Alireza Somarin

Dr. Alireza Somarin

Department of Geology, Brandon University, Brandon, MB R7A 6A9, Canada

Research Focus & Metrics

Academic Career Length

19Years (2008-Present)

(Calculated once Scilit publication data is synced: current year − year of first publication + 1)

Representative Publications

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10 June 2009 in Resource Geology
Verified
Journal Article
Open access
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ASAlireza Somarin
Alireza Somarin
SKStephen A. Kissin
Stephen A. Kissin
DHDonald D. Heerema
Donald D. Heerema
DBDaniel J. Bihari
Daniel J. Bihari
The Archean mafic–ultramafic complex of Lac des Iles, Ontario, Canada, hosts economic platinum group elements (PGE)‐Au‐Cu‐Ni mineralization in the Roby Zone. All lithologies in the North Roby Zone have been affected by hydrothermal alteration. The alteration products include talc (the most dominant mineral), anthophyllite, serpentine, actinolite, tremolite, chlorite, hornblende, zoisite, clinozoisite, epidote and sericite. In the altered rocks, light rare earth elements (La, Ce, Nd, Sm), Pb, Rb, Ba, Cs, S and possibly Y have been added by hydrothermal solution whereas Eu and heavy rare earth elements (Yb, Gd, Dy, Er) remained immobile. There are five types of fluid inclusions in the pegmatitic plagioclase with homogenization temperature and salinity ranging from 240°C to 445°C and 15.37 to 48.52 wt% equivalent NaCl, respectively. The δ18O and δD of talc range form 6.2‰ to 6.9‰ and −28‰ to −48‰, respectively. δ18O and δD water in equilibrium with talc during the hydrothermal alteration suggest a modified source for the hydrothermal solution. Microthermometry and stable isotope studies suggest that high temperature–high salinity fluid was diluted by, and mixed with, low temperature–low salinity meteoric solution. This mechanism precipitated the hydrothermal assemblage and redistributed trace elements during and after pegmatite formation in the North Ruby Zone.

25 November 2008 in International Journal of Earth Sciences
Verified
Journal Article
Closed access
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ASAlireza Somarin
Alireza Somarin

6 February 2016 in Minerals
Verified
Journal Article
Open access
PDF file
BTBatool Taghipour
Batool Taghipour
BTBatoul Taghipour
Batoul Taghipour
AZAlireza Zarasvandi
Alireza Zarasvandi
MBMichael Bird
Michael Bird
ASAlireza Somarin
Alireza Somarin
A new heterotrophic strain, named Providencia sp. JAT-1, was isolated and used in bioleaching of low-grade complex copper ore. The strain uses sodium citrate as a carbon source and urea as a nitrogen source to produce ammonia. The optimal growth condition of the strain is 30 C, initial pH 8, sodium citrate 10 g/L and urea 20 g/L, under which the cell density and ammonia concentration in the medium reached a maximum of 4.83 × 108 cells/mL and 14 g/L, respectively. Ammonia produced by the strain is used as the main lixiviant in bioleaching. Bioleaching results revealed that higher strain growth led to a higher copper recovery, while higher pulp density will cause a greater inhibitory effect on strain growth and ammonia production. The copper extraction reached the highest value of 54.5% at the pulp density of 1%. Malachite, chrysocolla and chalcocite are easy to leach out in this bioleaching system while chalcopyrite is difficult. Results of comparative leaching experiments show that bioleaching using JAT-1 is superior to ammonia leaching at the same condition. The metabolites produced by the strain other than ammonia are also involved in bioleaching.


18 March 2014 in Arabian Journal of Geosciences
Verified
Journal Article
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STSedigheh Taghipour
Sedigheh Taghipour
AKAli Kananian
Ali Kananian
MMMohammad Ali Mackizadeh
Mohammad Ali Mackizadeh
ASAlireza Somarin
Alireza Somarin