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  • 1
    Electronic Resource
    Electronic Resource
    Oxford UK : Blackwell Science Ltd
    Freshwater biology 47 (2002), S. 0 
    ISSN: 1365-2427
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Biology
    Notes: 1. Whitemere, a kettle-hole lake in north-west England (zm,14 m, area 22.5 ha) has extremely high maximal concentrations (around 1 mg L−1) of total phosphorus (TP) and soluble reactive phosphorus (SRP), and comparatively low maximal concentrations of dissolved inorganic nitrogen (〈0.5 mg N L−1). Bioassays indicate that its phytoplankton is nitrogen limited, and it has surface blue-green algal blooms in summer. Palaeoecological investigations have shown that high populations of cyanophytes occurred more than 6000 years ago, even before human settlement of the catchment.2. The reasons for this combination of features are not immediately clear. This paper attempts to distinguish between two hypotheses: that the high phosphorus concentrations arise from input of phosphate-rich groundwater; and that the high phosphorus concentrations arise from concentration and recycling mechanisms within the lake.3. The lake is entirely fed by ground water, direct rainfall and surface sheet flow. The concentrations of phosphorus in the ground water are much lower than in the lake water. The lake is stratified and has high phosphorus concentrations in the anaerobic hypolimnion in summer as a result of substantial release from the sediment. Vertical turbulence in the relatively weakly stratified water column may transfer substantial amounts to the epilimnion.There is also substantial phosphorus release from the sediments under the aerobic epilimnion.4. There is little outflow of water and phosphorus. Most of the phosphorus is returned to the sediment under winter isothermal conditions, to be released again the following summer. The lake has probably maintained these mechanisms for millennia. Recent eutrophication is likely to have been driven by nitrogen inputs from greater intensification of agriculture in the catchment.
    Type of Medium: Electronic Resource
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  • 2
    ISSN: 1573-5117
    Keywords: lake ; depth ; eutrophication ; restoration
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology
    Notes: Abstract Previous work on a set of small lakes, of varying depth, themeresof North West England, has shown that nitrogen availabilitycontrols the summer phytoplankton populations in the deeperones(max depth〉3 m) and zooplankton grazing in shallow ones. Themeres have generally high total phosphorus concentrations andthismay be a natural phenomenon dependent on the localgeochemistry.Some anthropogenic eutrophication has occurred, however, andfroma chain of three meres, sewage effluent was diverted in 1991.Theupper lake, Mere Mere, lying above the point of discharge, hasnotchanged in any systematic way since effluent diversion. Themiddlelake, the very shallow Little Mere, has changed markedly inwaterchemistry but not fundamentally in ecosystem structure. It wasandremains a clear-water, macrophyte dominated lake. The thirdlake,the deep Rostherne Mere, has shown no response inchlorophyll a concentrations in four years since effluent diversionthough inthe past two years there appears to be a downward trend intotalphosphorus. The reasons for this are explored in terms of ourunderstanding of lake eutrophication. Comparisons are madewithWhite Mere, a deep groundwater fed lake with a long retentiontimeand a very high total phosphorus concentration. The deep meresmayadd a new dimension to our understanding of natural andanthropogenic eutrophication.
    Type of Medium: Electronic Resource
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