الصفات الهيدروليكية لمكمن الجريبي الجيري شمال الموصل

الملخص EN

he Jeribe Limestone Formation represents the main confined aquifer withing the area of north Mosul.

The formation characterized by high voids, fractares which is affected by karstification.

The hydrauiic properties of aquifer (Jeribe), transmissivity, hydraulic conductivity and storage coefficient were found by using different methods of analysis of draw down in observation wells.

The results showed that the main aquifer (Jeribe) is of high transmissivity and it contains a large volume ofwatcr.