Pm. Visser et al., ARTIFICIAL MIXING PREVENTS NUISANCE BLOOMS OF THE CYANOBACTERIUM MICROCYSTIS IN LAKE NIEUWE-MEER, THE NETHERLANDS, Freshwater Biology, 36(2), 1996, pp. 435-450
1. Artificial mixing in the hypertrophic Lake Nieuwe Meer was successf
ul in preventing blooms of the cyanobacterium Microcystis. During the
2 years of artificial, deep mixing the number of colonies of Microcyst
is per litre and also per m(2) was lower than in the two preceding con
trol years. Hardly any nuisance scums of Microcystis occurred in the l
ake. 2. The phytoplankton shifted from a cyanobacteria-dominated commu
nity in summer to a mixed community of flagellates, green algae and di
atoms. Reduced sedimentation losses in the mixed lake, probably in com
bination with a lower pH, favoured nonbuoyant algae, while the entrain
ment of cyanobacteria in the turbulent flow nullified their advantage
of buoyancy. 3. The chlorophyll concentrations were much lower in the
mixed lake, but the euphotic depth did not show clear differences betw
een the years. The chlorophyll content integrated through depth (m(-2)
) increased in the artificially mixed lake. 4. The deep lake normally
stratified in summer, but artificial mixing of the lake in 1993 result
ed in a homogeneous temperature and oxygen distribution with depth. In
spring 1994, the mixing was applied intermittently with a reduction o
f 75% of the energy costs, while the mixing was still sufficient to pr
event stratification. 5. Determination of the buoyancy state of the co
lonies on a sunny and calm day showed that the buoyancy loss was low c
lose to the bubble plumes, and high at some distance from these plumes
. This suggests that Microcystis could escape the mixing at some dista
nce from the plumes, and could synthesize more carbohydrates during it
s stay in the upper illuminated layer of the lake than the deep mixed
colonies close to the bubble plumes. Determination of the buoyancy sta
te appeared to be a good and simple method to investigate the extent o
f entrainment of colonies in the turbulent flow.