Ice fraction level of superchilled salmon
Superchilling is a process by which the temperature of a food product is lowered to 1-2 ˚C below the initial freezing point of the product. The ice formed on the surface will absorb heat from the interior and will eventually reach equilibrium. A fraction of the water is transformed to ice and is used to protect it from heat impact instead of using surrounding ice. It has been shown that superchilling can increase the shelf life of fish and meat products without the same reduction in quality as seen during normal freezing.

At present there exist only calorimetric techniques to measure the ice fraction, which are far too laborious and time consuming for online applications.  Using NIR, in the wavelength range from 760nm to 1040nm, it is possible to detect shifts that occur in the second order water peak as the ice fraction level increases. By using non contact scanning it is possible to cope with the equilibrium state of the salmon, which is sensitive to external temperature changes when handled.

Norwegian Atlantic Salmon (Salmo salar), originating from a fish farm in mid-Norway, were used for the experiment. The fish was filleted and packed by Lerøy Midnor, Hitra, 5 to 7 days before superchilling and stored on ice. Superchilling was performed in a wind tunnel with an air velocity of 2 m/s, a temperature of -25 °C and at different time intervals in order to reach ice levels of 5, 10, 20 and 30 % in the salmon fillets.  NIR measurements were performed on superchilled samples immediately after using the non-line imaging scanner from QVision. The ice fraction level in the salmon fillets was determined using calorimetric methods. The level of ice in the product was estimated based on the temperature change as it melted and information about the product’s thermal and physical properties. A Partial Least Squares Model was built and with an estimated root mean square error (RMSEP) of the ice fraction model was 2.5%, and a correlation of 0.96.

If you are interested in more information please contact Marion O'Farrell .


Shift in water peak due to change in ice fraction level.


Published December 18, 2008



Scanner images with ice percentage from both PLS model and calorimeter methods (PLS% / Calorimeter%).