In a storage reservoir, which is artificially mixed in order to reduce
algal and especially cyanobacterial growth, the cyanobacterium Microc
ystis is still present. The aim of the research was to investigate why
Microcystis was able to grow in the artificially mixed reservoir. Fro
m the results it could be concluded that the large shallow area in the
reservoir allows this growth. The loss of buoyancy during the day was
much higher in this shallow part than in the deep part. Assuming that
the loss of buoyancy was the result of a higher carbohydrate content,
a higher growth rate in the shallow part may be expected. A higher re
ceived light dose by the phytoplankton in the shallow mixed part of th
e reservoir than in the deep mixed part explains the difference in buo
yancy loss. A significant correlation between the received light dose
(calculated for homogeneously mixed phytoplankton) and the buoyancy lo
ss was found. Apparently, the Microcystis colonies were entrained in t
he turbulent flow in both the shallow and the deep part of the reservo
ir. With a little higher stability on one sampling day, due to the lat
e start of the artificial mixing, the loss of buoyancy at the deep sit
e was higher than on the other days and almost comparable to the loss
at the shallow site. Although the vertical biomass distribution and th
e temperature profiles showed homogeneous mixing, the colonies in the
upper layers apparently received a higher light dose than those deeper
in the water column. Determination of the buoyancy state of cyanobact
eria appeared to be a valuable method to investigate the light history
and hence their entrainment in the turbulent flow in the water column
.