Results
Figure 3 plots transmission and backscattering intensities against the position within the two polystyrene suspensions. The colour-coding of the curves indicates the time at which they were recorded, from red (first measurement, t = 0 s) to purple (last measurement, t = 1 h). Every curve represents an individual measurement.
The transmission and backscattering diagrams in Figure 3 show clearly time-dependent as well as position-dependent changes of the signal, indicating a typical sedimentation process. One can see that the changes in transmission and backscattering of PS1 are much slower than those of PS2, owing to the smaller particle size of PS1 particles.
With the respective function in the MSC software, the change of the migration front can be analysed utilising transmission and backscattering signals, resulting in an average sedimentation rate of 0.6262 mm/min for the PS1 suspension (Figure 4 left). According to the above theory, the mean particle diameter of PS1 can now be obtained by simply clicking on ‘calculate’ within the software (Figure 4 right). Note that the trigger line (intersection line) in the migration front method for measuring the sedimentation rate is usually set at the median of transmission or backscattering values (Figure 3, purple dotted line), in this case at Tr = 50% for PS1, to ensure the accuracy of the calculation for the mean particle diameter.
Accordingly, sample PS2 was analysed, leading to the sedimentation rate and mean particle size as displayed in Table 2. The particle diameters of PS1 and PS2 are 19.88 µm and 39.54 µm, respectively. Notably, the calculated particle diameters of the two samples are almost the same as the values given by the producer (Table 1), which confirms that is it possible to calculate mean particle diameter utilising the sedimentation rate.
Furthermore, the mean particle diameters of PS1 and PS2 were calculated using backscattering signals by setting the trigger line at the median value of around 15 %. As shown in Table 2, the mean particle diameters calculated this way are around 20 µm (PS1) and 40 µm (PS2), which are similar to the results obtained using the transmission signals earlier. It can be concluded that the changes in both transmission and backscattering signals are able to be used for evaluating mean particle size utilising the sedimentation rate.
Evidently, the above results underline the excellent applicability of MultiScan MS 20 not only to analyse stability issues, but also to calculate mean particle size with high validity.