RESUMEN
Artificial oxygenation is a common management technique for lake restoration, but the use of hypolimnetic aeration in shallow basins can have dramatic effects on the dynamics of thermal stratification. This study presents the results of extensive field measurements performed in Lake Serraia (Trentino, Italy) after the installation of a Side Stream Pumping System, whereby oxygen-rich water is injected through 24 jets, uniformly distributed along an octagonal-shaped pipe at approximately 1 m above the sediment floor (10 m in depth). The lake is characterised by an average depth of 7 m, a volume of 3.1 × 10(6) m(3) and a residence time of about one year. Prior to the installation of the pumping system, the undisturbed hypolimnion thickness during summer stratification was relatively small. After the start of oxygen injection (up to 0.5 m(3)/s of oxygen-saturated water), an increase of in-lake temperature over the entire water column was noted with a maximum hypolimnetic temperature increase of up to 9 °C. The analysis of the flow field data and the results of numerical simulations (presented in the companion paper), indicate that the jets were solely responsible for the observed increase in temperature. Moreover, this study shows that modelling efforts are useful to provide guidelines for optimising contrasting needs (e.g., increase in oxygen supply versus jet discharge rate).
Asunto(s)
Restauración y Remediación Ambiental , Lagos , Oxígeno , Temperatura , Chlorophyta/crecimiento & desarrollo , Italia , Dinámica Poblacional , Calidad del AguaRESUMEN
At the end of July 2004, a "black-spot" appeared in the western portion of Lake Garda, an oligomictic lake classified as meso-oligotrophic. A few days later, this phenomenon spread throughout the lake. A first analysis by optical microscopy revealed that the origin of the black spot was a ciliated protozoan. Ciliates represent a small percentage of the total zooplanktonic community of Lake Garda and have never produced bloom episodes. Using morphological and molecular analysis, we characterized the protozoan responsible for the bloom as Stentor amethystinus and its symbiotic algae as a Chlorella sp. Continuous monitoring of the northeast of Lake Garda showed that the apex of the S. amethystinus bloom took place during the first 20 days of August, and the highest density of S. amethystinus occurred in the euphotic zone. During this period, high chlorophyll a values were obtained in water samples collected from the euphotic zone due to the presence of the endosymbiont Chlorella. After early September, the black spot completely disappeared, and the causative organism was detected at low concentration only in the southern basin of the lake. The results obtained on the progress of the black spot phenomenon led us to hypothesize that: (i) S. amethystinus was recently introduced in Lake Garda by anthropogenic activities or it was already a member of the zooplanktonic community but at a very low concentration; (ii) S. amethystinus blooms may have been driven by an unusual high availability of total phosphorous in the euphotic zone and (iii) Lake Garda is not the preferred habitat for S. amethystinus.