Show simple item record Jerz J.K. Rimstidt J.D. 2022-03-23T07:44:07Z 2022-03-23T07:44:07Z 2004
dc.identifier.citation Geochimica et Cosmochimica Acta, 2004, 68, 4, 701-714
dc.identifier.issn 0016-7037
dc.description.abstract The rate of pyrite oxidation in moist air was determined by measuring, over time, the pressure difference between a sealed chamber containing pyrite plus oxygen and a control. The experiments carried out at 25°C, 96.7% fixed relative humidity, and oxygen partial pressures of 0.21, 0.61, and 1.00 atm showed that the rate of oxygen consumption is a function of oxygen partial pressure and time. The rates of oxygen consumption (r, mol/m2sec) fit the expression (A) where P is the partial pressure of oxygen (atm) and t is time (sec). It appears that the rate slows with time because a thin layer of ferrous sulfate + sulfuric acid solution grows on the pyrite and retards oxygen transport to the pyrite surface. At very short reaction times, the rate of pyrite oxidation in air is slightly faster than the aqueous oxidation rate at the same oxygen partial pressure and temperature. At greater extents of reaction, the rate slows significantly and approaches the rates reported by humidity cell studies. This slower rate of oxidation in air appears to be more appropriate than the aqueous oxidation rate for modeling pyrite oxidation in unsaturated waste piles. At relative humidity less than 95%, a solid ferrous sulfate phase (melanterite or szolmonokite) becomes saturated and will precipitate from the ferrous sulfate + sulfuric acid solution in cracks and on the pyrite surface. These solids have the potential to wedge apart the sample leading to physical disaggregation of the pyrite as is often seen in museum samples.
dc.subject pyrite
dc.type Статья

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