From the pore scale to the lab scale: 3-D lab experiment and numerical simulation of drainage in heterogeneous porous media     

A. Papafotiou  R. Helmig  J. Schaap  P. Lehmann  A. Kaestner  H. Flühler  I. Neuweiler  R. Hassanein  B. Ahrenholz  J. Tölke  A. Peters  W. Durner 《Advances in water resources》2008

A well-controlled 3-D experiment with pre-defined block heterogeneities is conducted, where neutron tomography is used to map 3-D water distribution after two successive drainage steps. The material and hydraulic properties of the two sands are first measured in the laboratory with multistep outflow experiments. Additionally, the pore structure of the sands is acquired by means of image analysis of synchrotron tomography data and the structure is used for pore-scale simulation of one- and two-phase flow with Lattice-Boltzmann methods. This gives us another set of material and hydraulic parameters of the sands. The two sets of hydraulic properties (from the lab scale and from the pore scale) are then used in numerical simulations of the 3-D experiment.  相似文献   

Spectral classification of Be stars     

M. A. Hamdy  M. S. Abo Elazm  S. M. Somaya 《Astrophysics and Space Science》1990,167(1):167-169

In the course of observations of the LMC with the Glazar space telescope it was found that the star HD 269665 is unusually bright at 1640 A:m ₁₆₄₀ = 5 _. ^m ± 0 _. ^m 1,m ₁₆₄₀ –V = –6 _. ^m 2.  相似文献   

Genesis of secondary uranium minerals associated with jasperoid veins,El Erediya area,Eastern Desert,Egypt     

Hamdy H. Abd El-Naby 《Mineralium Deposita》2008,43(8):933-944

Uranium mineralization in the El Erediya area, Egyptian Eastern Desert, has been affected by both high temperature and low temperature fluids. Mineralization is structurally controlled and is associated with jasperoid veins that are hosted by a granitic pluton. This granite exhibits extensive alteration, including silicification, argillization, sericitization, chloritization, carbonatization, and hematization. The primary uranium mineral is pitchblende, whereas uranpyrochlore, uranophane, kasolite, and an unidentified hydrated uranium niobate mineral are the most abundant secondary uranium minerals. Uranpyrochlore and the unidentified hydrated uranium niobate mineral are interpreted as alteration products of petscheckite. The chemical formula of the uranpyrochlore based upon the Electron Probe Micro Analyzer (EPMA) is . It is characterized by a relatively high Zr content (average ZrO₂ = 6.6 wt%). The average composition of the unidentified hydrated uranium niobate mineral is , where U and Nb represent the dominant cations in the U and Nb site, respectively. Uranophane is the dominant U⁶⁺ silicate phase in oxidized zones of the jasperoid veins. Kasolite is less abundant than uranophane and contains major U, Pb, and Si but only minor Ca, Fe, P, and Zr. A two-stage metallogenetic model is proposed for the alteration processes and uranium mineralization at El Erediya. The primary uranium minerals were formed during the first stage of the hydrothermal activity that formed jasperoid veins in El Eradiya granite (130–160 Ma). This stage is related to the Late Jurassic–Early Cretaceous phase of the final Pan-African tectono-thermal event in Egypt. After initial formation of El Erediya jasperoid veins, a late stage of hydrothermal alteration includes argillization, dissolution of iron-bearing sulfide minerals, formation of iron-oxy hydroxides, and corrosion of primary uranium minerals, resulting in enrichment of U, Ca, Pb, Zr, and Si. During this stage, petscheckite was altered to uranpyrochlore and oxy-petscheckite. Uranium was likely transported as uranyl carbonate and uranyl fluoride complexes. With change of temperature and pH, these complexes became unstable and combined with silica, calcium, and lead to form uranophane and kasolite. Finally, at a later stage of low-temperature supergene alteration, oxy-petscheckite was altered to an unidentified hydrated uranium niobate mineral by removal of Fe.  相似文献   

Monazite chemistry: evidence for a prehistoric journey     

Yehia H. Dawood  Hamdy H. Abd El‐Naby 《Geology Today》2008,24(6):216-222

The chemistry of monazite from the black sand deposits of northern Sinai beach suggests that pegmatites and granites of the Eastern Desert of Egypt are the most likely source rocks. The floods associated with the pluvial periods prevailed in Egypt during the Pleistocene were able to erode the source rocks and liberate heavy minerals including monazite. The mineral grains were moved through several wadis and tributaries to the River Nile. At the confluence sites, these heavy minerals were mixed with the Ethiopian and central African heavy mineral assemblages. The grains continued to move together downriver until being deposited in their current locations.  相似文献   

Spectrophotometric studies of star HD 157978     

M. A. Hamdy  S. Abou Elazm 《Astrophysics and Space Science》1983,94(1):1-3

Examination of the stellar spectrum of this star reveals that it has a composite spectrum. It could be classified as (A7V+G5V). It contains three forbidden [Feii] lines which are of the essential features of η Carinae stars. The spectrum also contains H, Hei, Feii, Mni, Tiii, and other different lines. The K-line seems to be sharp double line while other lines appear single ones which suggest early component may be double. This also seems to be true according to radial velocity measurements.  相似文献   

Novel applications of fluid inclusions and isotope geochemistry in unravelling the genesis of fossil travertine systems   总被引：1，自引：0，他引：1       下载免费PDF全文

Hamdy El Desouky  Jeroen Soete  Hannes Claes  Mehmet Özkul  Frank Vanhaecke  Rudy Swennen 《Sedimentology》2015,62(1):27-56

The Denizli Basin is a fault‐bounded Neogene–Quaternary depression located in the Western Anatolian Extensional Province, Western Turkey. The basin is a unique geological site with abundant active and fossil (Quaternary) travertine and tufa deposits. Fluid inclusion microthermometry and isotopic analysis were applied to study the genesis of the Ball?k fossil travertine deposits, located in the south‐eastern part of the basin. Microthermometry on fluid inclusions indicates that the main travertine precipitating and cementing fluids are characterized by low salinity (<0·7 wt% NaCl equivalent) and variable temperatures that cluster at <50°C and ca 100°C. Fluids of meteoric origin have been heated by migration to the deeper subsurface, possibly in a local high geothermal gradient setting. A later uncommon cementation phase is related to a fluid with a significantly higher salinity (25·5 to 26·0 wt% bulk). The fluid obtained its salinity by interaction with Late Triassic evaporite layers. Strontium isotopes indicate that the parent carbonate source rock of the different travertine precipitates is very likely to be the Triassic limestone of the Lycian Nappes. Carbon isotopes suggest that the parent CO₂ gas originated from thermal decarbonation of the Lycian limestones with minor contributions of magmatic degassing and organic soil CO₂. Oxygen isotopes confirm the meteoric origin of the fluids and indicate disequilibrium precipitation because of evaporation and degassing. Results were integrated within the available geological data of the Denizli Basin in a generalized travertine precipitation model, which enhanced the understanding of fossil travertine systems. The study highlights the novel application of fluid inclusion research in unravelling the genesis of continental carbonates and provides several recommendations for hydrocarbon exploration in travertine‐bearing sedimentary basins. The findings suggest that travertine bodies and their parent carbonate source rocks have the potential to constitute interesting subsurface hydrocarbon reservoirs.  相似文献   

Testing the validity of detrital zircon chemistry as a provenance indicator     

Hamdy H. Abd El-Naby  Yehia H. Dawood 《Arabian Journal of Geosciences》2014,7(1):341-353

Zircon grains from the Nile Delta beach sediments were mineralogically investigated for their provenance perspective. Electron microprobe backscattered electron images, and wavelength dispersive spectroscopy line scans showed well-developed oscillatory and sector zoning in the majority of the studied zircon grains. In addition, some grains showed inclusions represented mainly by apatite. The zoning in zircon reflects compositional variations of Zr, Si, Hf, P, Y, and rare earth elements (REE). Based on the electron probe microanalyzer data, the calculated formula of the studied detrital zircon is ^A(Zr_3.82Hf_0.05Th_0.003Ca_0.10Fe_0.008REE_0.033Tl_0.03Y_0.001)∑_4.04 ^T(Si_3.90P_0.08Al_0.011V_0.003Sc_0.004)∑_4.00O₄. Th, Y, P, Sc, and Fe are substituted into zircon either by simple or coupled substitution mechanisms. Additional zircon grains separated from Abu Swayel granites and metamorphic gneisses, south Eastern Desert of Egypt were similarly investigated for comparison. Although evidence based on morphological characteristics, zoning, apatite inclusions, and mineral chemistry supports a derivation of zircon from granitic rocks including the hydrothermally altered varieties, the possibility that the zircon grains may have more than one source cannot be ruled out due to the large area of the Nile watershed.  相似文献   

Quaternary coral reefs of the Red Sea coast, Egypt: diagenetic sequence, isotopes and trace metals contamination   总被引：1，自引：1，他引：0  

Abdelbaset S. El-Sorogy  Hamdy Nour  Emad Essa  Mohamed Tawfik 《Arabian Journal of Geosciences》2013,6(12):4981-4991

This study focuses on the diagenetic sequence under marine and meteoric conditions as well as isotopes and trace metals contamination in Quseir and Gebel Zeit areas along the Egyptian Red Sea coast through a series of modern and fossil corals, Porites lutea and Favites pentagona. The diagenetic sequence begins with deposition of thin fringes of syntaxial aragonite and micritic high-magnesian calcite in the modern corals to completely altered Porites and partially altered Favites to low-magnesium calcite in the oldest Pleistocene unit. Average δ¹⁸O and δ¹³C values of Pleistocene corals in the two studied areas were lower than those of modern corals. Values of modern corals and lower fossil unit indicated coralline limestone, while those of middle and upper fossil units indicated fresh water influences. Average values of trace metals in modern corals were higher than those of Pleistocene counterpart except for Mn. Modern coral samples recorded enrichment in the average values of Pb, Zn, and Mn at Quseir area and enrichment in Co, Cu, and Ni at Gebel Zeit area. This may be attributed mostly to different tourist activities, landfill due to increase urbanization and nearby of Quseir area from the old phosphate harbor at El Hamrawin area, as well as oil exploration and production activities in the Gulf of Suez area. Also, results indicated that most samples of Porites have high concentration of trace metals than in Favites, especially in Cu, Zn, Mn, and Pb. This may due to high amounts of intergranular porosity and high total surface area of Porites in contrast to Favites.  相似文献   

Aeromagnetic data analysis to enhance the demonstration of the subsurface mineralized zone occurrences, As-Safra prospect area, Saudi Arabia     

Mansour A. Al-Garni  Hamdy I. E. Hassanein 《Arabian Journal of Geosciences》2012,5(2):313-326

The aeromagnetic survey was conducted by the French organization, BRGM in 1966, where As-Safra prospect area at the east of Al-Madinah city was included. The aeromagnetic data were then interpreted for potential occurrences of mineralization zones along with their extensions. Spectral analysis, using Filon Fourier transform, was implemented to extract the residual anomalies that can be attributed to mineralization zones. In this study, analytic signal, normalized standard deviation (NSTD), and 3D Euler deconvolution filters were used to enhance the demonstration of subsurface mineralized zones occurrences. Analytic signal and NSTD filters showed that the studied area is dominated by three main trends controlling the occurrences of mineralized zones, NNW-SSE, N-S, and E-W to ENE-WSW. On the other hand, 3D Euler deconvolution filter showed that the dominant structures are mostly the magnetic contacts, and their depths vary between 118 and 355?m.  相似文献   

Saudi Arabian White Silica as a Good Adsorbent for Pollutants          下载免费PDF全文

Islam Hamdy Abd El Maksod  Hassan M. AlBishri  Abdullah Saad Al‐bogami 《洁净——土壤、空气、水》2014,42(4):480-486

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