scholarly journals Nucleation of Surfactant–Alkane Mixed Solid Monolayer and Bilayer Domains at the Air–Water Interface

Materials ◽  
2022 ◽  
Vol 15 (2) ◽  
pp. 485
Author(s):  
Hiroki Matsubara ◽  
Rikako Mori ◽  
Eisuke Ohtomi

We investigated the wetting transitions of tetradecane and hexadecane droplets in dodecyltrimethylammonium bromide (C12TAB), tetradecyltrimethylammonium bromide (C14TAB), and hexadecyltrimethylammonium bromide (C16TAB) aqueous solutions. By varying the surfactant concentration, the formation of mixed monolayers of a surfactant and an alkane was observed at the air–water interface. Depending on the combination of surfactant and alkane, these wetting monolayers underwent another thermal phase transition upon cooling either to a frozen mixed monolayer (S1) or a bilayer structure composed of a solid monolayer of a pure alkane rested on a liquid-like mixed monolayer (S2). Based on the phase diagrams determined by phase modulation ellipsometry, the difference in the morphology of the nucleated S1 and S2 phase domains was also investigated using Brewster angle microscopy. Domains of the S1 phase were relatively small and highly branched, whereas those of the S2 phase were large and circular. The difference in domain morphology was explained by the competition of the domain line tension and electrostatic dipole interactions between surfactant molecules in the domains.

Langmuir ◽  
1998 ◽  
Vol 14 (8) ◽  
pp. 2139-2144 ◽  
Author(s):  
J. Penfold ◽  
E. Staples ◽  
I. Tucker ◽  
L. Soubiran ◽  
A. Khan Lodi ◽  
...  

Ocean Science ◽  
2013 ◽  
Vol 9 (2) ◽  
pp. 355-375 ◽  
Author(s):  
V. M. N. C. S. Vieira ◽  
F. Martins ◽  
J. Silva ◽  
R. Santos

Abstract. A numerical tool was developed for the estimation of gas fluxes across the air–water interface. The primary objective is to use it to estimate CO2 fluxes. Nevertheless application to other gases is easily accomplished by changing the values of the parameters related to the physical properties of the gases. A user-friendly software was developed allowing to build upon a standard kernel a custom-made gas flux model with the preferred parameterizations. These include single or double layer models; several numerical schemes for the effects of wind in the air-side and water-side transfer velocities; the effects of atmospheric stability, surface roughness and turbulence from current drag with the bottom; and the effects on solubility of water temperature, salinity, air temperature and pressure. An analysis was also developed which decomposes the difference between the fluxes in a reference situation and in alternative situations into its several forcing functions. This analysis relies on the Taylor expansion of the gas flux model, requiring the numerical estimation of partial derivatives by a multivariate version of the collocation polynomial. Both the flux model and the difference decomposition analysis were tested with data taken from surveys done in the lagoon system of Ria Formosa, south Portugal, in which the CO2 fluxes were estimated using the infrared gas analyzer (IRGA) and floating chamber method, whereas the CO2 concentrations were estimated using the IRGA and degasification chamber. Observations and estimations show a remarkable fit.


Atmosphere ◽  
2020 ◽  
Vol 11 (10) ◽  
pp. 1057
Author(s):  
Marc L. Mansfield

When they dissolve in water, aldehydes become hydrated to gem-diols: R−COH+H2O↔RCH(OH)2. Such reactions can complicate air–water transport models. Because of a persistent belief that the gem-diols do not exist in the vapor phase, typical models do not allow them to pass through the air–water interface, but in fact, they do. Therefore, transport models that allow both molecular forms to exist in both phases and to pass through the interface are needed. Such a model is presented here as a generalization of Whitman’s two-film model. Since Whitman’s model has fallen into disuse, justification of its use is also given. There are hypothetical instances for which the flux predicted by the current model is significantly larger than the flux predicted when models forbid the diol form from passing through the interface. However, for formaldehyde and acetaldehyde, the difference is about 6% and 2%, respectively.


Langmuir ◽  
1995 ◽  
Vol 11 (8) ◽  
pp. 3167-3176 ◽  
Author(s):  
A. Angelova ◽  
M. Van der Auweraer ◽  
R. Ionov ◽  
D. Vollhardt ◽  
F. C. De Schryver

Author(s):  
Karen A. Flack ◽  
Geoffrey B. Smith

Surface temperature fields and statistics are presented for the case of sub-surface grid-generated turbulence impacting an air/water interface. Temperature measurements are obtained with an infrared camera, sensitive in the 3–5 micron wavelength range. Results indicate that increased grid oscillation frequencies, and shallower grid depths, lead to increased surface mixing, yielding lower values of RMS temperature. Non-dimensionalization of the RMS temperatures using the difference in the average surface and the bulk fluid temperatures, collapses the data obtained for different grid depths and oscillation frequencies. This scaling is related to the thermal boundary layer thickness. The results are compared to the baseline case of turbulence due to evaporative convection without an oscillating grid.


Langmuir ◽  
1999 ◽  
Vol 15 (7) ◽  
pp. 2484-2492 ◽  
Author(s):  
Juan M. Rodríguez Patino ◽  
Cecilio Carrera Sánchez ◽  
M. Rosario Rodríguez Niño

Sign in / Sign up

Export Citation Format

Share Document