2.1. Preliminary Tests
The results of the tracer test and the hydraulic behavior test of the four SSFs are presented in
Figure 1.
Figure 1a shows that the water experimental residence time in the filtration system was 14 h for all the SSFs. The Kruskal–Wallis test revealed no significant differences in the residence time between the four SSFs, obtaining a
p-value of 0.767.
Figure 1b shows the total head loss over the 14 h of the tracer test on the four SSFs. The head loss stabilized at approximately 6 h after the start of the test. As expected, all SSFs showed the same stabilization trend over time. However, despite the similar stabilization trend, SSF2 showed an average total head loss 46.6% higher than the average of SSF1, SSF3, and SSF4. This difference was confirmed by the Kruskal–Wallis test, revealing a
p-value of 2.92 × 10
−8. Despite this difference, the removal efficiency of the different water quality parameters and head loss did not show distinctions between the SSFs during the experiments of this study.
Furthermore, Dunn’s multiple comparisons tests indicated that the most representative differences were between SSF2 and the filters SSF1 and SSF4, with adjusted p-values of 5.60 × 10−5 and 3.01 × 10−8, respectively. On the other hand, the differences between SSF2 and SSF3, as well as between SSF3 and SSF4, were considered in the margin of non-significance, with adjusted p-values of 0.0375 and 0.0112, respectively. These differences in the total head loss between the filters may have been influenced by different factors, such as the compaction of the filter media during the installation of the SSFs or the presence of impurities in the sand used as filter media. Such factors may have directly impacted the SSF’s media porosity and, consequently, the head loss over time in the hydraulic tests.
The results of the evaluation of CYN adsorption on the sand used as filter media are presented in
Figure 2. A similarity in the CYN concentration was observed within each replica’s samples. In replica 1, the average concentration of CYN was 32.6 µg/L. In replica 2, the average concentration was 34.7 µg/L.
For replica 1, the difference between the concentration in the samples did not exceed 2% compared to the replica mean. More specifically, the differences of each sample, relative to the mean, were −1.84%, 0.31%, and 1.23% for the control, sample 1, and sample 2, respectively. In replica 2, the differences were slightly more prominent compared to replica 1. The control, sample 1, and sample 2 showed differences compared to the mean of 3.46%, 0.29%, and −3.75%, respectively.
The results obtained were subjected to a two-way analysis of variance (two-way ANOVA), and the results are presented in
Table 1. The analysis revealed that variation in the data was mainly due to the test replicas, accounting for 20.96% of the variation. However, this variation was not significant (
p-value = 0.072). In addition, the different samples (control, sample 1, and sample 2) contributed only 1.62% of the variation in the data without statistical significance (
p-value = 0.865). Therefore, the results indicated that the sand used as filter media did not adsorb CYN, suggesting that adsorption was not a predominant removal mechanism for CYN in this study.
2.2. Monitoring of Operational and Water Quality Parameters
Monitoring the slow sand filtration system operation included three periods: ripening and two contamination peaks with CYN (contamination peak 1 and contamination peak 2). Filters SSF1 and SSF2 served as control and received water from Paranoá Lake during the filtration run. On the other hand, filters SSF3 and SSF4 received lake water spiked with CYN only during the contamination peaks. This group of SSFs was already used in previous experiments, and before the beginning of this study, they were submitted to the scraping and resanding process.
The ripening lasted 42 days, while each contamination peak lasted 5 days. The first peak occurred between the 43rd and 47th day of operation and the second between the 70th and 74th. The descriptive statistics of the raw and filtered water quality parameters are presented in
Table A1,
Table A2 and
Table A3.
In this study, the ripening period was twice as long as that reported in previous studies on Paranoá Lake water treatment by slow sand filtration [
45,
46,
47]. This behavior is probably due to insufficient incident light on the SSFs. Such insufficiency likely inhibited the primary metabolism of phytoplankton (photosynthesis), causing dissolved oxygen lacking in the raw water column above the top of the filter media [
48] and, consequently, impairing groups of aerobic microorganisms that are key to the SSFs ripening [
37].
Total coliform gradually reduced in all SSF effluents until the end of the ripening period (42 days), when this parameter reached a value less than or equal to 1 MPN/100 mL (see
Figure 3a).
During peak contamination 1, the effluent from all SSFs showed an increase in the total coliform count of approximately one order of magnitude compared to the last days of the ripening period. Total coliforms in the raw water reached values of 1.18 × 10
5 and 1.13 × 10
5 MPN/100 mL in the Paranoá lake water and the lake water with dissolved CYN, respectively. These values represented an increase of two orders of magnitude concerning the raw water of the last days of ripening. Hendricks and Bellamy [
49] indicate a direct correlation between the density of total coliforms in raw water and filtered water. Consequently, this may have been one of the causes of the rise in total coliform levels in the filtered water during the first contamination peak.
The second contamination peak was applied three weeks later. In this period, the total coliform density in the effluent from the SSFs decreased to 1 MPN/100 mL or lesser values. Such behavior may indicate a diversification and evenness of the biofilm microbial community (
schmutzdecke) over time. In the effluents from filters SSF3 and SSF4 exposed to CYN, the total coliform counts decreased to values less than or equal to 1 MPN/100 mL. This indicates that the cyanotoxin concentration in the raw water had no adverse effect on the removal efficiency of the filters. Thus, proper ripening and longer operating times were possibly the main contributing factors to this behavior. These results corroborate previous studies of Unger and Collins [
34] and Haig et al. [
44], who observed that the longer the SSF operation time favors the higher removal efficiency of different microbiological water quality parameters.
During the whole filtration run, the SSFs received, on average, raw water with an
E. coli density of 152.18 MPN/100 mL. For
E. coli, from the beginning of the operation, both pairs of SSFs that submitted to peaks of CYN and those not submitted produced filtered water with levels of this bacterium below the detection limit (1 MNP/100 mL); the results were not presented in
Table A1,
Table A2 and
Table A3. This fact is likely due to the proliferation of the microbiota remaining in the sand after the scraping and resanding process of the SSFs before the start of operation. Crittenden et al. [
50] argued that, after sequential filtration runs, the developed microbiota could establish along the first 15 cm depth of the filter media. These remaining microbiota may have been responsible for the reduction in
E. coli from the beginning of the operation of the slow sand filtration system [
51]. The absence of
E. coli during the CYN contamination peaks indicates that this cyanotoxin did not significantly impact the microorganisms and mechanisms involved in its removal. This efficiency was maintained over the filtration run, evidencing the robustness of the slow sand filtration system for
E. coli removal.
E. coli counts are presented in
Figure 3b.
Concerning water quality parameters,
Figure 4 shows the values measured in the raw and filtered water in the three monitoring periods. The removal of TOC, true color, and turbidity remained consistent during the ripening period and contamination peaks, indicating CYN did not influence the efficiency of the filters SSF3 and SSF4. The average TOC concentration in the raw water ranged from 3.874 to 5.638 mg/L, and the average TOC removal by the SSFs was approximately 33%, resulting in an average residual TOC in the effluent of 3.165 mg/L. The average removal of true color was about 55%, with average values of 5 Pt-Co in the effluent from the SSFs. The SSFs’ effluent turbidities varied between 0.18 and 0.40 NTU, meeting the Brazilian standards for slow sand filtration (1 NTU) [
52].
All the SSFs were variable in the ripening period regarding head loss. However, the head loss was stable in the contamination peaks and presented similar values among all SSFs (see
Figure 5a). According to Haig et al. [
44], the operating time of SSFs contributes to greater species diversity and evenness. This implies higher functional stability in SSFs. In this way, it is possible to explain the stabilization of the head loss over the filtration run of all SSFs. Only SSF3 showed an increase in head loss during the contamination peaks. Although the head loss of SSF3 was different from the other SSFs, in
Figure 5b, it is observed that the filtration rate was not affected.
2.3. Comparative Analysis of the Performance of the Slow Sand Filters
During each monitoring period of the slow sand filtration system, the four SSFs were compared to identify possible differences. To assess differences over time, the performance of each SSF in each of the monitoring periods was also compared. Possible significant differences were checked using the Kruskal–Wallis non-parametric test. The tests with positive significance were submitted to Dunn’s multiple comparisons test to identify the different pairs.
Concerning removing water quality parameters, the Kruskal–Wallis test did not reveal significant differences between the four SSFs over the filtration run. However, during contamination peak 1, there was a statistically significant difference in total coliform removal between the SSFs, with a
p-value of 0.00961.
Figure 6 compares the total coliform content distribution measured in the effluent of the SSFs during each period of the filtration run.
As shown in
Figure 6, the distribution of the SSF4 data during the first contamination peak led to the differences indicated in the removal of total coliforms. However, the residuals from SSF3, also exposed to contamination peaks, were similar to the controls (SSF1 and SSF2). Therefore, regardless of the presence of CYN in the raw water, the filters achieved similar total coliform removal to the controls.
When analyzing the hydraulic parameters of each SSF, an apparent difference was exhibited in the head loss during the ripening period (
Figure 7). However, the Kruskal–Wallis test showed that the observed variation was not statistically relevant.
Based on the results of Dunn’s test, presented in
Table 2, the SSF3 was identified as the SSF with the most remarkable significant differences in head loss compared to the other SSFs evaluated. The differential increase in the head loss of SSF3, observed in the contamination peaks (
Figure 7a), could be hypothetically attributed to the type of microorganisms established in the
schmutzdecke, which occupied the empty spaces at the top of the filter media differently than the microorganisms that colonized the other SSFs. This occupation probably hindered the passage of water through the filter media and, as a result, increased head loss.
The differences observed between the SSFs in each period were mainly related to the hydraulic parameters. This indicates that regarding reaching the expected water quality parameters, the filters presented similar performances to each other despite the presence of CYN in the water.
On the other hand, when comparing the performance of each SSF over the filtration run, significant differences were observed in the removal of TOC and turbidity (
Figure 8 and
Table 3). The concentration of CYN in the effluent did not significantly affect the removal of TOC. Although the TOC residuals in the SSF3 and SSF4 filters showed greater variability in contamination peak 2 (
Figure 8a), the filters’ medians remained close in all periods, and no marked differences were observed between the two contamination peaks.
Turbidity removal showed significant differences between contamination peak 1 and contamination peak 2 in all SSFs. The difference was due to reduced turbidity levels at the second contamination peak. This behavior is expected in slow sand filtration systems. The deposition of particulate material over time at the top of the filter media decreases the empty spaces and increases the retention of the turbidity particles [
53].
2.4. Evaluation of Cylindrospermopsin Removal
The results of CYN removal in filters SSF3 and SSF4 are shown in
Figure 9. The results revealed the efficiency of filters SSF3 and SSF4 after ripening them. The ripening of both SSFs submitted to peaks of CYN ensured the stability of the biological activity at the filter media, which contributed to reducing the cyanotoxin level in the SSF effluents. This evidence suggests that the stable biological activity at the filter media played a crucial role in efficiently removing CYN.
Both SSFs removed more than 33% of CYN during contamination peaks from the first day of each peak application. Furthermore, the CYN removal gradually raised over time, even as the CYN level in the raw water increased. The removal was higher during the second contamination peak applied three weeks after the first peak, suggesting that the SSFs’ colonizing microbiota became more stable and efficient with the SSFs’ operation time, as already proven in other studies [
44]. It is important to note that the operation time of SSFs played a crucial role in removal efficiency, allowing microbiota diversification, stabilizing biological activity, and adapting microorganisms to fluctuations in the quality of the inflowing water.
During contamination peak 1, the maximum CYN residual levels in the effluent from SSF3 and SSF4 were 0.784 µg/L and 0.774 µg/L (62.03% and 62.52% removal efficiency), respectively. In contamination peak 2, the maximum CYN residuals were 0.548 µg/L and 0.453 µg/L (72.39% and 77.18% removal efficiency), respectively. At the end of contamination peak 2, SSF4 removed CYN at a level not detectable. Notably, in both contamination peaks, the concentrations of CYN in the effluent from SSF3 and SSF4 remained below the limit of 1 µg/L established by Brazilian legislation for drinking water [
52].
These results demonstrate that slow sand filtration technology can effectively remove CYN to acceptable levels established for drinking water in Brazil. This study achieved these results when the concentration of CYN in the raw water was approximately 2 µg/L or lower, and the SSFs were properly ripened. These results are also promising concerning international standards recommended by the WHO of 0.7 µg/L for the CYN concentration in drinking water [
54].
Regarding the mechanisms contributing to the CYN removal, the adsorption evaluation on the sand used as filter media did not show interactions of the cyanotoxin with sand, suggesting that such a mechanism was not involved in CYN removal. On the other hand, biodegradation seems to be a strongly possible removal mechanism. However, in this study, the effluents from SSF3 and SSF4 were not submitted for investigation to identify potential by-products of CYN biodegradation. Besides biodegradation, this study did not prove other CYN removal mechanisms, such as adsorption on the biofilm [
55].
2.5. Characterization of the Microbiota in Slow Sand Filters
Optical microscopy analysis of the microbiota colonizing the SSFs throughout the filtration run identified 13 taxonomic classes from different taxonomic kingdoms.
Figure 10 shows the relative abundance of these classes in each SSF at the end of the filtration run.
Some of the classes identified on the SSFs, among others, have been previously recorded in the Paranoá Lake microbial community [
56]. In addition, in previous studies, these same classes were also identified in the system of slow sand filtration using this lake water [
45,
47,
57,
58].
The relative abundance of the classes in the SSFs did not necessarily reflect their relative abundance in the Paranoá Lake. The composition of the microbiota occurring in the SSFs was influenced by the specific environmental and operational conditions predominant in the ecosystem of the SSFs [
44,
59]. Considering this, in all SSFs, protozoa of the Imbricatea class and amoebas of the Lobosa class were predominant. However, the proportion of these classes varied in the SSFs exposed and unexposed to CYN during contamination peaks. In the unexposed SSFs, the Lobosa class predominated over Imbricatea, while in the exposed SSFs, the Imbricatea class showed a higher proportion than the Lobosa class. SSF1 and SSF2 exhibited a proportion of 40.11% and 53.08% of the Lobosa class, respectively, while in SSF3 and SSF4, it was 32.77% and 42.29%, respectively. On the other hand, the proportion of the Imbricatea class in SSF1 and SSF2 was 34.54% and 34.60%, respectively, while in SSF3 and SSF4, it was 57.06% and 41.14%, respectively. The higher proportion of the Imbricatea class in the SSFs exposed to CYN suggests its lower sensitivity to this cyanotoxin when compared to the Lobosa class.
Among the representatives of the Imbricatea class, protozoa from the genus
Euglypha, which occur naturally in aquatic environments with little contamination [
38], were the most dominant. These organisms are more abundant in oxygen-rich aquatic environments with a high diversity of planktonic species [
38]. Species of the genus
Euglypha play an essential role in the ecosystem, feeding on bacteria, algae, and other microorganisms present in the environment in which they occur.
Lobosa class representatives in the SSFs included genera Arcella, Centropyxis, and Amoeba microorganisms. These species are found in various aquatic habitats, such as lakes, ponds, wetlands, and rivers. Species of the genus Arcella are often found in sediments or decomposing vegetation, where they feed on bacteria, algae, and organic debris. Species of the genus Centropyxis are commonly found in sediments and the surface layer of humid soils, feeding on suspended organic particles and bacteria. The genus Amoeba can occur in various aquatic environments and feeds mainly on bacteria, algae, and other microorganisms. Notably, most of the microbiota found in SSFs are native to the sediment. Thus, finding it on top of the filter media is natural as this superior section can be a relatively similar substrate in the SSFs.
The high removal efficiency of total coliforms and E. coli in the SSFs can be attributed to the occurrence and predominance of species belonging to the classes Imbricatea and Lobosa, which feed mainly on bacteria and suspended organic particles, thus suggesting a predation mechanism of removal. Interestingly, despite the slightly different proportions, the predominant classes were the same in all SSFs, indicating that dissolved CYN did not significantly affect the high removal efficiency of total coliforms and E. coli.
The Eurotatoria class, represented by the Digononta, Monogononta, and Lecane groups, was found in the SSFs in proportions between 5% and 6%. These microorganisms, known as rotifers, are widely distributed in freshwater aquatic habitats such as lakes, ponds, rivers, streams, and wetlands. Their occurrence is often considered an indicator of good water quality.
Microorganisms of the Eurotatoria class feed on organic particles suspended in the water, such as algae, bacteria, organic detritus, and other microorganisms. Some rotifers are filter feeders with specialized structures, such as the ciliated crown, to capture food particles suspended in the water. In addition to contributing to nutrient cycling in aquatic ecosystems, rotifers also play an essential role in the population control of other microorganisms. Rotifers have also been of great sanitary interest. Studies have demonstrated the predation of
Cryptosporidium oocysts by different species of this group of microorganisms [
39,
40]. The occurrence of rotifers in SSFs shows the potential for pathogen control that slow sand filtration offers in water treatment.
The studied SSFs presented similar microbiota compositions. However, in some SSFs, other taxonomic classes occurred, differentiating them. Thus, Shannon diversity indices were calculated for each SSF. The SSF1 had a Shannon diversity index of 1.57, while SSF2, SSF3, and SSF4 had indices of 1.10, 1.04, and 1.31, respectively. These results indicated that exposure to CYN does not appear to be a determining factor in the diversity of the microbiota of the SSFs. SSF1 and SSF4, which were exposed and not exposed to CYN, respectively, had the highest Shannon diversity indices. This suggests that other factors may have played a more significant role in the observed diversity.
One of the main factors that possibly influenced the diversity of the microbiota was the bacterial community. In slow sand filters, bacteria contribute to the degradation of organic compounds and are a source of food for planktonic and benthonic organisms [
36,
60,
61,
62]. Alterations and differentiations in the bacterial community can influence the development of planktonic and benthic organisms due to trophic interactions between these groups. The lack of an analysis of the bacterial community did not allow the determination of its relationship with the composition of the remaining microbiota.
The positioning of the slow sand filtration system probably also influenced the differences in the microbiota diversity in the SSFs. The SSFs were arranged in increasing order of distance from one of the laboratory windows, with SSF1 being the closest and SSF4 the furthest. The SSF1 showed the highest diversity compared to the other SSFs. Despite all cares taken to prevent the incidence of light on the SSFs, the laboratory routine and the filtration system’s location allowed small plots of light to pass through, which likely promoted the occurrence of photosynthesizing microorganisms. The optical microscopy analysis of the microbiota from SSF1 revealed the occurrence of microalgae of the genus
Micrasterias belonging to the class Zygnematophyceae. These microalgae represented approximately 0.56% of the taxonomic classes identified in this SSF (
Figure 10). In addition to their contribution to oxygen production, microalgae of the genus
Micrasterias are known to form colonies and biofilms [
63], providing habitats, shelter, and food sources for a variety of aquatic organisms, such as small invertebrates and protozoa [
64]. The presence of microalgae of the genus
Micrasterias in the SSF1 may have been one of the factors contributing to the higher Shannon diversity index observed in this filter, also explaining the higher-class richness observed in SSF1 compared to the other SSFs.
The results of the Bray–Curtis dissimilarity analysis showed that SSF1 and SSF3 were the most differentiated among the four filters evaluated.
Figure 11 depicts the dendrogram of the data clustering, showing the dissimilarity in the community diversity in filters SSF1 and SSF3 compared to SSF2 and SSF4. The SSF1 stood out as the most dissimilar due probably to a combination of several factors, including the filtration system’s location, the incidence of light that favored photosynthesizing microorganisms developing, the formation of colonies and biofilms by microalgae of the genus
Micrasterias, and the consequent creation of habitats and shelter for other aquatic organisms. In contrast, SSF3 showed the lowest class richness among the SSFs evaluated, which may have contributed to its distinction from the others.