Summary
In accordance withKöhler's theory, considerable supersaturation is needed to get the entire body of condensation nuclei to grow into droplets; the degree of saturation is determined by the size of the individual nuclei and their solubility in the condensed liquid. Since it is known that in expansion meters all the atmospheric particles which count as condensation nuclei do in fact grow into droplets, it may be assumed that the designated supersaturation in the expansion chambers is achieved for at least a short space of time. The formation of the theoretically correct degree of supersaturation requires, however, that once the moisture saturation has been exceeded condensation should markedly lag behind pressure variation, in order to allow time for the requisite supersaturation to develop.
Experiments designed to test this question have established that condensation follows extraordinarily quickly on variation of pressure after moisture saturation has been exceeded. Condensation is also virtually uninfluenced by the choice of vapour used. At very high expansion speeds the condensation process is governed by the operative laws of diffusion. Measurements indicate that the degrees of supersaturation occurring in the expansion chambers lie considerably below the level of critical saturation even for the smallest nuclei.
Abbreviations
- dp :
-
Druckänderung
- I :
-
an der Photozelle wirksame Strahlungsintensität zu einem beliebigen Zeitpunkt [erg/cm2·s];
- I 0 :
-
wieI, jedoch zu Beginn der Expansion [erg/cm2·s];
- i :
-
van't Hoffscher Faktor;
- M i :
-
Molekulargewicht des Stoffesi [g/Mol];
- m i :
-
Menge des Stoffesi [g];
- P o :
-
Atmosphärendruck [dyn/cm2];
- p * :
-
p 0+dp [dyn/cm2];
- r :
-
Radius der Tröpfchen [cm];
- r kr :
-
Kritischer Gleichgewichtsradius [cm];
- S :
-
Übersättigung;
- S kr :
-
kritische Gleichgewichtsübersättigung;
- T :
-
Temperature [0K];
- ϱi :
-
Dichte des Stoffesi [g/cm3];
- ϱi/j :
-
Oberflächenspannung voni gegenj [dyn/cm]
ReferencesLiteraturverzeichnis
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Chr. Junge, Ann. Met.3, 129 (1950).
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B. J. Mason,The Physics of Clouds (Clarendon Press, Oxford 1957).
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W. A. Mordy undC. Rooth, Vortrag am 3. Symposium über Kondensationskerne in Cambridge, erscheint demnächst in Tellus.
H. Mache, Met. Z.50, 393 (1933).
Additional information
Osservatorio Ticinese della Centrale Meteorologica Svizzera.
Forschungsstelle am Osservatorio Ticinese der Eidgenössischen Kommission zum Studium der Hagelbildung und der Hagelabwehr.
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Bernasconi, S., Gotsch, G. & Locarno-Monti Über die Kondensation verschiedener Dämpfe bei adiabatischer Expansion. Journal of Applied Mathematics and Physics (ZAMP) 10, 509–519 (1959). https://doi.org/10.1007/BF01601359
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DOI: https://doi.org/10.1007/BF01601359