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African Water Development Report 2006 - United Nations Economic ...

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South Africa and Bophuthatswana. (DesertificationEnviro Facts, 2005).Box 6.5Groundwater Over abstraction and Seawater Intrusion in LibyaIn the northern parts of the continent Moroccois one of the countries affected by desertification.Here, desertification is caused by a combinationIn 1976, the Swani well field, consisting of 52 wells tapping the Quaternary aquifer south of Tripoli started operationand consequently resulted in the advance of the seawater intrusion front by more than 3 km southward bythe year 1979 The. figure reflects the changes in salinity in the Swani municipal well field in the period from 1976to 1993 before its closure.Protecting Ecosystems in AfricaNMediterranean SeaJanzurTripoliGargareshTajuraEl Maya19571972197919950 km10 kmFrom 1979 to 1995, high rates of population growth and fast urbanization, forced irrigated agriculture to movefurther south and necessitated the development of an additional well field consisting of 87 wells southeast ofTripoli, which also had to be abandoned after few years of operation. Sharp declines of the water table causedthe advance of the seawater intrusion front by 6 km in Tajura, 9 km in Gargaresh, 2 km in Janzur and 5 km in ElMaya and the total area affected by seawater intrusion reached 250 km2 (Al Fateh University 2002). The highestadvance of the seawater intrusion front in the Tripoli area took place from 1979 to 1995. During this period,the advance rate was estimated at 200 to 400 m/yr especially in the central zone south of Tripoli, while the leastadvance was in the area of Janzur due partly to the high elevation and the existence of a forest belt to the south.Previous master plans recommended the reduction of pumped groundwater in the subregion to 250 Mm3/yrby adopting certain measures.Source: AWDR National <strong>Report</strong> – Libya, 2005157

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