Speciation of Arsenic in Medium Containing Bacterial Strains of <i>Lysinibacillus boronitolerans</i> and <i>Bacillus cereus</i>: Mechanism of Arsenic Removal. [PDF]
Aguilar NC +8 more
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Geochemical Assessment of Sediment Heavy Metal(loid) Concentrations in Lofa County, Northwestern Liberia: A Comparative Analysis of Average Shale and Upper Continental Crust Background Values. [PDF]
Sow HM +6 more
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Speciation Characterization and Environmental Stability of Arsenic in Arsenic-Containing Copper Slag Tailing. [PDF]
You M, Hu Y, Zhou C, Liu G.
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Legacy effects of historical gold mining on floodplains of an Australian river. [PDF]
Colombi F +10 more
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Genesis of the hydrothermal gold system in the kibaran metallogenic province (D.R.Congo): A review for the Twangiza-Namoya gold belt. [PDF]
Heritier RN +4 more
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Pollution of water bodies and related impacts on aquatic ecosystems and ecosystem services: The case of Ghana's booming 'galamsey' industry. [PDF]
Bedu-Addo K +3 more
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Abiotic and biotic-controlled nanomaterial formation pathways within the Earth's nanomaterial cycle. [PDF]
Schindler M, Xu J, Hochella MF.
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Arsenopyrite (FeAsS) is the most common As-bearing sulfide mineral. Under oxidising conditions, such as those in mine waste systems, it breaks down to release acids of As and S into the environment, resulting in acid mine drainage with high concentrations of dissolved As.
Corkhill, C. L., Vaughan, D. J.
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Oxidation of arsenopyrite (FeAsS) in acid Part I: Reactivity of arsenopyrite
Journal of Applied Electrochemistry, 1996The oxidation reactivity of arsenopyrite FeAsS in dilute acid determines the recovery of gold from arsenopyritic gold ores by slurry electrolysis. Stoichiometric,sulfur- and arsenic- deficient arsenopyrite have practically the same oxidation rate. Arsenopyrite is covered with a metal deficient sulfide layer which appears to determine the restpotential ...
P. G. Fernandez +2 more
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Thermodynamics of roasting arsenopyrite
Metallurgical Transactions B, 1983Existing thermodynamic data for the Fe-As-S-0 system were evaluted and predominance area diagrams for that system were constructed at 798 and 973 K. Isopleths for the As/S and As/O atomic ratios in the vapor phase have been added to the diagrams by solving the complex equilibria.
N. Chakraborti, D. C. Lynch
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