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Assessing aquifer vulnerability to seawater
intrusion using GALDIT method: Part 2—GALDIT Indicators Description
A. G. CHACHADI1 & JOÃO PAULO LOBO FERREIRA2
1 Goa University, Dept. of Earth Science, Goa University, Goa – 403 206, India
chachadi1@rediffmail.com
2 Laboratório Nacional de Engenharia Civil (LNEC), Hydraulics and Environment Department (DHA), Groundwater Division (NAS), Av. do Brasil, 101, 1700-066 Lisboa, Portugal
Abstract This paper is Part 2 of a paper
submitted to the 4th InterCeltic Colloquium as Lobo-Ferreira et al. (2007). In this second part of
the paper the method for assessing GALDIT index parameters is fully explained.
The original development of the GALDIT index was done in the framework of the
EU-India INCO-DEV COASTIN project, aimed at the assessment of aquifer
vulnerability to seawater intrusion in coastal aquifers. The most important
factors controlling seawater intrusion were found to be the following: Groundwater occurrence (aquifer type;
unconfined, confined and leaky confined); Aquifer
hydraulic conductivity; depth to groundwater Level above the sea; Distance
from the shore (distance inland perpendicular from shoreline); Impact of existing status of seawater
intrusion in the area; and Thickness
of the aquifer, which is being mapped. The acronym GALDIT is formed from the
highlighted letters of the parameters for ease of reference. These factors, in
combination, are found to include the basic requirements needed to assess the
general seawater intrusion potential of each hydrogeological setting. GALDIT
factors represent measurable parameters for which data are generally available
from a variety of sources without detailed examination. A numerical ranking
system to assess seawater intrusion potential in hydrogeological settings has been
devised using GALDIT factors. The system contains three significant parts:
weights, ranges, and ratings. Each GALDIT factor has been evaluated with
respect to the other to determine the relative importance of each factor. In this part we also present the
first applications of the method developed for the Bardez aquifer in Goa,
India.
Key words aquifer vulnerability; groundwater
protection; modelling; seawater intrusion