Browsing Recursos geotérmicos en México by Title
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Laboratory and downhole corrosion measurements at Cerro Prieto geothermal wells.
Along with scaling, it is believed that corrosion was a prominent cause of failure in Cerro Prieto Geothermal Wells, leading to short lives or costly repairs and diminished production. To study the problem, an electrochemistry ... -
Laboratory and downhole corrosion measurements at Cerro Prieto Geothermal Wells.
Along with scaling, it is believed that corrosion is a prominent cause of failure in Cerro Prieto Geothermal Wells, leading to short lives or costly repairs and diminished productions. To study the problem, an electrochemistry ... -
Laboratory work on the response of reservoir rocks from the Los Humeros geothermal field, Puebla, Mexico, with acid solutions
Rock matrix stimulation is a methodology used to enhance well productivity in oil systems. Some years ago this methodology began to be applied in geothermal systems. In order to investigate the behavior of altered volcanic ... -
Land subsidence in the Cerro Prieto Geothermal Field, Baja California, Mexico, from 1994 to 2005. An integrated analysis of DInSAR, leveling and geological data
Cerro Prieto is the oldest and largest Mexican geothermal field in operation and has been producing electricity since 1973. The large amount of geothermal fluids extracted to supply steam to the power plants has resulted ... -
Late Pleistocene ignimbrites at Los Azufres volcanic center, Mexico. Implications for the present magmatic cycle
Since Lower Pleistocene, the Los Azufres volcanic center alternates the emission of acidic and basic matgmas. Considering this long history, the 'cyclic' pattern of the magamatic phases and the recent age of the last ... -
LBL resistivity studies at Cerro Prieto
In a joint venture, the LBL and CFE have undertaken a series of de resistivity studies at the Cerro Prieto geothermal field. In the present study dipole-dipole resistivity data have been collected and two-dimensional ... -
Le système hydrothermal actuel de Los Humeros (Mexique): Etat du système SO-- 4-SH2 à 300°C, origine du soufre et phénomènes d'oxydation associés à l'ébullition du fluide ascendant
In the geothermal system of Los Humeros, hydrothermal fluids are low in sulfur (7.7 mM/kg) and are slightly alkaline (pH of ca. 8.5) at depth. Nevertheless, the aqueous sulfate-sulfide species are in isotopic and chemical ...