a Map showing geographic location of the investigated area and b groundwater flow and the location of sampled wells in the Quaternary phreatic and Miopliocene aquifers
The main direction of flow is from south to north.
The average flow gradient is estimated to be 1.2%.
Viewing this image requires a subscription. If you are a subscriber, please log in.
This image is from the article titled "Hydrochemical and isotopic behaviour of a Saharan phreatic aquifer suffering severe natural and anthropic constraints (case of Oued-Souf region, Algeria)"
(from Hydrogeology Journal), which is copyrighted by Springer-Verlag. For more information on the
copyright for this image, please refer to the full image caption and to the
The image is being made available for non-commercial purposes for subscribers to SpringerImages. For more information on what you are allowed to do with this image, please see our copyright policy.
To request permissions to use any copyrighted material, please visit the source document.
Report a copyright concern regarding this image.
Log in or register to save your favorite images and download them as high-quality PowerPoint or PDF files.
Log in or register to save your search criteria.
© Springer, part of Springer Science+Business Media.
Remote Address: 22.214.171.124 Server: 19