:
    		•  2.571 km²
  • Model area:
    		•  2.816 km²
  • Length of model boundary:
    		•  257 km
  • Length of watercourse systems:
    		•  4.062 km
  • About 1.000.000 nodes
    		•