m
m
Line 57: Line 57:
 
<td>0.06-0.10</td>
 
<td>0.06-0.10</td>
 
<td>0.08</td>
 
<td>0.08</td>
 +
</tr>
 +
<tr>
 +
<td>Limestone with solution openings</td>
 +
<td>0.1 to 10<sup>-5</sup></td>
 +
<td>0.01</td>
 +
<td></td>
 +
<td></td>
 +
</tr>
 +
<tr>
 +
<td>Limestone </td>
 +
<td>10<sup>-5</sup> to 10<sup>-9</sup></td>
 +
<td>10<sup>-7</sup></td>
 +
<td>0.005 to 0.05</td>
 +
<td>0.01</td>
 +
</tr>
 +
<tr>
 +
<td>Sandstone</td>
 +
<td>10<sup>-5</sup> to 10<sup>-9</sup></td>
 +
<td>10<sup>-6</sup></td>
 +
<td>0.05 to 0.15</td>
 +
<td>0.10</td>
 +
</tr>
 +
<tr>
 +
<td>Shale</td>
 +
<td>10<sup>-8</sup> to 10<sup>-12</sup></td>
 +
<td>10<sup>-9</sup></td>
 +
<td>0.005 to 0.05</td>
 +
<td>0.01</td>
 
</tr>
 
</tr>
 
</table>
 
</table>

Revision as of 12:42, 3 April 2020

Horizontal saturated conductivity1 and specific yield2 of geologic materials. Sources:Duffield; Morris and Johnson
Link to this table

Material Range Ksat (m/s)3 Typical Ksat (m/s) Range specific yield Typical specific yield
Gravel 3×10-4 to 3×10-2 3×10-3 0.21-0.28 0.24
Coarse sand 9×10-7 to 6×10-3 5×10-5 0.26-0.30 0.26
Medium sand 9×10-7 to 5×10-4 1×10-5 0.26-0.30 0.26
Fine sand 2×10-7 to 2×10-4 5×10-6 0.20-0.30 0.21
Silt, loess 1×10-9 to 2×10-5 1×10-7 0.15
Till 1×10-12 to 2×10-6 1×10-9 0.06-0.16 0.10
Clay 1×10-11 to 4.7×10-9 1×10-10 0.06-0.10 0.08
Limestone with solution openings 0.1 to 10-5 0.01
Limestone 10-5 to 10-9 10-7 0.005 to 0.05 0.01
Sandstone 10-5 to 10-9 10-6 0.05 to 0.15 0.10
Shale 10-8 to 10-12 10-9 0.005 to 0.05 0.01

1vertical saturated conductivity is considered to be one-tenth the value of horizontal saturated conductivity.
2Specific yield is expressed here as a fraction. It is often reported as a percentage in the literature.
31 meter = 3.28 feet