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handle: 2445/18161
Un estudio de los diferentes complejos de azufre en las solucioneshidrotermales (S=, HS-, H,S, HSO, y SO; ) ha sido efectuado, considerando como variables lg fo PH, T y molalidad de la soluci6n de NaCl. Se observa que la zona de mayor concentración dentro de la solución de los complejos H2S y HSO; aumenta con la temperatura, a base de disminuir la zona de existencia del ión SO; . Los resultados obtenidos se comparan con algun ejemplo de yacimiento hidrotermal.
Mineralogia, Termodinàmica, Sofre, Alteració hidrotermal, Thermodynamics, Mineralogy, Sulfur, Hydrothermal alteration
Mineralogia, Termodinàmica, Sofre, Alteració hidrotermal, Thermodynamics, Mineralogy, Sulfur, Hydrothermal alteration
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