1. Introduction
The large extended presence of antibiotics in wastewater and in agricultural products is an issue of high concern due to their persistence and the potential risk for living organisms [
1,
2]. Antibiotics are only partially digested and absorbed by humans and animals. Approximately half of the antibiotics administered to humans and animals are actively excreted unchanged within 8–24 h after consumption, primarily through urine and feces. The literature reports an incomplete absorption of 20% to 95% of the administered antibiotics, and the production of metabolites, which form after degradation, can be even more toxic than the original compound. The metabolites can accumulate in all habitats, especially surface waters, groundwaters, soils and sediments, through treated or untreated wastewater [
2,
3,
4,
5].
Conventional wastewater treatment plants (WWTPs) are based on chemical and physical processes, such as filtration, flocculation, coagulation, sedimentation and biological processes that mostly occur on activated sludge [
6]. The main historical objective in WWTPs was the removal of solids and the reduction of organic matter. In the last few decades, technology has been implemented to eliminate nutrients, such as nitrates and phosphates, increase the yields in all the processes and, in general, improve the quality of the outflow water and take advantage of the residues, such as the sludge and the produced gas, that could be considered as a resource for different applications. However, for the removal of antibiotics in wastewater effluents and sludges, additional treatments need to be provided before effluents are discharged to the environment or sludges are used for other purposes, such as agricultural [
3].
Various additional treatment technologies have been shown to remove antibiotics from wastewaters, for instance, physical treatments [
4], disinfection [
7], advanced oxidation [
8] and filtration with a permeable material with a high adsorption capacity, such as activated carbon [
9]. The use of low-cost materials, such as clays, for adsorption of antibiotics from wastewaters, in addition to other organic and inorganic pollutants, has been extensively studied. Clay-based adsorbents have high adsorption potential, but a significant remaining gap exists between theoretical studies and laboratory-scale experiments, and their real application at industrial scale [
10].
Natural clays are mostly composed of clay minerals, in addition to accessory minerals and other possible minor components, such as oxides and organic matter, typically in very minor concentration. In general, they exhibit good properties for adsorption due to their adequate physico-chemical properties: small particle size, high surface area, cation exchange capacity with fast kinetic mechanism and channels or zones to accumulate a high number of molecules [
11].
Kaolinite, sepiolite, palygorskite, rectorite, illite and the smectite montmorillonite have been studied as the most promising clay minerals to use for the adsorption of antibiotics [
12,
13,
14,
15]. However, clay minerals have been demonstrated to be very sensible to external parameters, such as pH, temperature, salinity and competition with other organic compounds [
10].
Thiebault et al. [
16] showed that the efficiency of a geofilter made of a mixture of sand and montmorillonite requires low clay content and a clay material that provides functional permeability. In their study, they demonstrated that Na-montmorillonite exerted high swelling pressure in the filter, limiting the permeability of the porous media, even at a low clay percentage (5%), whereas a Ca-montmorillonite allowed better percolation.
Stevensite, a 2:1 trioctahedral smectite with an octahedral sheet rich in Mg, is grouped within the Mg-smectite minerals and exhibits additional promising properties. However, it has been less studied because it is found at commercial grade in few places around the world [
17]. Mg-clays are frequent and exploited in the Madrid Basin [
18]. Such clays have good adsorbing capacities due to cationic exchanges and other molecular interactions. Previous studies [
19,
20] have shown that the commercial clay Minclear N100
TM, distributed by Tolsa (Spain) and composed of >90% stevensite (Si
4Al
0.4Fe
0.1Mg
2.1M
+0.3O
10(OH)
2, from X-ray fluorescence analysis of Ca-homoionized <2 µm size fraction [
21]), <10% illite and dolomite and <1% feldspars and quartz, has excellent properties for TC adsorption, both in batch experiments (static conditions) and in flow-through transport experiments (dynamic conditions), not only at low pH conditions, but also at neutral pH (6–8), which is normally the range of pH of wastewaters in urban WWTPs. However, the nanometric to micrometric size of the clay particles makes them lose out during transport with the mobile solution by colloidal dispersion. Fernández et al. [
20] designed their transport experiment by adding to a cylindrical column a mixture of finely grinded silica sand and stevensite in mass ratio 10:1 in order to prevent excessive swelling. Polypropylene filters of 0.45 µm pore size, geotextile filters and porous Teflon filters were added to both sides of the column to maintain the stevensite on site and prevent loss of clay.
In the present work, the stevensite clay material Minclear N100TM has been hydrothermally modified over the temperature of reversible dehydration and below the temperature of dehydroxilation with the aim to limit even more colloidal dispersion and swelling. Due to the applied physical treatment, stevensite thin (<2 mm diameter) pellets with centimetric length were obtained with a rigid macroscopic structure.
Similar approaches, such as the work from Polubesova et al. [
22] that created a micelle-clay filter made of benzyldimethylhexadecylammonium (BDMHDA)montmorillonite in a cylindrical column mixed with quartz sand at 100/1 (
w/
w) sand:BDMHDA–clay complex ratio, demonstrated high efficiency for the removal of negatively charged tetracycline and sulfonamide antibiotics from water at pH 8.5 (>90%). Biofilters are also used to reduce the concentration of antibiotics in water. Ligninolytic enzymes, such as laccase and peroxidase, facilitate the biodegradation of organic pollutants, such as environmentally persistent pharmaceutical pollutants [
23]. Laccase enzyme is a non-selective oxidase implied in many degradation processes. The large spectra of organic compounds degradable by laccase can be useful for wastewater treatment, even more so if the enzyme is immobilized on the clay substrate, avoiding its wide spread in the environment.
To study the filtering capacity, transport reactive tests must be conducted. In the present study, the adsorption capacities of the clay have been tested after different hydrothermal treatments with different concentrations of the injected solution, with or without enzyme, in order to find the best performance for the filter.
Reactive transport tests are conducted at the laboratory scale through relatively small filter cells. The perspective of this study is to develop a filter that could be used in WWTPs to reduce the concentration of antibiotics in their effluents. Filters can also be designed in smaller sizes for domestic or agricultural use to remove antibiotics from water before reusing it.
In addition, modelling according to reactive transport equations in porous media have been used to determine the hydrodynamic parameters of the filter, namely the retardation factor and the degradation term. Those two parameters are characteristic of the quality of the filter, such that the higher they are, the better the filtering capacity is. Modelling allows prediction of the application of this filter at different scales.
Most of the experiments have been carried out with tetracycline hydrochloride solution (TC), the most used derivative from tetracycline for veterinary purposes (
Figure 1). Tetracycline, even in low concentrations (in the order of 10 ppb), has a selection effect on antibiotic resistance genes [
24] and a selection effect on resistant bacteria in our environment. Furthermore, high concentrations of tetracycline are found in many effluents in Europe; for example, concentrations above 100 ppb were found in the final effluents of WWTPs in Ireland, Norway and Portugal [
25].
Therefore, to adsorb and then degrade the antibiotics, the present study employs a filter based on stevensite clay with immobilized laccase enzymes on it. The main objective of the present research work is to develop such a filter, to determine its characteristics and to carry out laboratory tests on the transport of antibiotics through this filter. The filter must be resistant to colloidal dispersion, must adsorb tetracycline and must degrade the tetracycline in an enzymatic way. The hydrodynamic characteristics, calculated by the STANMOD model, will allow proposing a prediction of the filter behaviour at large scale.
3. Results
3.1. CEC and Specific Surface Area of Pellets
The CEC and the BET-specific surface area were determined in the original clay and in all hydrothermally treated samples with the objective to predict the adsorption capacities of the stevensite pellets (
Figure 3).
The CEC of the stevensite clay material is 42.5 cmol(+)/kg and the BET-specific surface area is 238 m
2/g. Both properties were mostly conserved when treated hydrothermally and under hermetic conditions with steam up to 200 °C [
21]. In general, a decrease in both properties is observed with increasing thermal treatment.
After the enzyme immobilization on the pellets, those previous characteristics changed. The BET-specific surface area in the sample treated at 200 °C decreases to 94.6 ± 0.2 m²/g, which is around half of the area of the initial pellets.
Treatment at 200 °C was initially preferred over higher temperatures due to the higher CEC and surface area and lower energy consumption required to produce the pellets. However, the physical cohesion of the pellets immersed in water had stronger results with the increasing temperatures when they were shaken. Therefore, subsequent experiments performed on reactive transport were performed with selected pellets, either treated 200 °C (as representative of low-temperature treatment) or 500 °C (representative of high-temperature treatment). Finally, for the experiments performed with the immobilized enzyme on the stevensite pellets, the material treated at 300 °C was used, as it presented better enzymatic fixation than at 200 °C (further explanation is given below).
3.2. Determination of the Hydrodynamic Parameters of the Geofilter by Non-Reactive Transport
In order to obtain confidence on the homogeneity of the porous filter, considering stable hydrodynamic conditions, it was necessary to repeat and compare different transport experiments.
To determine the hydrodynamic parameters, three replicates of the non-reactive transport experiments using NaNO
3 were performed with pellets treated at 200 °C. The anionic transport was studied, as nitrate is not adsorbed by the stevensite clay (
Figure 4).
For the present fit, the retardation factor was adjusted to 1, as nitrate is considered non-reactive and no degradation was assumed. Thereafter, by the inverse method with STANMOD, and were determined as 0.38 and 0.43, respectively. Although larger errors are found at short term, the experimental data in the three replicates converge with the increasing time. The regression coefficient for the curve fitting is 0.99.
3.3. Reactive Transport of TC through the Geofilter
To illustrate the effect of the adsorption capacity of tetracycline as a function of the temperature treatment of the clay pellets, reactive transport experiments were carried out with pellets treated at 200 and 500 °C. These experiments were performed with a constant concentration of TC solution of 1 g/L injected through the filter. The breakthrough curves are presented in
Figure 5. Experiments were ended once a plateau of the relative concentration was reached. It can be observed that slightly higher adsorption is obtained with the pellets treated at 200 °C, but at long term, over 170 min, both experiments reach the same plateau. Assuming that the dispersion coefficient and the porewater velocity obtained by the non-reactive experiments are valid under reactive conditions, the retardation and degradation factors are calculated with STANMOD by the inverse curve fitting of the experimental data. A retardation factor of 8.43, a degradation factor of 0.07 and a regression coefficient of 0.99 were obtained at both temperatures, 200 and 500 °C. The retardation factor is far above 1, indicating significant adsorption of TC on the stevensite pellets. The low positive value for the degradation factor indicates insignificant degradation, although complexation reactions on the surface of the stevensite clay are not discarded, preventing TC degradation.
3.4. Desorption of TC
In the perspective of a real case scenario, the filter should exhibit desorption capacity, so that once the filter is saturated, it could be renovated by desorption of the organic contaminants by the outflow of a new inflow solution with capacity to exchange adsorption positions on the stevensite, recovering the filter in similar conditions as in its initial state and collecting the contaminant in a short time stage. A 1 M Mg(NO
3) solution at pH = 2 was used for desorption due to the high affinity of Mg
2+ to the cation exchange sites in stevensite (
Figure 6).
A relatively fast desorption can be observed as, after two hours, a negligible concentration of TC remains in the filter. Then, a new transport experiment could be carried out. All thermally treated stevensite clays conserve their sorption/desorption capacity.
3.5. Transports with Different Organic Molecules
In order to evaluate the adsorption capacity of the stevensite pellets, transport experiments were performed with 3 different organic molecules: TC (cationic at pH < 3.3, polar), eriochrome cyanine R (ECR; anionic at neutral pH, polar) and 4-nitrophenol (NP; neutral at controlled pH, weekly polar).
The 3 injected concentrations are 100 mg L−1.
The transport of ECR admitted a retardation factor of 1.67, calculated by STANMOD. Anions and anionic molecules, in general, are poorly retained by clays. However, a certain reactivity was observed in this assay.
Significant retention of the neutral organic molecule NP indicated that ion exchange was not the only mechanism of adsorption on the clay surface, presumably due to the action of van der Waals interaction with the polar surface of the clay. The retardation factor calculated by STANMOD for NP was 3.04.
In contrast, the cationic form of TC was clearly highly efficiently retained by the geofilter. A high retardation factor of 52.8 indicates that the stevensite pellets are good candidates to retain cationic molecules. Comparing the
with an injected TC solution at 100 and 1000 ppm, it can be deduced that the retardation factor also depends on the concentration of the inflow solution. More importantly, a positive and relatively high factor of degradation of 0.13 has been required by STANMOD to fit the experimental curve. Although not shown in
Figure 7, the three curves fitted with STANMOD exhibited regression coefficients higher than 0.996.
3.6. Transport with Enzymes Immobilized on the Stevensite Clay
Once the process of enzyme fixation was completed, the laccase activity of the stevensite clay—immobilized laccase pellets was confirmed by visual observation of the oxidation of 2,6-dimethoxyphenol. The laccase activity of the stevensite clay—immobilized laccase pellets cannot be quantified because the oxidation product was adsorbed on pellets. The results of the test are shown in
Table 1.
For the transport experiment performed with the biogeofilter, only pellets treated at lower temperature were studied. However, the pellets treated at 200 °C presented dispersion of aggregates in solution during the process of enzymatic fixation. Therefore, it was chosen to work with the pellets treated at 300 °C because they resist the enzymatic fixation process better. Transport experiments of a solution of TC were performed at 100 mg L
−1 through the filter with the two kinds of enzymes immobilized on it, purified under laboratory conditions and commercial (
Figure 8).
The degradation of TC with the purified enzyme was significant. The concentration was nearly one third of the initial concentration after 360 min of transport. This significant degradation observed in the filter with the purified enzyme can also be illustrated by a higher degradation factor obtained with STANMOD, compared to the filter without enzyme and with non-purified enzyme, equal to 0.29 (r2 = 0.998), 0.133 (r2 = 0.99) and 0.172 (r2 = 0.998), respectively.
The retardation factor was also higher in the experiment with the purified enzyme. A value of 103.3 (r2 = 0.998) was obtained with STANMOD for this experiment, while for the transport experiment without enzyme and with the non-purified enzyme, the retardation factor was 52.8 (r2 = 0.99) and 47 (r2 = 0.998), respectively.
Reactive transport with 3 different concentrations of TC injected solution—200, 100 and 50 mg L
−1—were carried out with a filter, with and without enzyme. The area ratios were calculated once plateaus were reached, after 400 min (
Table 2).
During the transport, the TC was not totally degraded, but there were many degradation intermediates going out of the filter. On the UV-visible spectrum performed after HPLC separation, seven products of degradation can be detected after the transport, but their identification lies out of the scope of the present study.
4. Discussion
4.1. Hydrothermal Treatment
The hydrothermal treatment allows the modification of manufactured stevensite clay pellets, with physical cohesion maintained within the filter and, consequently, inducing a better longevity in the filter material. All the results show that the stevensite pellets still maintain large adsorption capacity. Considering a TC concentration of 1 g/L, after 3 h of transport, the outflow concentration is about 60% of the initial concentration using a filter manufactured with commercial powder stevensite [
20]. Under the same experimental conditions, the outflow concentration is about 70% with the stevensite pellets in the current work.
The choice of the temperature of the thermal treatment has no significant effect on the breakthrough curve of the TC transport. The CEC, as well as the specific surface area, vary according to the heat treatment applied. Samples treated at lower temperature, 200 and 300 °C, have higher CEC and specific surface area than those treated at higher temperature, 400 and 500 °C. However, numerical values for both properties remain at the same order of magnitude and, thus, have little effect on the reactive transport. Therefore, the use of a low-temperature treatment (200 °C or 300 °C) was preferred because of the lower energy consumption. Samples treated at 300 °C resisted the enzymatic immobilization process, while those at 200 °C disperse. Hence, it is recommended to manufacture the stevensite pellets after treatment at 300 °C (as representative of low-temperature treatment) to make a biogeofilter with enzymes immobilized on the clay.
4.2. Interpretation of Transport Results
It can be observed that the breakthrough curves always followed the same tendency. A first increase of the relative concentration with a quasi-linear behaviour, then the relative concentration increased with a lower slope, reaching a long-time regime of very slow increase of relative concentration.
It can be assumed that the first part of the transport depends on the adsorption equilibrium of the TC on the clay. The second part is considered more dependent on the time, controlled by kinetics, for instance on diffusion of the solute inside the pellets, with the achievement of a relative high adsorption with time.
This interpretation is supported by the case of transport with the non-purified enzyme attached (
Figure 9). It can be observed in the first part of the curve that TC was less absorbed in the presence of enzymes. This would agree with the presence of glutaraldehyde on exchange sites on the surface of the clay. Furthermore, in the second part of the curve, a lower increasing trend is witnessed. Degradation can be observed in a significant way. When the enzymatic activity was low, the adsorption of TC by the stevensite clay was the main phenomenon that varied the concentration of tetracycline. Whereas when the enzymatic activity was high (case of purified enzyme), degradation was a much more preponderant phenomenon, and it decreased the outflow of the TC concentration from the start of the transport.
With the CXTFIT model, either equilibrium transport or non-equilibrium can be modelled. The non-equilibrium situation can take several forms and interpretations. We decided to use the module with two sites of non-equilibrium chemical, which represents a situation of two different sorption sites on clays. The two sites model can be interpreted as a mobile and a stationary phase during transport. As observed in
Figure 9, the experimental data was between the prediction by the one site equilibrium model and the two sites non equilibrium model.
However, in the case of transport at lower concentrations, especially with the enzymes immobilized on the stevensite clay, the model produced a beta value very close to 1. This means that the situation was better simulated by the one site equilibrium model, thus the use of the non-equilibrium model was not necessary in this case.
4.3. Determination of the Retardation Factor
Depending on the method of solving the retardation factor, very different results can be obtained [
39]. Methods based on different analytical solutions, but applied to the same experimental data, will lead to different values for the retardation factor [
40]. To be able to compare the different retardation factors, it is necessary that they were calculated with the same method.
The retardation factor was calculated by different theoretical methods for the transport experiment performed with 1000 mg L
−1 of TC (
Table 3).
The retardation factor depends on the concentration of the injected solution. To make predictions at low concentration, it is necessary to find a relation between the retardation factor and the concentration injected. By means of the experiments performed in the present study with TC solutions of 50, 100, 200 and 1000 mg L−1, the mathematical function (r2 = 0.92) has been obtained to relate the normalized retardation factor () as a function of the TC concentration injected ().
Therefore, using this mathematical function to predict the retardation factor for low concentrations, values of 156 and 644 are found for inflow concentrations of 1 mg L−1 and 1 µg L−1, respectively.
4.4. Determination of the Degradation Factor
Now, assuming the same calculation as for the values in
Table 2, the area ratio increases with the concentration, following exponential Equation (7):
For low concentrations, the
A ratio might be considered independent of the concentration and equal to 0.315. Low degradation percentages can be assumed in aqueous solutions containing only TC, but in complex matrices solutions, this assumption would probably not be valid. Therefore, the degradation for low concentrations can be predicted (
Table 4). As for the data in
Table 2, the area ratios were calculated after 400 min.
4.5. Direct Method Approach for a Real Case Scenario
For technical reasons, we were not able to carry out experiments with concentrations lower than 50 mg L−1. In addition to much longer experimental times, the fast track of the outflow concentration during the run of experiments could not have been possible with the available equipment. However, the actual concentrations of antibiotics in the wastewater is in the range of μg L−1.
Making use of the above estimations performed in the present work, we have performed an exercise to predict the efficiency of the biogeofilter with TC concentration of 100 μg L−1. To do that, we use a direct approach with the STANMOD program with the following parameters:
= 0.38 cm/min;
= 0.43 cm
2/min, estimated with the same proportion of mixture clay:sand 1:1; hydrodynamic parameters are approximately conserved. The values for
and
were estimated in the previous
Table 3 and
Table 4. The results of the present estimation are shown in
Figure 10 and
Table 5.
The projection shown in
Figure 10 indicates that retention and degradation of TC in the biogeofilter is very efficient, working continuously for 3.5 days. A plateau is reached at around 0.15 times the initial concentration (15 µg L
−1), indicating a long lifespan of the filter. Hence, 85% of the initial concentration can be retrieved with only 4.5 g of stevensite treating nearly 6 L of TC solution, therefore accounting for 1.3 m
3/kg.
These estimated calculations are based on a solution containing only TC, however. In a real case scenario, either for irrigation systems or for additional water treatment in WWTP, the water matrix will be rich in organic and inorganic compounds that will compete and probably hinder the performance of the biogeofilter. Although the analytical identification and quantification of TC might be difficult, further experimental studies should be focused on the evaluation of the performance of the biogeofilter in complex matrices, simulating contaminated waters.
The capacity for desorption is also an important feature in the biogeofilter if it is escalated to large scale. As in the study by Fernández et al. [
20] for a geofilter made with a mixture of stevensite powder and quartz sand, the present study shows good desorption capacity for the geofilter made with stevensite pellets and quartz sand. In both cases, desorption has taken place fast, recovering mostly all adsorbed TC and regenerating the cation exchange positions of the stevensite by Mg
2+. Further studies should also be focused on the evaluation of the desorption capacity of the biogeofilter.
4.6. Filter Length
In order to lower the output concentration, it is possible to increase the filter length. STANMOD modelling by direct method can be done by changing the filter length and keeping the other parameters constant (
Figure 11).
It can be observed in
Figure 11 that the longer the filter is, the lower the final output concentration achieved. Assuming a 5 cm length filter with 1 cm radius, 11.25 g of stevensite clay will be required to retrieve 99% of 6 L of TC. That is explained by the increase of the residence time of the reactant in the filter, thus with the same kinetic model, degradation is much higher.
4.7. Large Scale Prediction
In all previous tests, the flow rate was imposed at 1 mL min−1, which results in a pore linear velocity of 0.38 cm min−1. With 4.5 g of clay in a 1:1 mixture (clay:sand), the TC concentration at the outflow is 16% of the initial concentration for a filter of 2 cm length.
If constant porosity is assumed and 1000 times higher volume is to be processed, 1000 times more mass of clay material is required. Therefore, to treat a flux of 1 L min−1 with an efficiency of 99%, 11.52 kg of stevensite pellets would be needed, with a filter of 5 cm length and 32 cm of radius.
Finally, the predictions considered in the present study are based on hydrodynamic properties calculated by the laboratory experiments that were performed at relatively low flow. Real case scenarios at large scale might require treating large volumes of solution. Therefore, the fluid flow might be higher, hence the interaction time between solutes and the surface of the geo- or biogeofilter would decrease due to a kinectic effect that should be considered in further studies.