Study of Hydrocarbon Potentials and Sedimentary Properties of Ispartaçay Formation, Turkey

The idea of the current work was the combination of the organic geochemical analyses, and the study of sedimentology characteristics of the source rock samples collected from the Ispartaçay Formation (Cretaceous period) between the city of Antalya and the city of Isparta, southwestern Turkey. Total Organic Carbon analysis and Rock-Eval pyrolysis were performed on the 24 samples taken from the study area, in order to evaluate quantitatively, and qualitatively organic matter and thermal maturity to determine the potential for hydrocarbon production. As well as studying the petrographic features (component and diagenesis), microfacies analysis, and sedimentary environment of the Ispartaçay Formation. The successions of the Ispartaçay Formation are poor to fair organic matter content and consist of dark grayish limestone, marly limestone, shale, massive cherty limestone, and thin-bedded radiolarian limestone. Total Organic Carbon values indicate that Ispartaçay Formation rocks are fair potential. Besides this, most of the samples from the Ispartaçay Formation contain mature to pot-mature (Type III -Type IV) kerogen. Petrographically, the particle portion of the Ispartaçay sediments is composed mainly of radiolarians, and planktonic foraminifera, In addition to the presence of a proportion of benthic foraminifera, whereas the groundmass is composed of micrite. Generally, the present sediments are subjected to some diagenetic processes like silicification, cementation, and dissolution. The microfacies analysis revealed that the succession of the Ispartaçay Formation is composed of alternations of two major microfacies, namely lime mudstone and lime wackestone microfacies. Depending on the facies and petrographic evidence, Ispartaçay Formation represents sediments deposited in the mid to outer ramp environment

Geochemistry, Depositional Environment, and Provenance of the Cretaceous Radiolarian Chert in Northeastern Kurdistan, Iraq

The radiolarian chert rocks are one of the most important indications of the existence of ophiolites because they are a source of silica supply. These rocks have been studied to refute and reject the idea that ophiolites do not existed. The Si/(Si+Al+Fe+Ca) ratio in the radiolarian chert indicates that the silica is of biogenic origin and adds SiO2 from the shale fraction through diagenetic processes. The high values of Fe2O3 content indicate the hydrothermal effect during precipitation. This effect is controlled by the distance between the sediments and the mid-oceanic ridge or sea floor metamorphism. The phosphorus could be a direct result of volcanic activity associated with ophiolitic rocks, whereas, the negative correlation coefficient of phosphorous with calcium (r = -0.53) supports the idea that the source of phosphorous is volcanic activity that is not related to the carbonate fluorapatite mineral. REEs shows a basic difference as a positive cerium anomaly in section Q2 and a negative cerium anomaly in section Q1. The Al-Fe-Mn diagram shows that all samples fall into the field I non-hydrothermal zone, but in the SiO2 vs Al2O3 diagram the samples of the Q1 section fall into the hydrothermal field, and samples of the Q2 section fall into the non-hydrothermal field. The input materials in Qulqula radiolarian chert come from terrigenous sediments in both sections. On the other hand, the Al/(Al+Fe+Mn) ratio range, (between 0.61 to 0.70), is very close to the average shale composite value, (0.6.19), which may reflect the contribution from continental and non-hydrothermal sediments, while the lower values of this ratio reflect hydrothermal source input. The MnO2 /TiO2 ratios ranged between 0.06 to 2.37 in section Q1 which represents typical characteristics of the deep ocean, trenches, and basaltic plateau sediments

دور التمويل الأصغر الإسلامي في معالجة البطالة في اليمن دراسة تطبيقية عن اليمن

Islamic microfinance in Yemen, faces many challenges that undermine its vital role. Therefore it was necessary to continue to evaluate and develop it. Therefore, this paper aimed to assess the role of Islamic microfinance institutions in reducing the unemployment rate through the development of micro-entrepreneurship. It also aimed to propose Waqf, zakat, and crowdfunding as sustainable sources of financing Islamic microfinance institutions. To achieve the objectives of this study, the researcher used the quantitative and qualitative approach, whereby questionnaires were distributed to clients of Islamic microfinance institutions in Sana'a, The study revealed that Islamic microfinance institutions have a significant impact on micro-entrepreneurship in Yemen. It found that microentrepreneurship has a negative impact on the unemployment rate in Yemen. It also revealed that the sources of waqf, zakat, and crowdfunding will have a great impact on the development of Islamic microfinance institutions in Yemen. Moreover, the findings of the study therefore provide guidance for policymakers and microfinance institutions as well as the microenterprises to develop and improve their business activities

Comparison of Oral, Tympanic and Fresh Urine Temperature in Healthy Young Adult Males in Kingdom Suadi Arabia

Background: Core body temperature (CBT) is commonly evaluated by measuring oral (OT) and tympanic membrane (TT) temperatures; however, there are considerable debates on which of these methods is the most appropriate.Objective: To evaluate concordance of OT and TT with CBT.Material and Methods: OT, TT and fresh urine temperature (FUT) were measuredsimultaneously in 45 apparently healthy young adult males from Buraydah, Qassim, KSA during July 2015. All readings were obtained between 7:00 and 10:00 pm according to the standard methods. FUT was used as indicator of CBT.Results: OT (36.35±0.41° C) was significantly higher compared with TT (35.99±0.81° C, P = 0.013) as well as FUT (35.55±0.76° C, P < 0.001). TT was significantly higher compared with FUT (P = 0.003). Using one sample t-test, the difference between OT and TT (0.36±0.92° C, P = 0.011), OT and FUT (0.80±0.90° C, P < 0.001) and TT and FUT (0.44±0.80° C, P = 0.001) were significantly above zero. Disconcordance of the OT, TT and FUT measurements are further illustrated by Bland-Altman plots. There were no significant correlations between OT and TT as well as between OT and FUT. However, TT correlated positively with FUT (r = 0.48, P = 0.001).Conclusions: OT and TT are inappropriate measures for CBT. CBT has influence on TT, but not OT.Key words: Core body temperature, oral, tympanic, urine

Shielding Properties of Some Marble Types: A Comprehensive Study of Experimental and XCOM Results

In this work, some marble types were collected from Egypt, and their shielding characteristics were estimated. Their rigidity, in addition to their elegant shape, led us to consider their use as a protective shield, in addition to making the workplace more beautiful. The mass attenuation coefficient (μ/ρ) was calculated for three types of marble (Breshia, Galala, and Trista) experimentally, using a narrow gamma ray source and high pure germanium (HPGe). The results obtained were compared with the XCOM program and indicated a very good agreement between the two methods. The linear attenuation coefficient (μ) was evaluated to calculate the half and tenth value layers. The maximum μ value of 1.055, 1.041, and 1.024 cm−1 was obtained for Breshia, Galala, and Trista, respectively, at 0.06 MeV. The mean free path for studying the materials was compared with other shielding materials and showed good results at different energy scales. The energy absorption (EABF) and exposure buildup factors (EBF) were determined at different mean free paths. The fast neutron removal cross section ΣR was calculated and expresses the ability of the marbles to slow down fast neutrons through multiple scattering. This is the ability of the marbles to shield fast neutrons

The effect of physical properties of lost petroleum quantities in vertical tanks at (NRC) Baiji

One of the main sources of crude oil and product losses in refineries is the storage tanks. The lightest hydrocarbons in these tanks evaporate during operation, causing not only a loss of the precious raw hydrocarbon material but also a source of dangerous gas pollution. For calculating these losses, several direct and indirect approaches have been devised. In this study, we used a method based on the comparison of the differences in the characteristics of crude oil or other products. This work aimed to find the specifications of two products, kerosene and gas oil, and calculate the losses that occur for the quantities in the dispatch warehouse in the NRC. Four samples of kerosene were used and named: kero@02-1, kero@05-2, kero@10-3, and kero@11-4, while four samples of gas oil were named: gaso@02-1, gaso@05-2, gaso@10-3, and gaso@11-4. Also, they depend on the date of certificate issue, respectively. The received quantities were calculated in ml and converted to cubic meters using the tank coefficient (kerosene tank coefficient 0.638 and gas oil tank coefficient 0.408). Calculations were made of 1500 ml for kerosene and 2500 ml for gas oil. In addition, this project dealt with a simplified method of work that includes the physical properties to find the actual quantities that are lost for the mentioned petroleum products. Moreover, the highest losses were for kerosene (5 m 3 ) at sp. gr 0.750, and the highest losses were for gas oil (5 m 3 ) at sp. gr 0.820. The results showed that there is a quantity of fluctuating losses that does not exceed 5 m 3 / 1000 m 3 and that these losses are in accordance with the permissible limits. The results recommend directing the laboratory tester's teams in the NRC Baiji to conduct periodic examinations of the petroleum products, as well as not to collusion when receiving a low product with laboratory examination specifications to reduce losses in quantities

The Potentials of Egyptian and Indian Granites for Protection of Ionizing Radiation

This paper aims to study the radiation shielding characteristics and buildup factor of some types of granite in Egypt. The mass attenuation coefficient (MAC) for three types of granite (gandola, white halayeb, and red aswani) was experimentally determined, and the experimental results were validated by XCOM software. The relative deviation between the two methods does not exceed 3% in all discussed granite samples, which means that MAC calculated through the experimental and XCOM are in suitable agreement. The effective atomic number (Zeff) varies from 13.64 to 10.69, 13.68 to 10.59, and 13.45 and 10.66 for gandola, white halayeb, and red aswani, respectively. As well as the equivalent atomic number (Zeq) was calculated in a wide range of energy to deduce the exposure (EBF) and energy absorption (EABF) buildup factors for the studied granite materials. The linear attenuation coefficient (LAC), half-value layer (HVL), mean free path (MFP) were calculated at each investigated energy and showed that the most effective shielding ability at high energy was red aswani, while at low energy, the shielding ability was nearly constant for studied granites. The present study forms the first endeavor to obtain the radiation shielding properties of the studied materials to be used in practical applications