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العنوان
ground penetrating radar applied geoenvironmental protection at mar-mina area near burg el-arab city, egypt /
المؤلف
ahmed, amin ibrahim mohammed.
هيئة الاعداد
باحث / أمين إبراهيم محمد أحمد
مشرف / أحمـد سمـير محمـد علـي
مشرف / ماهر عبدالفتاح مصباح
مشرف / شاكر أبوالفتوح إبراهيم
الموضوع
radar- egypt.
تاريخ النشر
2011.
عدد الصفحات
200 p. :
اللغة
الإنجليزية
الدرجة
ماجستير
التخصص
علوم البيئة
تاريخ الإجازة
1/1/2011
مكان الإجازة
جامعة الزقازيق - كلية العلوم - الجيولوجيا
الفهرس
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Abstract

Mar-Mina area is located at the northern border of the Western Desert between Latitudes 30o 49’ 39’’ N and 30o 51’ 27’’ N and between Longitudes 29o 39’ 9’’ E and 29o 41’ 24’’ E. The whole historical site covers an area of about 980 acres
around which two large agricultural zones are located in the northeast and southwest respectively.
The rise of water table has implemented sever disastrous effects on the limestone walls and encountered structures, swamps and lakes are formed inside and all around the site.
The main purpose of the present investigation is to study the
applicability of non-destructive geophysical techniques to solve particular environmental problems in the area. Accordingly, the investigations involved 2D ground penetrating radar, 1D and 2D electrical resistivity methods
designed to cover two district areas; (i) around the ring road bounding a safe area, and (ii) within the limits of the historical Mar-Mina Church. Eleven 2D GPR profiles were conducted at the western part of Mar-Mina
area and nine profiles within the limits of the historical site. A 250 megahertz (MHz) monostatic shielded antenna was used for the entire data gathering. The
time window used during GPR data acquisition is about 180 ns. Calculation of factors affecting the interpretation, such as, velocity of electromagnetic waves, absorption coefficient, dielectric constant, vertical resolution and horizontal resolution were carried out. The processed GPR profiles carried out at the western part are noisy below the time window 40 ns and haven’t any evidences about the shallow layered sediments or any subsurface archaeological structures. The depth to the water table was deduced from these radargrams is equals to about 1 m.