An aquifer is a natural underground reservoir of water that can be extracted for human use. It is typically made up of layers of permeable rock or sediments, such as sand, gravel, or porous rock, that can hold and transmit water. Aquifers are a crucial source of fresh water for drinking, irrigation, and industrial purposes.
There are two main types of aquifers: confined (or artesian) aquifers and unconfined (or water-table) aquifers. Confined aquifers are trapped between impermeable layers of rock, while unconfined aquifers are closer to the surface and have a water table that fluctuates with rainfall and other factors.
Human activities such as excessive pumping, pollution, and urban development can deplete or contaminate aquifers, leading to serious water shortages and environmental problems.
By understanding the principles and significance of aquifers, we can work towards preserving these valuable sources of fresh water for future generations.
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