HYDROLOGICAL MODEL OF PEAT-MOUND FORM WITH VERTICALLY VARYING HYDRAULIC CONDUCTIVITY - DISCUSSION

Citation
Aj. Baird et Sw. Gaffney, HYDROLOGICAL MODEL OF PEAT-MOUND FORM WITH VERTICALLY VARYING HYDRAULIC CONDUCTIVITY - DISCUSSION, Earth surface processes and landforms, 21(8), 1996, pp. 765-767
Citations number
12
Categorie Soggetti
Geosciences, Interdisciplinary
ISSN journal
01979337
Volume
21
Issue
8
Year of publication
1996
Pages
765 - 767
Database
ISI
SICI code
0197-9337(1996)21:8<765:HMOPFW>2.0.ZU;2-0
Abstract
In this comment we argue that the premise on which the peat mound mode l developed by Armstrong (Earth Surface Process and Landforms, 1995, 2 0, 473-477) is based, that hydraulic conductivity shows an exponential decline with depth in bog peats, is unsound. Empirical evidence in th e literature for such an exponential decline is less sound than Armstr ong suggests. In addition, Armstrong's suggestion that the hypothesis of Baird and Gaffney (Earth Surface Processes and Landforms, 1995, 20, 561-566) supports an exponential decline is shown to be erroneous.