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1

Zalety ozonowania wody

Kępa Urszula

Wodociągi - Kanalizacja

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2023

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nr 10

16--22

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Analiza zależności między wskaźnikami jakości wody w Jeziorze Goczałkowickim w aspekcie zakwitów fitoplanktonu

Czaplicka-Kotas A., Ślusarczyk Z., Pięta M., Szostak A.

Ochrona Środowiska

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2012

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Vol. 34, nr 1

21-27

PL

Analizie statystycznej poddano zawartość azotu amonowego, azotynów, azotanów, ortofosforanów i fosforu ogólnego w wodzie Jeziora Goczałkowickiego w latach 1994-2009. Wyodrębniono grupę punktów pomiarowych usytuowanych przy powierzchni lustra wody oraz grupę punktów pomiarowych usytuowanych na głębokościach 2 m i 6 m. Za pomocą testu równości średnich sprawdzono, że wartości wskaźników jakości wody na różnej głębokości podczas zakwitu okrzemek, sinic lub zielenic różniły się od wartości tych wskaźników w czasie braku zakwitu. W przypadku wody pobranej z powierzchni istotne różnice wartości podczas zakwitu i jego braku wykazały azot amonowy, azotyny i azotany. Stwierdzono, że większość wskaźników jakości wody miała istotne sezonowe zróżnicowanie, a jedynie azot amonowy i azotyny nie wykazywały istotnych zmian ze względu na porę roku. Wykazano również, że zakwit fitoplanktonu wpływał na związki korelacyjne pomiędzy badanymi wskaźnikami jakości wody. W wielu przypadkach nieistotne wartości współczynnika korelacji Spearmena przy braku zakwitu były istotne podczas zakwitu.

EN

Statistical relations between the water quality parameters were determined based on the analysis of ammonia nitrogen, nitrite, nitrate, orthophosphate and total phosphorus concentrations observed in Lake Goczalkowickie (impounding reservoir) over the period of 1994-2009. Measuring stations were divided into two groups: those located on the surface of the lake water and those situated at the depth of 2 m and 6 m. The mean value equality test verified that at either of the two depths the values of the water quality parameters measured during blooms of diatoms, cyanobacteria and green algae were different from the values of these parameters measured over the period with-out blooms. When water samples were taken from the surface of the lake, significant differences in the values measured during blooms and the lack thereof were observed with ammonia nitrogen, nitrites and nitrates. The water quality parameters examined exhibited significant differences in their seasonal patterns, except ammonia nitrogen and nitrites, which did not show any significant seasonal variations. The study revealed that phytoplankton bloom affected the correlation between the water quality parameters tested. In many instances, Spearman correlation coefficient values that were insignificant in the absence of blooms became significant when blooms were present.

3

Winter versus summer blooming of phytoplankton in a shallow lake: effect of hypertrophic conditions

Toporowska M., Pawlik-Skowrońska B., Krupa D., Kornijów R.

Polish Journal of Ecology

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2010

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Vol. 58, nr 1

3-12

EN

The comparison of species richness, abundance and diversity of phytoplankton blooms, which developed both in winter and summer seasons as an effect of lake hypertrophy, was the aim of this study. In the ice-covered lake (0.30 mg PO[4]-P L[^-1], 1.35 mg NH[4]-N L[^-1]; TSI[SD] = 64; TSI[chl] = 93), the algal bloom, responsible for high concentration of dissolved oxygen in water, consisted mainly of the centric diatom Stephanodiscus minutulus (3.9 x 10[^7] ind. L[^-1]) accompanied by Limnothrix redekei (Cyanobacteria), Koliella longiseta (Chlorophyceae), > 1.1 x 10[^6] ind. L[^-1] each, as well as Mallomonas sp. (Chrysophyceae) and Monoraphidium komarkovae (Chlorophyceae), >5.0 x 10[^5] ind. L[^-1] each. The toxic cyanobacterium Planktothrix agardhii of extremely long trichomes (up to 0.93 mm) and potentially toxic dinoflagellate Peridinium aciculiferum f. inerme occurred also in high numbers (1.9 x 10[^5] ind. L[^-1] and 7.7 x 10[^4] ind. L[^-1], respectively). In summer (0.05 mg PO[4]-P L[^-1]; 0.42 mg NH[4]-N L[^-1]; TSI[SD] = 78; TSI[chl] = 102), the phytoplankton bloom consisted of P. agardhii (average total abundance 49.4 x 10[^6] ind. L[^-1]) and ten other taxa of Cyanobacteria, Bacillariophyceae, Chlorophyceae and Cryptophyceae (average total abundance 17.9 x 10[^6] ind. L[^-1]). The total phytoplankton abundance was 1.5 times higher in summer than in winter and the total biomass of the most abundant species was approximately 4 times higher in warm (139.8 mg L[^-1]) than in cold season (32.5 mg L[^-1]). The values of the Shannon-Weaver diversity index were very low, however, over 2 times higher in summer (0.60) than in winter (0.31). The obtained results revealed that in the hypertrophic lake the very high nutrient concentrations (especially NH[4]-N and PO[4]-P), found both in winter and summer, were responsible for year-long mass development of phytoplankton. The winter phytoplankton was composed mainly of very small centric diatoms, whereas summer blooms were created by filamentous cyanobacteria (mainly Oscillatoriales; 98%).