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Open Journal of Geology 2024年第4期14卷 569-577页

作者： Elias Salameh hani khoury Department of Geology University of Jordan Amman Jordan

Geode, boudinage, and undulation structures are widely distributed in the siliceous beds of the Upper Cretaceous/Tertiary rocks in Jordan. Their formation was attributed to tectonic forces, syngenetic processes, organic disintegration processes, subaquatic gliding, compaction and settlement, and meteoritic impacts. In this work, the structural features in the siliceous beds of Jordan are attributed to an interplay of load and directed pressures, and mineralogical transformation processes (opal-A to opal-CT to quartz), governed by pH changes. Tectonic directed pressure was acting in an ESE-WSW direction and is common in the silicified limestone of Upper Cretaceous.

关键词： Undulations Geodes Boudinages Opal-A Porcelanite Chert Transformations pH Changes Stress Fields Jordan

Removal of Pb(II) from Aqueous Solutions by Zeolites, Porcelanite and Sands: Correlation of Morphology and Chemical Composition to Batch Removal Efficiency

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American Journal of Analytical Chemistry 2015年第4期6卷 297-304页

作者： Fawwaz Jumean Lucia Pappalardo hani khoury Department of Biology Chemistry and Environmental Sciences American University of Sharjah Sharjah United Arab Emirates Department of Geology The University of Jordan Amman Jordan

Chemical compositions of natural zeolites, porcelanite (opal-CT) and local sands were determined by X-ray fluorescence (XRF) and correlated with their Pb(II) removal efficiencies. Zeolites and porcelanite were from the Mikawer, Aritain and Hannon areas in Jordan. Sands (white, red and yellow) were from the United Arab Emirates (UAE). The effect of Pb(II) concentration and zeolite dosage on removal efficiency was investigated at 25.0°C using the batch equilibrium method. Commercial kaolinite, silica and alumina were also studied for comparison. Removal efficiencies, in mg Pb(II)/g adsorbent, were: 76.9, 52.7 and 42.1 for Hannon, Mikawer and Aritain zeolites, respectively;58.2 for porcelanite;29.7, 11.0 and 8.5 for yellow, red and white sand, respectively;7.2, 3.3 and 1.3 for kaolinite, silica and alumina, respectively. XRF data indicate that adsorbents with intermediate molar ratios of Si/Al, in the range 2.70 - 2.93, are most efficient in Pb(II) removal. Scanning electron microscope (SEM) images of adsorbents suggest that morphology, in addition to chemical composition, plays a key role. In particular, a combination of factors, including shapes and sizes of crystals, channels in zeolites and pores in porcelanite, appear to favor removal of Pb(II).

关键词： Zeolites Sands XRF SEM Pb(II) Removal

Synthesis of Electroconducting Hydroxy-Sodalite/Graphite Composite: Preparation and Characterization

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Advances in Materials Physics and Chemistry 2019年第3期9卷 25-36页

作者： Rima Alomari Muayed Esaifan Mohammed Khair Hourani Hiba Al Amayreh Mohammed Amayreh hani khoury Department of Chemistry The University of Jordan Amman Jordan Department of Chemistry Faculty of Arts and Sciences University of Petra Amman Jordan Department of Physics and Basic Science Faculty of Engineering Technology Al-Balqa Applied University Amman Jordan Department of Geology The University of Jordan Amman Jordan

Electroconductive hydroxy-sodalite/graphite composites were synthesized by alkali-activation of kaolinite in the presence of sodium hydroxide as the alkali activator and graphite as a conductive filler. Thermal, morphological and microstructural properties in addition to direct current (D.C.) conductivity of the prepared composites were investigated. Thermogravimetric analysis (TGA), Fourier transform infrared spectroscopy in the attenuated total reflection mode (FTIR/ATR), X-ray diffraction (XRD), scanning electron microscope/energy dispersive using X-ray analysis (SEM/EDX) and DC conductivity measurements were used to characterize the prepared composites. The effect of the hydroxyl-sodalite-to-graphite and NaOH-to-kaolinite ratios on the electrical conductivity was investigated and evaluated on the generated composite specimens made of Jordanian kaolinite or pure kaolinite. It was demonstrated that increasing the mass ratio of graphite-to-kaolinite in the clay-based composites increased the electrical conductivity of the resultant composites. It was also observed that using 1:1 graphite-to-pure kaolinite mass ratio showed the best electrical conductivity value of 3 × 10-3 s/cm, among the other mass ratios used for pure kaolinite specimens, while using 1:1 mass ratio of graphite-to-Jordanian kaolinite showed a conductivity of 1.6 s/cm.

关键词： Kaolinite Graphite Composite Inorganic Polymers Electroconductive Composites

Dolomitization in Campanian Oil Shale Rocks from South-Western Jordan

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Open Journal of Geology 2015年第10期5卷 689-700页

作者： hani M. Alnawafleh Khalid E. Tarawneh hani N. khoury Nafeth A. Abdelhadi Osama Y. Shakkoury Reyad A. Dwairi Mazen N. Amaireh Faculty of Engineering Al-Hussein Bin Talal University Ma’an Jordan Faculty of Engineering Isra University Amman Jordan Department of Geology The University of Jordan Amman Jordan Faculty of Engineering Technology Al Balqa Applied University Salt Jordan Natural Resources Authority Amman Jordan Faculty of Engineering Tafila Technical University Tafila Jordan

This work represents the first detailed study of an oil shale (OS) section from the Upper Campanian Amman Silicified Limestone (ASL) Formation in south-western part of Jordan. More than five meters of oil shale have been recorded. Using the petrography and geochemistry, this study aims to focus on such non-conventional types of oil shale rocks in Jordan and to shed some light on their composition and formational environment. Unlike oil shale from Maastrichtian to early Tertiary, this type of oil shale is highly dolomitized. The dolomite is diagenetic in origin. This oil shale type contains considerable amount of OM and remarkably enriched in some trace elements and shows quite low sulfur content. Results suggest that the formation of dolomite appears to be limited by the rate of organic matter oxidation.

关键词： Jordan Oil Shale Dolomitization Campanian