Staff Publications

Staff Publications

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    'Staff publications' is the digital repository of Wageningen University & Research

    'Staff publications' contains references to publications authored by Wageningen University staff from 1976 onward.

    Publications authored by the staff of the Research Institutes are available from 1995 onwards.

    Full text documents are added when available. The database is updated daily and currently holds about 240,000 items, of which 72,000 in open access.

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Record number 489819
Title Iron Addition as a shallow lake restoration measure: impacts on charophyte growth
Author(s) Immers, A.K.; Sande, M.T. van der; Zande, R.M. van der; Geurts, J.J.M.; Donk, E. van; Bakker, E.S.
Source Hydrobiologia 710 (2013). - ISSN 0018-8158 - p. 241 - 251.
Department(s) Forest Ecology and Forest Management
Plant Ecology and Nature Conservation
Publication type Refereed Article in a scientific journal
Publication year 2013
Keyword(s) fresh-water wetlands - potamogeton-pectinatus - aquatic plants - submerged macrophytes - chara - netherlands - phosphorus - phosphate - toxicity - biomanipulation
Abstract Eutrophication has caused a decline of charophyte species in many shallow lakes in Europe. Even though external inputs of phosphorus are declining, internal loading of P from the sediment seems to delay the recovery of these systems. Iron is a useful chemical binding agent to combat internal phosphorus loading. However, the effects of iron addition on charophytes are not yet known. In this study we experimentally tested the potential toxicity of iron(III)chloride (FeCl3) on two different charophytes, Chara virgata Ku¨tzing and Chara globularis Thuiller added at the concentration of 20 g Fe m-2 and 40 g Fe m-2 to the surface water. C. virgata growth was not significantly affected, whereas C. globularis growth significantly decreased with increasing iron concentrations. Nonetheless, biomass of both species increased in all treatments relative to starting conditions. The decrease of C. globularis biomass with high iron additions may have been caused by a drop in pH and alkalinity in combination with iron induced light limitation. Iron addition over a longer time scale, however, will not cause this rapid drop in pH. Therefore, we conclude that adding iron(III)chloride in these amounts to the surface water of a lake can potentially be a useful restoration method.
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