dor_id: 4132172

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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

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

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856.4.0.u: http://revistagi.geofisica.unam.mx/index.php/RGI/article/view/503/519

100.1.#.a: Gomes De Oliveira, Vitor Manuel; Tavares Ribeiro, Luís Filipe; Rosalino Da Silva, María Catarina

524.#.#.a: Gomes De Oliveira, Vitor Manuel, et al. (2014). Hydrogeologic characterization of the abandoned mining site of Castelejo, Portugal by VLF-EM & RMT-R geophysical surveying. Geofísica Internacional; Vol. 53 Núm. 2: Abril 1, 2014; 135-151. Recuperado de https://repositorio.unam.mx/contenidos/4132172

245.1.0.a: Hydrogeologic characterization of the abandoned mining site of Castelejo, Portugal by VLF-EM & RMT-R geophysical surveying

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

561.1.#.a: Instituto de Geofísica, UNAM

264.#.0.c: 2014

264.#.1.c: 2014-04-01

653.#.#.a: prospección geofísica; acuífero fisurado; agua de mina; VLF; RMT-R; geophysical surveying; fissured aquifer; mine water; VLF; RMT-R

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041.#.7.h: spa

520.3.#.a: There are about 175 abandoned mining sites in Portugal, of which about 60 are old uranium workings. The Castelejo mine is an old uranium located about 2 km W of Vila Cortés da Serra, in Guarda district, on the River Mondego basin. In geologic terms, the mine is located in medium-grained two-mica monzonitic granite, with porphyroidal tendency. Exploitation started with two open cast mines between 1979 and 1990 which produced about 132 tonnes U3O8.From 1992, production started to be carried out through the in situ H2SO4 leaching of the mine’s low-grade materials. The superficial and groundwater circulation are structurally conditioned by the intense fracturing in the area. Two exploratory geophysical field campaigns were conducted in order to characterize the fracturing. The first was a VLF survey that allowed us to identify major fault systems that may provide paths for groundwater flow. From the second campaign, hich was an RMT survey conducted at a fault gauge which records the mine natural gradient flow, we obtained the resistivities and thicknesses of the weathered granite material. The profiles obtained show that resistivity declines with increasing depth. This fact may arise from natural causes - the material which fills the fault gauge is more weathered at depth than on the surface - or it may indicate contamination at depth, due to acid mine drainage.doi: doi: https://doi.org/10.1016/S0016-7169(14)71496-5

773.1.#.t: Geofísica Internacional; Vol. 53 Núm. 2: Abril 1, 2014; 135-151

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: 135-151

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

doi: https://doi.org/10.1016/S0016-7169(14)71496-5

handle: 00cf0277e4cf2e0a

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

856.#.0.q: application/pdf

file_creation_date: 2014-04-07 16:31:03.0

file_modification_date: 2022-07-07 18:48:37.0

file_creator: Vitor Manuel Gomes de Oliveira

file_name: d93e96a8ec3d99f21c2d6f509bbb162d6e2197b437fac91c8a7579e2ad9b3fa6.pdf

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245.1.0.b: Hydrogeologic characterization of the abandoned mining site of Castelejo, Portugal by VLF-EM & RMT-R geophysical surveying

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

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Artículo

Hydrogeologic characterization of the abandoned mining site of Castelejo, Portugal by VLF-EM & RMT-R geophysical surveying

Gomes De Oliveira, Vitor Manuel; Tavares Ribeiro, Luís Filipe; Rosalino Da Silva, María Catarina

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

Gomes De Oliveira, Vitor Manuel, et al. (2014). Hydrogeologic characterization of the abandoned mining site of Castelejo, Portugal by VLF-EM & RMT-R geophysical surveying. Geofísica Internacional; Vol. 53 Núm. 2: Abril 1, 2014; 135-151. Recuperado de https://repositorio.unam.mx/contenidos/4132172

Descripción del recurso

Autor(es)
Gomes De Oliveira, Vitor Manuel; Tavares Ribeiro, Luís Filipe; Rosalino Da Silva, María Catarina
Tipo
Artículo de Investigación
Área del conocimiento
Físico Matemáticas y Ciencias de la Tierra
Título
Hydrogeologic characterization of the abandoned mining site of Castelejo, Portugal by VLF-EM & RMT-R geophysical surveying
Fecha
2014-04-01
Resumen
There are about 175 abandoned mining sites in Portugal, of which about 60 are old uranium workings. The Castelejo mine is an old uranium located about 2 km W of Vila Cortés da Serra, in Guarda district, on the River Mondego basin. In geologic terms, the mine is located in medium-grained two-mica monzonitic granite, with porphyroidal tendency. Exploitation started with two open cast mines between 1979 and 1990 which produced about 132 tonnes U3O8.From 1992, production started to be carried out through the in situ H2SO4 leaching of the mine’s low-grade materials. The superficial and groundwater circulation are structurally conditioned by the intense fracturing in the area. Two exploratory geophysical field campaigns were conducted in order to characterize the fracturing. The first was a VLF survey that allowed us to identify major fault systems that may provide paths for groundwater flow. From the second campaign, hich was an RMT survey conducted at a fault gauge which records the mine natural gradient flow, we obtained the resistivities and thicknesses of the weathered granite material. The profiles obtained show that resistivity declines with increasing depth. This fact may arise from natural causes - the material which fills the fault gauge is more weathered at depth than on the surface - or it may indicate contamination at depth, due to acid mine drainage.doi: doi: https://doi.org/10.1016/S0016-7169(14)71496-5
Tema
prospección geofísica; acuífero fisurado; agua de mina; VLF; RMT-R; geophysical surveying; fissured aquifer; mine water; VLF; RMT-R
Idioma
spa
ISSN
ISSN-L: 2954-436X; ISSN impreso: 0016-7169

Enlaces