کد مقاله کد نشریه سال انتشار مقاله انگلیسی نسخه تمام متن
4700926 1637739 2007 11 صفحه PDF دانلود رایگان
عنوان انگلیسی مقاله ISI
Rate law for galena dissolution in acidic environment
موضوعات مرتبط
مهندسی و علوم پایه علوم زمین و سیارات ژئوشیمی و پترولوژی
پیش نمایش صفحه اول مقاله
Rate law for galena dissolution in acidic environment
چکیده انگلیسی

A dissolution rate law for galena in acidic environment was derived from the steady-state dissolution rates using flow-through experiments. The influence of temperature, dissolved oxygen concentration and pH between 1 and 3 was assessed. This rate law can be used for predicting galena dissolution behavior in a wide range of conditions analogous to Acid Rock Drainage.For pH below 2, the dissolution rate law can be expressed as:RGn,pH<2=10−5.7±0.4e−23±3RTaH+0.43±0.05where RGn is the galena dissolution rate (mol m− 2 s− 1), R is the gas constant (kJ mol− 1 K− 1) , T   is the temperature (K) and aH+aH+ is the activity of hydrogen ion in the solution.Galena dissolution rate law for pH between 2 and 3 can be expressed as:RGn,pH=2−3=10−8.5±0.4e−15±2RTaH+−0.78±0.04aO2(aq)0.30±0.03where aO2(aq)aO2(aq) is the activity of dissolved oxygen.XPS (X-ray Photoelectron Spectroscopy) examination of the reacted galena samples shows the formation of a lead-deficient and sulfur-rich surface layer, consistent with the observed non-stoichiometry between dissolved sulfur and lead in all the studied solutions.Based on the S/Pb ratio observed in solution and the reacted surfaces and the pH and dissolved oxygen dependence of the rates, two possible reactions for galena dissolution in acidic aqueous solution are proposed; (1) at pH ≤ 2 the rate seems to be determined by the protonation of surface sulfur atoms, and (2) at pH ≥ 2 the rate seems to be controlled by the attachment of oxygen to surface sulfur atoms.The values obtained for the activation energies (15 ± 2 kJ mol− 1 at pH 3 and 23 ± 3 kJ mol− 1 at pH 1) suggest that galena dissolution is controlled by diffusion processes or mixed-controlled by diffusion of reactants and products between the bulk solutions and the reacting surfaces.

ناشر
Database: Elsevier - ScienceDirect (ساینس دایرکت)
Journal: Chemical Geology - Volume 245, Issues 3–4, 15 November 2007, Pages 219–229
نویسندگان
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