Articles | Volume 26, issue 2
https://doi.org/10.5194/hess-26-483-2022
https://doi.org/10.5194/hess-26-483-2022
Research article
 | 
31 Jan 2022
Research article |  | 31 Jan 2022

Evidence for high-elevation salar recharge and interbasin groundwater flow in the Western Cordillera of the Peruvian Andes

Odiney Alvarez-Campos, Elizabeth J. Olson, Lisa R. Welp, Marty D. Frisbee, Sebastián A. Zuñiga Medina, José Díaz Rodríguez, Wendy R. Roque Quispe, Carol I. Salazar Mamani, Midhuar R. Arenas Carrión, Juan Manuel Jara, Alexander Ccanccapa-Cartagena, and Chad T. Jafvert

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Cited articles

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Alvarez Campos, O., Olson, E., Welp, L. R., and Frisbee, M. D.: Groundwater chemistry within Arequipa, Peru in the Characato, Chiguata, and Lagunas Salinas study areas, Purdue University Research Repository [data set], https://doi.org/10.4231/PJRM-Q992, 2021. 
Benavente, C., Delgado, G., García, B., Aguirre, E., and Audin, L.: Neotectónica: evolución del relieve y peligro sísmico en la región Arequipa, INGEMMET, Boletín, Serie C: Geodinámica e Ingeniería Geológica, 64, 370 pp., 2017. 
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Short summary
We present results of a hydrologic study of groundwater recharge near the city of Arequipa, Peru. There are a number of springs below a high-elevation salar that show some chemical evidence of connectivity to the salar basin, possibly facilitated by faults in region. These results suggest that this salar basin is not a strictly terminal lake but that some interbasin groundwater flow exists. In addition, a high-elevation forest ecosystem seems important for groundwater recharge as well.
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