GROUNDWATER MODELING IN THE COCHABAMBA VALLEY USING MODFLOW

In the Cochabamba metropolitan area, 65% of water for human consumption comes from groundwater extracted from the west side of the Central Valley. There has been an intense exploitation in the area with growth of operating wells. The objective of this study is to update and extend well monitoring, a...

Full description

Bibliographic Details
Main Authors: Jenny T. Saavedra, Laura A. Rosales, Oliver C. Saavedra
Format: Article
Language:English
Published: Universidad Privada Boliviana 2020-07-01
Series:Investigación & Desarrollo
Online Access:http://www.upb.edu/revista-investigacion-desarrollo/index.php/id/article/view/212
id doaj-c4f8ac59db4a4dc3a9e5306834d5b4e9
record_format Article
spelling doaj-c4f8ac59db4a4dc3a9e5306834d5b4e92020-11-25T03:14:45ZengUniversidad Privada BolivianaInvestigación & Desarrollo1814-63332518-44312020-07-0120110.23881/idupbo.020.1-6i204GROUNDWATER MODELING IN THE COCHABAMBA VALLEY USING MODFLOWJenny T. Saavedra0Laura A. Rosales1Oliver C. Saavedra2Universidad Privada BoliviaUniversidad Privada BoliviaUniversidad Privada BoliviaIn the Cochabamba metropolitan area, 65% of water for human consumption comes from groundwater extracted from the west side of the Central Valley. There has been an intense exploitation in the area with growth of operating wells. The objective of this study is to update and extend well monitoring, and improve understanding of groundwater flow through a hydrogeological model. The study area is an attractive region for groundwater exploitation due to the presence of an alluvial fan to the north that encourages the recharge of the aquifer. The MODFLOW computer package has been used for the modeling, using hydrogeology data of precipitation, temperature, evapotranspiration, stratigraphic profiles, and piezometric levels. As for latter, measurement campaigns were carried out at identified wells within the study area. The study area is made up of unconfined aquifers with high piezometric levels. The results of the calculated heads against the observed ones in the calibration process, gave a correlation coefficient of 0.76 and a root mean square (RMS) of 6.2 m. The model was simulated at steady state, showing a balance without evidence of exploitation, with an input of 77 m3 to the system. The main flow direction is from north to south with evident changes in direction due to the presence of rivers. The average level of the water table is 4.9 m below the surface in the southern zone and 130 m below the surface in the northern zone. The water balance generated by the model presents an input to the system of river infiltration and recharge. The output of the system is mainly due to evapotranspiration.http://www.upb.edu/revista-investigacion-desarrollo/index.php/id/article/view/212
collection DOAJ
language English
format Article
sources DOAJ
author Jenny T. Saavedra
Laura A. Rosales
Oliver C. Saavedra
spellingShingle Jenny T. Saavedra
Laura A. Rosales
Oliver C. Saavedra
GROUNDWATER MODELING IN THE COCHABAMBA VALLEY USING MODFLOW
Investigación & Desarrollo
author_facet Jenny T. Saavedra
Laura A. Rosales
Oliver C. Saavedra
author_sort Jenny T. Saavedra
title GROUNDWATER MODELING IN THE COCHABAMBA VALLEY USING MODFLOW
title_short GROUNDWATER MODELING IN THE COCHABAMBA VALLEY USING MODFLOW
title_full GROUNDWATER MODELING IN THE COCHABAMBA VALLEY USING MODFLOW
title_fullStr GROUNDWATER MODELING IN THE COCHABAMBA VALLEY USING MODFLOW
title_full_unstemmed GROUNDWATER MODELING IN THE COCHABAMBA VALLEY USING MODFLOW
title_sort groundwater modeling in the cochabamba valley using modflow
publisher Universidad Privada Boliviana
series Investigación & Desarrollo
issn 1814-6333
2518-4431
publishDate 2020-07-01
description In the Cochabamba metropolitan area, 65% of water for human consumption comes from groundwater extracted from the west side of the Central Valley. There has been an intense exploitation in the area with growth of operating wells. The objective of this study is to update and extend well monitoring, and improve understanding of groundwater flow through a hydrogeological model. The study area is an attractive region for groundwater exploitation due to the presence of an alluvial fan to the north that encourages the recharge of the aquifer. The MODFLOW computer package has been used for the modeling, using hydrogeology data of precipitation, temperature, evapotranspiration, stratigraphic profiles, and piezometric levels. As for latter, measurement campaigns were carried out at identified wells within the study area. The study area is made up of unconfined aquifers with high piezometric levels. The results of the calculated heads against the observed ones in the calibration process, gave a correlation coefficient of 0.76 and a root mean square (RMS) of 6.2 m. The model was simulated at steady state, showing a balance without evidence of exploitation, with an input of 77 m3 to the system. The main flow direction is from north to south with evident changes in direction due to the presence of rivers. The average level of the water table is 4.9 m below the surface in the southern zone and 130 m below the surface in the northern zone. The water balance generated by the model presents an input to the system of river infiltration and recharge. The output of the system is mainly due to evapotranspiration.
url http://www.upb.edu/revista-investigacion-desarrollo/index.php/id/article/view/212
work_keys_str_mv AT jennytsaavedra groundwatermodelinginthecochabambavalleyusingmodflow
AT lauraarosales groundwatermodelinginthecochabambavalleyusingmodflow
AT olivercsaavedra groundwatermodelinginthecochabambavalleyusingmodflow
_version_ 1724642706464964608