4.5 Article

The Effect of Pseudofrazil Particle Entrainment on Salinity Measurements

Journal

EARTH AND SPACE SCIENCE
Volume 10, Issue 1, Pages -

Publisher

AMER GEOPHYSICAL UNION
DOI: 10.1029/2022EA002564

Keywords

supercooling; frazil ice; conductivity measurements; particles in conductivity cells; ice-ocean interaction; salinity measurements in high latitudes

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The effects of particles, such as suspended sediments or small ice crystals, on conductivity cells have been studied. These particles can affect the measurements of conductivity, salinity, and supercooling. Entraining microplastics into conductivity cells can simulate the effect of ice crystals, and the results show that it can lead to significant changes in conductivity and supercooling measurements. Correcting for the presence of these particles is important in accurately measuring salinity in high frazil concentration areas.
Salinity effects of particles entrained into conductivity cells have previously mainly been studied in the context of suspended sediment. Particles influencing conductivity cells can also be small ice crystals (frazil) that may form in supercooled water. The detection of supercooled water depends on accurate, high precision temperature, salinity and pressure measurements. As it is currently not possible to measure salinity in situ, the standard procedure is to measure conductance over a known volume and calculate salinity. Frazil ice entrained into a conductivity cell changes the volume of conductive fluid in the conductivity cell, thus changing the conductivity, salinity and supercooling measurements. We present results on the effect of entraining microplastic into a Sea-Bird Electronics conductivity cell to simulate the effect of frazil. We show that particle volumes comparable to frazil volumes observed in the ocean change the measured conductivity and led to changes in calculated supercooling between 0.3 and 10 mK, possibly up to the same order of magnitude as naturally observed supercooling in the ocean. Further, we demonstrate that where supercooling is present, natural frazil ice concentrations can have an appreciable effect on parameters calculated with both the Equation of State of Seawater 1980 and Thermodynamic Equation of Seawater 2010 equations of state of seawater. Thus, to ensure accurate measurements in locations of very high frazil concentration, the entrainment of frazil needs to be prevented, which is not possible with methods currently available, or corrected for. An example for such a correction is given and could be modified to be applicable to other particles, for example, sediment.Supercooling in the ocean (water colder than its freezing point but still liquid) has wide-ranging impacts on heat and salt transport, both in the water and in neighboring ice shelves and sea ice. However, oceanographic instruments currently in use are not designed to measure supercooling. Small ice crystals called frazil ice, which may form in supercooled water, led to falsely low salinity measurements which leads to falsely high levels of supercooling being recorded. Here we present a study that quantifies the salinity effect of frazil ice in seawater by studying the effect of plastic particles with similar material properties as frazil ice. We present measurements and calculations which can be used to correct for this effect in certain novel instruments or where frazil/particle concentration and conductivity is known. This research is of interest not only for oceanographers working in high latitude oceans but also for those working in waters with suspended matter such as sediments in estuaries and requiring highly accurate salinity values. To facilitate this, we compare our results to previously published studies of the effect of sediment-water mixtures flushed into conductivity cells.

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