Estudio hidrogeológico del campus norte de la UNACH mediante tomografías eléctricas de resistividad y pruebas de bombeo.

This research aims to analyze the hydrogeological characteristics of the North campus of UNACH, determining the possible impact of the water table on problems such as earth movements that affect the campus infrastructure. The research was carried out using electrical resistivity tomography on the surface of the campus, thus evaluating the stratigraphy of the terrain up to 60 meters deep; this approach allowed an understanding of the composition of the subsoil, including layers of rock, soil, sediments, other materials and especially the presence of water mass. In addition, a topographic survey was carried out using a drone with an accuracy of 1 cm, which allows better identification of both the surface strata and the height of the piezometric water level of the well located within the institutional property. The piezometric level data was interpreted to complement this work, obtaining a piezometric map of groundwater. These data allowed configuring the conceptual model of the aquifer present in the area of the university campus, in which it was shown that the groundwater of the aquifer is at a depth that ranges from 2725 to 2714 meters above sea level in the UNACH well, that is, at a depth of 58 meters, concerning the foundation of the buildings, thus demonstrating that the piezometric level of the aquifer in the North campus of the UNACH does not have direct contact with the foundations of the buildings.

• Príomhchruthaitheoir: Heredia Morquecho, Nicole Stefany (author)
• Formáid: bachelorThesis
• Teanga: spa
• Foilsithe / Cruthaithe: 2025
• Ábhair: Tomografías; Acuífero; Conductividad hidráulica; Modelo matemático
• Rochtain ar líne: http://dspace.unach.edu.ec/handle/51000/14695