Total Area 2,944 km2
Land 2,934 km2
Water 10 km2
Highest Elevation  1,857 m

Land Use
Arable 21.13%
Perm. Crop 24.3%
Other 54.57% (2005)

Population 214,265 (July 2007 est.)
Population Growth Rate 1.291% (July 2007 est.)

GDP per capita (PPP) $2,100 (2005 est.)

Water Statistics
Avg Rainfall

3,000 mm per annum

Status of Water Resources

Problems with Water Resources and Associated Environment Issues
Surface water and groundwater are the only sources of water used for water supply provision, with the exception of rainwater harvesting practiced widely in the Falealupo Peninsula and in otherwise isolated and rural households. Piped water supply access is estimated at between 90-95% of the population.
There has been no national assessment to date on the stress put upon the individual catchments and aquifers. This work will be undertaken as part of an on-going EU funded water sector support program (WaSSP). Limited historical surface water monitoring, and a lack of raw water abstraction metering, to date prevents accurate assessment of water withdrawal against low flow yields.
The competition for water resources appears in the Fuluasou and Vaisigano water catchments around Apia, where both public water supply and public energy supply are provided by the same river systems. Hydropower operations in Fuluasou river catchment is now non-operational due to insufficient water quality and complete infilling of the intake reservoir with sediment.
There is no known water quality monitoring for wastewater associated pollution. An on-going Asian Development Bank (ADB) funded Apia wastewater and drainage project is presently in the design phase and is about to commence baseline monitoring. There is however ample visual evidence of wastewater contamination of streams around the urban Apia area. Solid waste disposal is also a problem within the low-lying populated areas, with obvious uncontrolled tipping into valleys. Sediment erosion is the most visible surface water pollutant within the catchments. Perhaps the most stark reminder of sedimentation in the watersheds is the complete infilling of the now abandoned Fuluasou Hydropower Dam reservoir. Salinisation is known to occur at some boreholes in Savaii, although this is generally thought to be saline up-coning (i.e. over-pumping of an individual borehole) rather than saline intrusion (over-abstraction from the aquifer as a whole). However a lack of systematic monitoring and groundwater investigation prevent further assessment.

Diagnostic Report
Demonstration Proposal
Hot Spot Analysis

Information on this page obtained from Integrated Water Resources Management programme's Diagnostic Reports (SOPAC 2007)
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