[EAN: 9783844317008], Nouveau livre, [SC: 10.99], [PU: LAP LAMBERT Academic Publishing], nach der Bestellung gedruckt Neuware - Printed after ordering - A two-dimensional shallow resistiv… Plus…
[EAN: 9783844317008], Nouveau livre, [SC: 10.99], [PU: LAP LAMBERT Academic Publishing], nach der Bestellung gedruckt Neuware - Printed after ordering - A two-dimensional shallow resistivity survey of the groundwater potential of Ahmadu Bello University, Kongo Campus, Zaria Kaduna State, Nigeria using electrical imaging technique was carried out. Six image lines were measured at different strategic locations of the study area based on the fractured map of the area and Borehole log data information obtained from the area. Results from the interpretation of the data collected suggest 2-4 layers in the area studied.The resistivity value for the first layer (Topsoil) varies from 10 to 400 ohmm with thickness ranging from 1-14m. The second layer (Weathered Basement) has resistivity values between 120 and 500 ohm-m and thickness ranging from 5-11m. The third layer (Fractured basement) has resistivity values ranging from 500-1000 ohm-m and thickness between 3 and 6m. The fourth layer is the Fresh Basement (Bedrock) has resistivity values greater than 1000 ohm-m and infinite thickness.The southwest (SW) of the study area does represent a promising Aquifer with reasonable thickness of Weathered Basement and Fractured Zone. Also, the area seems to be a zone of high hydraulic conductivity because of its low resistivity values. 80 pp. Englisch, Books<
[EAN: 9783844317008], Neubuch, [PU: LAP Lambert Acad. Publ. Mrz 2011], This item is printed on demand - Print on Demand Neuware - A two-dimensional shallow resistivity survey of the groun… Plus…
[EAN: 9783844317008], Neubuch, [PU: LAP Lambert Acad. Publ. Mrz 2011], This item is printed on demand - Print on Demand Neuware - A two-dimensional shallow resistivity survey of the groundwater potential of Ahmadu Bello University, Kongo Campus, Zaria Kaduna State, Nigeria using electrical imaging technique was carried out. Six image lines were measured at different strategic locations of the study area based on the fractured map of the area and Borehole log data information obtained from the area. Results from the interpretation of the data collected suggest 2-4 layers in the area studied.The resistivity value for the first layer (Topsoil) varies from 10 to 400 ohmm with thickness ranging from 1-14m. The second layer (Weathered Basement) has resistivity values between 120 and 500 ohm-m and thickness ranging from 5-11m. The third layer (Fractured basement) has resistivity values ranging from 500-1000 ohm-m and thickness between 3 and 6m. The fourth layer is the Fresh Basement (Bedrock) has resistivity values greater than 1000 ohm-m and infinite thickness.The southwest (SW) of the study area does represent a promising Aquifer with reasonable thickness of Weathered Basement and Fractured Zone. Also, the area seems to be a zone of high hydraulic conductivity because of its low resistivity values. 80 pp. Englisch<
A two-dimensional shallow resistivity survey of the groundwater potential of Ahmadu Bello University, Kongo Campus, Zaria Kaduna State, Nigeria using electrical imaging technique was carr… Plus…
A two-dimensional shallow resistivity survey of the groundwater potential of Ahmadu Bello University, Kongo Campus, Zaria Kaduna State, Nigeria using electrical imaging technique was carried out. Six image lines were measured at different strategic locations of the study area based on the fractured map of the area and Borehole log data information obtained from the area. Results from the interpretation of the data collected suggest 2-4 layers in the area studied.The resistivity value for the first layer (Topsoil) varies from 10 to 400 ohmm with thickness ranging from 1-14m. The second layer (Weathered Basement) has resistivity values between 120 and 500 ohm-m and thickness ranging from 5-11m. The third layer (Fractured basement) has resistivity values ranging from 500-1000 ohm-m and thickness between 3 and 6m. The fourth layer is the Fresh Basement (Bedrock) has resistivity values greater than 1000 ohm-m and infinite thickness.The southwest (SW) of the study area does represent a promising Aquifer with reasonable thickness of Weathered Basement and Fractured Zone. Also, the area seems to be a zone of high hydraulic conductivity because of its low resistivity values. Bücher, Hörbücher & Kalender / Bücher / Sachbuch / Naturwissenschaften / Geowissenschaften / Mineralogie<
Dodax.de
Nr. TEKTV730U8L. Frais d'envoi, Lieferzeit: 5 Tage, DE. (EUR 0.00) Details...
(*) Livre non disponible signifie que le livre est actuellement pas disponible à l'une des plates-formes associées nous recherche.
[EAN: 9783844317008], Nouveau livre, [SC: 10.99], [PU: LAP LAMBERT Academic Publishing], nach der Bestellung gedruckt Neuware - Printed after ordering - A two-dimensional shallow resistiv… Plus…
[EAN: 9783844317008], Nouveau livre, [SC: 10.99], [PU: LAP LAMBERT Academic Publishing], nach der Bestellung gedruckt Neuware - Printed after ordering - A two-dimensional shallow resistivity survey of the groundwater potential of Ahmadu Bello University, Kongo Campus, Zaria Kaduna State, Nigeria using electrical imaging technique was carried out. Six image lines were measured at different strategic locations of the study area based on the fractured map of the area and Borehole log data information obtained from the area. Results from the interpretation of the data collected suggest 2-4 layers in the area studied.The resistivity value for the first layer (Topsoil) varies from 10 to 400 ohmm with thickness ranging from 1-14m. The second layer (Weathered Basement) has resistivity values between 120 and 500 ohm-m and thickness ranging from 5-11m. The third layer (Fractured basement) has resistivity values ranging from 500-1000 ohm-m and thickness between 3 and 6m. The fourth layer is the Fresh Basement (Bedrock) has resistivity values greater than 1000 ohm-m and infinite thickness.The southwest (SW) of the study area does represent a promising Aquifer with reasonable thickness of Weathered Basement and Fractured Zone. Also, the area seems to be a zone of high hydraulic conductivity because of its low resistivity values. 80 pp. Englisch, Books<
[EAN: 9783844317008], Neubuch, [PU: LAP Lambert Acad. Publ. Mrz 2011], This item is printed on demand - Print on Demand Neuware - A two-dimensional shallow resistivity survey of the groun… Plus…
[EAN: 9783844317008], Neubuch, [PU: LAP Lambert Acad. Publ. Mrz 2011], This item is printed on demand - Print on Demand Neuware - A two-dimensional shallow resistivity survey of the groundwater potential of Ahmadu Bello University, Kongo Campus, Zaria Kaduna State, Nigeria using electrical imaging technique was carried out. Six image lines were measured at different strategic locations of the study area based on the fractured map of the area and Borehole log data information obtained from the area. Results from the interpretation of the data collected suggest 2-4 layers in the area studied.The resistivity value for the first layer (Topsoil) varies from 10 to 400 ohmm with thickness ranging from 1-14m. The second layer (Weathered Basement) has resistivity values between 120 and 500 ohm-m and thickness ranging from 5-11m. The third layer (Fractured basement) has resistivity values ranging from 500-1000 ohm-m and thickness between 3 and 6m. The fourth layer is the Fresh Basement (Bedrock) has resistivity values greater than 1000 ohm-m and infinite thickness.The southwest (SW) of the study area does represent a promising Aquifer with reasonable thickness of Weathered Basement and Fractured Zone. Also, the area seems to be a zone of high hydraulic conductivity because of its low resistivity values. 80 pp. Englisch<
A two-dimensional shallow resistivity survey of the groundwater potential of Ahmadu Bello University, Kongo Campus, Zaria Kaduna State, Nigeria using electrical imaging technique was carr… Plus…
A two-dimensional shallow resistivity survey of the groundwater potential of Ahmadu Bello University, Kongo Campus, Zaria Kaduna State, Nigeria using electrical imaging technique was carried out. Six image lines were measured at different strategic locations of the study area based on the fractured map of the area and Borehole log data information obtained from the area. Results from the interpretation of the data collected suggest 2-4 layers in the area studied.The resistivity value for the first layer (Topsoil) varies from 10 to 400 ohmm with thickness ranging from 1-14m. The second layer (Weathered Basement) has resistivity values between 120 and 500 ohm-m and thickness ranging from 5-11m. The third layer (Fractured basement) has resistivity values ranging from 500-1000 ohm-m and thickness between 3 and 6m. The fourth layer is the Fresh Basement (Bedrock) has resistivity values greater than 1000 ohm-m and infinite thickness.The southwest (SW) of the study area does represent a promising Aquifer with reasonable thickness of Weathered Basement and Fractured Zone. Also, the area seems to be a zone of high hydraulic conductivity because of its low resistivity values. Bücher, Hörbücher & Kalender / Bücher / Sachbuch / Naturwissenschaften / Geowissenschaften / Mineralogie<
Nr. TEKTV730U8L. Frais d'envoi, Lieferzeit: 5 Tage, DE. (EUR 0.00)
1Comme certaines plateformes ne transmettent pas les conditions d'expédition et que celles-ci peuvent dépendre du pays de livraison, du prix d'achat, du poids et de la taille de l'article, d'une éventuelle adhésion de la plateforme, d'une livraison directe par la plateforme ou via un prestataire tiers (Marketplace), etc. il est possible que les frais de livraison indiqués par eurolivre ne correspondent pas à ceux de la plateforme qui propose l'article.
Données bibliographiques du meilleur livre correspondant
A two-dimensional shallow resistivity survey of the groundwater potential of Ahmadu Bello University, Kongo Campus, Zaria Kaduna State, Nigeria using electrical imaging technique was carried out. Six image lines were measured at different strategic locations of the study area based on the fractured map of the area and Borehole log data information obtained from the area. Results from the interpretation of the data collected suggest 2-4 layers in the area studied.The resistivity value for the first layer (Topsoil) varies from 10 to 400 ohmm with thickness ranging from 1-14m. The second layer (Weathered Basement) has resistivity values between 120 and 500 ohm-m and thickness ranging from 5-11m. The third layer (Fractured basement) has resistivity values ranging from 500-1000 ohm-m and thickness between 3 and 6m. The fourth layer is the Fresh Basement (Bedrock) has resistivity values greater than 1000 ohm-m and infinite thickness.The southwest (SW) of the study area does represent a promising Aquifer with reasonable thickness of Weathered Basement and Fractured Zone. Also, the area seems to be a zone of high hydraulic conductivity because of its low resistivity values.
Informations détaillées sur le livre - Ground-water exploration
EAN (ISBN-13): 9783844317008 ISBN (ISBN-10): 3844317007 Version reliée Livre de poche Date de parution: 2011 Editeur: AV Akademikerverlag GmbH & Co. KG.
Livre dans la base de données depuis 2008-01-21T01:52:46+01:00 (Paris) Page de détail modifiée en dernier sur 2023-06-16T12:29:19+02:00 (Paris) ISBN/EAN: 3844317007
ISBN - Autres types d'écriture: 3-8443-1700-7, 978-3-8443-1700-8 Autres types d'écriture et termes associés: Auteur du livre: felix Titre du livre: ground water, exploration
