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    Thermal Inertia of Conductivity Cells: Theory

    Source: Journal of Atmospheric and Oceanic Technology:;1990:;volume( 007 ):;issue: 005::page 741
    Author:
    Lueck, Rolf G.
    DOI: 10.1175/1520-0426(1990)007<0741:TIOCCT>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The temperature anomaly of a fluid moving through circular and rectangular cylinders induced by the heat stored in the walls of these hollow cylinders is derived under the assumption of quasi-steady heat transfer. These geometries correspond closely to the SBE-4 conductivity cell manufactured by Sea-Bird Electronics (SBE) and the NBIS Mark III cell made by EG&G Ocean Products (NBIS). For a step change of ambient temperature, the initial volume-weighted thermal anomalies are 4.3 and 12%, and the relaxation times are 4.3 and 0.23 s, for the SBE and NBIS cells, respectively, under typical operating conditions. The error in the measured conductivity is significant both in magnitude and longevity. Ale magnitude and the relaxation time of the anomaly can be considerably reduced by increasing the rate of flow through a cell, by forcing the flow to be turbulent, and by appropriate changes in the wall thickness and material. The wall is not a source or sink of salt, consequently no analogous effect is produced by changes in the ambient salinity. The effect of the thermal inertia of the wall has not been previously reported because frequency response calibrations have been made in isothermal salt-stratified tanks. The signal reported by a conductivity cell is governed by: (i) the initial flushing by the free stream in the cell, (ii) the thermal and saline boundary layers on the wall of the cell and (iii) the heat stored in the wall of the cell. The bulk of the response is determined by the flushing of the cell, which has a time scale of order L/u≈0.05 s and should be nearly the same for conductivity changes imposed by either temperature or salinity. The boundary layer is not the same for temperature and salinity because the diffusivities of heat and salt differ by a factor of 100. The time scale of boundary layer diffusion is approximately 0.1 s for heat and 0.4 s for salt. Finally, the heat stored in the wall influences the temperature in the boundary layer. The time scale of this influence is determined by the dimensions and geometry of the cell, the thermal properties of the wall, and the flow through the cell. It is impossible, in principle, to remove transient salinity errors by merely matching the response of a conductivity cell to the response of a thermometer because the temperature and salinity responses of a cell are different.
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      Thermal Inertia of Conductivity Cells: Theory

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4201289
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    contributor authorLueck, Rolf G.
    date accessioned2017-06-09T16:05:14Z
    date available2017-06-09T16:05:14Z
    date copyright1990/10/01
    date issued1990
    identifier issn0739-0572
    identifier otherams-606.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4201289
    description abstractThe temperature anomaly of a fluid moving through circular and rectangular cylinders induced by the heat stored in the walls of these hollow cylinders is derived under the assumption of quasi-steady heat transfer. These geometries correspond closely to the SBE-4 conductivity cell manufactured by Sea-Bird Electronics (SBE) and the NBIS Mark III cell made by EG&G Ocean Products (NBIS). For a step change of ambient temperature, the initial volume-weighted thermal anomalies are 4.3 and 12%, and the relaxation times are 4.3 and 0.23 s, for the SBE and NBIS cells, respectively, under typical operating conditions. The error in the measured conductivity is significant both in magnitude and longevity. Ale magnitude and the relaxation time of the anomaly can be considerably reduced by increasing the rate of flow through a cell, by forcing the flow to be turbulent, and by appropriate changes in the wall thickness and material. The wall is not a source or sink of salt, consequently no analogous effect is produced by changes in the ambient salinity. The effect of the thermal inertia of the wall has not been previously reported because frequency response calibrations have been made in isothermal salt-stratified tanks. The signal reported by a conductivity cell is governed by: (i) the initial flushing by the free stream in the cell, (ii) the thermal and saline boundary layers on the wall of the cell and (iii) the heat stored in the wall of the cell. The bulk of the response is determined by the flushing of the cell, which has a time scale of order L/u≈0.05 s and should be nearly the same for conductivity changes imposed by either temperature or salinity. The boundary layer is not the same for temperature and salinity because the diffusivities of heat and salt differ by a factor of 100. The time scale of boundary layer diffusion is approximately 0.1 s for heat and 0.4 s for salt. Finally, the heat stored in the wall influences the temperature in the boundary layer. The time scale of this influence is determined by the dimensions and geometry of the cell, the thermal properties of the wall, and the flow through the cell. It is impossible, in principle, to remove transient salinity errors by merely matching the response of a conductivity cell to the response of a thermometer because the temperature and salinity responses of a cell are different.
    publisherAmerican Meteorological Society
    titleThermal Inertia of Conductivity Cells: Theory
    typeJournal Paper
    journal volume7
    journal issue5
    journal titleJournal of Atmospheric and Oceanic Technology
    identifier doi10.1175/1520-0426(1990)007<0741:TIOCCT>2.0.CO;2
    journal fristpage741
    journal lastpage755
    treeJournal of Atmospheric and Oceanic Technology:;1990:;volume( 007 ):;issue: 005
    contenttypeFulltext
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