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About Groundwater Lecture Notes
The document discusses groundwater and aquifers. It defines an aquifer as a saturated layer of permeable rock that allows groundwater to flow through it. Groundwater occurs in both unconfined and confined aquifers. Unconfined aquifers have water at atmospheric pressure at the water table, while confined aquifers are under pressure and wells can produce artesian flow. The hydraulic conductivity of an aquifer determines the rate of groundwater flow according to Darcy's law. Higher conductivity materials like sand and gravel allow faster flow than low conductivity materials like clay or granite.
Detailed Information
| Author: | ['Gourav Panda'] |
|---|---|
| Publication Year: | 2016 |
| Pages: | 16 |
| Language: | English |
| Format: | |
| Price: | FREE |
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