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Ammonium uptake in alpine streams in the High Tatra Mountains (Slovakia)

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Abstract

Uptake of NH sup+inf4 -N by streambed biota of mountain brooks was studied in the alpine zone of the High Tatra Mountains. Experiments were performed involving in situ dosing of ammonium directly to the acidified stream and incubations of ammonium and streambed bryophytes in enclosures within a range of pH from 4.45 to 8.10.

NH sup+inf4 -N uptake length decreased with decreasing stream discharge, while comparable values of discharge-normalized uptake lengths were found during two in situ experiments.

Maximum uptake rates of NH sup+inf4 -N obtained during the incubation of bryophytes (6 to 11 mg m−2 h−1) were comparable with results of two in situ experiments (8 and 12 mg m−2 h−1). The average NH sup+inf4 -N uptake rates observed during incubations lasting 3 to 5 hours (4.3 mg m−2 h−1) were not related to the pH of stream water. Nitrification of about 50% of the NH sup+inf4 -N added was observed in non-acidified streams, but was negligible in acidified streams. Significant photoinhibition of nitrification was observed in non-acidified streams during enclosure experiments.

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Kopáček, J., Blažzka, P. Ammonium uptake in alpine streams in the High Tatra Mountains (Slovakia). Hydrobiologia 294, 157–165 (1994). https://doi.org/10.1007/BF00016856

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