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Título del libro: 10aiche - 2010 Aiche Spring Meeting And 6th Global Congress On Process Safety
Título del capítulo: Physical-chemical model of the Los Humeros geothermal field, México

Autores UNAM:
EDUARDO GONZALEZ PARTIDA;
Autores externos:

Idioma:

Año de publicación:
2010
Palabras clave:

Reaching geochemical equilibrium; Vapor dominated


Resumen:

Departing of updated information of chemical composition of the download fluids of a wells section (H-012, H-015, H-016, H-017, H-019, H-039) of the Los Humeros geothermal reservoir, Puebla, Mexico, the anions, cations, and gases graphics proposed by Giggenbach (1988) and Giggenbach and Goguel, (1989) were discussed. In the reservoir, two types of fluids (or two reservoirs), existed: meteoric waters and fluids of magmatic origin. The geothermal deposit was not in a state of chemical equilibrium between the fluids and minerals, but these fluids and minerals were in process of reaching such state of geochemical equilibrium. This is an abstract of a paper presented at the AIChE Ethylene Producers Conference (San Antonio, TX 3/21-25/2010).


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