Zobrazeno 1 - 4
of 4
pro vyhledávání: '"Barhoum, Sarah"'
Autor:
Barhoum, Sarah
L’aquifère de la craie est un milieu hétérogène complexe lié à une large gamme de porosités (matrice, fractures et conduits karstiques), entrainant une forte hétérogénéité des processus et des vitesses de transfert (de 10-8 m s-1 à plu
Externí odkaz:
http://www.theses.fr/2014PA066395/document
Autor:
Pasquet, Sylvain, Guerin, Roger, Barhoum, Sarah, Audebert, Marine, Bodet, Ludovic, Dangeard, Marine, Gombert, Philippe, Valdes-Lao, Danièle, Vitale, Quentin
Publikováno v:
Symposium on the Application of Geophysics to Engineering and Environmental Problems (SAGEEP 2016)
Symposium on the Application of Geophysics to Engineering and Environmental Problems (SAGEEP 2016), Mar 2016, Denver, United States
Symposium on the Application of Geophysics to Engineering and Environmental Problems (SAGEEP 2016), Mar 2016, Denver, United States
An abandoned underground quarry of Chalk located near Beauvais (France) is of particular interest to study infiltration and dissolution processes in the vadose zone. The presence of permanent underground lakes created by the outcroping water table al
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::3a0894ef3b16b213b6e93db594c7e2c3
https://hal-ineris.archives-ouvertes.fr/ineris-01853024
https://hal-ineris.archives-ouvertes.fr/ineris-01853024
Autor:
Barhoum, Sarah
Publikováno v:
Hydrologie. Université Pierre et Marie Curie-Paris VI, 2014. Français. ⟨NNT : 2014PA066395⟩
The Chalk aquifer is a complex and heterogeneous system associated with a wide range of porosity (matrix, fractures and karstic conduits). These characteristics lead to a high heterogeneity of transfer processes and speed (ranging between 10-8 m s-1
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::514092b01f4a2b9e752438cf65a974d2
https://tel.archives-ouvertes.fr/tel-01165048
https://tel.archives-ouvertes.fr/tel-01165048
Publikováno v:
EGU General Assembly 2013
EGU General Assembly 2013, Apr 2013, Vienne, Austria
EGU General Assembly 2013, Apr 2013, Vienne, Austria
Chalk is complex because of its dual porosity and because of superficial layers more or less thick and more or less permeable. Furthermore there is few knowledge in understanding of groundwater infiltration and dissolution processes in the chalk unsa
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::7354a62dedacf30ef5b7ec08c7819283
https://ineris.hal.science/ineris-00971132
https://ineris.hal.science/ineris-00971132