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  • Oxygen  (1)
  • lake level  (1)
  • Springer  (2)
  • 1
    Electronic Resource
    Electronic Resource
    Springer
    Hydrobiologia 339 (1996), S. 149-160 
    ISSN: 1573-5117
    Keywords: lake level ; Seiche ; sediment resuspension and focusing
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology
    Notes: Abstract The surface level of Lake Kinneret is regulated to remain between −209 m and −213 m msl. During the stratified period, soluble reactive phosphorus (SRP), ammonium (NH inf4 sup+ ) and dissolved sulphide (H2S) accumulate in the hypolimnion. The concentration of these solutes, which are direct and indirect products of the decomposition of organic matter, increase considerably in summers with lower lake levels. A numerical model describing depth-averaged hypolimnion and epilimnion current velocities for high and low lake levels was adapted for Lake Kinneret. Simulated hypolimnetic currents were shown to be stronger for low lake levels as a result of the fact that low lake levels are characterized by a thinner hypolimnion while the thickness of the epilimnion remains unchanged. We suggest that the stronger hypolimnetic currents have the following consequences: 1. turbulence is induced, 2. the enhanced turbulence results in higher resuspension, 3. because SO4= is available to bacteria on resuspended particles, mineralization rates are enhanced, and 4. focusing of fine sediments and associated organic matter to the pelagic zone is enhanced.
    Type of Medium: Electronic Resource
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  • 2
    Electronic Resource
    Electronic Resource
    Springer
    Hydrobiologia 197 (1990), S. 99-104 
    ISSN: 1573-5117
    Keywords: Oxygen ; solubility ; brines ; temperature ; methods
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology
    Notes: Abstract The solubility of the O2 in the Dead Sea brine was determined over the temperature range 5 °C–50 °C using a modified Winkler titration, volumetric analysis, and a polarographic sensor. The solubility at room temperature and 1 atmosphere pressure was ca. 1 mg l−1, and the temperature coefficient 0.006 mg 1−1° C−1 . The data are nearly consistent with sea water solubility extrapolated to Dead Sea brine salinity.
    Type of Medium: Electronic Resource
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