dor_id: 4133047

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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)

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

883.#.#.a: Revistas UNAM

590.#.#.a: Coordinación de Difusión Cultural

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/1216/1150

100.1.#.a: Rudolph, D.L.; Herrera, I.; Yates, R.

524.#.#.a: Rudolph, D.L., et al. (1989). Groundwater flow and solute transport in the industrial well fields of the Texcoco saline aquifer system near Mexico City. Geofísica Internacional; Vol. 28 Núm. 2: Abril 1, 1989; 363-408. Recuperado de https://repositorio.unam.mx/contenidos/4133047

245.1.0.a: Groundwater flow and solute transport in the industrial well fields of the Texcoco saline aquifer system near Mexico City

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

561.1.#.a: Instituto de Geofísica, UNAM

264.#.0.c: 1989

264.#.1.c: 1989-04-01

653.#.#.a: Agua subterránea; Flujo; Transporte; Solutos; Pozos industriales; Sistema acuífero; Texcoco; México; Groundwater; Flow; Transport; Solutes; Industrial wells; Aquifer system

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/1216

001.#.#.#: 063.oai:revistagi.geofisica.unam.mx:article/1216

041.#.7.h: spa

520.3.#.a: The hydraulic behavior of the Texcoco saline aquifer system near Mexico City is investigated through the evaluation of historical data, field studies, and numerical analysis of groundwater flow and solute transport within a large well field which is extracting the saline water for industrial purposes. The two thin aquifers under production in this area are bounded by highly compressible aquitards which supply tremendous volumes of water to the aquifers through leakage. A quasi three-dimensional integrodifferential equation scheme is used for the Flow modelling and is solved numerically with a triangular finite element scheme. The solute mass transport model is based on the method of characteristics combined with a particle tracking scheme. The models are accurately calibrated to piezometric field measurements and concentration distribution data from the production wells. Piezometric nests installed in the surficial cJay aquitard indicate that in the heavily pumped areas, infiltrating rainfall is diJuting the pore water concentrations in the aquitard which may account for declining concentrations in the production wells which have been recently observed. Analysis of the field data also indica tes that the surficíal aquitard is fractured and that the fracture network may play an important role in the movement of solutes in the aquitard. The models are currently being used to investigate alternative management strategies to optimize production from the industrial well field.doi: https://doi.org/10.22201/igeof.00167169p.1989.28.2.1035

773.1.#.t: Geofísica Internacional; Vol. 28 Núm. 2: Abril 1, 1989; 363-408

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: 363-408

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

doi: https://doi.org/10.22201/igeof.00167169p.1989.28.2.1035

handle: 00ba24a5a28f6442

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

856.#.0.q: application/pdf

file_creation_date: 2008-05-22 17:13:27.0

file_modification_date: 2022-07-19 14:14:03.0

file_creator: D. L. Rudolph

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245.1.0.b: Groundwater flow and solute transport in the industrial well fields of the Texcoco saline aquifer system near Mexico City

last_modified: 2023-06-20 16:00:00

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Artículo

Groundwater flow and solute transport in the industrial well fields of the Texcoco saline aquifer system near Mexico City

Rudolph, D.L.; Herrera, I.; Yates, R.

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

Rudolph, D.L., et al. (1989). Groundwater flow and solute transport in the industrial well fields of the Texcoco saline aquifer system near Mexico City. Geofísica Internacional; Vol. 28 Núm. 2: Abril 1, 1989; 363-408. Recuperado de https://repositorio.unam.mx/contenidos/4133047

Descripción del recurso

Autor(es)
Rudolph, D.L.; Herrera, I.; Yates, R.
Tipo
Artículo de Investigación
Área del conocimiento
Físico Matemáticas y Ciencias de la Tierra
Título
Groundwater flow and solute transport in the industrial well fields of the Texcoco saline aquifer system near Mexico City
Fecha
1989-04-01
Resumen
The hydraulic behavior of the Texcoco saline aquifer system near Mexico City is investigated through the evaluation of historical data, field studies, and numerical analysis of groundwater flow and solute transport within a large well field which is extracting the saline water for industrial purposes. The two thin aquifers under production in this area are bounded by highly compressible aquitards which supply tremendous volumes of water to the aquifers through leakage. A quasi three-dimensional integrodifferential equation scheme is used for the Flow modelling and is solved numerically with a triangular finite element scheme. The solute mass transport model is based on the method of characteristics combined with a particle tracking scheme. The models are accurately calibrated to piezometric field measurements and concentration distribution data from the production wells. Piezometric nests installed in the surficial cJay aquitard indicate that in the heavily pumped areas, infiltrating rainfall is diJuting the pore water concentrations in the aquitard which may account for declining concentrations in the production wells which have been recently observed. Analysis of the field data also indica tes that the surficíal aquitard is fractured and that the fracture network may play an important role in the movement of solutes in the aquitard. The models are currently being used to investigate alternative management strategies to optimize production from the industrial well field.doi: https://doi.org/10.22201/igeof.00167169p.1989.28.2.1035
Tema
Agua subterránea; Flujo; Transporte; Solutos; Pozos industriales; Sistema acuífero; Texcoco; México; Groundwater; Flow; Transport; Solutes; Industrial wells; Aquifer system
Idioma
spa
ISSN
ISSN-L: 2954-436X; ISSN impreso: 0016-7169

Enlaces