Abstract The Sarir Sandstone in Messla Oil Field are of Lower Cretaceous ageAptian Alpian and occur in the subsurface of the eastern part of the Messla high in the southeast Sirt Basin. The Sarir Sandstone interpret as fluvial and alluvial fan deposits whereas the Lower Sarir Sandstone were deposited in a braided system as inter-channel bars. The Upper Sarir Sandstone were deposited in the meandering belt of the fluvial system. The Sarir Sandstone is on-lapping Formation and wedge out against Rakb Group. The Sarir Sandstone is unconformable overlies the Pre-Cambrian Basement and unconformable overlain by the Upper-Cretaceous Rakb Group where it is pinching (wedging) out against the Bald Basement; Messla High)). Lithostratigraphic correlations of borehole logs ((well logs)) in concession 65 suggests that deposits gradually downed a fault controlled topographic surface increased in thickness on the down-thrown side of a fault controlled the topographic surface of Pre-Upper Cretaceous Unconformity. IV M. Sc. Hassin Haweel “Sedimentological Aspects of the Sarir Sandstone in Messla Oil Field”, 2015 Core Samples record mainly sandstone units interbedded with sandstone and shale and minor streaks and the Red Shale Unit. Estimation of depositional environment has thus been made from grain size analyses using thin sections. Petrographic studies show that the Sarir Sandstone in composition from (subarkose to arkosic arenite). The Sandstones range from texturally immature to submature, however, much of the clay content is diagenetic in origin and not a function of the depositional regime. Diagenetic studies reveal a gnite complex paragenesis. During early diagenesis, the Sarir Sandstones were modified by Calcite, dolomite, and locally pyrite, diagenesis process; replacements of corroded silica by carbonates. Cementation fluvial sandstones Intrastratal dissolution and precipitation of kaolinite in the resulting pore space. Deformation of micas between more resistant grainy pre-dates one phase of quartz overgrowth, probably the carbonates.The purpose of this study was to investigate in detail the characteristics of the Sarir Sandstone in Messla Oil Field. Another aim was to find out the relation to the adjacent area. The method of this study was conducted with the review of the previousworks in Messla Oil Field; published papers, the open file of the Arabian Gulf Oil Company (AGOCO), well files for the data to be used in constructing maps, cross sections and profiles. Four cored wells (418 feet) V M. Sc. Hassin Haweel “Sedimentological Aspects of the Sarir Sandstone in Messla Oil Field”, 2015 were used for the core descriptions and cut samples that represent the Sarir Sandstone and (130) thin sections were used for the Petrographic analysis with polarized and scanning electron microscopes (SEM). On the other hand, XRD and XRF were not available. The results of the study were: Subsurface investigations including cores (conventional and side walls), petrographic analysis, and wire-line logs suggested that this formation (Sarir Sandstone) can be divided in to three main units in Messla Oil Field; these units are: The Lower Sarir Sandstone, the Red Shale, and the Upper Sarir Sandstone. In the adjacent area Sarir Formation was divided in to five members; Pre-Upper Cretaceous Member-1 unconformably overlying Pre-Cambrian Basement, and upwards; Member 2, Member 3, Member 4, and Member 5 unconformably overlain by Rakb Group. The Lower Sarir Sandstone in Messla Oil Field is characterized by the presence of gravely sandstone, gradually changes in to the Red Shale. Also, from the core descriptions plotted sheets, and the well logs it is finning upwards. The quarzitic sandstones of (the Lower and the Upper Sarir Sandstones) are considered to be the main producing horizons where quartz grains have undergone a complex diagenetic history, including: Authigenesis, quartz and feldspar overgrowths, dissolution, carbonates cementation, and replacement. The principal conclusion was that: the gravelly sandstone unit at the Lower part of the Lower Sarir Sandstone was deposited, most likely in a braided system as inter-channel bars. The sandstone unit of the Upper Sarir VI M. Sc. Hassin Haweel “Sedimentological Aspects of the Sarir Sandstone in Messla Oil Field”, 2015 Sandstone was deposited in the meandering belt of the fluvial system. The shale facies of the Red Shale unit represents a well-developed break between the Lower Sarir Sandstone and Upper Sarir Sandstone units; it also provides a good seal for the underlying sandstone of the Lower Sarir Sandstone. The nature of the shale facies, (i.e. lack of organic content, and presence of oxidizing conditions indicated by iron oxides color, indicate that they are not a significant source of hydrocarbons. On the other hand, the Rakb Shale isthe only source rock in the studied and adjacent areas.
حسين محمد علي حويل (2015)

تمّ في هذا البحث تصميم وبناء منظومة مسح ليزرية ثنائية الأبعاد محلياً (جامعة الفاتح/كلية العلوم/قسم الفيزياء) بدقة 0.480 mmواستُخدمت في عدة تطبيقات فيزيائية :- عملية مسح لمرآة مستوية, إيجاد معامل انكسار الزجاج, عمل مقارنة بين مقدار انعكاسية سطوح معادن مختلفة, مقارنة بين الدراسة العملية والنظرية لإنعكاسية النمط الكهربي المستعرض في الزجاج وتحقيق قانون مالوس.المكونات الرئيسية للمنظومة :- 1 – مصدر لشعاع الليزر.2- مجس ضوئي.3- دائرة استقبال وتحويل الإشارة الكهربية إلى إشارة رقمية متصلة بالحاسب الآلي.4- برنامج لعرض ورسم البيانات مباشرة على الحاسب الآلي.تمّ استخدام ليزر الهيليوم - نيون بقدرة mW 1 وبزاوية سقوط مقدارها ◦45, مجس ضوئي (الفوتوترانزستور) باستجابة للأطوال الموجية في المدى من1130 nm  400nm يتصل المجس بدائرة الكترونية لتحويل الإشارة الكهربية العادية إلى إشارة رقمية بعد أن يتم تكبيرها لتلائم التطبيق. يتحرك كلاً من مصدر الليزر والمجس الضوئي حركة آلية في اتجاه محور X كما تتحرك العينة أيضاً آلياً باتجاه محورY. دائرة الربط بالحاسب الآلي تتكون من مكبر إشارة لتكبير الإشارة الكهربية ومحول رقمي لتحويلها إلى إشارة رقمية تغذي الحاسب الآلي، يتم رسم الإشارة الناتجة وكذلك طباعة وتخزين البيانات في ملف خاص حتى تتم معالجتها لاحقاً وذلك عن طريق برنامج بلغة C. أثبتت المنظومة كفاءتها في سرعة نقل المعلومات على الأسطح دون لمس العينة المراد دراستها والتحكم فيها آلياً. Abstract In this Thesis, a two-dimensional laser scanning system was designed and constructioned accuracy was 0.480 mm. It was used in several physical applications :- a scanning of a plane mirror, determination of refractive index of glass, a comparison between reflectivity several surfaces of different metals, a comparison between practical and theoretical reflectivity of Transverse Electric Mode of glass and Malus’ Law.Main components of the system:- 1- laser beam source. 2- Light sensor. 3- Computer interface (An electronic digital circuit to convert electrical signal to digital signal). 4- A computer Software program using C – Language for data analysis. A helium - neon laser Source with output power 1 mW was used, with incidence angle of 45˚. The signal was received by a photo–transistor (response 400 nm → 1130 nm). The triangulation method was used in this system. The electrical signal from the sensor is amplified using OP amplifier and then converted to a digital signal using A/D converter. Both the Laser source and photo – transistor moves automatically in X – direction, the sample as will moves automatically in Y – direction. Computer interface consist of OP amplifier to amplify the electrical signal and a A/D converter to convert the signal to digital signal. The data was collected automatically using a – C – language program. The output data also can be plotted directly in X-Y plot on the screen. The system was very efficient and very fast data collection and transfer as a non–contact method.
نادية مسعود محمد الربع (2010)

Efficient extraction of genomic DNA (gDNA) from biological materials found in harsh environments is the first step for successful forensic DNA profiling. This study aimed to evaluate two methods for DNA recovery from animal tissues (livers, muscles), focusing on the best storage temperature for DNA yield in term of quality, quantity, and integrity for use in several downstream molecular techniques. Six male Swiss albino mice were sacrificed, liver and muscle tissues (n=32) were then harvested and stored for one week in different temperatures, -20C, 4C, 25C and 40C. The conditioned animal tissues were used for DNA extraction by Chelex-100 method or NucleoSpin Blood and Tissue kit. The extracted gDNA was visualized on 1.5% agarose gel electrophoresis to determine the quality of gDNA and analysed spectrophotometrically to determine the DNA concentration and the purity. Both methods, Chelex-100 and NucleoSpin Blood and Tissue kit found to be appropriate for yielding high quantity of gDNA, with the Chelex100 method yielding a greater quantity (P < 0.045) than the kit. At -20C, 4C, and 25C temperatures, the concentration of DNA yield was numerically lower than at 40C. The NucleoSpin Blood and Tissue kit produced a higher (P=0.031) purity product than the Chelex-100 method, particularly for muscle tissues. The Chelex-100 method is cheap, fast, effective, and is a crucial tool for yielding DNA from animal tissues (livers, muscles) exposed to harsh environment with little limitations.
Huda H. Al-Griw, Zena A. Zraba, Salsabiel K. Al-Muntaser, Marwan M. Draid, Aisha M. Zaidi, Refaat M. Tabagh , Mohamed A. Al-Griw(8-2017)