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| DOI | 10.1016/J.SCITOTENV.2019.06.356 | ||||
| Año | 2019 | ||||
| Tipo | artículo de investigación |
Citas Totales
Autores Afiliación Chile
Instituciones Chile
% Participación
Internacional
Autores
Afiliación Extranjera
Instituciones
Extranjeras
These three processes reflect water-rock interactions. The delta B-11 of groundwater generally up to +13 parts per thousand, does not increase along the regional groundwater flow path, discarding fractionation by interaction with clays. These results improve the understanding of the groundwater evolution in hyper-arid systems through a new conceptual model. (C) 2019 Elsevier B.V. All rights reserved.
| Ord. | Autor | Género | Institución - País |
|---|---|---|---|
| 1 | Gamboa, C. | Mujer |
UCN - Chile
Universidad Católica del Norte - Chile |
| 2 | Godfrey, L. | Mujer |
RUTGERS STATE UNIV - Estados Unidos
Rutgers University–New Brunswick - Estados Unidos |
| 3 | HERRERA-LAMELI, CHRISTIAN OSVALDO | Hombre |
UCN - Chile
Universidad Católica del Norte - Chile |
| 4 | Custodio, E. | Hombre |
Tech Univ Catalonia - España
Universitat Politècnica de Catalunya - España |
| 5 | Soler i Gil, Albert | Hombre |
UB - España
Universitat de Barcelona - España |
| Fuente |
|---|
| Comisión Nacional de Investigación Científica y Tecnológica |
| Generalitat de Catalunya |
| Universitat de Barcelona |
| Comisión Nacional de Investigación CientÃfica y Tecnológica |
| Consejo Nacional de Innovacion, Ciencia y Tecnologia |
| CONICYT of Chile |
| Anillo Project of the CONICYT of Chile |
| CONICYT-PCHA/Doctorado Nacional of Carolina Gamboa |
| Universitat Politecnica de Catalunya |
| UPC |
| Department of Civil and Environmental Engineering of the Technical University of Catalonia |
| Carolina Gamboa |
| Centro de Investigación Tecnológica del Agua en el Desierto |
| Agradecimiento |
|---|
| This research was supported by the Anillo Project ACT1203 of the CONICYT of Chile and funded by a Ph.D. grant CONICYT-PCHA/Doctorado Nacional/2016-21160152 of Carolina Gamboa. Part of the research was partially supported by the Generalitat de Catalunya through the consolidate research groups (2017SGR-1733), and research time has been contributed by the Department of Civil and Environmental Engineering of the Technical University of Catalonia (UPC, Spain), the Universitat de Barcelona (UB Spain), and the "Centro de Investigacion Tecnologica del Agua en el Desierto" (CEITSAZA) in Antofagasta. In addition, we appreciate the work of Morris Peshtani from Rutgers University of the leaching experiments on surface salts. |
| This research was supported by the Anillo Project ACT1203 of the CONICYT of Chile and funded by a Ph.D. grant CONICYT-PCHA/Doctorado Nacional/2016-21160152 of Carolina Gamboa. Part of the research was partially supported by the Generalitat de Catalunya through the consolidate research groups (2017SGR-1733), and research time has been contributed by the Department of Civil and Environmental Engineering of the Technical University of Catalonia (UPC, Spain), the Universitat de Barcelona (UB Spain), and the “Centro de Investigación Tecnológica del Agua en el Desierto” (CEITSAZA) in Antofagasta. In addition, we appreciate the work of Morris Peshtani from Rutgers University of the leaching experiments on surface salts. |