Hydrological, Hydro-Geological, Hydrodynamic Behavior of Mikkes Basin (Paperback)
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Hydrological, hydro-geological, hydrodynamic behavior of Mikkes basin (2013)
DE PB NW RP
ISBN: 9783659373084 bzw. 3659373087, in Deutsch, Taschenbuch, neu, Nachdruck.
Von Händler/Antiquariat, AHA-BUCH GmbH [51283250], Einbeck, NDS, Germany.
This item is printed on demand - Print on Demand Titel. - The Mikkes basin is located at the north center of Morocco. It comprises three distinct zones presenting diversified geological formations and sheltering a phreatic, a confined aquifer in Saïs basin, and a shallow aquifer in the Tabular Atlas. The interpretation of Mikkes piezometric data suggests the existence of a hydraulic connection between the groundwater and the River. The important decrease of water level in the Mikkes aquifers, observed since the beginning of the 1980 s, is probably due to a combined effect of dryness and overexploitation. The Saïs phreatic groundwater springs have shown the greatest depletion, whereas the deep or mixed-origing springs experienced lesser flow variations. This can be explained to the relative position of piezometric level compared to the River level. For the Saïs groundwater, the positive correlation between the River flow and the piezometric levels outside flood periods, suggests the assumption of a supply-drainage relationship between the aquifer and the River. The hydrochemistry of Mikkes basin waters is largely related to the geology of formations traversed. It may also be related to the interaction of surface water and groundwater. 284 pp. Englisch.
This item is printed on demand - Print on Demand Titel. - The Mikkes basin is located at the north center of Morocco. It comprises three distinct zones presenting diversified geological formations and sheltering a phreatic, a confined aquifer in Saïs basin, and a shallow aquifer in the Tabular Atlas. The interpretation of Mikkes piezometric data suggests the existence of a hydraulic connection between the groundwater and the River. The important decrease of water level in the Mikkes aquifers, observed since the beginning of the 1980 s, is probably due to a combined effect of dryness and overexploitation. The Saïs phreatic groundwater springs have shown the greatest depletion, whereas the deep or mixed-origing springs experienced lesser flow variations. This can be explained to the relative position of piezometric level compared to the River level. For the Saïs groundwater, the positive correlation between the River flow and the piezometric levels outside flood periods, suggests the assumption of a supply-drainage relationship between the aquifer and the River. The hydrochemistry of Mikkes basin waters is largely related to the geology of formations traversed. It may also be related to the interaction of surface water and groundwater. 284 pp. Englisch.
2
Symbolbild
Hydrological, hydro-geological, hydrodynamic behavior of Mikkes basin
DE PB NW
ISBN: 9783659373084 bzw. 3659373087, in Deutsch, Taschenbuch, neu.
Von Händler/Antiquariat, BuySomeBooks [52360437], Las Vegas, NV, U.S.A.
This item is printed on demand. Paperback. The Mikkes basin is located at the north center of Morocco. It comprises three distinct zones presenting diversified geological formations and sheltering a phreatic, a confined aquifer in Sas basin, and a shallow aquifer in the Tabular Atlas. The interpretation of Mikkes piezometric data suggests the existence of a hydraulic connection between the groundwater and the River. The important decrease of water level in the Mikkes aquifers, observed since the beginning of the 1980s, is probably due to a combined effect of dryness and overexploitation. The Sas phreatic groundwater springs have shown the greatest depletion, whereas the deep or mixed-origing springs experienced lesser flow variations. This can be explained to the relative position of piezometric level compared to the River level. For the Sas groundwater, the positive correlation between the River flow and the piezometric levels outside flood periods, suggests the assumption of a supply-drainage relationship between the aquifer and the River. The hydrochemistry of Mikkes basin waters is largely related to the geology of formations traversed. It may also be related to the interaction of surface water and groundwater. This item ships from La Vergne,TN.
This item is printed on demand. Paperback. The Mikkes basin is located at the north center of Morocco. It comprises three distinct zones presenting diversified geological formations and sheltering a phreatic, a confined aquifer in Sas basin, and a shallow aquifer in the Tabular Atlas. The interpretation of Mikkes piezometric data suggests the existence of a hydraulic connection between the groundwater and the River. The important decrease of water level in the Mikkes aquifers, observed since the beginning of the 1980s, is probably due to a combined effect of dryness and overexploitation. The Sas phreatic groundwater springs have shown the greatest depletion, whereas the deep or mixed-origing springs experienced lesser flow variations. This can be explained to the relative position of piezometric level compared to the River level. For the Sas groundwater, the positive correlation between the River flow and the piezometric levels outside flood periods, suggests the assumption of a supply-drainage relationship between the aquifer and the River. The hydrochemistry of Mikkes basin waters is largely related to the geology of formations traversed. It may also be related to the interaction of surface water and groundwater. This item ships from La Vergne,TN.
3
Hydrological, hydro-geological, hydrodynamic behavior of Mikkes basin (2013)
EN PB NW
ISBN: 9783659373084 bzw. 3659373087, in Englisch, 284 Seiten, LAP LAMBERT Academic Publishing, Taschenbuch, neu.
Lieferung aus: Vereinigte Staaten von Amerika, Usually ships in 24 hours.
Von Händler/Antiquariat, Amazon.com.
The Mikkes basin is located at the north center of Morocco. It comprises three distinct zones presenting diversified geological formations and sheltering a phreatic, a confined aquifer in Saïs basin, and a shallow aquifer in the Tabular Atlas. The interpretation of Mikkes piezometric data suggests the existence of a hydraulic connection between the groundwater and the River. The important decrease of water level in the Mikkes aquifers, observed since the beginning of the 1980’s, is probably due to a combined effect of dryness and overexploitation. The Saïs phreatic groundwater springs have shown the greatest depletion, whereas the deep or mixed-origing springs experienced lesser flow variations. This can be explained to the relative position of piezometric level compared to the River level. For the Saïs groundwater, the positive correlation between the River flow and the piezometric levels outside flood periods, suggests the assumption of a supply-drainage relationship between the aquifer and the River. The hydrochemistry of Mikkes basin waters is largely related to the geology of formations traversed. It may also be related to the interaction of surface water and groundwater. Paperback, Label: LAP LAMBERT Academic Publishing, LAP LAMBERT Academic Publishing, Produktgruppe: Book, Publiziert: 2013-04-25, Freigegeben: 2013-04-25, Studio: LAP LAMBERT Academic Publishing.
Von Händler/Antiquariat, Amazon.com.
The Mikkes basin is located at the north center of Morocco. It comprises three distinct zones presenting diversified geological formations and sheltering a phreatic, a confined aquifer in Saïs basin, and a shallow aquifer in the Tabular Atlas. The interpretation of Mikkes piezometric data suggests the existence of a hydraulic connection between the groundwater and the River. The important decrease of water level in the Mikkes aquifers, observed since the beginning of the 1980’s, is probably due to a combined effect of dryness and overexploitation. The Saïs phreatic groundwater springs have shown the greatest depletion, whereas the deep or mixed-origing springs experienced lesser flow variations. This can be explained to the relative position of piezometric level compared to the River level. For the Saïs groundwater, the positive correlation between the River flow and the piezometric levels outside flood periods, suggests the assumption of a supply-drainage relationship between the aquifer and the River. The hydrochemistry of Mikkes basin waters is largely related to the geology of formations traversed. It may also be related to the interaction of surface water and groundwater. Paperback, Label: LAP LAMBERT Academic Publishing, LAP LAMBERT Academic Publishing, Produktgruppe: Book, Publiziert: 2013-04-25, Freigegeben: 2013-04-25, Studio: LAP LAMBERT Academic Publishing.
4
Hydrological, hydro-geological, hydrodynamic behavior of Mikkes basin (2013)
EN NW
ISBN: 9783659373084 bzw. 3659373087, in Englisch, 284 Seiten, LAP LAMBERT Academic Publishing, neu.
Lieferung aus: Italien, Generalmente spedito in 1-2 giorni lavorativi.
Von Händler/Antiquariat, BOOKS etc.
Die Beschreibung dieses Angebotes ist von geringer Qualität oder in einer Fremdsprache. Trotzdem anzeigen
Von Händler/Antiquariat, BOOKS etc.
Die Beschreibung dieses Angebotes ist von geringer Qualität oder in einer Fremdsprache. Trotzdem anzeigen
5
Belhassan, K: Hydrological, hydro-geological, hydrodynamic b bei averdo
DE NW
ISBN: 9783659373084 bzw. 3659373087, in Deutsch, neu.
Lieferung aus: Deutschland, Lieferart: Flat, Lieferung: Österreich, Deutschland, Artikelstandort: Deutschland.
Von Händler/Antiquariat, averdo-online.
Festpreisangebot.
Von Händler/Antiquariat, averdo-online.
Festpreisangebot.
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