dor_id: 4133283

506.#.#.a: Público

590.#.#.d: Los artículos enviados a la revista "Geofísica Internacional", se juzgan por medio de un proceso de revisión por pares

510.0.#.a: Consejo Nacional de Ciencia y Tecnología (CONACyT); Scientific Electronic Library Online (SciELO); SCOPUS, Dialnet, Directory of Open Access Journals (DOAJ); Geobase

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650.#.4.x: Físico Matemáticas y Ciencias de la Tierra

336.#.#.b: article

336.#.#.3: Artículo de Investigación

336.#.#.a: Artículo

351.#.#.6: http://revistagi.geofisica.unam.mx/index.php/RGI

351.#.#.b: Geofísica Internacional

351.#.#.a: Artículos

harvesting_group: RevistasUNAM

270.1.#.p: Revistas UNAM. Dirección General de Publicaciones y Fomento Editorial, UNAM en revistas@unam.mx

590.#.#.c: Open Journal Systems (OJS)

270.#.#.d: MX

270.1.#.d: México

590.#.#.b: Concentrador

883.#.#.u: https://revistas.unam.mx/catalogo/

883.#.#.a: Revistas UNAM

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883.#.#.1: https://www.publicaciones.unam.mx/

883.#.#.q: Dirección General de Publicaciones y Fomento Editorial

850.#.#.a: Universidad Nacional Autónoma de México

856.4.0.u: http://revistagi.geofisica.unam.mx/index.php/RGI/article/view/652/655

100.1.#.a: García, A.; Ascencio, F.; Espinosa, G.; Santoyo, E.; Gutiérrez, H.; Arellano, V.

524.#.#.a: García, A., et al. (1999). Numerical modeling of high-temperature deep wells in the Cerro Prieto geothermal field, Mexico. Geofísica Internacional; Vol. 38 Núm. 4: Octubre 1, 1999; 251-260. Recuperado de https://repositorio.unam.mx/contenidos/4133283

245.1.0.a: Numerical modeling of high-temperature deep wells in the Cerro Prieto geothermal field, Mexico

502.#.#.c: Universidad Nacional Autónoma de México

561.1.#.a: Instituto de Geofísica, UNAM

264.#.0.c: 1999

264.#.1.c: 1999-10-01

653.#.#.a: pozos geotérmicos; simulación de flujo; perdidas de calor; zonas secundarias de alimentación; estimulación de pozos; inyección de gas; geothermal wells; flow simulation; heat losses; secondary feedzones; well stimulation; gas injection

506.1.#.a: La titularidad de los derechos patrimoniales de esta obra pertenece a las instituciones editoras. Su uso se rige por una licencia Creative Commons BY-NC-SA 4.0 Internacional, https://creativecommons.org/licenses/by-nc-sa/4.0/legalcode.es, para un uso diferente consultar al responsable jurídico del repositorio por medio del correo electrónico revistagi@igeofisica.unam.mx

884.#.#.k: http://revistagi.geofisica.unam.mx/index.php/RGI/article/view/652

001.#.#.#: 063.oai:revistagi.geofisica.unam.mx:article/652

041.#.7.h: spa

520.3.#.a: A numerical modeling study of three non-producing deep geothermal wells from Cerro Prieto is presented. We compute the expected production characteristics of these wells in order to determine if their inability to sustain flow was due to (i) heat loss effects in the well, (ii) the influence of production casing diameters, (iii) the transient heat loss during the first few days of well discharge, or (iv) the effect of secondary low-enthalpy inflows. A new version of the wellbore flow simulator called GEOPOZO v2.0 was developed to solve the equations of conservation of mass, mo- mentum and energy for steady or transient one- and two-phase flow in geothermal wells. It was found that all three wells should have sustained production. The early heat losses were so large that the wells need to be induced and they would only sustain flow after several days of induced discharge. For well M-202 the match between measured and computed temperature profiles for a secondary feedzone suggests that the inflow of colder waters was responsible for stopping the flow of this well.doi: https://doi.org/10.22201/igeof.00167169p.1999.38.4.507

773.1.#.t: Geofísica Internacional; Vol. 38 Núm. 4: Octubre 1, 1999; 251-260

773.1.#.o: http://revistagi.geofisica.unam.mx/index.php/RGI

022.#.#.a: ISSN-L: 2954-436X; ISSN impreso: 0016-7169

310.#.#.a: Trimestral

300.#.#.a: Páginas: 251-260

264.#.1.b: Instituto de Geofísica, UNAM

doi: https://doi.org/10.22201/igeof.00167169p.1999.38.4.507

handle: 5bc19fdc9a380fac

harvesting_date: 2023-06-20 16:00:00.0

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file_creator: A. García

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245.1.0.b: Numerical modeling of high-temperature deep wells in the Cerro Prieto geothermal field, Mexico

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Artículo

Numerical modeling of high-temperature deep wells in the Cerro Prieto geothermal field, Mexico

García, A.; Ascencio, F.; Espinosa, G.; Santoyo, E.; Gutiérrez, H.; Arellano, V.

Instituto de Geofísica, UNAM, publicado en Geofísica Internacional, y cosechado de Revistas UNAM

Licencia de uso

Procedencia del contenido

Entidad o dependencia
Instituto de Geofísica, UNAM
Revista
Repositorio
Contacto
Revistas UNAM. Dirección General de Publicaciones y Fomento Editorial, UNAM en revistas@unam.mx

Cita

García, A., et al. (1999). Numerical modeling of high-temperature deep wells in the Cerro Prieto geothermal field, Mexico. Geofísica Internacional; Vol. 38 Núm. 4: Octubre 1, 1999; 251-260. Recuperado de https://repositorio.unam.mx/contenidos/4133283

Descripción del recurso

Autor(es)
García, A.; Ascencio, F.; Espinosa, G.; Santoyo, E.; Gutiérrez, H.; Arellano, V.
Tipo
Artículo de Investigación
Área del conocimiento
Físico Matemáticas y Ciencias de la Tierra
Título
Numerical modeling of high-temperature deep wells in the Cerro Prieto geothermal field, Mexico
Fecha
1999-10-01
Resumen
A numerical modeling study of three non-producing deep geothermal wells from Cerro Prieto is presented. We compute the expected production characteristics of these wells in order to determine if their inability to sustain flow was due to (i) heat loss effects in the well, (ii) the influence of production casing diameters, (iii) the transient heat loss during the first few days of well discharge, or (iv) the effect of secondary low-enthalpy inflows. A new version of the wellbore flow simulator called GEOPOZO v2.0 was developed to solve the equations of conservation of mass, mo- mentum and energy for steady or transient one- and two-phase flow in geothermal wells. It was found that all three wells should have sustained production. The early heat losses were so large that the wells need to be induced and they would only sustain flow after several days of induced discharge. For well M-202 the match between measured and computed temperature profiles for a secondary feedzone suggests that the inflow of colder waters was responsible for stopping the flow of this well.doi: https://doi.org/10.22201/igeof.00167169p.1999.38.4.507
Tema
pozos geotérmicos; simulación de flujo; perdidas de calor; zonas secundarias de alimentación; estimulación de pozos; inyección de gas; geothermal wells; flow simulation; heat losses; secondary feedzones; well stimulation; gas injection
Idioma
spa
ISSN
ISSN-L: 2954-436X; ISSN impreso: 0016-7169

Enlaces