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Analysis of events leading to frostbite

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Abstract

Upon exposure of the middle phalanx of the finger to air at -10° to-15°C moving at 10 m/sec, the surface temperature cooled not toward air temperature but toward a higher temperature, T′ = (Ta + τ). This was due to heat input, about 118 joule over 4.3 min, by conduction from the proximal and distal phalanges not exposed to the cold air. Calculated thermal constants for the finger are somewhat different from those for water and account for the rapidity of the cooling. The incidence of either freezing or cold-induced vasodilatation could not be correlated with the relative cooling rate because of the occurrence of indeterminate supercooling. Within the same range of supercooled temperatures, freezing occurred in 16 cases, cold induced vasodilatation in 7 cases, and nothing in 3 cases. The factors which induce crystallization on the one hand or vasodilatation on the other hand, remain to be discovered.

Zusammenfassung

Wenn das Mittelglied eines Fingers einer Temperatur von -10° bis -15°C bei einem Wind von 10 m/sec ausgesetzt wurde, kühlte die Hauttemperatur nicht bis zur Lufttemperatur, sondern bis zu einer höheren Temperatur T′ = (Ta + τ) ab. Dies war Folge des Wärmezuflusses, etwa 118 joule über 4.3 min, durch Konduktion von den nicht exponierten proximalen und distalen Fingergliedern. Die berechneten Wärmekonstanten für den Finger waren verschieden von denen für Wasser und erklären die Schnelligkeit der Abkühlung. Die Häufigkeit von Erfrieren oder kältebedingter Gefässerweiterung liess sich wegen des Auftretens unbestimmter Ueberkühlung nicht mit der relativen Abkühlungsrate korrelieren. Innerhalb des gleichen Bereiches überkühlter Temperaturen traten in 16 Fällen Erfrierungen, in 7 Fällen kältebedingte Gefässerweiterung und in 3 Fällen nichts auf. Die Faktoren die entweder Kristallisation oder Gefässerweiterung bedingten, sind unbekannt.

Resume

Lorsque l'on expose la deuxième phalange à une température de -10° à -15°C par un vent de 10 m/sec, sa température de surface ne s'abaisse pas jusqu'à celle de l'air ambiant, mais seulement jusqu'à une valeur T′ = (Ta + τ). Ceci est dû à l'échange de chaleur — environ 118 joules pour 4,3 min — provenant de la troisième et de la première phalange non exposées à l'air froid. Les constantes thermiques calculées sont différentes de celles de l'eau, ce qui explique le refroidissement rapide du corps humain. Les causes de gelure ou de vasodilatation due au froid ne peuvent pas être mises en corrélation avec le taux de refroidissement relatif en raison de l'apparition inexpliquée de phénomènes de surrefroidissement. Dans le même intervalle de températures basses, on a constaté 16 cas de gelures, 7 de vasodilatation due au froid et, dans 3 cas, aucune modification n'est apparue. Les faits qui provoquent soit la cristallisation, soit la vasodilatation ne sont pas connus jusqu'ici.

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Molnar, G.W., Wilson, O. & Goldman, R.F. Analysis of events leading to frostbite. Int J Biometeorol 16, 247–258 (1972). https://doi.org/10.1007/BF01553736

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