|
|||||
|
|
REPLY: PEAT MOUNDS WITH NON-UNIFORM PROPERTIES |
|
| Authors: | ADRIAN ARMSTRONG |
| Abstract: | In estimating the form of a peat mound from the equilibrium water table position, the assumption that hydraulic conductivity shows an exponential decline with depth (as used in the Armstrong (Earth Surface Processes and Landforms, 1995, 20 , 473–477) analysis) may be questioned in some circumstances. However, this does not invalidate the use of the hydrologic model for peat mounds, and results are presented which could be used to evaluate other forms of the depth-dependent relationship. |
| Keywords: | hydraulic conductivity Girinsky seepage potential |