This research discuss the method followed to specify water transmissivity;
using the water balance data related to the natural model of aquifer; in order
to pinpoint this transmissivity values on vast areas and; therefore; drawing of
the regional
water transmissivity
This method is based on the steady relation between water transmissivity
and the amount of natural charging is case of constant motion that is reflected
on the piezometeric surface of the artesian water and the depth of water level
with regard to free aquatic.
Undoubtfuly, pinpointing transmissivity values and then drawing charts of
regional water transmissivity depending on this method have a great
significance practically, especially when complicated hydrogeological
conditions are modeled. All the places of hidden tectonic dislocations can be
clarified and scrutinized, bicides, there is then an ability to specify all charging
and discharging areas, and explain the transformation of rock characters.
Over, and above, all the results attained correspond with the geological,
structural, and lythological characteristics of studied area.
