Spatial and temporal changes in groundwater levels and salinity
The levels and quality of groundwater are periodically monitored in all regions of
the country and these measured data from observation wells are used to identify areas
of low water level and groundwater salinity. For example, during the period 1969-2009,
a significant change in groundwater levels and salinities was observed. The decline
in the groundwater table in the middle of the distance between Dhayed and Hamrania
during that period exceeded 100 meters. The decrease in the groundwater level was
accompanied by an average increase in salinity of 15 g/l. This change in the groundwater
levels disturbs the pattern of regional groundwater flow and significantly increases
the groundwater salinity, whether because of horizontal seawater intrusion or vertical
upward of deep saline groundwater.
Salinity increases of the Surficial /Quaternary aquifer in 1969-2009 with contours
of decline in water table elevation
Groundwater salinity in the Surficial /Quaternary aquifer in 2012