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The experimental data, again, support the proposed mixed modes of particle nucleation when [S] > CMC.
Conductivity measurements during polymerization also support the mixed modes of particle nucleation.
An accurate root-searching computer programme has been used to find the natural frequencies and corresponding modes of particle displacement.
The mixed modes of particle nucleation (micellar and homogeneous nucleation) were proposed when the surfactant concentration ([S]) is above its critical micelle concentration (CMC).
When the surfactant concentration ([S]) is above its critical micelle concentration (CMC), the mixed modes of particle nucleation (micellar and homogeneous nucleation) are operative in the polymerization system.
These model experiments dramatically reveal the primary modes of particle deformation and the nature of the morphologies at short mixing times.
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Below 57 km, three modes of particles were described by Knollenberg and Hunten (1980).
The LCPS observations are calculated using the three modes of particles defined by Knollenberg and Hunten (1980) and are designated in all cases as diamonds.
In situ observations of the condensational clouds by Pioneer Venus LCPS suggest that two size modes of particles are seen above 57 km, while three modes are seen between 48 and 57 km (Knollenberg and Hunten 1980; Blamont et al. 1986).
The LCPS data were interpreted to show that two modes of particles were found above an altitude of about 57 km (Knollenberg and Hunten 1980), with modal radii being consistent with those found via polarimetry (Kawabata et al. 1980).
Carlson et al. identified five branches of m parameter in Galileo/NIMS data and interpreted them as variations in mixing ratio of two distinctive modes of particles (one is ({sim} 3,upmu hbox {m}) and another is ({sim} 7,upmu hbox {m}) in diameter).
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