Body of rock that holds water which is exploited as a resource
For a rock to form an aquifer it must have certain features
Porosity
Measure of the proportion of a rock's volume that is space and could therefore hold water
Porous rocks that can form aquifers
Chalk
Limestone
Sandstone
Permeability
Measure of the ease with which fluids may flow through a rock because of the interconnections between the spaces and their size
Impermeable rocks
Granite
Clay
Aquifer recharge
1. Natural flow or seepage of water into the aquifer
2. Water that flows out of the aquifer
Abstraction of water by humans greater than recharge rate
Volume of water in the aquifer will decline
Most aquifer recharge takes place as precipitation landing on the ground surface infiltrates and percolates through soil and rock to the aquifer
Water abstraction from aquifers that are recharged by surface water can be sustainable as long as it does not exceed the recharge rate
Some aquifers were recharged during the last ice age 10-20,000 years ago when the global climate was wetter
Ancient aquifer water is often saline and can cause soil salinization as irrigation water evaporates, leaving the salt behind
Lowering of water table
Reduces or stops the outflow of water into wetlands, causing them to dry up
Lowering of water table
Plants with higher water requirement will die or become less abundant as they fail to compete with plants that have a lower requirement for water
Wetlands drying out
Aquatic or semi-aquatic animals will die
Overexploitation of aquifer
Seawater from the sea, or in the rock under the sea, flows sideways into the aquifer to replace the freshwater, making the aquifer water unsuitable for irrigation
Water no longer present in the interstitial spaces in the rock
Rock particles will be compacted by the weight of material above, causing subsidence at the surface
Extraction rate exceeding recharge rate
Volume of water available for abstraction will be reduced
Nearly half the world's population live in countries that are over-exploiting their aquifers
GRACE satellites
NASA operates two satellites that can detect changes in the mass of water in aquifers below their flight path