Abstract
In the present paper the spatial distribution and temporal evolution of the saline intrusion in the most important aquifer of Havana province is presented. Results were obtained through the application of hydrochemical and isotopic tools. Studies were carried out within the framework of the IAEA Regional Project RLA/8/041. The survey was carried out in 2008 during the dry and rainy seasons. Sampling points were selected according to a monitoring network located along the north-south line following the main groundwater flow direction. Stable isotopes ({sup 2}H and {sup 18}O) were used to identify and characterize the groundwater origin and mixing processes. Changes in the chemical composition of groundwater were shown to be mainly controlled by the groundwater and seawater mixing process, followed by cation exchange reactions and a Ca-Mg precipitation process due to the strong influence of the costal wetland. A gradual decreasing of the spatial and temporal saline intrusion was observed. (author)
Alvarez, A. M.;
Bombuse, D. L.;
Estevez Alvarez, J. R.;
[1]
others, and
- Centro de Aplicaciones Tecnologicas y Desarrollo Nuclear (CEADEN), Havana (Cuba)
Citation Formats
Alvarez, A. M., Bombuse, D. L., Estevez Alvarez, J. R., and others, and.
Evaluation of the Marine Intrusion in Havana Province Groundwater Using Hydrochemical and Isotopic Tools.
IAEA: N. p.,
2013.
Web.
Alvarez, A. M., Bombuse, D. L., Estevez Alvarez, J. R., & others, and.
Evaluation of the Marine Intrusion in Havana Province Groundwater Using Hydrochemical and Isotopic Tools.
IAEA.
Alvarez, A. M., Bombuse, D. L., Estevez Alvarez, J. R., and others, and.
2013.
"Evaluation of the Marine Intrusion in Havana Province Groundwater Using Hydrochemical and Isotopic Tools."
IAEA.
@misc{etde_22122086,
title = {Evaluation of the Marine Intrusion in Havana Province Groundwater Using Hydrochemical and Isotopic Tools}
author = {Alvarez, A. M., Bombuse, D. L., Estevez Alvarez, J. R., and others, and}
abstractNote = {In the present paper the spatial distribution and temporal evolution of the saline intrusion in the most important aquifer of Havana province is presented. Results were obtained through the application of hydrochemical and isotopic tools. Studies were carried out within the framework of the IAEA Regional Project RLA/8/041. The survey was carried out in 2008 during the dry and rainy seasons. Sampling points were selected according to a monitoring network located along the north-south line following the main groundwater flow direction. Stable isotopes ({sup 2}H and {sup 18}O) were used to identify and characterize the groundwater origin and mixing processes. Changes in the chemical composition of groundwater were shown to be mainly controlled by the groundwater and seawater mixing process, followed by cation exchange reactions and a Ca-Mg precipitation process due to the strong influence of the costal wetland. A gradual decreasing of the spatial and temporal saline intrusion was observed. (author)}
place = {IAEA}
year = {2013}
month = {Jul}
}
title = {Evaluation of the Marine Intrusion in Havana Province Groundwater Using Hydrochemical and Isotopic Tools}
author = {Alvarez, A. M., Bombuse, D. L., Estevez Alvarez, J. R., and others, and}
abstractNote = {In the present paper the spatial distribution and temporal evolution of the saline intrusion in the most important aquifer of Havana province is presented. Results were obtained through the application of hydrochemical and isotopic tools. Studies were carried out within the framework of the IAEA Regional Project RLA/8/041. The survey was carried out in 2008 during the dry and rainy seasons. Sampling points were selected according to a monitoring network located along the north-south line following the main groundwater flow direction. Stable isotopes ({sup 2}H and {sup 18}O) were used to identify and characterize the groundwater origin and mixing processes. Changes in the chemical composition of groundwater were shown to be mainly controlled by the groundwater and seawater mixing process, followed by cation exchange reactions and a Ca-Mg precipitation process due to the strong influence of the costal wetland. A gradual decreasing of the spatial and temporal saline intrusion was observed. (author)}
place = {IAEA}
year = {2013}
month = {Jul}
}