Bibliographic citations
Paredes, A., (2019). Potencial acuífero mediante el sondeo eléctrico vertical (SEV) en las unidades litoestratigráficas en la zona de Agocucho 2019 [Tesis, Universidad Privada del Norte]. https://hdl.handle.net/11537/21795
Paredes, A., Potencial acuífero mediante el sondeo eléctrico vertical (SEV) en las unidades litoestratigráficas en la zona de Agocucho 2019 [Tesis]. PE: Universidad Privada del Norte; 2019. https://hdl.handle.net/11537/21795
@misc{sunedu/3037124,
title = "Potencial acuífero mediante el sondeo eléctrico vertical (SEV) en las unidades litoestratigráficas en la zona de Agocucho 2019",
author = "Paredes Ruiz, Alexis Valentin",
publisher = "Universidad Privada del Norte",
year = "2019"
}
Agocucho Area, located in Cajamarca Basin has a limited supply of potable water. Groundwater has been identified as the best supply source for water supply in rural zones. This study was carried out with the aim of investigating the aquifer potential in lithostratigraphic units in Agocucho área using resistivity method. Vertical electrical sounding (VES) method was applied using Schlumberger configuration to determinate the resistivity and delineate the aquifer that help to develop wells. A total of 7 VES points were probed in the research area, The collected data was analysed using IPI2SIN software which were identified 3 geoelectric layers. The first formation is clay-sandstones with resistivity ranging from 66,15 Ω.m to 84,11 Ω.m and thickness of 15m. The second formation are sediments with resistivity ranging from 216 Ω.m to 302,83 Ω.m and thickness ranging from 25m to 85m. The third formation is characterized by fresh rock (limestone) with resistivity ranging from 513 Ω.m to 895,30 Ω.m and thickness ranging from 25m to 95m. The results of this study shows aquifer potential is located in the second geoelectric layer at shallow depths ranging between 25m to 85m, based on the geological setting this layer is aluviall deposit.
This item is licensed under a Creative Commons License