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Effects of large woody debris on surface structure and aquatic habitat in forested streams, southern interior British Columbia, Canada
Author(s) -
Chen Xiaoyong,
Wei Xiaohua,
Scherer Rob,
Hogan Dan
Publication year - 2008
Publication title -
river research and applications
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.679
H-Index - 94
eISSN - 1535-1467
pISSN - 1535-1459
DOI - 10.1002/rra.1105
Subject(s) - streams , large woody debris , channel (broadcasting) , hydrology (agriculture) , habitat , debris , sediment , stream restoration , environmental science , watershed , stream bed , aquatic ecosystem , ecology , geology , geomorphology , biology , oceanography , riparian zone , computer network , geotechnical engineering , machine learning , computer science , electrical engineering , engineering
It is well known that large woody debris (LWD) plays an important functional role in aquatic organisms' life. However, the influence of LWD on channel morphology and aquatic environments at watershed levels is still unclear. The relationships between wood and surface structure and aquatic habitat in 35 first through fifth order streams of southern interior British Columbia were investigated. Study streams in the channel networks of the study watersheds were classified into four size categories based on stream order and bankfull width: Stream size I: bankfull width was less than 3 m, Stream size II: 3–5 m, Stream size III: 5–7 m, Stream size IV: larger than 7 m. We found the number of functional pieces increased with stream size and wood surface area in stream sizes I, II and III (24, 28 and 25 m 2 /100 m 2 , respectively) was significantly higher than that in stream size IV (12 m 2 /100 m 2 ). The contribution of wood pieces to pool formation was 75% and 85% in stream sizes II and III, respectively, which was significantly higher than those in stream size I (50%) and size IV (25%). Between 21% and 25% of wood pieces were associated with storing sediment, and between 20% and 29% of pieces were involved in channel bank stability in all study streams. Due to long‐term interactions, LWD in the intermediate sized streams (Size II and III) exhibited much effect on channel surface structure and aquatic habitats in the studied watersheds. Copyright © 2008 John Wiley & Sons, Ltd.