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    Field Calibration of a Microhole Potentiostatic Oxygen Sensor for Oceanic CTDs

    Source: Journal of Atmospheric and Oceanic Technology:;1995:;volume( 012 ):;issue: 002::page 390
    Author:
    Thomas, F. I. M.
    ,
    Atkinson, M. J.
    DOI: 10.1175/1520-0426(1995)012<0390:FCOAMP>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: A new type of oxygen sensor for use on oceanic profiling CTDs has a response time that ranges from 0.4 to 0.7 s, depending on temperature. This oxygen (O2) sensor was calibrated in the field against O2 concentrations that were determined from Winkler titrations of Niskin-bottle water samples. Calibration coefficients were obtained from single casts and composite casts. When casts were calibrated separately, the mean error in predicting O2 concentrations was 1.22 ± 0.72 µM O2, n = 19 casts, and was not significantly different from the error between Niskin-bottle samples, which was 1.01 ± 2.33 µm O2, n = 33 triplicate or duplicate bottles. When casts wore combined into a composite cast for an entire cruise, however, the mean error in the calibrations increased to 5.03 ± 4.06 µm O2, n = 19 casts. These results also indicate that only three Niskin bottles on a cast are required to obtain an error of 1.0 µm in predicted oxygen. For routine use, we recommend calibrating each cast separately using either three or four measured O2 concentrations to obtain calibration coefficients.
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      Field Calibration of a Microhole Potentiostatic Oxygen Sensor for Oceanic CTDs

    URI
    http://yetl.yabesh.ir/yetl1/handle/yetl/4145435
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    • Journal of Atmospheric and Oceanic Technology

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    contributor authorThomas, F. I. M.
    contributor authorAtkinson, M. J.
    date accessioned2017-06-09T13:58:57Z
    date available2017-06-09T13:58:57Z
    date copyright1995/04/01
    date issued1995
    identifier issn0739-0572
    identifier otherams-1033.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4145435
    description abstractA new type of oxygen sensor for use on oceanic profiling CTDs has a response time that ranges from 0.4 to 0.7 s, depending on temperature. This oxygen (O2) sensor was calibrated in the field against O2 concentrations that were determined from Winkler titrations of Niskin-bottle water samples. Calibration coefficients were obtained from single casts and composite casts. When casts were calibrated separately, the mean error in predicting O2 concentrations was 1.22 ± 0.72 µM O2, n = 19 casts, and was not significantly different from the error between Niskin-bottle samples, which was 1.01 ± 2.33 µm O2, n = 33 triplicate or duplicate bottles. When casts wore combined into a composite cast for an entire cruise, however, the mean error in the calibrations increased to 5.03 ± 4.06 µm O2, n = 19 casts. These results also indicate that only three Niskin bottles on a cast are required to obtain an error of 1.0 µm in predicted oxygen. For routine use, we recommend calibrating each cast separately using either three or four measured O2 concentrations to obtain calibration coefficients.
    publisherAmerican Meteorological Society
    titleField Calibration of a Microhole Potentiostatic Oxygen Sensor for Oceanic CTDs
    typeJournal Paper
    journal volume12
    journal issue2
    journal titleJournal of Atmospheric and Oceanic Technology
    identifier doi10.1175/1520-0426(1995)012<0390:FCOAMP>2.0.CO;2
    journal fristpage390
    journal lastpage394
    treeJournal of Atmospheric and Oceanic Technology:;1995:;volume( 012 ):;issue: 002
    contenttypeFulltext
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