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Guarani Aquifer

Guarani Aquifer is a science topic covered in the lgStudy science library. This page brings together a partial reference excerpt, illustrations, worked examples, real-world applications and a short study plan, so you can understand Guarani Aquifer rather than just read about it. In short: The Guarani Aquifer, is the second largest known aquifer system in the world and is an important source of fresh water. Located beneath the parts of Argentina, Brazil, Paraguay, and Uruguay, it covers 1,200,000 km2 (460,000 sq mi), with a volume of about 40,000 km3 (9,600 cu mi), a thickness of between 50 m (160 ft) and 800 m (2,600 ft) and a maximum depth of about 1,800 m (5,900 ft).

Guarani Aquifer — main illustration
Guarani Aquifer — illustration

Key takeaways

  • Guarani Aquifer belongs to science; place it in that map before memorising details.
  • Learn the definition first, then one example that makes the definition concrete.
  • Connect Guarani Aquifer to a quantity you can measure, compute or draw — that is where exam questions come from.
  • Reproduce the core statement of Guarani Aquifer from memory before moving on to harder problems.

Reference excerpt

The Guarani Aquifer, is the second largest known aquifer system in the world and is an important source of fresh water. Located beneath the parts of Argentina, Brazil, Paraguay, and Uruguay, it covers 1,200,000 km2 (460,000 sq mi), with a volume of about 40,000 km3 (9,600 cu mi), a thickness of between 50 m (160 ft) and 800 m (2,600 ft) and a maximum depth of about 1,800 m (5,900 ft). It is estimated to contain about 37,000 km3 (8,900 cu mi) of water, with a total recharge rate of about 166 km3/year from precipitation. It was named by uruguayan geologist Danilo Antón after the Guarani people, an indigenous group that inhabited roughly the same area.

Geology of the aquifer

The Guarani Aquifer consists primarily of fluvial sandstones of the Piramboia Formation and aeolian sandstones of the Botucatu Formation, which were deposited during the Triassic and Jurassic periods. Over 90% of the total area is overlain by early Cretaceous basalts of the Serra Geral Formation. The basalt's low permeability allows it to act as an aquitard, 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, subsequent surface-associated losses due to evaporation and evapotranspiration, and potential contamination. The erosion exposes pieces of sandstone on aquifer's banks, which are called outcrops. This is where the rain comes in and also where the contamination might happen. In general, the aquifer comprises a variety of quartz sand, well-rounded format, and has low clay content. Granulometric data indicate that over 50% of the grains have a diameter between 0.125 and 0.250 millimetres (125 and 250 μm; 4.9 and 9.8 thou).

Recharge of the aquifer The recharge distribution is related to precipitation rate. Its complexity is due to the indirect relation between them. The infiltration rate depends on parameters that are variables in time and space. Another important factor that contributes to the aquifer's recharge is the importance of evapotranspiration. The soil, plants and atmosphere could be considered as components of a system physically related and dynamic. In some regions, the quantity of water that evaporates is larger than the runoff flow. A study by Brazilian Agricultural Research Corporation (Embrapa) in Ribeirão Preto - Brazil, from 1994 to 2001 indicates that agricultural activity using chemical products offers risk of contamination for the groundwater. Vegetal interception is another factor that directly influences the quantity of water that infiltrates into the soil, according to Soares and Almeida (2001) who realized a study in the Eucalyptus area between October 1995 and September 1996. The interception during this period was evaluated in 11% of the precipitation value.

See also Aquifer Fossil water Groundwater Ogallala Aquifer

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» "Waters that unite: Footprints of the Guarani Aquifer System". IW:Learn. January 26, 2024.

Illustrations

Guarani Aquifer: The Guarani Aquifer
The Guarani Aquifer
Guarani Aquifer: Map of the aquifer overlaid with political boundaries.
Map of the aquifer overlaid with political boundaries.

Worked examples

Example 1 — a first encounter with Guarani Aquifer

Start with the simplest possible case. Write down what Guarani Aquifer claims or describes in one sentence, then invent the smallest concrete situation in which that sentence is true. In science, the smallest case is usually a single object, a single equation or a single measurement. Check that every symbol or term in your sentence has a meaning in that case.

Example 2 — changing one variable

Take the situation from Example 1 and change exactly one quantity: double it, halve it, or set it to zero. Predict what should happen to Guarani Aquifer before you calculate. Comparing your prediction with the result is the fastest way to find out whether you understand the idea or only the words.

Example 3 — an exam-style question

Typical questions about Guarani Aquifer ask you to (a) state it precisely, (b) apply it to given data, and (c) explain a limitation. Practise writing all three answers in under five minutes; the third part is what separates a full-mark answer from an average one.

Applications of Guarani Aquifer

In research
Guarani Aquifer appears in science research whenever the underlying quantities have to be modelled precisely. Papers usually cite it as a starting assumption and then explore where it breaks down.
In technology and industry
Engineering practice reuses Guarani Aquifer in design rules, simulations and safety margins. Knowing the idea lets you read a specification sheet and understand why the numbers look the way they do.
In the classroom
Guarani Aquifer is common in secondary-school and first-year university syllabi. It links to neighbouring topics Aquifers in Brazil, Aquifers of South America, Geography of South America, so understanding it makes those chapters shorter.
In everyday life
Look for Guarani Aquifer outside the textbook — in sport, cooking, traffic, electronics or the sky above you. An example you found yourself is remembered far longer than one you were given.
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How to study Guarani Aquifer in 20 minutes

  1. Read the reference excerpt below once, without taking notes.
  2. Close the page and write down what Guarani Aquifer means in your own words.
  3. Compare your version with the excerpt and mark what you missed.
  4. Work through the three examples above with pen and paper.
  5. Explain Guarani Aquifer out loud to somebody else — or to Teacher Smith in the lgStudy chat.

Frequently asked questions

What is Guarani Aquifer in simple terms?

The Guarani Aquifer, is the second largest known aquifer system in the world and is an important source of fresh water. Located beneath the parts of Argentina, Brazil, Paraguay, and Uruguay, it covers 1,200,000 km2 (460,000 sq mi), with a volume of about 40,000 km3 (9,600 cu mi), a thickness of bet…

Why does Guarani Aquifer matter?

Because it connects several science ideas at once: it gives you a definition you can apply, a quantity you can calculate, and a way to check whether a result is plausible.

How should I study Guarani Aquifer?

Read the excerpt, restate it from memory, then work through the examples and applications listed on this page. The five-step study plan above takes about twenty minutes.

What does this page cover?

It gives you a compact reference excerpt plus original lgStudy explanations, examples, applications and study material on Guarani Aquifer.

Tags

  • Aquifers in Brazil
  • Aquifers of South America
  • Geography of South America
  • International aquifers
  • Paraná Basin
  • Springs of Argentina
  • Springs of Brazil
  • Springs of Paraguay
  • Springs of Uruguay

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