Water Quality and Phytoplankton Community in Selected Recreational Lakes and Reservoirs Under Restoration Measures in Western Poland (original) (raw)

The primary production of phytoplankton in the restored Maltañski Reservoir in Poland

Hydrobiologia, 2003

The paper presents the results of the seasonal fluctuation of planktonic primary production (gross and net), respiration and photosynthetic activity of water in the completely restored Maltañski Reservoir in Poznañ (mid-west Poland), in which a biomanipulation experiment was conducted. Water samples were taken from 1992 to 1997 every month or in vegetation seasons every fortnight. Primary production measurements were made in a deep section of the reservoir with 1-meter intervals between surface and 3-meter depth, using dark and light bottles (oxygen-technique). Maximal productivity was noted in the surface layer of the reservoir with wide seasonal variation: from 0.1 to 6.8 mg C l−1 d−1 and from 0.08 to 4.7 g C m−2 d−1. The highest monthly average values of primary production were observed in summer when cyanobacteria were dominated. The phytoplankton productivity was significantly correlated with water temperature, insolation, Secchi depth and chlorophyll-a. Only weak correlation of primary production and total phosphorus was noted. Biomanipulation experiment carried out in the reservoir led to temporary decreasing of primary production in 1993 and increasing specific primary production, up to 14.1 μg C μg Chl−1h−1.

Changes in Phytoplankton and Water Quality during Sustainable Restoration of an Urban Lake Used for Recreation and Water Supply

Water

Groundwater intake near Lake Głębokie, situated in the city of Szczecin in Northwestern Poland, resulted in a distinct decrease in the lake water level. Water intake from a river and a neighboring urban area led to eutrophication and a strong cyanobacterial water bloom. Both the water intake and recreation were threatened due to the possible influence of cyanobacterial toxins. The lake was subjected to three sustainable restoration methods: aeration of sediment-water; iron addition to precipitate P, and; biomanipulation. The goal of our study was to determine the changes in the taxonomic composition of phytoplankton and chemical water variables during restoration measures. A comparison of the data obtained during this research with the pre-restoration data showed that, as a result of the treatments orthophosphates decreased, rarely exceeding 0.06 mg P•L −1 , and cyanobacterial water blooms disappeared. Cyanobacteria were found in the lake but they were not abundant. Chrysophytes and diatoms were the most abundant in springtime of each year. Green algae, desmids and chrysophytes were particularly abundant in summer, while cryptophytes predominated in autumn. Algae from all these groups do not pose a threat to either recreation or water intake. The deep chlorophyll maximum occurring in summer at a depth of 5 m as a result of restoration confirms the lower trophic status of the lake, alluding to mesotrophic conditions.

Functional Groups of Phytoplankton and Their Relationship with Environmental Factors in the Restored Uzarzewskie Lake

Water

Uzarzewskie Lake is a small, postglacial lake, located in western Poland. The lake is under restoration treatment since 2006. At first, iron treatment was done for 2 years. In the second stage, spring water was directed into the hypolimnion in order to improve water oxygenation near the bottom sediments. The purpose of our research was to determine changes in the contribution of functional groups to the total number of taxa and total biomass of phytoplankton due to changes in the physical and chemical characteristics of the restored lake. Phytoplankton composition was analyzed in three periods: (1) before restoration; (2) during the first method of restoration; and (3) when the second method was implemented in the lake. Epilimnetic phytoplankton was sampled every year monthly from March to November. The relationship between phytoplankton groups and environmental factors (water temperature, ammonium nitrogen, nitrate nitrogen, dissolved phosphorus, conductivity and pH) was examined, ...

Phytoplankton of eutrophic lakes in Western Poland

Verhandlungen, 1991

The investigations were carried out on a group of 20 lakes situated in the Miçdzychód-Sieraków Lake District on the left bank of the Warta River. Al! of them were formed during PoznaiÍ substage of the Baltic glaciation so they are the reservoirs of equal age. However, they differ with respect to size (1.96 to 304.3ha), maximum depth (from 3.5 to 45.0 m), mean deRth (from 1.7 to 20.2 m), volume (0.034 to 25.06 mln m), catchment area (30 to 6060 ha) and management (e. g. forest coverage-3 to 100%), and also to the degree of contamination with municipal sewage and with loads from non-point pollution sources. This had a considerable effect on trophic state of the lakes expressed, for example, as different species composition and abundance of phytoplankton.

Functioning of the Lake Rusalka ecosystem in Poznan (western Poland)

2010

Lake Rusałka is a shallow, artificial, strongly eutrophic reservoir. Thermal stratification is weak and comprises only about 8% of the bottom surface. In summer, the epilimnion is oversaturated with oxygen due to intensive phytoplankton growth (chlorophyll a up to 80.2 µg l -1 ), while conditions in the hypolimnion are anaerobic. The high concentration of ammonium nitrogen and low N:P ratio stimulated intense growth of cyanobacteria in the period from June to November. The domination of rotifers in the metazooplankton and low diversity and biomass of benthic macroinvertebrates was the cause of low top-down pressure of these 66 organisms on the phytoplankton. The most advantageous restoration measures were identified to improve water quality and make the recreational use of the lake possible.

Functioning of the Lake Rusałka ecosystem in Poznań (western Poland)

Oceanological and Hydrobiological Studies, 2010

Functioning of the Lake Rusałka ecosystem in Poznań (western Poland) Lake Rusałka is a shallow, artificial, strongly eutrophic reservoir. Thermal stratification is weak and comprises only about 8% of the bottom surface. In summer, the epilimnion is oversaturated with oxygen due to intensive phytoplankton growth (chlorophyll a up to 80.2 μg l-1), while conditions in the hypolimnion are anaerobic. The high concentration of ammonium nitrogen and low N:P ratio stimulated intense growth of cyanobacteria in the period from June to November. The domination of rotifers in the metazooplankton and low diversity and biomass of benthic macroinvertebrates was the cause of low top-down pressure of these organisms on the phytoplankton. The most advantageous restoration measures were identified to improve water quality and make the recreational use of the lake possible.

Planktonic Indices in the Evaluation of the Ecological Status and the Trophic State of the Longest Lake in Poland

Due to the intensive mixing polymictic lakes should be homogenous. However, morphometric diversity and high water dynamics contribute to the differentiation of many parameters in various areas of the lakes. This study analyzes both phytoplankton and zooplankton to assess differences in water quality along the north-south axis of the longest lake in Poland. New phytoplankton indicators were applied for determining the lake's ecological status: the Q index based on functional groups and the PMPL (Phytoplankton Metric for Polish Lakes) index based on phytoplankton biomass. TSI ROT index (Rotifer Trophic State Index), which comprises the percentage of species indicating a high trophic state in the indicatory group and the percentage of bacteriovorus in the Rotifera population, was used for zooplankton analysis.

Trends in the Phytoplankton Variability of the Selected Polish Lakes

2019

The directional changes of phytoplankton in Polish lakes were presented to show some tendency concerning the total biomass, composition, and biodiversity as related to environmental variables. The selected lakes were analyzed concerning various types of antropopressure, e.g., relatively low, medium, and huge human impact including sewage inflow history, different hydrological regime nature as natural phenomenon of flow-through lakes and as a consequence of artificial including into water-cooling system with short retention time, and different restoration actions (biomanipulation and artificial aeration).