dor_id: 4132504

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

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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/650/1171

100.1.#.a: Steinich, Birgit; Simón, Isabel; Chavarría, J. Andrés; Marín, Luis E.

524.#.#.a: Steinich, Birgit, et al. (1997). Geophysical investigations of the vadose zone in the Valley of Hermosillo aquifer, Sonora, Mexico. Geofísica Internacional; Vol. 36 Núm. 3: Julio 1, 1997; 191-200. Recuperado de https://repositorio.unam.mx/contenidos/4132504

245.1.0.a: Geophysical investigations of the vadose zone in the Valley of Hermosillo aquifer, Sonora, Mexico

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

561.1.#.a: Instituto de Geofísica, UNAM

264.#.0.c: 1997

264.#.1.c: 1997-07-01

653.#.#.a: Valle de Hermosillo; zona vadosa; sondeos de resistividad; salinización del suelo; Valley of Hermosillo; vadose zone; resistivity measurements; salinisation of the soil

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/650

001.#.#.#: 063.oai:revistagi.geofisica.unam.mx:article/650

041.#.7.h: spa

520.3.#.a: Seven Schlumberger soundings and three azimuthal soundings were conducted in the Valley of Hermosillo, Sonora, northwestern Mexico, in order to investigate the vadose zone above the Valley of Hermosillo aquifer. This coastal aquifer system, which is considered unconfined in its upper part, consists of alluvial material. The resistivity soundings show that lateral changes of the resistivity can be interpreted with respect to a "background" value of 100 Ωm. Resistivity values less than 50 Ωm were found near the coast and near the population centers Hermosillo and Miguel Aleman. These relatively low values may reveal the presence of low quality pore water due to irrigation with ground water mixed with brackish ground water from sea water intrusions and with untreated sewage, or as a result of pollution by domestic and/or industrial sewage. The porosity of these low resistivity areas was estimated to be on the order of 25 %, based on Archie"s law. Azimuthal resistivity surveys show that there is only superficial resistivity anisotropy which may be related to a rearrangement of grains by infiltrated irrigation water.

773.1.#.t: Geofísica Internacional; Vol. 36 Núm. 3: Julio 1, 1997; 191-200

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: 191-200

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

doi: https://doi.org/10.22201/igeof.00167169p.1997.36.3.650

handle: 009191eb083b1301

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

856.#.0.q: application/pdf

file_creation_date: 2022-07-07 12:09:57.0

file_modification_date: 2022-07-12 22:01:40.0

file_creator: Birgit Steinich

file_name: c484d02b3906b274a289127ec1a3c2afa030a2ebf288fa5330911f824aa539c7.pdf

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245.1.0.b: Geophysical investigations of the vadose zone in the Valley of Hermosillo aquifer, Sonora, Mexico

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

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Artículo

Geophysical investigations of the vadose zone in the Valley of Hermosillo aquifer, Sonora, Mexico

Steinich, Birgit; Simón, Isabel; Chavarría, J. Andrés; Marín, Luis E.

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

Steinich, Birgit, et al. (1997). Geophysical investigations of the vadose zone in the Valley of Hermosillo aquifer, Sonora, Mexico. Geofísica Internacional; Vol. 36 Núm. 3: Julio 1, 1997; 191-200. Recuperado de https://repositorio.unam.mx/contenidos/4132504

Descripción del recurso

Autor(es)
Steinich, Birgit; Simón, Isabel; Chavarría, J. Andrés; Marín, Luis E.
Tipo
Artículo de Investigación
Área del conocimiento
Físico Matemáticas y Ciencias de la Tierra
Título
Geophysical investigations of the vadose zone in the Valley of Hermosillo aquifer, Sonora, Mexico
Fecha
1997-07-01
Resumen
Seven Schlumberger soundings and three azimuthal soundings were conducted in the Valley of Hermosillo, Sonora, northwestern Mexico, in order to investigate the vadose zone above the Valley of Hermosillo aquifer. This coastal aquifer system, which is considered unconfined in its upper part, consists of alluvial material. The resistivity soundings show that lateral changes of the resistivity can be interpreted with respect to a "background" value of 100 Ωm. Resistivity values less than 50 Ωm were found near the coast and near the population centers Hermosillo and Miguel Aleman. These relatively low values may reveal the presence of low quality pore water due to irrigation with ground water mixed with brackish ground water from sea water intrusions and with untreated sewage, or as a result of pollution by domestic and/or industrial sewage. The porosity of these low resistivity areas was estimated to be on the order of 25 %, based on Archie"s law. Azimuthal resistivity surveys show that there is only superficial resistivity anisotropy which may be related to a rearrangement of grains by infiltrated irrigation water.
Tema
Valle de Hermosillo; zona vadosa; sondeos de resistividad; salinización del suelo; Valley of Hermosillo; vadose zone; resistivity measurements; salinisation of the soil
Idioma
spa
ISSN
ISSN-L: 2954-436X; ISSN impreso: 0016-7169

Enlaces