Table 3.
Quantities used in Darcy’s law for porous media. Here the units are the ones usually used in groundwater hydrology
Symbol | Meaning | Dimension | Unit |
---|---|---|---|
| |||
q | specific flux in the whole porous media, q = ϕu | length/time | cm/s |
K | hydraulic conductivity, K = ρgk/μ | length/time | cm/s |
k | intrinsic permeability | length2 | 2 cm |
φ | piezometric head, φ = p/(ρg) + z | length | cm |
u | flow velocity in empty space | length/time | cm/s |
ϕ | porosity or fraction of empty space | dimensionless | |
μ | fluid dynamic viscosity | force·time/length2 | dyn·s/cm2. |
ρ | fluid density | mass/volume | g/cm3 |
g | gravitational acceleration | length/time2 | cm/s2 |
p | hydraulic pressure | force/area | dyn/cm2 |
z | height | length | cm |