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Phytoplankton-nutrient relationships during the early spring and the late autumn in a shallow and polluted reservoir

Identyfikatory
Warianty tytułu
Języki publikacji
EN
Abstrakty
EN
The reservoir where the studies were carried out was originated by modification of an old oxbow lake of the Vistula River. The most important sources of inflowing waters are industrial waters from "Puławy Fertilizer Factory". The highest variability of concentration, was NH4 +-N and also Cl-, Ntot., and PO4 -3. Some significant correlations between chemical properties of water and algae (especially green algae and diatoms) were found, which suggested that this phytoplankton was mainly responsible for the biogeochemical cycles in the shallow, strongly polluted reservoir. Another interesting phenomenon was the statistically positive correlation between the density of cyanobacteria and potassium, which suggested that it may play an important role in their abundance.
Słowa kluczowe
Rocznik
Strony
75--87
Opis fizyczny
Bibliogr. 15 poz., tab., wykr.
Twórcy
  • Polish Academy of Sciences, Institute of Freshwater Biology, Sławkowska 17, 31-016 Kraków, Poland
autor
  • Agricultural University, Institute of Soil Science and Environment Management, ul. Leszczyńskiego 7, 20-069 Lublin, Poland
Bibliografia
  • [1]. Cole G.A., 1983. Textbook of limnology, The C.V. Mosby Company. St. Louis, Toronto, London, 401.
  • [2]. Hermanowicz W., Dożańska W., Dojlido J., Koziorowski B., Zerbe J., 1999. Physico-chemical investigations of water and sewages, Arkady, Warszawa, 556.
  • [3]. Koschel R., Benndorf J., Proft G., Recknagel F., 1983. Calcite precipitation as a natural control mechanism of eutrophication, Arch. Hydrobiol., 98, 380-408.
  • [4]. Koschel R.H., 199,7. Structure and function of pelagie calcite precipitation in lake ecosystem. Verh. Internat., Verein. Limnol., 26, 343-349.
  • [5]. Lund J., Kipling W:G.D., Le Cren E.D., 1958. The inverted microscopic method of estimating algal numbers and the statistical basis of estimations by count., Hydrobiol., 11, 143-170.
  • [6]. Nalewajko C., Lean D.R.S., 1980. Phosphorus. [In]: The physiological ecology of phytoplankton, Morris I. (Ed.), Blackwell Sci. Publ. Oxford, 235-258.
  • [7]. Pliński M., 1999. Hydrobiologia-podstawy, Ocean, Dział wydawniczy Sopockiego Instytutu Ekologicznego, Sopot, 138 (in Polish).
  • [8]. Reynolds C.S., 1984. The ecology of the freshwater phytoplankton, Cambridge studies in ecology, Cambridge Univ. Press, 384.
  • [9]. Sommer U., Gliwicz Z.M., Lampert W., Duncan A., 1986. The PEG-model of seasonal succession of planktonie events in fresh waters, Arch. Hydrobiol, 106, 433-471.
  • [10]. Starmach, K., 1955. Metody badań planktonu. PWRiL, Warszawa, 133 (in Polish).
  • [11]. Staub R., 1961. Erndhrungsphysiologisch-autkologische Untersuchungen an der planktischen Blaualge Oscillatoria rubescens DC. Schweiz., Z. Hydrol., 23, 82-198.
  • [12]. Trainor F.R., 1993. Cyclomorphosis in Scenedesmus subspicatus R. Chod. Cell behavior during the unicell-colony transformation of a phenotypicly plastic organism, Arch. Protistenkd, 143, 55-61.
  • [13]. Trainor F. R., 1998. Biologicil aspects of Scenedesmus (Chlorophyceae) - phenotypic plasticity, Nova Hedwigia, 117: 1-367.
  • [14]. Wilk-Woźniak E., Kosiński M., 2001. Effect of allochthonous and autochthonous factors on phytoplankton biomass in a submontane dam reservoir (S Poland), Biologia, Bratislava, 56, 345-354.
  • [15]. Wojciechowski I., 1987. Ekologiczne podstawy kształtowania środowiska. PWN, Warszawa, 450 (in Polish).
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-article-BUS8-0013-0037
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