Results 11 to 20 of about 110 (90)
Abstract Arc volcanoes, created by magma generated from the dehydration of subducting slabs, show great variability in their sizes and along‐arc spatial distributions. In this study, we address a fundamental question, namely, how do subduction zones and volcanic arcs respond to the subduction of “atypical” oceanic lithosphere.
Claudia Adam +3 more
wiley +1 more source
Comparison of measured and simulated pressure and temperature profiles in geothermal wells [PDF]
The correct application of geothermal wellbore flow simulators is a useful tool since their adequate calibration and use often avoids the need to perform costly experimental PTQ logs inside geothermal wells. Two existing wellbore flow simulators, GEOPOZO
E. González +3 more
doaj
Hot springs of the volcanic zones are characterized for having high sulfur content in the form of sulphate and other ions resulting from chemical reactions. Sources with these types of elements are of great interest for the tourism and geothermal industry because of their highlighted properties which include therapeutic treatments, relaxation baths ...
Darwin Augusto Torres-Ceron +3 more
wiley +1 more source
Variation of gaseous species concentration in the Los Azufres geothermal wells as a tool to study the reinjection effect [PDF]
Since 1982 the concentration of gaseous species (CO2, H2S, CH4, N2, H2, Ar, and He) has been monitored periodically in the Los Azufres geothermal field, Mich., Mexico by CFE.
M.C. Suárez +3 more
doaj
Pilot fruit drier for Los Azufres geothermal field, Michoacan, Mexico [PDF]
Comision Federal de Electricidad (CFE) has a Division in charge of the exploration of a geothermal reservoir located in Los Azufres, State of Michoacan. At present, CFE is only using the steam of the wells and rejecting the hot water that comes off associated with the steam.
openaire +4 more sources
Emission of some rare gases at the Los Azufres, Mexico, geothermal reservoir [PDF]
The chemistry of fluids in the Los Azufres, Mexico geothermal field originated from volcanic processes and is controlled by temperatures at depth, mineral solubility, pH values and mineral equilibrium.
Mario César Suárez Arriaga
doaj
Formation permeability at the feedzone of geothermal wells employing inflow type-curves [PDF]
Geothermal Inflow Performance Relationships (GIPR) may be used to estimate formation permeability, by overlapping the well inflow curve with different theoretical GIPR curves. This method does not require field measurement of the well inflow curve.
Alfonso García +3 more
doaj
Three-dimensional thermal sensitivity analysis of cooling of a magma chamber in the Los Azufres geothermal field, Michoacán, Mexico [PDF]
We present three-dimensional simulation of cooling of 63 models of a magma chamber in the Los Azufres geothermal field by varying the top of the chamber depth between 5 and 9 km (centroid from about 7 to 13 km) and its volume between 300 and 600 km3.
Verma, Surendra P, Gómez-Arias, Efraín
openaire +1 more source
Isotopes data help to understand the GW‐SW connectivity, the recharge elevations, and evaporation in a volcanic lake basin. ABSTRACT Understanding groundwater (GW) to surface water (SW) connectivity (i.e., the exchange of water and solutes between aquifers and surface bodies) is increasingly important under changing climate conditions, where ...
L. Ramírez‐González +9 more
wiley +1 more source
Groundwater Flow System and Hydrogeochemical Evolution in Central Mexico's Major Lakes
Conceptual model of groundwater flow paths within the Cuitzeo GFS. The inset shows a percentage distribution of flow path contributions.. ABSTRACT This study investigated the groundwater dynamics within the Cuitzeo groundwater flow system, an area encompassing central Mexico's second and third largest lakes.
Olea‐Olea Selene +11 more
wiley +1 more source

