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The distribution of large woody debris accumulations and pools in relation to woodland stream management in a small, low‐gradient stream
Author(s) -
Gurnell A. M.,
Sweet R.
Publication year - 1998
Publication title -
earth surface processes and landforms
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.294
H-Index - 127
eISSN - 1096-9837
pISSN - 0197-9337
DOI - 10.1002/(sici)1096-9837(199812)23:12<1101::aid-esp935>3.0.co;2-o
Subject(s) - channelized , large woody debris , debris , woodland , geology , hydrology (agriculture) , deciduous , channel (broadcasting) , range (aeronautics) , habitat , ecology , oceanography , geotechnical engineering , telecommunications , materials science , engineering , riparian zone , computer science , electrical engineering , composite material , biology
This paper focuses upon the natural dynamics of large woody debris (LWD), the impact of management on LWD dynamics, and the impact of LWD removal and channelization on the distribution and size of pools in a British, second to third order, headwater catchment. The study stream is rather different from those subject to LWD accumulations which have been studied in North America. The most important contrast is that it is surrounded by predominantly deciduous rather than coniferous woodland. In terms of its width (1·8–4·5 m) and gradient 0·013 m m −1 ), it falls within the lower range of channels studied in North America. Nevertheless, there are similarities in LWD dam and pool spacing with some North American studies. The information on LWD dynamics during a period without management and on recovery of LWD dams after clearance covers a 16 year period (1982–1997). The paper illustrates that seven to eight years after clearance the total number of LWD dams has recovered but the most hydraulically active dam type has not recovered to pre‐clearance levels. An analysis of geomorphological maps of the channel surveyed in 1982 and 1996/97 shows an overall decrease in the number and size of pools along the section that was cleared of LWD dams. The magnitude of the decrease and the associated adjustments in pools through changes in their size and location differ according to location with respect to a section of the study stream which was channelized in c. 1966 and which has subsequently incised its bed. Copyright © 1998 John Wiley & Sons, Ltd.