التصوير الطبقي ذو المعاوقة الكهربائية (EIT) هو تقنية تسمح بإعادة بناء صور المقطع العرضي المتعلقة بالمعاوقة الكهربائية من خلال مجموعات مقاسه من سطحها، الدافع الرئيسي من تطوير التصوير الطبقي ذي المعاوقة الكهربائية(EIT)هواحتمالية تطبيقه في مجالات التصوير الطبية، وكما هو معروف فأن النسيج الحيوي له مدي معاوقة كهربائية واسع والعديد من الأحداث الفسيولوجية محسوبة بتغيرات المعاوقة الكهربائية، و موصلية نسيج جسم الإنسان فيها اختلافات كبيرة، لذا يجب أن تعطي صور الموصلية مقارنة عالية بين الأنسجة الناعمة. وتعتمد تقنية التصوير الطبقي ذي المعاوقة الكهربائية على إعادة بناء توزيع الموصلية في جسم الإنسان، وذلك من خلال القياسات الخارجية التي يتم قياسها عند تمرير التيار خلال المجسات الموجودة على الجسم والتيار المار، والجهد المقاس يعتمد على الموصلية المراد إيجادها، وتهدف كل خوارزمياتِ وإعادةَ البناء إلي تَقليل الأخطاءِ، والحصول على صور ممتازةِ. إعادة بناء الموصلية في التصوير الطبقي ذي المعاوقة الكهربائية (EIT) تعتبر مشكلة، وبشكل عملي تحل هده المشكلة ببعض طرق التنظيم أو الفرضيات المطبقة لتحسين نوعية الصورة.للحصول على أفضل بناء صورة ممكنه للتصوير الطبقي ذي المعاوقة الكهربائية تم في هذا العمل إجراء مقارنة بين العديد من طرق التنظيم وكانت معتمدة على تعديل النسبة بين أكبر وأصغر القيم الصغيرة والقريبة للصفر داخل مصفوفة الحساسية وتم تطبيق ذلك في طريقة جديدة.كما تم في هذا العمل أيضاً تطوير طريقة جديدة تتعلق بالتصوير الطبقي ذي المعاوقة الكهربائية وتسجيل الصورة و تم الحصول على المعلومات الكاملة في الصورة الجديدة. Abstract Electrical Impedance Tomography (EIT) is a technique which allowscross-section images related to the local electrical impedance within an object to be reconstructed from sets of measurements made on its surface. The main drive behind the development of Electrical Impedance Tomography (EIT) has been its possible application in medical imaging, as biological tissues are known to exhibit a wide range of electrical impedances and many physiological events are computed by electrical impedance changes. The conductivity of the human tissue has large variations so images of the conductivity distribution should give high contrast of soft tissues. In electrical impedance tomography (EIT) the conductivity distribution is reconstructed from measured boundary potential when current sources are applied to the boundary of the object. Both internal current paths and potential distribution depend on the unknown conductivity distribution. All considerations of the reconstruction algorithms aim to minimize the errors, and to obtain quality images.Reconstruction of the conductivity distribution in electrical impedance tomography (EIT) is an un-determined and ill-posed problem. Typically requiring simplifying assumption or regularization methods to improve image quality.To improve the system’s conditioning and to determine the best image reconstruction in electrical impedance tomography (EIT) several regularization methods in this work are compared, and based on modification of the ratio between the largest and the smallest non-zero singular value of the sensitivity matrix, a new method has been developed.Also in this work a new method concerning electrical impedance tomography image registration has been developed and the full information contained in the new image can be obtained.
زينب احمد العزابى (2008)

Abstract Reinforced concrete slabs are among the most common structural elements, but despite the large number of slabs designed and built, the details of the elastic and plastic behavior of slabs are not always appreciated or properly taken into account. The problem for the designer is to decide which method is most appropriate for a given slab. It must be determined whether the chosen method satisfies strength and serviceability requirements and whether the solution is economical from both a design and construction point of view. The purpose is to examine different methods of two-way slab design and compare the results to assess the relative merits of design methods. However, commercially available finite element softwares are not designed for this task as most of them have been developed to be used as verification rather than design tools. 'Home-written' software can be designed to achieve this task, however it may suffer from serious drawbacks such as bugs, lack of user friendliness, lack of generality, and unproven reliability.
ماجد يوسف زقوت (2009)

Abstract The accurate detection and confirmation of formation pore pressure and fracture gradient has become almost essential to the drilling of deep wells with higher than normal pore pressure. Generally, the formation pressure is the presence of the fluids “oil, gas or salt water” in the pore spaces of the rock matrix. Therefore, the fluid confined in the pores of the formation rock occur under certain degree of pressure, generally called formation pore pressure. Formation pore pressure is defined as the pressure acting on the fluids in the pore space of the rock, which is equal to the difference between the total overburden stress and grain to grain stress. Normal formation pressure is equal to the hydrostatic head of the native formation fluid or water exerting from the top of water table to the subsurface formation depth. Hydrostatic pressure is the pressure in a column of salt water or usually defined as the pressure exerted by a column of fluid, the pressure is a function of the average fluid density and the vertical height or depth of the fluid column. In most cases, the fluid vary from fresh water with a density of (8.33 Ib/gal) (0.433 psi/ft) to salt water with a density of (9 Ib/gal) (0.465 psi/ft). Consequently the hydrostatic pressure gradient of such system will be greater in terms of (psi/ft) than that of a fresh water system and will be displayed on pressure depth plot by pressure gradient line whose slope is greater than that of fresh water hydrostatic pressure. Indeed, formation pore pressure depending on the magnitude of the pore pressure, it can be described as being either normal, abnormal or subnormal. Whereas defined as follows, we had defined normal pore pressure which is equal to the hydrostatic pressure, abnormal pore pressure is defined as any pore pressure that is greater than the hydrostatic pressure of the formation water occupying the pore space, and sometimes called overpressure or geopressure. Subnormal pore pressure is defined as any formation pressure that is less than the corresponding fluid hydrostatic pressure at a given depth. The objectives of this study are:To determine the origin, nature, causes and the location of the subnormal and overpressued formations in part of Sirte basin area. To determine a graphical correlation relating formation pore pressure and fracture gradients to depth for selected areas extending fromfurther east to North West in the basin.This study is determining the pore pressure and fracture gradient, for selected fields from eastern, central and western Sirte basin, using existing correlations which utilize log and drilling data measured for the selected wells in these areas. The casing setting depths as well as the maximum and the minimum mud weight gradients to be used for future drilling activities in these selected areas in Sirte basin have been determined. The location and the magnitude of the lost circulation zones as well as the overpressured zones have been determined and correlated with depth depending on the location of the studied area in the basin. It was found that the lost circulation zones are located at depths of approximately in the range 3000 to 6000 ft from east toward west. It is concluded that the calculated pore pressure and the fracture gradients values obtained from the log data are in good agreement with the values obtained form the drilling data. It is concluded that the results obtained in this study for the eastern part of Sirte basin was satisfactory and can be used with good confident for future drilling activities in the area, where the obtained results for either the central or the western parts of the basin are not enough to draw final conclusions for future mud design programs in these areas. It is therefore recommended that further investigation and extensive study should be conducted for these two areas by gathering enough log and drilling data from different fields in these area which was not available during this study.
احمد خليفة رمضان طنيش (2009)