The following table shows representative values of hydraulic conductivity for
various unconsolidated sedimentary materials, sedimentary rocks and crystalline
rocks (from
Domenico and
Schwartz 1990):
Unconsolidated Sedimentary Materials
Material
Hydraulic Conductivity
(m/sec)
Gravel
3x10-4 to 3x10-2
Coarse sand
9x10-7 to 6x10-3
Medium sand
9x10-7 to 5x10-4
Fine sand
2x10-7 to 2x10-4
Silt, loess
1x10-9 to 2x10-5
Till
1x10-12 to 2x10-6
Clay
1x10-11 to 4.7x10-9
Unweathered marine clay
8x10-13 to 2x10-9
Sedimentary Rocks
Rock Type
Hydraulic Conductivity
(m/sec)
Karst and reef limestone
1x10-6 to 2x10-2
Limestone, dolomite
1x10-9 to 6x10-6
Sandstone
3x10-10 to 6x10-6
Siltstone
1x10-11 to 1.4x10-8
Salt
1x10-12 to 1x10-10
Anhydrite
4x10-13 to 2x10-8
Shale
1x10-13 to 2x10-9
Crystalline Rocks
Rock Type
Hydraulic Conductivity
(m/sec)
Permeable basalt
4x10-7 to 2x10-2
Fractured igneous and metamorphic rock
8x10-9 to 3x10-4
Weathered granite
3.3x10-6 to 5.2x10-5
Weathered gabbro
5.5x10-7 to 3.8x10-6
Basalt
2x10-11 to 4.2x10-7
Unfractured igneous and metamorphic rock
3x10-14 to 2x10-10
To Convert From
m/sec To
Multiply
By
cm/sec
100
gal/day/ft2
2.12x106
ft/sec
3.28
Porosity (n)
Porosity is defined as the void space of a rock or unconsolidated material:
n = Vv/VT
where Vv is void volume and VT is total volume.
The following tables show representative porosity values for
various unconsolidated sedimentary materials, sedimentary rocks and crystalline
rocks (from Morris and
Johnson 1967):