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Title: Hydrogeophysical investigation at Luxor, southern Egypt
Author (s): Ismail, Ahmed
Anderson, Neil L.
Rogers, David
Department/Lab Affiliations: Center for Infrastructure Engineering Studies
Geological Sciences & Engineering
Materials Research Center
Natural Hazard Mitigation Institute (NHMI)
University Transportation Center
Keywords: Aswan dam
archaeological sites
electrical sounding
seismic methods
Subject Terms: Africa.
Issue Date: 2005
Publisher: Environmental and Engineering Geophysical Society EEGS
Citation: Ismail, Ahmed, Neil L. Anderson, and J. David Rogers. “Hydrogeophysical investigation at Luxor, southern Egypt.” Journal of Environmental & Engineering Geophysics, 10 (1): 35-50 (2005).
Abstract: Over the past 35 years, the exposed stone foundations of the ancient Egyptian monuments at Luxor have deteriorated at an alarmingly accelerated rate. Accelerated deterioration is attributable to three principal factors: 1) excavation and exposure of foundation stone; 2) construction of the Aswan High Dam; and 3) changes in the regional groundwater regime. In an effort to better elucidate the hydrostratigraphy in the Luxor study area that extends from the River Nile to the boundaries of the Nile Valley and covers about 70 km2, a geophysical/hydrological investigation was conducted. Forty Schlumberger vertical electrical soundings (VES), two approximately 6 km long seismic refraction profiles and a total number of 39 groundwater and surface water samples were acquired. Based on the integrated interpretation of the acquired geophysical/hydrological data, the main contributions of this study were the geophysical definition of the hydrostratigraphy using resistivity (seven distinct geologic/hydrologic units were mapped), the mapping of the water table using seismic refraction and the mapping of groundwater salinity trends through geochemical sampling. The factors contributing to the rise of groundwater and its accompanying increase in salinity were identified and documented. This characterization establishes a model for evaluating various plans to lower groundwater levels and salinities in the areas of archeological monuments.
Type: Article - Journal
text
In Title: Journal of Environmental & Engineering Geophysics
Copyright Notice: This material is presented to ensure timely dissemination of scholarly and technical work. Copyright and all rights therein are retained by authors or by other copyright holders. All persons copying this information are expected to adhere to the terms and constraints invoked by each author's copyright. In most cases, these works may not be reposted without the explicit permission of the copyright holder.
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http://www.eegs.org/
Publisher URL:
http://dx.doi.org/10.2113/JEEG10.1.35
Link to this page:
http://scholarsmine.mst.edu/post_prints/HydrogeophysicalInvestigationAtLuxo_09007dcc80536330.html



titleHydrogeophysical investigation at Luxor, southern Egypt
contributor.authorIsmail, Ahmed
contributor.authorAnderson, Neil L.
contributor.authorRogers, David
contributor.deptlabCenter for Infrastructure Engineering Studies
contributor.deptlabGeological Sciences & Engineering
contributor.deptlabMaterials Research Center
contributor.deptlabNatural Hazard Mitigation Institute (NHMI)
contributor.deptlabUniversity Transportation Center
subjectAswan dam
subjectarchaeological sites
subjectelectrical sounding
subjectseismic methods
subject.LCSHAfrica.
date.issued2005
publisherEnvironmental and Engineering Geophysical Society EEGS
identifier.citationIsmail, Ahmed, Neil L. Anderson, and J. David Rogers. “Hydrogeophysical investigation at Luxor, southern Egypt.” Journal of Environmental & Engineering Geophysics, 10 (1): 35-50 (2005).
identifier.pub.URI
http://dx.doi.org/10.2113/JEEG10.1.35
description.abstractOver the past 35 years, the exposed stone foundations of the ancient Egyptian monuments at Luxor have deteriorated at an alarmingly accelerated rate. Accelerated deterioration is attributable to three principal factors: 1) excavation and exposure of foundation stone; 2) construction of the Aswan High Dam; and 3) changes in the regional groundwater regime. In an effort to better elucidate the hydrostratigraphy in the Luxor study area that extends from the River Nile to the boundaries of the Nile Valley and covers about 70 km2, a geophysical/hydrological investigation was conducted. Forty Schlumberger vertical electrical soundings (VES), two approximately 6 km long seismic refraction profiles and a total number of 39 groundwater and surface water samples were acquired. Based on the integrated interpretation of the acquired geophysical/hydrological data, the main contributions of this study were the geophysical definition of the hydrostratigraphy using resistivity (seven distinct geologic/hydrologic units were mapped), the mapping of the water table using seismic refraction and the mapping of groundwater salinity trends through geochemical sampling. The factors contributing to the rise of groundwater and its accompanying increase in salinity were identified and documented. This characterization establishes a model for evaluating various plans to lower groundwater levels and salinities in the areas of archeological monuments.
typeArticle - Journal
type.DCMITypetext
relation.isPartOfJournal of Environmental & Engineering Geophysics
rightsThis material is presented to ensure timely dissemination of scholarly and technical work. Copyright and all rights therein are retained by authors or by other copyright holders. All persons copying this information are expected to adhere to the terms and constraints invoked by each author's copyright. In most cases, these works may not be reposted without the explicit permission of the copyright holder.
rightsPolicy Unknown
rights.URI
http://www.eegs.org/
date.available2008-07-29T13:51:41Z
identifier.persist.URI
http://scholarsmine.mst.edu/post_prints/HydrogeophysicalInvestigationAtLuxo_09007dcc80536330.html