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Mohammad Ghannadi‐Maragheh

Nuclear Science and Technology Research Institute

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Meisam Torab‐Mostaedi

Atomic Energy Organization of Iran

Rezvan Torkaman

Nuclear Science and Technology Research Institute

Ali Akbar Salehi

Sharif University of Technology

Mehdi Asadollahzadeh

Atomic Energy Organization of Iran

Mohammad Hadi Moayed

Ferdowsi University of Mashhad

Samaneh Ziapour

Atomic Energy Organization of Iran

Saeid Setayeshi

Amirkabir University of Technology

K. Nazari

Islamic Azad University, Tehran

H. Khalafi

Atomic Energy Organization of Iran

Mohammad Yazdi

Shahid Beheshti University

Cooperative Institutions

Atomic Energy Organization of Iran

Nuclear Science and Technology Research Institute

University of Tehran

And Technology Research (United Kingdom)

Iran University of Science and Technology

Shahid Beheshti University

University of Isfahan

Amirkabir University of Technology

Sharif University of Technology

Islamic Azad University, Tehran

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Characterizations of strontium(II) and barium(II) adsorption from aqueous solutions using dolomite powder

Journal of Hazardous Materials (2011)

Ahad Ghaemi Meisam Torab‐Mostaedi Mohammad Ghannadi‐Maragheh

Langmuir adsorption model

Barium

Exothermic reaction

10.1016/j.jhazmat.2011.04.006

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Citations (257)

A review on the water-energy nexus for drinking water production from humid air

Renewable and Sustainable Energy Reviews (2019)

Ali Akbar Salehi Mohammad Ghannadi‐Maragheh Meisam Torab‐Mostaedi Rezvan Torkaman Mehdi Asadollahzadeh

Water-energy nexus

10.1016/j.rser.2019.109627

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Citations (158)

Investigation of efficient 131I production from natural uranium at Tehran research reactor

Annals of Nuclear Energy (2005)

H. Khalafi K. Nazari Mohammad Ghannadi‐Maragheh

Radioactive iodine

Natural uranium

10.1016/j.anucene.2004.12.008

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Citations (9)

Estimation of the radon concentration in soil related to the environmental parameters by a modified Adaline neural network

Applied Radiation and Isotopes (2003)

Ali Negarestani Saeid Setayeshi Mohammad Ghannadi‐Maragheh B. Akashe

10.1016/s0969-8043(02)00304-4

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Citations (37)

Preparation of a novel PAN–zeolite nanocomposite for removal of Cs+ and Sr2+ from aqueous solutions: Kinetic, equilibrium, and thermodynamic studies

Chemical Engineering Journal (2013)

Hossein Faghihian Mozhgan Iravani Mohammad Hadi Moayed Mohammad Ghannadi‐Maragheh

Thermogravimetric analysis

Endothermic process

Ammonium bromide

Nanocrystalline material

Ammonium hydroxide

10.1016/j.cej.2013.02.035

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Citations (107)

Formation and evolution of Th–REE mineralizing fluids at the Kiruna‐type Choghart iron oxide–apatite deposit, Central Iran: Insights from fluid inclusions and H‐C‐O isotopes

Geological Journal (2022)

Khalegh Khoshnoodi Mohammad Yazdi Mohammad Ghannadi‐Maragheh Samaneh Ziapour Saleh Deymar

The Choghart iron oxide–apatite (IOA) deposit is one of the largest iron mines of the Bafq district in Central Iran. This deposit is hosted by the Early Cambrian rhyolites, and diabase dikes crosscut both host rocks and the ore bodies. The Choghart rhyolites erupted in a continental arc setting, while the Choghart diabase dikes formed in a back‐arc basin environment. Thorite, minor titanite, and REE‐oxide are the main hosts of Th and REEs. The mineralogy and geochemistry support that the Th–REE mineralization formed at relatively reduced conditions. The presence of calcite accompanied by thorite and titanite suggests that Th and REE probably migrated as carbonate complexes in the mineralizing hydrothermal fluids. Microthermometric data of calcite associated with thorite indicate that the salinity of the ore‐forming fluids varies from 20 to 30 wt% NaCl equivalent with temperature estimates between 300 and 370°C. The narrow range of homogenization temperature and low salinities of the fluid inclusions imply the presence of only one fluid phase in the Th–REE mineralization. The calcite δ 13 C PDB (−3.9 to −4.1‰) and δ 18 O SMOW (6.6–7.0‰) support a magmatic source for the ore‐forming fluids. Actinolite δD (5.55–6.72‰) and δ 18 O (−100.8 to −82.4‰) also suggest a magmatic source of the ore‐forming fluids. Microthermometric data imply that fluid–rock interaction and cooling were critical factors triggering the thorite precipitation at Choghart IOA deposit. Stable isotopic data indicate that post‐magmatic fluids derived from rhyolitic magmas played a significant role in the Th–REE mineralization.

Titanite

Magmatic water

10.1002/gj.4399

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An overview of sustainable energy development by using cogeneration technology and opportunity for improving process

International Journal of Energy Research (2020)

Ali Akbar Salehi Mohammad Ghannadi‐Maragheh Meisam Torab‐Mostaedi Rezvan Torkaman Mehdi Asadollahzadeh

Cogeneration

Sustainable Energy

10.1002/er.5742

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Citations (12)