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Sediment and pore water composition as a basis for the trophic evaluation of standing waters

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Abstract

Sediments and pore water samples from four reservoirs in eastern Germany with different trophic characteristics have been examined (Neunzehnhain I – oligotrophic; Muldenberg – oligotrophic, dystrophic; Saidenbach – mesotrophic; Quitzdorf – highly eutrophic). Several parameters were analyzed regarding the dependence on the trophic state and the possibility to use them for the trophic evaluation of standing waters. The strongest influence of the trophic state could be found in the case of the parameters SRP, alkalinity and ammonium in the pore water. For the dry sediment, it could be concluded that the most important factor affecting the trophic state is the ratios of Fe:P and Al:P, which were summarized to a metal:phosphorus sum ratio (MPS) and showed a clear threshold value for the potential to immobilize phosphorus in the sediment. Also, with the P fractions of the sediment samples, differences between the trophic levels became evident. Higher percentages of the reductively soluble, iron-bound fraction and of the biogenic fraction occurred in the reservoirs with higher trophic state, while comparitively higher percentages of the stable aluminum-bound fraction could be measured in the reservoirs with lower trophic state.

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Abbreviations

BD:

bicarbonate-dithionite-extractant

DW:

dry weight

MPS:

metal:phosphorus sum ratio

Mul:

Muldenberg

Neu:

Neunzehnhain

NRP:

non-reactive phosphorus

POC:

particulate organic carbon

Qui:

Quitzdorf

R.:

reservoir

Sai:

Saidenbach

SRP:

soluble reactive phosphorus

TP:

total phosphorus

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Maassen, S., Uhlmann, D. & Röske, I. Sediment and pore water composition as a basis for the trophic evaluation of standing waters. Hydrobiologia 543, 55–70 (2005). https://doi.org/10.1007/s10750-004-5946-0

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