Assessment of vulnerability to seawater intrusion and potential remediation measures for coastal aquifers: a case study from eastern India

2013 ◽  
Vol 70 (3) ◽  
pp. 1197-1209 ◽  
Author(s):  
M. Santha Sophiya ◽  
Tajdarul H. Syed
2004 ◽  
Vol 36 (4) ◽  
pp. 1952 ◽  
Author(s):  
K. Βουδούρης ◽  
K. Νίκας ◽  
A. Αντωνάκος

Seawater intrusion problems are recorded in coastal aquifers, which constitute the main sources of drinking water and agricultural irrigation in many countries. The aim of this work is to describe the evolution of the salinity distribution by seawater intrusion, based on results from chemical analyses, of 29 groundwater samples in the NWAchaia area (Peloponnesus, Greece). The study of these data indicates that aquifer waters in large part of area reflect salinization related to seawater intrusion. The occurrence of Ca-CI hydrochemical types of groundwater indicates active seawater intrusion. Cation exchange is the most noticeable hydrogeochemical process in the movement of the saline front in the coastal aquifer. Geographical distribution of Careact index was mapped. The areas with advance or decline of the seawater intrusion front are defined from this map.


2021 ◽  
Vol 11 (24) ◽  
pp. 11681
Author(s):  
Lucija Plantak ◽  
Ranko Biondić ◽  
Hrvoje Meaški ◽  
Denis Težak

Monitoring and detection of seawater intrusion in coastal aquifers in Croatia are one of the water management measures that attempt to notice an increase in salinity in time. Bokanjac-Poličnik is the coastal aquifer in Croatia that is at the risk of seawater intrusion. In that area, analysis of hydro-chemical indicators will be conducted due to the occasional seawater intrusion that occurs on wells that are included in the water supply system for the City of Zadar and surrounding villages. Due to the increased exploitation during the tourism season in summer and climate changes, salinization process is more intense. The presented results indicate that two of four wells on the case study area are under the influence of salt marine water.


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