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Chapter 16 Groundwater
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Groundwater Water that fills and moves through pores in rock and sediment Important part of fresh water
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Aquifer Body of rock or sediment where large amounts of water flow or is stored
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Porosity % of the rock or sediment with open space
Sorting affects porosity
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Permeability Ability of a rock or sediment to let fluids pass through
Impermeable – water cannot flow Clay
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Aquifers Gravity pulls water down until it reaches an impermeable layer
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Zones of Aquifers Saturation – pore space is completely filled with water Water table – upper layer of zone
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Aeration – Between surface and water table
3 layers 1. Soil moisture 2. Dry 3. Capillary fringe – attraction of water molecules
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Water Tables Change
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Conserving Groundwater
Water moves slowly Years to replace Recharge zone – water travels to reach an aquifer Sensitive to pollution
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Ordinary Well
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Ordinary Spring
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Cone of Depression
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Artesian Formation Permeable rock between impermeable rock Sloped
No pumping
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Geysers and Hot Springs
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Hard vs Soft Water Hard – lots of minerals Soft – low amounts
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Cavern Large cave with smaller chambers
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Stalactites – top Stalagmites – bottom Column - connect
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Sinkholes Water dissolves rock
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Karst Topography Caverns and sinkholes in limestone
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