Oil and gas play and prospect assessments of Babel,Diwania and Karbala Governorates (Middle Euphrates Region), Iraq     

Amer Jassim Al-Khafaji  Thamer Al-Ameri  Qusay Abeed 《Arabian Journal of Geosciences》2014,7(8):3147-3161

This study was based on the results of geochemical analysis of 332 core and 10 cutting rock samples from Triassic Jurassic, Cretaceous, and Triassic age, in addition to seismic sections, logs, initial drilling results, final reports of oil wells, and previous studies. Constructing models from these data are to assess new oil reservoirs, evaluation, and development of the existing oil reservoirs and hydrocarbon potential, and suggesting petroleum systems in order to reduce exploration risk and develop simple risk assessment of oil fields in the studied area. In general, Abu-Jir fault zone divides the studied area into two petroleum provinces: Mesopotamian Foredeep Basin and Widyan Basin–Interior Platform. The Mesopotamian Fordeep basin are thick stratigraphic sequences with no exploration for oil or gas source rock intervals within the Paleozoic sequence. while the Mesozoic sequence offers the best potential. The transitional sequence of the Triassic period is expected to contain occasional fair to good quantity of oil source rock intervals. The Widyan Basin–Interior Platform is an area with possible deployment of low to moderate risk of Paleozoic play and Lower Mesozoic plays with fair Triassic and Mesozoic objectives. Oil has generated and expelled into traps in the studied area during two phases; the first is during Early Palaeogene that accumulated in traps of the Cretaceous structural deformation, while the second is during Late Neogene.  相似文献   

Petrographical and petrophysical characteristics of asynchronous beachrocks along Al-Shoaiba Coast, Red Sea, Saudi Arabia     

Ibrahim M. Ghandour  Hamad A. Al-Washmi  Rashad A. Bantan  Mohamed M. Gadallah 《Arabian Journal of Geosciences》2014,7(1):355-365

The present study describes the petrographic and petrophysical characteristics of three stratigraphically asynchronous beachrocks (A, B, and C) along the Red Sea coast at Al-Shoaiba area, Saudi Arabia, to identify the compositional, depositional, and diagenetic controls on beachrock formation and their petrophysical properties. The beachrocks at the three locations consist basically of calcareous skeletal remains of different types and grain size reflecting the composition of adjacent beach sediments and the depositional conditions. They were cemented by aragonite and high-Mg calcite (HMC) in intertidal zone. The cement exhibits three major fabrics: (1) micritic coatings, (2) isopachous to asymmetric aragonite rim, and (3) cryptocrystalline pore-fillings HMC. In addition, some intergranular and intragranular pores were partially filled with infiltrated silt-sized carbonate and siliciclastic sediments. The cementation was accomplished by the combination of inorganic and organic processes, and the former was dominant through evaporation of pore-filling seawater under hot and dry climatic conditions. Cementation in the present beachrocks is selective; carbonate grains are cemented, whereas siliciclastic grains are cement free. The cement nucleation on carbonate grains was easier than on siliciclastic grains which do not provide good "seed crystals" for carbonate cement growth. The petrophysical measurements are in agreement with petrographic studies. The degree of cementation is the major control on petrophysical characteristics where the lowest and highest porosity and permeability values were obtained from the least cemented beachrocks of location A and the highest cemented beachrocks of location B, respectively. The thickness of cement seems to be controlled by cement precipitation rate, grain size, and size and shape of pore spaces. The coarse sediments of beachrocks at location B were deposited under higher depositional energy than those at locations A and C, and therefore, their primary pore spaces were large enough to be filled with seawaters. Under hot and dry climate, cement precipitation increases leading to partial to complete occlusion of pore spaces.  相似文献   

Modeling nutrients profiles at the sediment–water interface. Calibration and validation from two climatically contrasted estuaries: Seine (France) and Somone (Senegal)     

Valérie Mesnage  Nicolas Lecoq  Issa Sakho  Arnaud Vennin 《Comptes Rendus Geoscience》2013,345(11-12):439-445

The dialysis porewater sampler, type Hesslein, allows sampling of sediment interstitial water according to a continuous gradient between sediment and the water column. Its equilibration time fluctuates according to the nature of sediment, so it has to be measured in each kind of sediment. The aim of this work is to develop a physical diffusion model in order to determine an equilibration time without using extensive field experiments. The model is validated by real nutrient concentration profiles obtained on two estuaries under different climates, moderate climate (estuary of the Seine) and tropical dry climate (estuary of Somone, Senegal). The results highlight that the equilibration of the dialysis porewater sampler is not homogeneous over the full sediment height investigated. Other sediment characteristics as compaction, rate of bioturbation or bacterial density must be taken into account in order to find a well-calculated value of the equilibration time.  相似文献   

Spaxel analysis: probing the physics of star formation in ultraluminous infrared galaxies     

Michael A. Dopita  Jeffrey Rich  Frédéric P. A. Vogt  Lisa J. Kewley  I-Ting Ho  Hassan M. Basurah  Alaa Ali  Morsi A. Amer 《Astrophysics and Space Science》2014,350(2):741-754

This paper presents a detailed spectral pixel (spaxel) analysis of the ten Luminous Infrared Galaxies (LIRGs) previously observed with the Wide Field Spectrograph (WiFeS), an integral field spectrograph mounted on the ANU 2.3 m telescope, and for which an abundance gradient analysis has already been presented by Rich et al. (Astrophys. J., 753:5, 2012). Here we use the strong emission line analysis techniques developed by Dopita et al. (Astrophys. J. Suppl. Ser., accepted, 2013) to measure the ionisation parameter and the oxygen abundance in each spaxel. In addition, we use the observed Hα flux to determine the surface rate of star formation ( $\mathrm {M}_{\odot }{\rm yr}^{-1}$ kpc^?2) and use the [S II] λλ6717/6731 ratio to estimate the local pressure in the ionised plasma. We discuss the correlations discovered between these physical quantities, and use them to infer aspects of the physics of star formation in these extreme star forming environments. In particular, we find a correlation between the star formation rate and the inferred ionisation parameter. We examine the possible reasons for this correlation, and determine that the most likely explanation is that the more active star forming regions have a different distribution of molecular gas which favour higher ionisation parameters in the ionised plasma.  相似文献   

Archimedes spiral and the surface distribution of dark clouds in M31, III     

I. A. Issa 《Astrophysics and Space Science》1991,184(2):227-234

The surface distribution of dark clouds along the major and minor axes were compiled to give a general formula expressing the surface distribution along both axes simultaneously. Absorption values were determined, assuming the parameters of the standard cloud model as a function of the distance from the two-dimensional distribution of dark clouds. Iso-cloud line numbers were drawn as a function of bothX andY. Two knots appeared in the new distribution function. This may announce the beign of the spiral arms. The knots may indicate the least possible number of the dark clouds per kiloparsec beyond which spiral structure may be possible. The projected distance of the two knots on the X-axis may correspond to some spiral features found by other investigators.  相似文献   

Palynofacies and hydrocarbon generation potential of the upper Triassic Kurrachine Formation and lower part of the Baluti Formation, Mosul Block, Northwestern Iraq     

Thamer K. Al-Ameri  Qusay H. Al-Dolaimy  Amer Jassim Al-Khafaji 《Arabian Journal of Geosciences》2009,2(3):273-283

Three exploration wells were selected near Mosul city (Az-29, Bm-15, and Kd-1) to study the palynozones and hydrocarbon generation potential of the Upper Triassic Baluti and Kurrachine Formations. This study was completed in two phases: The first was a study of palynofacies and their paleoenvironmental indications, degree of preservation, diversity of palynomorphs, and organic maturity of the rocks according to palynomorphs’ color using a refracted light microscope. More than 80 slides of organic matter were used for this study. Four palynofacies were tentatively recognized. (1) The first palynofacies is diagnostic of the Baluti Formation in the Az-29 and Kd-1 wells; (2) The second palynofacies appeared at different depths in the Kurrachine Formation in three wells. (3) The third was only found between the depths of 4,534 to 4,685 m in the well Az-29. (4) The fourth was only found between 3,500- and 3590-m depth in the well Bm-15. A distal coastal marine environment is suggested for the Baluti Formation and restricted lagoonal environment for the Kurrachine Formation. The second phase used organic geochemical analyses to confirm the suggested paleoenvironmental and hydrocarbon generation material. Three techniques were used, namely total organic carbon, pyrolysis, and pyrolysis gas chromatography, on more than 35 samples from different depths in three wells. The analyses proved that a sufficient quantity of organic matter occurs that and has suitable maturity for hydrocarbon generation potential of oil and gas.  相似文献   

Disaster prevention,disaster preparedness and local community resilience within the context of disaster risk management in Cameroon     

Aka  Festus Tongwa  Buh  Gaston Wung  Fantong  Wilson Yatoh  Issa  Zouh  Isabella Tem  Djomou  Serges Laurent Bopda  Ghogomu  Richard Tanwi  Gibson  Terry  Marmol del  Mary-Ann  Sigha  Luc Nkamdjou  Ohba  Takeshi  Kusakabe  Minoru  Yoshida  Yutaka  Tanyileke  Gregory  Nnange  Joseph Metuk  Hell  Joseph Victor 《Natural Hazards》2017,87(1):57-81

This paper presents a simulation of three components of near-field ground shaking recorded during the main shock at three stations of the September 16, 1978, Tabas (M _w = 7.4), Iran, earthquake, close to the causative fault. A hybrid method composed of a discrete wavenumber method developed by Bouchon (Bouchon in Bull Seismol Soc Am 71:959–971, 1981; Cotton and Coutant in Geophys J Int 128:676–688, 1997) and a stochastic finite-fault modeling based on a dynamic corner frequency proposed by Motazedian and Atkinson (Bull Seismol Soc Am 95:995–1010, 2005), modified by Assatourians and Atkinson (Bull Seismol Soc Am 97:935–1949, 2007), is used for generating the seismograms at low (0.1–1.0 Hz) and high frequencies (1.0–20.0 Hz), respectively. The results are validated by comparing the simulated peak acceleration, peak velocity, peak displacement, Arias intensity, the integral of velocity squared, Fourier spectrum and acceleration response spectrum on a frequency-by-frequency basis, the shape of the normalized integrals of acceleration and velocity squared, and the cross-correlation with the observed time-series data. Each characteristic is compared on a scale from 0 to 10, with 10 being perfect agreement. Also, the results are validated by comparing the simulated ground motions with the modified Mercalli intensity observations reported by reconnaissance teams and showed reasonable agreement. The results of the present study imply that the damage distribution pattern of the 1978 Tabas earthquake can be explained by the source directivity effect.  相似文献   

Rate of seawater intrusion estimated by geophysical methods in an arid area: Al Khabourah, Oman     

Osman A. E. Abdalla  Mubarik Ali  Khalifa Al-Higgi  Hilal Al-Zidi  Issa El-Hussain  Said Al-Hinai 《Hydrogeology Journal》2010,18(6):1437-1445

Seawater intrusion and its spreading rate are the challenging problems in over-pumped coastal aquifers of arid zones like the Batinah region of Oman. The study delineates the saline plume, identifies saline/freshwater zones, and estimates the migration rate of the plume in the Al Khabourah area of the Batinah coast. Time domain electromagnetic surveys, aided by vertical electrical sounding surveys, and seismic refraction methods have defined the locus of the saline/freshwater interface in the area. The current (2007) interface position, when compared with that determined during 2002, indicates a prominent recession in the saline plume and suggests an average annual recession rate of 120 m. This recession may be attributed mainly to the recharging dam of Wadi Al Hawasinah, constructed in 1995, and the enforcement of new water resources legislation. This study reveals the shielding role of the recharging dam to counter advancing saline intrusion.  相似文献   

Sudan and the Nile Basin   总被引：1，自引：0，他引：1  

Osman El-Tom Hamad  Atta El-Battahani 《Aquatic Sciences - Research Across Boundaries》2005,67(1):28-41

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Application of GPS in Traffic Management Systems     

Ardeshir Faghri  Khaled Hamad 《GPS Solutions》2002,5(3):52-60

Integrated Traffic Management Systems (ITMS) need reliable, accurate, and real-time data. Travel time, speed, and delay are three of the most important factors used in ITMS for monitoring, quantifying, and controlling congestion. GPS has recently become available for civil applications. Because it provides real-time spatial and time measurements, it has an increasing use in conducting different transportation studies. This article presents the application of GPS in collecting travel time, speed, and delay information of 64 major roads in the state of Delaware. A comparative statistical analysis was performed on data collected by GPS, with data collected simultaneously by the conventional method. The GPS data proved to be at least as accurate as the data collected by the conventional method, and it was 50% more efficient in terms of manpower. Moreover, the sample-size requirement was determined to maintain 95% confidence level throughout the controlled test. Benefiting from the Geographic Information System's dynamic segmentation tool, our travel time, delay, and speed information were integrated with other relevant traffic data. This was presented graphically on the Internet for public use. Statistical trend analysis for the data collected in 1997, 1998, 1999, and 2000 are also presented and applications on the overall ITMS are discussed. ? 2002 Wiley Periodicals, Inc.  相似文献