34
M.
Ś
LESICKI
•
Selection of mathematical model. To accomplish the aims formulated in prepara-
tory stage one may select one of the existing models or prepare the author’s pro-
gramme. Selected model should undergo preliminary verification consisting in
comparison of numerical solution generated by the model with analytical solu-
tions or with other numerical solutions.
•
Construction of a model. In this stage the scope of modelling
is being estimated
through: division of modelled area into elements of calculation grid, selection of
calculation time steps, establishment of borders, initial and edge conditions and
preliminary selection of parameter values.
•
Model calibration. Calibration is aimed at estimating to what degree results of
calculations based on selected model agree with field measurements.
Calibration
is usually made with the method of consecutive approximations for various sets
of parameters.
•
Analysis of model sensitivity. Calibrated model bears a burden of error due to
indeterminacy and of errors in the reproduction of spatial and temporal parame-
ter distribution in studied area and inaccuracy of edge conditions. Analysis of
model sensitivity is carried out to establish the effect of these errors on solution
with the use of special methods and algorithms.
•
Model verification. The model is verified to increase its reliability through cal-
culations for some sets of parameter
values in order to choose one, optimum set
characterising the modelled medium.
•
Prognosis. It gives answer to system behaviour in predicted conditions and con-
sists in making calculations for given values of time limits.
•
Presentation of simulation results. Models of ground waters usually generate
many data whose interpretation may be difficult. Clear presentation, preferably
in a graphical form, is important for illustrating and understanding the effects of
modelling.
•
Another analysis after some time. Re-analysing carried
out some time after the
study has been accomplished is recommended only when there is a possibility
and need of verification of adopted prognostic assumptions. In this case new
field data are collected to check the correctness of the prognosis. Performed
analysis enables to find new system behaviours which may lead to improvement
of the concept or to changes in model parameters.
Results of calculations and prognosis obtained with model studies are usually
used as a basis for designing decisions or to formulate the strategy of protective
actions. Presented algorithm of creation and initiation
of the model guarantees,
with sufficient probability, that obtained results are possibly the best reflection of
behaviours of studied area.
Complex character of problems associated with groundwater flow and numer-
ous physical and chemical processes involved make the creation of a universal
model that would describe all phenomena and simulate their temporal variability