Publication

Back to overview

The role of contact angle and pore width on pore condensation and freezing

Type of publication Peer-reviewed
Publikationsform Original article (peer-reviewed)
Author David Robert O., Fahrni Jonas, Marcolli Claudia, Mahrt Fabian, Brühwiler Dominik, Kanji Zamin A.,
Project Elucidating Ice Nucleation Mechanisms Relevant to the Atmosphere: Is deposition nucleation really immersion freezing in pores?
Show all

Original article (peer-reviewed)

Journal Atmospheric Chemistry and Physics
Volume (Issue) 20(15)
Page(s) 9419 - 9440
Title of proceedings Atmospheric Chemistry and Physics
DOI 10.5194/acp-20-9419-2020

Open Access

URL http://doi.org/10.5194/acp-20-9419-2020
Type of Open Access Publisher (Gold Open Access)

Abstract

Abstract. It has recently been shown that pore condensation and freezing (PCF) is a mechanism responsible for ice formation under cirrus cloud conditions. PCF is defined as the condensation of liquid water in narrow capillaries below water saturation due to the inverse Kelvin effect, followed by either heterogeneous or homogeneous nucleation depending on the temperature regime and presence of an ice-nucleating active site. By using sol–gel synthesized silica with well-defined pore diameters, morphology and distinct chemical surface-functionalization, the role of the water–silica contact angle and pore width on PCF is investigated. We find that for the pore diameters (2.2–9.2 nm) and water contact angles (15–78∘) covered in this study, our results reveal that the water contact angle plays an important role in predicting the humidity required for pore filling, while the pore diameter determines the ability of pore water to freeze. For T>235 K and below water saturation, pore diameters and water contact angles were not able to predict the freezing ability of the particles, suggesting an absence of active sites; thus ice nucleation did not proceed via a PCF mechanism. Rather, the ice-nucleating ability of the particles depended solely on chemical functionalization. Therefore, parameterizations for the ice-nucleating abilities of particles in cirrus conditions should differ from parameterizations at mixed-phase clouds conditions. Our results support PCF as the atmospherically relevant ice nucleation mechanism below water saturation when porous surfaces are encountered in the troposphere.
-