Presentado en el V Seminario Peruano de Geoingeniería.

Por: A.M. Martínez, Miner S.A, Carmen de Atrato, Chocó, Colombia.

Abstract

This study presents the results obtained regarding the potential hydraulic connection between the surface water runoff of the Telly Creek and the groundwater inputs or outputs that occur in Level 2000 crosscuts of the El Roble Mine, through the implementation of hydrogeological and hydrochemical methods, such as testing by tracer technique, which in the case of this study was saline (NaCl).

It compiles the data of the physicochemical parameters taken strategically along the surface water runoff (Telly Creek) and Aguacerales located within the LVL 2000 crosscut, as well as the taking of samples for hydrochemical tests before and after the application of the tracer and its corresponding statistical analysis, which allowed inferring the hydraulic connection between these surface water and groundwater flows.