The hydrogeologic units UH7 (mid-Jurassic) and UH2 (mid-Miocene) mainly support the whole of the
groundwater abstractions in the Mancha Oriental System (SMO). In both units, the empirical relationship
among transmissivity and specific yield data has been determined on a prediction interval equal to 90%.
Once the values of transmissivity have been estimated from the linear relatonship between log-T and logq,
it has been determined the most representative interval of transmissivity values. In this sense, the
highest transmissivity values belong to the UH7 and are found in the SE block of the «Multiple Fracturation
Line (MFL)». On the other hand, the lowest ones are found in the carbonte deposits of the UH2