Town/City: |
Canberra |
State/Province: |
Australian Capital Territory |
Country: |
Australia |
Latitude/Longitude: |
35S 149E |
Information supplied byGerry JacobsonGJACOBSO@AGSO.GOV.AUDated Fri Jan 12 10:35:48 1996 |
Population 0.3 million, city centre at 149 deg 10 min E, 35 deg 15 min S, totally planned city, national capital, growth rate 3%, light industry, offices and residential development.
Annual rainfall 650 mm, evenly spread. Evaporation 1500 mm mainly in summer months.
Fractured rock aquifers (Silurian sandstone, limestone) with bore yields commonly 1-3 L/s, and salinity 300-2000 mg/L. Recharge from infiltrating rainfall is seasonal, in colder months, May to October. Local flow systems discharge to rivers, providing baseflow, and to seasonal springs and swamps at foot of slopes.
The municipal water supply is derived from surface water storages. Groundwater (about 3 million cubic metres per year) is used by a number of institutions privately, mainly for irrigation of sports fields.
There is a marked seasonal variation in potentiometric level. Chemistry of fractured rock aquifers is variable on a local scale.
Local hill and valley flow systems commonly have high potentiometric surface on lower slopes with drainage problems affecting residential development. There are a number of groundwater pollution problems from hydrocarbons and industrial effluent. At present there is no regulation of groundwater abstraction.
Groundwater is now regarded as a useful, if supplementary, local water source, and measures for regulating abstraction may be introduced in the near future.
1. Jacobson, G., 1982, Groundwater in fractured rock aquifers of the Australian Capital Territory - a valuable resource... or a major problem? Papers, Groundwater in Fractured Rock Conference, Australian Water Resources Council, Conference Series 5, 109-118.
2. Jacobson, G., 1983, Pollution of a fractured rock aquifer by petrol - a case study, BMR Journal of Australian Geology & Geophysics, 8, 313-322.
3. Evans, W.R., 1987, Hydrogeology of the Australian Capital Territory and Environs, Bureau of Mineral Resources, Australia, Report 263.
Gerry Jacobson, Australian Geological Survey Organisation (ph: +61-61-499758) can provide more information.