Synopsis top ↑
Numerous hydrological projects have been carried out using isotopic methods
over the last two decades in the ESCWA region, which includes the
Arabian Peninsula, the Arabian countries to the north, and Egypt. The
large amount of data obtained from groundwater samples has been
evaluated together with the hydrogeological, hydrochemical and water
management data available for the area. Analyses of the stable
isotopes of oxygen, hydrogen, and carbon in the groundwater samples,
as well as the naturally occurring radioactive isotopes of hydrogen
and carbon are used for the localization of groundwater recharge
areas; determination and quantification of mixtures of groundwater
from different sources; reconstruction of groundwater flow systems on
regional and local scales; determination of the paleoclimatic effects
on the geohydraulic conditions; determination of groundwater ages,
i.e., residence times; and distinguishing between renewable and fossil
groundwater resources. Extensive hydrological studies using isotopic
methods have been conducted in the ESCWA region on the following
aquifer systems and topics: isotopic composition of precipitation in
Jordan and Syria; groundwater turnover in karst aquifers in the
highlands of western Jordan, the mountains in western Syria and the
West Bank; groundwater recharge from precipitation and surface water
on the Damascus plain; origin and age of groundwater in the basalt
aquifer system in Jordan and Syria; recently recharged freshwater
lenses and fossil groundwater in Badiye and Hamad (steppe and desert
regions in Syria and eastern Jordan and the adjacent areas in Iraq and
Saudi Arabia); low of fossil groundwater and local, recently recharged
groundwater in Paleogene carbonate aquifers in eastern Saudi Arabia,
the Golf region, and southern Oman; groundwater recharge from flash
floods in the aquifers in unconsolidated rock in wadis and coastal
plains of the Arabian Peninsula; age and origin of groundwater in
aquifers in consolidated rock in the mountains of Oman.
The discussion of the hydrogeological significance of isotope data is
supplemented by comments on the most important current hydrogeological
problems in the ESCWA region that could be investigated using isotopic
methods. These include problems of groundwater recharge, the provenance of
groundwater, groundwater flow systems on regional and local scales,
paleohydrological conditions, and groundwater quality, particularly
contamination by human activities. All available publications on the isotope
hydrology of the ESCWA region are listed in the bibliography, as well as
basic publications on isotope hydrology in arid regions.
(Isotope geochemistry, isotope ratios, stable isotopes, O16, O18, O18/O16,
C14, radioactive isotopes, iritium, absolute age, atmospheric precipitation,
groundwater, currents, groundwater provinces, groundwater quality, sampling,
groundwater recharge, climate, paleoclimate,
aquifer, sandstone, limestone, dolomite, volcanic rocks, quaternary aquifer,
unconsolidated sediments
Bahrain, Jemen, Jordan, Lebanon, Qatar, Kuwait, Saudi Arabia, Syria, Oman,
United Arabic Emirates)