Mechanical resuspension of autochthonous calcite (Seekreide) failed to control internal phosphorus cycle in a eutrophic lake

Citation
M. Hupfer et al., Mechanical resuspension of autochthonous calcite (Seekreide) failed to control internal phosphorus cycle in a eutrophic lake, WATER RES, 34(3), 2000, pp. 859-867
Citations number
26
Categorie Soggetti
Environment/Ecology
Journal title
WATER RESEARCH
ISSN journal
00431354 → ACNP
Volume
34
Issue
3
Year of publication
2000
Pages
859 - 867
Database
ISI
SICI code
0043-1354(200002)34:3<859:MROAC(>2.0.ZU;2-R
Abstract
The attempt to restore the highly eutrophic Lake Arendsee (Germany) by mean s of artificial resuspension of calcareous mud (Seekreide) and capping of t he natural bottom sediments in 1995 did not show the expected effects of de creasing the phosphorus (P) content in the water body. To understand this, the sorption characteristics and the mechanisms of P uptake of Seekreide we re studied with laboratory experiments. These experimental results were com bined with model simulations at field conditions to evaluate the efficiency of Seekreide for controlling the P cycle in the lake. The littoral deposit s of Seekreide in Lake Arendsee mainly consist of calcite (70-87% dw) and a re characterised by low contents of organic matter (5-8% dw), total P (0.13 -0.47 mg g(-1) dw) and iron (3.2-3.8 mg g(-1) dw). Phosphorus uptake under laboratory conditions could be described with Langmuir sorption isotherms. A substantial portion of this uptake was not due to sorption to the CaCO3 s urfaces but to iron oxihydroxides, since most P was found in the reductant- soluble fraction (BD-P). Although the theoretical maximum of sorbed P range d between 0.19 and 0.22 mg g(-1) dw, no substantial P uptake occurred under held conditions. The model predicted that resuspension of about 25,000 ton s of littoral sediment would transiently remove not more than 0.3 tons of P from the water column (1.3% of TPtake) during sedimentation. After deposit ion of resuspended Seekreide, anaerobic conditions prevented any additional P retention. The close agreement of laboratory based simulations with fiel d observations indicates: (1) capping of the lake sediments did not signifi cantly prevent P-release, and, therefore (2) the -negligible- total effect of the large scale treatment and the failure to decrease P concentration in Lake Arendsee may be explained by and predictable from P uptake experiment s, only (C) 2000 Elsevier Science Ltd. All rights reserved.