Effect of drying conditions on drying rate
Carstensen and Zoglio (
20) have suggested that, during tray drying of a bed of granular material, the reduction in liquid content with time should obey a log–lin relationship,
i.e. ln
mt/
m0 relates linearly to the drying time.
In this study, log-lin drying profiles of the agglomerates could be described as linear. Thus, the slope values from the relationship between ln
mt/
m0 and the drying time (drying rate constant , K
D) are used as measures of the drying rate of the agglomerates (
Table 1).
Carstensen and Zoglio (
20) have suggested that the slope of the log–lin drying rate profile depends on and is inversely related to bed thickness. The thickness of the particle bed was, therefore, kept approximately constant for all the series of granular materials used in this study.
| agglomerates driedat different temperatures(oC) | Drying rate constanta(min-1) | ParticleSizedln± σ (µm) | Sphericity | Particle porosity(%) | EffectiveParticle density(g/cm3) | Compressive strength (Kg/cm2) | Tensile strength of tablets(Kg/cm2) |
|---|
| 25 | 0.11 (0.99) | 951±168 | 0.89±0.04 | 20.3±0.8 | 1.03±0.02 | 4.75±0.20 | 13.8±1.6 |
| 35 | 0.13 (0.98) | 1050±237 | 0.88±0.05 | 28.6±0.9 | 0.92±0.03 | 3.99±0.21 | 18.9±1.5 |
| 45 | 0.23 (0.99) | 1237±231 | 0.87±0.06 | 33.8±1.1 | 0.86±0.02 | 3.28±0.20 | 24.3±1.4 |
| 55 | 0.32 (0.98) | 1420±226 | 0.88±0.05 | 41.6±0.9 | 0.75±0.03 | 2.72±0.18 | 27.1±1.5 |
Effect of drying rate on shape and porosity of dried particles
It has been reported that fracturing of agglomerates may occur during drying and that the drying stresses developed within the agglomerates, which can explain such fracturing, may vary according to the drying rate (
27). The dry particles were, therefore, characterized in terms of shape and appearance. Visual examination of the particles by light microscopy indicated that the particles had generally smooth surface (
Figure 1). This inspection did not reveal any cracks on the surface of the particles. In addition, there did not appear to be a general effect of drying rate on the appearance of the particles. The sphericity values (
Table 1) confirmed that the shape of the particles was not affected by the drying rate.
According to results, after drying at different rates, the final porosity of the particles was markedly different (
Table 1).
SEM photographs of the agglomerates dried with the highest (a) and the lowest (b) drying rate constant.
The effect of drying rate on the final particle porosity can be easily interpreted in terms of an effect of the drying rate on particle contraction during drying. Comparing the size of the dried agglomerates at different temperature, showed that an increase in the drying rate led to larger agglomerates (
Figure 2 and
Table 1). In other words, an increased drying rate gave more porous particles, due to decreased particle contraction during the drying process as described below.
The distribution histograms of the agglomerates dried at different temperatures
The capillary forces and subsequent compression stresses developed within agglomerate are a result of pressure gradients in the liquid in the pores (
27-
29).
It has been proposed that an increased drying rate increases the driving force for contraction
i.e. the pressure gradient in the liquid is increased (
29).
On the other hand, it can be assumed that the liquid is descending into the pores during the drying phase, i.e. at least for a fraction of the pores. The formation of dry pore surfaces may counteract contraction and thus represent a counteracting force towards contraction. The drying behavior will thus depend on the balance between the driving and the counteracting forces for contraction. It can be hypothesized that the formation of dry pore surfaces is dependent on drying rate in such a way that the evaporation of liquid is not balanced
by a contraction of the pore system, i.e. drying and subsequent contraction involves a time factor. A possible reason is that all pores of the agglomerate is not emptied in parallel, i.e. the larger pores will be emptied first and liquid will flow from the larger pores to the smaller ones that have a higher capillary pressure. It cannot be excluded that with increased drying rate, evaporation will be faster than internal liquid flow which leads to lower contraction during drying. As expected, increasing drying rate led to the agglomerates with lower density as a consequence of lower contraction of particles.
On the other hand, as indicated in
Table 1, there is a clear correlation between particle density and force needed to break the particle.
Blandin
et al. (
7) have shown that the compressive strength of the agglomerates is due to the two contributions: first, a mechanical contribution due to the very tight piling up of the particles inside the agglomerates and second, the contribution of crystalline bridges.
Therefore, it is reasonable to assume that piling up the primary crystals more compactly in denser agglomerates results in higher mechanical contribution and consequently higher compressive strength of particles.
On the other hand, solid bridges formation occurred during agglomeration but can be continued upon drying. According to literature, final bridge microstructure is not obtained immediately and develop from a mostly non-crystalline (liquid) and amorphous state to a crystalline structure (
30,
31) which is time consumer in the order of hours to days. It is reasonable to assume that development of solid bridge at various drying rate may be different. This fact can thus be account as another reason why the strength of the agglomerates dried at different temperature varies considerably.
It is should be mentioned that reported standard deviations for the compressive strength of the agglomerates are relatively high which may be result of brittle structure of the agglomerates. Because it has been shown that Brittle breakage is difficult to measure quantitatively and reproducible (
32).
Tableting
As a means of investigating the significance of drying-related contraction behaviour and subsequent differences in porosity of particles, the particles were characterized in terms of tablet-forming ability. Earlier experience of the tabletting behaviour of granules (
33) has shown that, for granules compacted at a given applied pressure, granule porosity will be critical for the structure and tensile strength of the formed tablets. These observations were explained as an effect of porosity on the degree of deformation, which the particles undergo during compression. In this study also the porosity of the particles affected the tensile strength of the tablets formed at an applied pressure of 200 MPa (
Table 1) in such a way that tablet strength increased with increased particle porosity. In fact a difference in drying rate may significantly affect the tensile strength of tablets formed from agglomerates, modulated by a change in particle porosity. It is possible that a variation in the moisture content of the agglomerates can explain the influence of drying rate on the strength of the tablets (
34,
35). In this study, however, the agglomerates were conditioned before tabletting and can thus be assumed to have had similar moisture content,
i.e. the differences in particle compactability cannot be explained by differences in the moisture content of the particles.
Drying may in addition affect the shape and surface structure of particles. Such an effect may also explain the reported observations, but the characterisation performed in this study indicates that the different drying temperature did not generally affect the shape and surface structure of the particles. Thus, the drying-related change in the tabletting behaviour of the agglomerates is most probably explained by a change in the porosity of the agglomerates, due to differences in their contraction during the drying phase (
36).