Geophysical Studies of the ground water occurrences affected the Giza Pyramids area , Giza , Egypt / Zein Elabedin Diab Abdelfattah Hassan ; Supervised Sharafeldin Mahmoud Sharafeldin , Khalid Sayed Ahmed Tawfik Essa , Mohamed Ahmed Shokery Youssef
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- دراسات جيوفزيقيه لتأثير تواجد المياه الجوفيه لمنطقة اهرامات الجيزة - الجيزة - مصر [Added title page title]
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Item type | Current library | Home library | Call number | Copy number | Status | Barcode | |
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قاعة الرسائل الجامعية - الدور الاول | المكتبة المركزبة الجديدة - جامعة القاهرة | Cai01.12.16.M.Sc.2017.Ze.G (Browse shelf(Opens below)) | Not for loan | 01010110074351000 | ||
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مخـــزن الرســائل الجـــامعية - البدروم | المكتبة المركزبة الجديدة - جامعة القاهرة | Cai01.12.16.M.Sc.2017.Ze.G (Browse shelf(Opens below)) | 74351.CD | Not for loan | 01020110074351000 |
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Thesis (M.Sc.) - Cairo University - Faculty of Science - Department of Geophysics
Nowadays Egyptian Great Pyramids and Great Sphinx are suffering from rising of Groundwater table. This problem promoted the need to characterize the groundwater occurrences in and around Pyramids Plateau. Multidisciplinary geophysical techniques deployed at the Pyramids Plateau area where, electric resistivity, seismic refraction, and georadar techniques, conducted to delineate the water table. The groundwater table located at elevations of 13 to 17 m asl at the Great Sphinx area, in urbanized area surrounded the Pyramids plateau, located at elevations of 4 to 62 m asl. The groundwater table detected is above the marly limestone which is the formation of the Sphinx, which causes a serious problem of dissolution that cause the monuments fractures. It is recommended to lower the water table by a system of dewatering borehole. Sewage water from the near residence places, nearby Canals, are a sustainable threat for the heritage sites
Issued also as CD
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