3.1. Effective Range of Prefactor 
The prefactor 
 is an important parameter to describe the structural and morphological properties of aggregates, as shown in 
Figure 4. Therefore, and with values of 
 being in the range of 1 to 3, the question arises about the effective range that values of the prefactor 
 may attain. For a first orientation, we summarized values of 
 for aggregates with different 
 from the literature in 
Table 1.
Table 1 shows a spread of 
 from 1.27 to 9.0. However, the variation of 
 is small in the previous research, and derivations are not always detailed and clear. Therefore, we have decided to test the effective range of 
 with the help of aggregates generated by the MPTSA model.
 In the power law relationship (Equation (1)), the radius of gyration 
 can describe the spatial mass distribution around the mass center of the aggregate. As a criterion for the effective range of 
, we compare the radius of gyration calculated by Equation (1), denoted by 
, to the radius of gyration from generated aggregates according to Equation (2), denoted by 
. Both 
 and 
 are obtained with the same input parameters. The comparison is quantified by the ratio
        
If  of the generated aggregate is greater than 99.99%, then  is assumed to have been in its effective range.
Next, we generated in the frame of this evaluation two groups of aggregates with different fractal dimensions and prefactors. In the first group, the number of primary particles was 
 = 50, with 
 = 1.8:0.2:2.8 and 
 varying from 0.9 to 5.0 in steps of 0.1. As for the second group, it had 
 = 300, 
 = 1.8:0.2:2.8, and 
 = 0.9:0.1:10. The radius of primary particles 
 was constant and equal to 0.2 mm, but the absolute value of this variable has no influence on the results. The relationship of 
 and 
 with 
, based on two different values of 
, is shown in 
Figure 5.
As can be seen in 
Figure 5a,b, all the curves show the same trend: at the beginning, 
 of the aggregates does not change with increasing 
, being on a plateau with 
. Then, as 
 increases, all curves show an inflection point, after which 
 decreases dramatically. When 
 is the same, the main difference among the curves is in the length of their plateau regions; aggregates with a smaller 
 show a longer plateau with 
 over 
. This means that the aggregates with smaller 
 have a broader effective range of 
. Besides, by comparing 
Figure 5a,b at the same 
, we can find that the effective range of 
 of aggregates with smaller 
(=50) is narrower than in the case of larger 
(=300). The horizontal axis coordinates of the inflection points on each curve are considered as the upper limit of the effective range of 
 under conditions specified by different 
 and 
. Respective values are shown in 
Table 2.
In 
Figure 5a, when 
 is larger than 4.7 at 
 = 50 and 
 = 1.8, then the 
 of the aggregates is less than 1. This is since with an additional increase of 
 (>4.7), the primary particles of these aggregates can no longer be concentrated further in space. So, 
 of these aggregates does not change with further increasing 
. For example, as shown in 
Figure 4, the structural and morphological characteristics of the aggregate with 
 = 1.8 and 
 = 4.7 are the same as those of the aggregate with 
 = 1.8 and 
 = 7.0, with 
 of these two aggregates being same and equal to 0.74 mm. However, 
 calculated formally from Equation (1) continues to decrease as 
 increases, namely from 
 = 0.74 mm for aggregates with 
 = 1.8 and 
 = 4.7, to 
 = 0.6 mm for aggregates with 
 = 1.8 and 
 = 7.0. Therefore, when 
 = 1.8 and 
 > 4.7, the ratio 
 of the aggregates is less than unity, meaning that 
 has moved outside of its effective range.
As to the lower limit of 
, it has been determined by decreasing its value in steps of 0.1. This process stops when the MPTSA model ceases being able to generate the aggregate. Until then, the values of 
 of the generated aggregates remain equal to 1. The minimum 
 at which aggregates can be generated is the lower limit of the effective range. Values for different 
 and 
 are shown in 
Table 2.
In addition to the above method that presupposes the generation of agglomerates by means of the MPTSA algorithm, a much simpler, algebraic estimation of the limits of the effective range of 
 has also been implemented in the present work. According to Equation (1), 
 shows a negative relationship to 
 under fixed 
 and 
,
        
Therefore, when 
 and 
 are fixed and 
 minimal, 
 takes its upper limit value. The lower limit of 
 occurs when the situation is conversed (
 at maximum value). The radius of gyration 
 of an aggregate shows the mass distribution around the aggregate center of mass. In our present work, the radius of primary particles 
 is constant at 0.2 mm. Therefore, when two aggregates with the same 
 show different 
, the lower value of 
 indicates that the mass (primary particles) of the aggregate is more concentrated at the center of mass. So, the minimum 
 is reached when the morphology of the aggregate is like that of a sphere, which is here assumed to happen for an aggregate with 
 = 3.0 and 
 = 1.0. On the contrary, the relative gyration radius 
 of the aggregates is maximum when the primary particles of the aggregates are most dispersed, assumed here to be the case for aggregates with 
 = 1.7 and 
 = 1.0. Minimal 
 (at 
 = 3.0 and 
 = 1.0) and maximal 
 (at 
 = 1.7 and 
 = 1.0) of aggregates with different 
 are calculated by Equation (1), the results are summarized in 
Table 3.
Then, minimal 
 and maximal 
 of the aggregates with different 
 are substituted into Equation (10), and upper and lower limits of the effective range are obtained for different 
, respectively. The lower and upper limits of the effective range of 
 that have been estimated in this way are shown in 
Table 4.
Comparing 
Table 2 and 
Table 4, we can find that the upper limit of 
 obtained by use of the MPTSA model is close (slightly smaller) to the results of the simplified estimation. The lower limit of 
 in 
Table 2 is nearly equal to the lower limit value of 
 for aggregates with the smallest 
 (= 5) in 
Table 4.
  3.2. Relationship between BC Fractal Properties and PL Fractal Properties
In this section, we generated a series of aggregates with different fractal properties (
 and 
) and 
 by the MPTSA model, with 
 varying from 100 to 300 in steps of 50 and 
 = 1.8:0.2:2.8. The investigated range of 
 for each 
 is shown in 
Table 5. Those ranges correspond to the ranges for 
 = 100 from 
Table 4, being more restrictive in comparison to the ranges for aggregates with a larger number of primary particles. Consequently, all the generated aggregates are safely within the effective range of 
 values. The primary particles of generated aggregates are monodispersed in the present work, with the radius of primary particles formally set at 0.2 mm. To capture stochastic variations, each aggregate is generated five times with the same input parameters.
In the further course of evaluation, a projection method proposed by [
28] is applied to get 2D data for the generated aggregates. Then, both 3D and 2D box-counting methods are applied to estimate 3D BC fractal properties (
 and 
) and 2D BC fractal properties (
 and 
) of the generated aggregates. Next, aggregates generated with different 
 (=100, 200 and 300) and 
 (=1.8 and 2.8) are chosen to investigate the relationships between 
 and 
 with 
. The averages of 
 and 
 over the five realizations are shown in 
Figure 6 for the selected aggregates. Furthermore, averages (
 and 
) over each entire aggregate series (with 
 = 100:50:300) are also plotted in 
Figure 6 against 
.
All the curves in 
Figure 6 show the same trend, namely of BC fractal dimensions increasing with increasing 
. This is due to the fact that with the increase of 
, the distribution of primary particles becomes more and more concentrated (as shown in 
Figure 4). In the BC method, the number of boxes (
) occupied by aggregates is larger when the primary particles of aggregates are more concentrated [
28]. According to Equation (4), 
 and BC fractal dimensions show a positive relationship. Therefore, the BC fractal dimension increases as 
 increases.
Moreover, the trend in the variation of 
 with 
 in 
Figure 6d (
 = 2.8 and BC in 2D) is slightly different from the other three figures (
Figure 6a–c). In 
Figure 6d, 
 initially increases with increasing 
 (0.4 to 0.8), but then the value of 
 starts fluctuating around 1.91 as 
 further increases. This is because the calculation of the 2D BC fractal dimension of the aggregates is based on their projection. The purpose of projection method in this work is to get the least overlapping between primary particles (the maximum projected area of the aggregates) [
28]. The morphology of the aggregates is though close to spherical when aggregates with a high fractal dimension and prefactor are considered [
27] (i.e., 
 = 2.8 and 
 > 0.8). Therefore, the 2D maximum projection area of these aggregates is almost constant with increasing 
, and the same holds for 
 values since these are directly affected by the projection area (positive relationship). Therefore, the 
 value of the mentioned kind of aggregates floats around 1.91. In less obvious but analogous way, it can be seen from 
Figure 6c that the 
 values of fluffy aggregates also float around 1.91 when the value of 
 is large enough (> 5.5, in this case). In addition, the values of averages (
 and 
) over the entire aggregate series (with 
 = 100:50:300) are generally close to the values for primary particle number in the middle of the series (
 = 200).
  3.3. Correlation between 3D BC Fractal Properties and 2D BC Fractal Properties
It is hard or even impossible to obtain the 3D fractal properties of aggregates composed of very small primary particles or nanoparticles by X-ray µ-CT, because of limitation in the spatial resolution of this imaging method. However, the 2D fractal properties of such aggregates can easily be retrieved by SEM or TEM. Therefore, a correlation between 2D and 3D fractal properties is necessary to be established. In this section, the correlation between 2D and 3D BC fractal properties is discussed first. Furthermore, the correlation between 2D BC and 3D PL fractal properties is discussed in the next section.
In 
Figure 7, the relationship between 
 and 
 for the aggregates with various 
 (=1.8:0.2:2.8) is shown. Values of 
 and 
 have been averaged over all 
 (from 100 to 300 in steps of 50) of the entire aggregate series and then over five realizations.
As shown in 
Figure 7, 
 increases with 
 for any value of power law fractal dimension. All data points can, thus, be described by one and the same power regression,
        
The average values of 
 (over five iterations) and 
 for the aggregates with different 
 are plotted in 
Figure 8. From 
Figure 8 we can find that the value of 
 is linearly increasing with 
. The respective linear regression for all the aggregates is
        
A combination of Equations (11) and (12) can be used to obtain 3D BC fractal properties ( and ) from a given 2D BC prefactor  or, by additionally involving the later Equation (17), from a given 2D BC fractal dimension .
  3.4. Correlation between 2D BC Fractal Properties and PL Fractal Properties
The relationship between 
 and 
 for aggregates with various 
(=1.8:0.2:2.8) is shown in 
Figure 9. Values of 
 have been averaged over all 
 (from 100 to 300 in steps of 50) of the entire aggregate series and then over five realizations.
In 
Figure 9, 
 is seen to increase with increasing 
; however, the growth rate of 
 decreases as 
 increases. As pointed out in 
Section 3.2, 2D BC fractal properties of aggregates are influenced by the 2D projection area [
28], being positively interrelated. And when the morphology of the aggregates with higher 
 or 
 has approached that of a sphere (as shown in 
Figure 4), the projection area of these aggregates changes only slightly with further increase in 
. Therefore, the rise of 
 with 
 flattens up at larger 
 or 
. Here, an exponential function can be used for regression,
        
In Equation (13), the curves with different 
 have different values of 
, 
, and 
, as summarized in 
Table 6.
Then, correlations between, first, 
 and 
, and second, between 
 and 
 are developed as follows:
The average value of  = 5.208 is used to represent this parameter.
Combining Equations (13)–(15), the correlation between 
 and power law fractal properties is obtained:
The averages of 
 and 
 over five realizations are plotted in 
Figure 10 for aggregates with different 
. As shown in 
Figure 10, 
 increases linearly with 
, according to the regression
        
Equations (16) and (17) are very important. Combining these two equations enables to predict power law fractal properties ( and ) of aggregates from their 2D box-counting fractal properties ( and ), the determination of which from microscope images is fast and easy in practice.
Therefore, the reliability of these two correlations is tested by a new series of aggregates generated by the MPTSA model. Here, three different values of 
 are used, namely 
 = 1.9, 2.3, and 2.7. The input number of primary particles 
 varied from 100 to 300 in steps of 50. The prefactor 
 of the aggregates takes values from 0.9 to the upper limit of its effective range for each 
 (according to 
Table 5). The primary particles are still monodispersed, and the radius of primary particles is kept same as for the previously generated aggregates. Each aggregate with the same input parameters is generated five times. Then, the aggregates that have been generated in 3D are projected onto a 2D plane by the projection method from [
28], and the 2D BC method is applied to estimate the 2D BC fractal properties for those projections. Then, the averages of 
 and 
 for each aggregate are calculated over five realizations. Substituting 
 and 
 into Equations (16) and (17), values of power law fractal properties (
 and 
) are finally calculated. Examples of calculated results for aggregates with 
 = 1.9 are summarized in 
Table 7.
In 
Table 7, there is a notable difference between the input fractal parameters and the calculated values. This is due to the difficult inversion of Equations (16) and (17) for given 
 and 
. This is done by numerical optimization, which is though confronted with several flat and similar optima.
Whereas further improvement is desirable at this point, the ratio 
, which is an important parameter for the morphological analysis of aggregates, can be applied to test the predicted values from Equations (16) and (17). It is recalled that Wang et al. [
28] have recently established an original correlation between 2D BC fractal dimension and PL fractal dimension. This correlation, however, neglected the influence of 
 and kept this parameter constant (=1). The correlation is
        
Predicted results (
 and 
) from Equations (16) and (17) are substituted to Equation (1) to calculate 
 of the new series of aggregates (
 = 1.9, 2.3, and 2.7, 
 = 100, 200, and 300). For the sake of comparison, 
 of the new generated aggregates are substituted to Equation (18) to estimate their 
. Then, keeping 
 as constant and equal to 1, another 
 is estimated by means of 
 predicted from Equation (18). Finally, the two kinds of 
 are compared in 
Figure 11 based on three 
 (= 100, 200, and 300). 
 calculated from prediction results of the equations in this research (Equations (16) and (17)) are denoted by “present”, 
 calculated from the correlation of the previous work (Equation (18)) are denoted by “previous”. In addition, the standard 
 which is calculated from the input parameters (
, 
, and 
) of the MPTSA model is also shown in 
Figure 11 (dotted lines). The R-square analysis represents the deviation of the predicted 
 (present or previous) to standard 
.
As shown in 
Figure 11, when both 
 and 
 are small (
 = 1.9 and 
 = 100), the difference between present predicted results (Equations (16) and (17)) and previous predicted results (Equation (18)) is insignificant, the R
2 of the two sets of results to the standard (input, reference) data being 0.923 and 0.929, respectively. However, when 
 or 
 increases, the R
2 of previous results decreases significantly. Especially when the aggregates with 
 = 2.7 and 
 = 300 are considered, the R
2 of previous results reaches a very low value of 0.439. However, the changes in 
 or 
 hardly affect the accuracy of the present results, which are based on predictions from Equations (16) and (17). In 
Figure 11, the minimum R
2 of present results is equal to 0.868 when 
 = 2.7 and 
 = 100.