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This work presents the results of research on physico-chemical and microbiological amounts of heterotrophic bacteria, Actinomycetes, filamentous and yeast fungi in underground waters of aquifers of Omulewskie Reservoir in the Mazurian Lake District in 1989-1992/1993. The examination included water from 11 wells (20-64 m) and 3 piezometric bore-holes (6.5-23.5 m) on woodland (control well), managed by individual farmers and on large farms. Colour of water, pH, dry mass, and total hardness of the examined water samples did not exceed the values accepted for natural hydrochemical background. Electrolytic conductivity rarely exceeded 400 μS/cm. The concentration of the main cations and anions classifies the waters of the examined wells into four types: 1. carbonate-calcium-magnesium; 2. carbonate-calcium; 3. carbonate-chloride-calcium and 4. carbonate-calcium-sulphate. The concentration of oxygen was the lowest in the water from wells situated on large farms, the highest on the area of woodland; on the contrary BOD5. Oxidability only in the water of the wells on the woodland area was the same as the values accepted for the natural hydrochemical background. The amount of total nitrogen was the lowest in the water from the wells situated on large farms and it was correlated with respectively low or high amounts of total phosphorus. The amount of iron reached higher values only in the water of some wells on the area of large farms. Heterotrophic bacteria with higher optimal temperatures and oligotrophic bacteria were the most numerous among heterotrophic microorganisms. Actinomycetes and filamentous fungi were rare and in minimal quantities. There were more yeast fungi, especially those which did not produce carotenoid dyes.
Studies were made on the content of nitrogen substances and chlorides, as well as the counts of ammonifying, nitrifying and denitrifying bacteria in the underground waters of water-bearing formations in the Omulewski Aquifer in Mazuria. Water samples were collected from 11 water-wells (20-67 m deep) and 3 piezometric wells (bore-holes) (6.8-23.5 m). These wells were located in forested areas at Sedańsk and Narty, areas used by individual farmers at Jedwabno and Kot, and in commercial agricultural and animal breeding farms at Janowo, Dzierzki, Wesolówko, Wielbark, Przezdzięk, Baranowo and Wyżegi. Organie nitrogen (0.01-5.07 mg/dm3), NH4-N (<0.01-7.70 mg/dm3), N02-N (<0.001-0.192 mg/dm3) and N03-N (<0.01-29.00 mg/dm3) content in water samples collected from water-wells and piezometric bore-holes varied depending on land use and sampling date. Underground waters were less polluted by these substances in forested land and more on arable land. Numbers of bacteria of the nitrogen cycle usually did not exceed 14000 MPN/1 cm3 (bacteria liberating NH3 and H2S from peptone), 2400 (Nitrobacter), 11000 (bacteria reducing N03-N to N02-N), 14000 (bacteria reducing N02-N to NH4-N), 46000 (bacteria reducing N02-N to N2/N20) and 140000 (Nitrosomonas and bacteria reducing NO3 —N to gaseous nitrogen) MPN/100 cm3. Frequently these bacteria were not found in volume water inoculations. There were also no clear relationships between well depth and the content of nitrogen compounds, chlorides and nitrogen cycle bacteria.
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