Darcy's Law Flashcards
Limitation: Assumes rock is homogeneous:
Most rocks tend to be heterogeneous - they have different properties at different locations.
Also, permeability varies with direction.
Three limitations:
Assumes rock is homogeneous.
Doesn’t account for tortousity.
Applies only to slow moving ground water.
Limitation: Doesn’t account of tortousity:
Tortousity - The fact water must flow around individual grains.
Flow of water (l) is actually longer than l because fluid has to travel around grains of rock.
Limitation: Applies only to slow moving ground water:
Laminar flow - streamline.
As fluid speed increases, flow becomes turbulent. This modifies the relationship between the hydraulic head and fluid speed.
Darcy’s law is used to
Calculate ground water speed.
Equation for Darcys law:
v = K h/l
K - hydraulic conductivity
h/l - hydraulic gradient
The value of K depends on rock permeability and
The density and viscosity of the fluid.
The larger K is, the more
Easily water flows through the rock.
Equation for hydraulic conductivity (K):
K = pg k/v
p - fluid density
g - acceleration due to gravity
k - permeability of the rock
v - fluid viscosity
K is large for coarse materials and
Small for fine materials.