Zobrazeno 1 - 6
of 6
pro vyhledávání: '"Taoufiq Kouz"'
Publikováno v:
Revue des Sciences de l’Eau. 32:317-334
L'urbanisation rapide et les rejets des eaux usées correspondants, ainsi que l’utilisation de plus en plus intensive d'engrais chimiques, constituent un risque potentiel pour la pollution des eaux souterraines. La cartographie de la vulnérabilit
Publikováno v:
La Houille Blanche. 106:63-73
Many methods for assessing the vulnerability of groundwater against anthropogenic pollution have been developed in the past decades. However, if aquifer vulnerability concept is well defined and th...
Autor:
Issam Etebaai, Zerrouk Mohammed Hassani, Soukaina Mansour, Taoufiq Kouz, Taoufik Mourabit, Hinde Cherkaoui Dekkaki
Publikováno v:
La Houille Blanche. 105:16-25
In the North East of the Moroccan Mediterranean coast, 15 km south east of the Al Hoceima city, the coastal aquifer of Ghiss-Nekkour occupies an area of 100 km2 . Its exploitation constitutes a priority economic imperative for the city of Al Hoceima
Autor:
Taoufiq Kouz, Hinde Cherkaoui Dekkaki, Soukaina Mansour, Mohammed Hassani Zerrouk, Mohammed Thaiki, Taoufik Mourabit, Abdellah Ouhadi, Hakim Mesmoudi, Houria Dakak
Publikováno v:
Arabian Journal of Geosciences. 14
Assessing the degree of vulnerability of surface water intended for drinking water supply has become a major necessity in water resource management and decision-making; it allows to identify high-risk areas and provide all the necessary measures for
Publikováno v:
E3S Web of Conferences, Vol 298, p 05005 (2021)
The salinization of surface water in a coastal context leads to a qualitative degradation of this resource by various sources of anthropogenic and natural pollution. In this context, we present the results of a comparative study using "DKPR" and "RUS
Publikováno v:
Environmental Earth Sciences ISBN: 9783319693552
The Ghiss-Nekor coastal aquifer is considered among the most important aquifers in the Moroccan Mediterranean. It covers about 100 km2 and consists of plio-quaternary alluvium composed of detrital sediments crossed by discontinuous clay levels. This
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b2df1f88f2ceb60b37f0327481b2ae5f
https://doi.org/10.1007/978-3-319-69356-9_20
https://doi.org/10.1007/978-3-319-69356-9_20