Catastrophic floods and prolonged periods of drought are the main 'water' c
hallenges facing Oman. So the inhabitants have had to resort to ingenious w
ays of utilising the available-water resources, such as through building fa
laj systems and the optimal selection of suitable crops, but nevertheless w
hen exposed to extremely-dry weather conditions, temporary and even permane
nt migration is still the only option left to some of those adversely affec
ted. The water problem has been compounded as a result of the rapid economi
c development of Oman since the beginning (in 1967) of the extraction there
of crude oil in commercial quantities. During this period, the general hea
lth of the population has improved, the average family-size has grown, and
the mean life-expectancy has increased. Also, as the economy has prospered,
the number of immigrant workers has risen to become today approximately 25
% of the total population. Thus the requirement for more reliable supplies
of potable water has increased substantially and is still growing. The dema
nds placed upon natural groundwater resources (i.e. fresh-water aquifers) h
ave become excessive: seawater intrusion has occurred into some fresh-water
aquifers as a result of the over-extraction of ground water and, in others
, the aquifers have simply dried up. The Government has resorted to the use
of desalination technologies for producing the additional potable-water su
pplies needed. However, desalination is relatively expensive and energy int
ensive! So a programme of better water-resource management is being impleme
nted. This has required the collection of meteorological data for many regi
ons of Oman. It is realised that the construction of darns across the wadi
watercourses, to harness flash-flood water during storms, has the potential
for reducing the need for the non-sustainable over-exploitation of undergr
ound aquifers. Also the possibility of utilising images taken from Earth-or
biting satellites for the exploration for ground-water fracture-zone aquife
rs is being considered in order to try to locate substantial resources, whi
ch have failed to be detected by conventional drilling methods, because suc
h water is often at great depths (exceeding 1 km). (C) 1998 Published by El
sevier Science Ltd. All rights reserved.