|
Mussel debris consists
of shells and fine, organically enriched mud. The
shells increase the roughness of the surface of
the seabed and generate dense backscatter on the
side-scan record.
At the two low-energy
sites the mussel debris predominantly occurred
directly beneath the farm. The sonar traces showed
a strong contrast between the area under the farm
and the areas immediately around it, highlighting
the distinctive nature of the mussel shell debris
compared to the natural sediment deposits.
By contrast, at the
high-energy site there was little sign of any
mussel debris under the farm. The seafloor
sediment was relatively homogeneous, indicating
that there was sufficient wave and current energy
at this site to transport and dissipate the mussel
debris over a wide area, making it difficult to
detect any changes to the natural sediment.
In summary,
side-scan sonar is a useful tool for seabed
mapping in mussel culture areas. Mussel debris is
readily identified. Side-scan imagery can easily
map large tracts of seafloor, and, in combination
with grain size data and photographic records, can
provide a good understanding of the sediment
dispersal footprints of mussel farms.
Neil
Hartstein
[ n.hartstein@niwa.co.nz ]
|