Summary: Groundwater Processes
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1 Introduction
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1.1 Powerpoint
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What are three things you need to know about ground water?
1. Resupplied by infiltration
2. Often cleaner than surface water
3. Accessed by wells -
On what two things does the velocity of ground water depends on?
1. Slope
2. Permeability -
What are typical artesian systems? (4 things)
-Dunes with peat grow
-Glacial systems with outwash (stuwwallen )
-Permafrost systems
-Fracture zones incristaline rock -
2 Principles of Saturated flow
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2.1 Powerpoint
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What is \/H (triangle)?
A vector of H that point to the location where the increase of H is the strongest. -
What are three limitations to Darcy's law?
1.Neglectance of velocity head
2.Doesn't work when reynolds number >1
3.Doesn't work when groundwater density (rho) variesspatially -
When is the hydraulic head not a correct measure for energy?
When the density differs. -
3 Permeability and resistance
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3.1 Powerpoint
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When is a layer isotropic?
When the hydraulic conductivity K at each location is the same in all directions. -
When is a layer heterogeneity?
When the K is not the same at every location. -
When is a layer anisotropy?
When the value of K at a location depends on the direction. -
What is shear flow?
Flow rate varies perpendicular to flow direction.
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