HR: 1340h
AN: H53D-0494 [Abstracts]
TI: The Effect of Large Woody Debris Dams Upon Flow Resistance
AU: * Kitts, D R
EM: D.R.Kitts@soton.ac.uk
AF: University of Southampton, Highfield Campus, Southampton, SO17 1BJ
United Kingdom
AU: Sear, D A
EM: D.A.Sear@soton.ac.uk
AF: University of Southampton, Highfield Campus, Southampton, SO17 1BJ
United Kingdom
AU: Darby, S E
EM: S.E.Darby@soton.ac.uk
AF: University of Southampton, Highfield Campus, Southampton, SO17 1BJ
United Kingdom
AB:
The flow resistance offered by vegetation is a critical issue in fluvial studies. One type of vegetation that has a
significant impact upon flow resistance is Large Woody Debris (LWD). LWD accumulations, such as debris dams, can account for
significant proportions of flow resistance despite only covering a small proportion of the channel bed. Current approaches
to predicting the resistance rely upon the drag force approach that is often used for rigid standing vegetation (Petryk and
Bosmajian, 1975). However, this does not take into account the different types of LWD accumulations that are present within
river systems. For example, accumulations with high blockage ratios or those in high-energy, high-gradient channels have a
significant amount of spill resistance that is not accounted for in the drag-force approach. Data collected from the
Highland Water, a 3rd order stream flowing through the New Forest in southern England, together with Froude-scaled flume
experiments are herein combined with data from previous studies (Shields and Gippel, 1995; Curran and Wohl, 2003) to identify
some general trends associated with the flow resistance offered by LWD accumulations in a range of fluvial environments.
The results show that there is a trend of increasing resistance with slope and blockage ratio. When using the drag force
approach, large residual errors between measured and predicted resistance have been identified for LWD dams subject to spill
resistance. A method to account for the spill resistance associated with different types of LWD dams is required in order to
allow accurate prediction of the flow resistance contributed by LWD accumulations. Spill resistance is known to be related
to Froude number which can affect the friction factor when variations in free-surface occur. Therefore, Froude number was
used to account for some (~70%) of the residual error between measured and predicted flow resistance especially where
channel gradient is high (S>0.01), and where blockage ratios tend to one.
DE: 1856 River channels (0483, 0744)
SC: Hydrology [H]
MN: Fall Meeting 2005