Guarani Aquifer: Difference between revisions
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The Guarani Aquifer consists primarily of [[sediment]]ed [[sandstone]]s deposited by [[fluvial]] and [[Aeolian processes|eolian]] processes during the [[Triassic]] and [[Jurassic]] periods (between 200 and 130 million years ago), with over 90% of the total area overlaid with [[basalt]] of a low-permeability, deposited during the [[Cretaceous]] period, acting as an [[aquitard]] and providing a high degree of containment. This greatly reduces the rate of [[infiltration (hydrology)|infiltration]] and subsequent recharge, but also isolates the aquifer from the [[Vadose zone]] and subsequent surface-associated losses due to [[evaporation]] and [[evapotranspiration]]. |
The Guarani Aquifer consists primarily of [[sediment]]ed [[sandstone]]s deposited by [[fluvial]] and [[Aeolian processes|eolian]] processes during the [[Triassic]] and [[Jurassic]] periods (between 200 and 130 million years ago), with over 90% of the total area overlaid with [[basalt]] of a low-permeability, deposited during the [[Cretaceous]] period, acting as an [[aquitard]] and providing a high degree of containment. This greatly reduces the rate of [[infiltration (hydrology)|infiltration]] and subsequent recharge, but also isolates the aquifer from the [[Vadose zone]] and subsequent surface-associated losses due to [[evaporation]] and [[evapotranspiration]]. |
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Research and monitoring of the aquifer in order to better manage it as a resource is considered important, as the [[population growth]] rate within its area is relatively high — resulting in higher [[Consumption (economics)|consumption]] and [[pollution]] risks. |
Research and monitoring of the aquifer in order to better manage it as a resource is considered important, as the [[population growth]] rate within its area is relatively high — resulting in higher [[Consumption (economics)|consumption]] and [[pollution]] risks. |
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The countries over the aquifer are also the original four [[Mercosur]] countries. |
The countries over the aquifer are also the original four [[Mercosur]] countries. |
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Revision as of 00:02, 16 May 2013
The Guarani Aquifer, located beneath the surface of Argentina, Brazil, Paraguay, and Uruguay, is one of the world's largest aquifer systems and is an important source of fresh water.[1] Named after the Guarani people, it covers 1,200,000 km², with a volume of about 40,000 km³, a thickness of between 50 m and 800 m and a maximum depth of about 1,800 m. It is estimated to contain about 37,000 km³ of water (arguably the largest single body of groundwater in the world, although the overall volume of the constituent parts of the Great Artesian Basin is much larger), with a total recharge rate of about 166 km³/year from precipitation. It is said that this vast underground reservoir could supply fresh drinking water to the world for 200 years. However, at closer inspection, if the world population were to stay at an equilibrium of about 6.96 billion, not even taking into account that babies need less water than grown adults, this figure reaches 1600 years, allowing about 9 liters per day per person. Due to an expected shortage of fresh water on a global scale, which environmentalists suggest will become critical in under 20 years, this important natural resource is rapidly becoming politicized, and the control of the resource becomes ever more controversial.
Geology of the aquifer
The Guarani Aquifer consists primarily of sedimented sandstones deposited by fluvial and eolian processes during the Triassic and Jurassic periods (between 200 and 130 million years ago), with over 90% of the total area overlaid with basalt of a low-permeability, deposited during the Cretaceous period, acting as an aquitard and providing a high degree of containment. This greatly reduces the rate of infiltration and subsequent recharge, but also isolates the aquifer from the Vadose zone and subsequent surface-associated losses due to evaporation and evapotranspiration.
Research and monitoring of the aquifer in order to better manage it as a resource is considered important, as the population growth rate within its area is relatively high — resulting in higher consumption and pollution risks.
The countries over the aquifer are also the original four Mercosur countries.
References
External links
- Official Site for the book about the Aquifer, by Nadia Rita Boscardin Borghetti, José Roberto Borghetti and Ernani Francisco da Rosa Filho (in Brazilian Portuguese)
- Conference «The Management of the Guarani Aquifer System: An Example of Cooperation»