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Quantifying the potential seepage from porphyry copper tailing impoundments using a multi-isotopic approach
Indexado
WoS WOS:001024750700001
Scopus SCOPUS_ID:85160412642
DOI 10.1016/J.SCITOTENV.2023.164446
Año 2023
Tipo artículo de investigación

Citas Totales

Autores Afiliación Chile

Instituciones Chile

% Participación
Internacional

Autores
Afiliación Extranjera

Instituciones
Extranjeras


Abstract



Porphyry-style copper deposits are characterized by low Cu grades and high tonnages, resulting in large mine tailing volumes disposed in impoundments. Due to the mining tailing sizes, waterproofing techniques cannot be applied along the dam base. Therefore, to minimize seepage towards the aquifers, pumping wells are usually installed as hydraulic barriers. Currently, there is a controversy over whether or not the water extracted from hydraulic barriers should be counted as the use of new water rights. Consequently, a growing interest to develop tools to trace and quantify the tailing impacts in groundwater and to determine the water pumped amount subjected to water rights exist. In the present study, isotope data (δ2H-H2O, δ18O-H2O, δ34S-SO42− and δ18O-SO42−) are proposed as a tool to quantify tailings seepage towards groundwater and to assess hydraulic barriers effectiveness. To illustrate this approach usefulness, the Quillayes porphyry Cu tailing impoundment (Chile) case study is presented. The multi-isotopic approach revealed that tailing waters are highly evaporated showing high SO42− content (~1900 mg L−1) derived from primary sulfate ore dissolution, whereas freshwaters, derived from recharge water, have low SO42− contents (10–400 mg L−1) resulting from the interaction with geogenic sulfides from barren host rock. The δ2H and δ18O values of groundwater samples collected downstream from the impoundment suggest a mixing at different proportions of highly evaporated water from the mine tailing waters and non-evaporated regional fresh groundwater. Cl−/SO42−, δ34S-SO42−/δ18O-SO42−, δ34S-SO42−/ln(SO42−) and δ2H-H2O/δ18O-H2O mixing models allowed to determine that groundwater located closer to the impoundment had a mine tailing water contribution from 45 to 90 %, whereas those located farther away had lower contribution (5–25 %). Results confirmed the stable isotope usefulness to determine the water origin and to calculate the hydraulic barrier efficiencies and the pumped water proportions unrelated to the mining tailing subject to the water rights.

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Disciplinas de Investigación



WOS
Environmental Sciences
Scopus
Waste Management And Disposal
Pollution
Environmental Engineering
Environmental Chemistry
SciELO
Sin Disciplinas

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Publicaciones WoS (Ediciones: ISSHP, ISTP, AHCI, SSCI, SCI), Scopus, SciELO Chile.

Colaboración Institucional



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Autores - Afiliación



Ord. Autor Género Institución - País
1 Navarro-Ciurana, Didac - Universitat de Barcelona - España
Univ Barcelona UB - España
2 Saleta-Daví, Agnés - Universitat de Barcelona - España
Univ Barcelona UB - España
3 Otero, Neus - Universitat de Barcelona - España
Generalitat de Catalunya - España
Univ Barcelona UB - España
Generalitat Catalunya - España
4 Torrentó, Clara - Universitat de Barcelona - España
Generalitat de Catalunya - España
Univ Barcelona UB - España
Generalitat Catalunya - España
5 Quintana-Sotomayor, Carlos Hombre Departamento de Conservación y Protección de Recursos Hídricos - Chile
Direcc Gen Aguas - Chile
6 Miguel-Cornejo, Diego San - Departamento de Conservación y Protección de Recursos Hídricos - Chile
Direcc Gen Aguas - Chile
6 San Miguel-Cornejo, Diego Hombre Direcc Gen Aguas - Chile
Departamento de Conservación y Protección de Recursos Hídricos - Chile
7 Musalem-Jara, Mónica - Departamento de Conservación y Protección de Recursos Hídricos - Chile
Direcc Gen Aguas - Chile
8 Novoa-Godoy, Gullibert - Servicio Nacional de Geología y Minería - Chile
9 Carrasco-Jaramillo, Cristóbal - Servicio Nacional de Geología y Minería - Chile
10 Aguirre-Dueñas, Evelyn - Comision Chilena de Energia Nuclear - Chile
11 Escudero-Vargas, Manuel A. - Comision Chilena de Energia Nuclear - Chile
12 Soler i Gil, Albert Hombre Universitat de Barcelona - España
Univ Barcelona UB - España

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Financiamiento



Fuente
SERNAGEOMIN
International Atomic Energy Agency
Direction Générale de l’Armement
Comisión Chilena de Energía Atómica
Dirección General de Aguas Chilena
Catalan Government of Spain
El Servicio Nacional de Geología y Minería Chileno
El Servicio Nacional de Geologia y MineriaChileno (SERNAGEOMIN)
Consolidate Research Group MAG from the Catalan Government of Spain
Comision Chilena de Energia Atomica (CCHEN)
Direccion General de Aguas Chilena (DGA)
project of the International Atomic Energy Agency (IAEA)

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Agradecimientos



Agradecimiento
This study was funded by the CHI-7013 project of the International Atomic Energy Agency (IAEA), the Comisión Chilena de Energía Atómica (CCHEN), the Dirección General de Aguas Chilena (DGA) and the El Servicio Nacional de Geología y Minería Chileno (SERNAGEOMIN). Support for the research was received also through the project 2022-SGR-00308 (Consolidate Research Group MAG) from the Catalan Government of Spain .
This study was funded by the CHI-7013 project of the International Atomic Energy Agency (IAEA), the Comisión Chilena de Energía Atómica (CCHEN), the Dirección General de Aguas Chilena (DGA) and the El Servicio Nacional de Geología y Minería Chileno (SERNAGEOMIN). Support for the research was received also through the project 2022-SGR-00308 (Consolidate Research Group MAG) from the Catalan Government of Spain .
This study was funded by the CHI-7013 project of the International Atomic Energy Agency (IAEA) , the Comision Chilena de Energia Atomica (CCHEN), the Direccion General de Aguas Chilena (DGA) and the El Servicio Nacional de Geologia y MineriaChileno (SERNAGEOMIN) . Support for the research was received also through the project 2022-SGR-00308 (Consolidate Research Group MAG) from the Catalan Government of Spain.

Muestra la fuente de financiamiento declarada en la publicación.