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Phosorus availability in an acidified watershed‐lake ecosystem
Author(s) -
Kopáček Jiřĺ,
Hejzlar Josef,
Borovec Jakub,
Porcal Petr,
Kotorova Ivana
Publication year - 2000
Publication title -
limnology and oceanography
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.7
H-Index - 197
eISSN - 1939-5590
pISSN - 0024-3590
DOI - 10.4319/lo.2000.45.1.0212
Subject(s) - alkalinity , environmental chemistry , watershed , anoxic waters , soil water , sulfate , nitrate , environmental science , ecosystem , ammonium , phosphorus , trophic state index , terrestrial ecosystem , hydrology (agriculture) , chemistry , nutrient , ecology , phytoplankton , geology , soil science , biology , geotechnical engineering , organic chemistry , machine learning , computer science
Acid precipitation has been shown to reduce phosphorus (P) outputs from terrestrial sources. We present field evidence that the in‐lake P cycle may also be disrupted in atmospherically acidified watershed‐lake ecosystems. Plešné Lake in the Bohemian Forest is an acidified forest lake with epilimnetic pH of 4.5–4.9, total P concentration of ∼10 μg L −1 , and pronounced anoxia above the bottom during winter and summer stratification periods. The water chemistry of the anoxic zone develops in a predictable way: After depletion of dissolved oxygen, concentrations of nitrate and sulfate decrease while concentrations of ammonium, iron, alkalinity, and pH increase; the only exception to the general pattern is a permanently low concentration of dissolved reactive P (<1 μg L −1 ) above the sediment. This in‐lake P inactivation can be explained by the acidification of soils in the watershed and subsequent precip‐itation of Al in the lake. The suggested mechanism is as follows: atmospheric deposition of strong acids has resulted in strong acidification and nitrogen saturation of soils in the Plešné Lake watershed and, consequently, in high terrestrial losses of Al (0.78–1.04 mg L −1 ), SO 4 2− (4.5–7.7 mg L −1 ), and NO 3 − (0.48 –1.15 mg L −1 NO 3 ‐N) to the lake. Biological removal of NO 3 − and SO 4 2− by both assimilatory and dissimilatory reduction contributes greatly to the total in‐lake alkalinity generation and to the increase in water pH. Under higher pH, ionic Al species hydrolyze and form colloidal Al hydroxides (Al part ), which coagulate dissolved organic carbon and adsorb orthophosphate in the water column. The Al hydroxides settle and increase the P sorption capacity of the sediment. The elevated content of fresh Al oxyhydroxides in the surface sediment reduces P release to the water column after orthophosphate liberation from ferric oxyhydroxides during anoxia, because Al part complexes are not sensitive to redox changes. The example of Plešné Lake shows that atmospheric acidification of a watershed‐lake ecosystem may provide the natural conditions for in‐lake P inactivation similar to the lake restoration technique based on the artificial addition of Al salt to the water column.