Fluxes and pathways of silicon in a marine rainbow trout cage farm wer
e studied. The measured fluxes included those carried by fish food, ju
veniles, harvest, fish loss (death and escape), sedimentation from the
cages, and benthic release measured with flux chambers in-situ. Two d
ifferent types of Si mass balances for the farm were constructed. The
mass balance according to the flux method was based on the measured fl
uxes and constructed for each of two consecutive growing seasons. The
mass balance constructed according to the accumulation method was base
d on the total input and removal of Si to the cages of the farm since
it was started, and the recovery of Si in the sediment originating fro
m the farm. In both types of mass balances external input was the majo
r source of Si, contributing a minimum of 55-80% of the total biogenic
silica in the material collected in sediment traps below the farm and
of the material accumulated in the farm-derived sediment. The Si remo
ved from the farm with harvest contributed a very small part, approxim
ately 0.3%, of the amount of Si supplied to the farm with fish food an
d juveniles. The loss of Si to the environment was 2.4 kg (1985), 2.5
kg (1986) and 2.5 kg (1980-86) for each ton of fish produced. On a sea
sonal basis, about 4.5% of the sedimented biogenic Si was returned in
dissolved form from the sediment to the overlying water. This constitu
ted about 0.3% of the biogenic Si content in the farm-derived sediment
. The flux of reactive silicate from sediment below the fish farm was
enhanced about 2.5 times compared to nearby sediments unaffected by th
e farm.