C. Soulsby et al., Fine sediment influence on salmonid spawning habitat in a lowland agricultural stream: a preliminary assessment, SCI TOTAL E, 265(1-3), 2001, pp. 295-307
Spawning habitat utilized by Atlantic Salmon (Salmon salar) and Sea Trout (
Salmo trutta) was characterized in a 1.6-km reach of the Newmills Burn, a s
mall, highly canalized tributary of the River Don in Aberdeenshire. The New
mills Burn is typical of the intensively farmed lower sub-catchments of the
major salmon rivers on the east coast of Scotland. Such streams have subst
antial potential in providing spawning and juvenile habitat for salmonids,
with high redd densities resulting in egg deposition rates of >5 m(2). Howe
ver, in comparison with upland spawning tributaries draining less intensive
ly managed catchments, canalization and intensive cultivation has seriously
degraded the physical characteristics of aquatic habitats in many streams.
In the Newmills Burn, spawning gravels have a relatively high (> 20% by ma
ss) fine sediment (< 2 mm in size) content. The burn is characterized by hy
draulic conditions that are suitable for salmonid spawning, with modal velo
cities of 0.50-0.65 m s(-1) and depths of 0.20-0.25 m. However, infiltratio
n of fine sediments into gravels is rapid during hydrological events in the
winter months. Thus, complete siltation of open gravel matrices (simulated
redds) can occur within a week, and probably within a single moderate to l
arge storm event. Appreciable, but small, deposition of organic and silt/cl
ay particles can also affect spawning gravels. Egg mortalities in redds fol
lowing spawning are variable, but can be as high as 86% in the Newmills Bur
n. This may be related to fine sediment infiltration, reduced permeability
of spawning gravels and reduced oxygen supply to ova. It appears that the m
ain cause of high influx is sediment loads mobilized from intensively manag
ed land. It is suggested that fundamental changes to the management of agri
cultural land is required if fish habitats are to he improved and degraded
streams are allowed to re-naturalize. The need for closely focused investig
ations of the causal relationships between fine sediment infiltration and e
gg survival is stressed. (C) 2001 Elsevier Science B.V. All rights reserved
.