Magnitud y rango de transmisividades en las unidades acuíferas carbonatadas UH7 y UH2 del Sistema Mancha Oriental (SMO) SE Español

• Autores: David Sanz Martínez
• Localización: Geogaceta, ISSN 0213-683X, Nº. 39, 2005, págs. 119-122
• Idioma: español
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• Resumen

  • 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 log-q, 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.