@article{10272/8672,
year = {2005},
url = {http://hdl.handle.net/10272/8672},
abstract = {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},
publisher = {Sociedad Geológica de España},
title = {Magnitud y rango de transmisividades en las unidades acuíferas carbonatadas UH7 y UH2 del Sistema Mancha Oriental (SMO). SE Español},
title = {Magnitude and range of transmissivities in the aquifer units UH7 y UH2 of the Mancha Oriental System (MOS), SE
Spain},
author = {Sanz Mangas, David and Castaño Fernández, Santiago and Gómez Alday, Juan José and Martínez Alfaro, P.E.},
}