Yongyuan Yina,
Xuetao Guo*a,
Chen Yangb,
Liangmin Gaoa and
Youbiao Hua
aSchool of Earth and Environment, Anhui University of Science and Technology, Huainan 232001, China. E-mail: guoxuetao2005@163.com; Fax: +86-554-6668004; Tel: +86-554-6668004
bCollege of Environment and Energy, South China University of Technology, Guangzhou, 510006, China
First published on 23rd September 2016
Renewable agricultural residues are produced in large quantities as waste, and their storage and management create environmental problems. Similarly, antibiotics could cause harm to the ecosystem and to the growth of plants and animals. As one of the widely used antibiotics in the world, the environmental risks of tylosin (TYL) are receiving increasing attention. In order to find a clean and effective method for TYL removal from an aqueous solution, maize straw (MS) is modified by goethite and the sorption capacity of the natural and modified forms (MSF) is determined for TYL removal. The characterisations of MS and MSF were carried out by XRD, FTIR, XPS and SEM-EDS. The characteristics of the sorption behavior of TYL on MS and MSF are systematically investigated. The results indicate that the sorption capacity of TYL on MSF is significantly higher than MS, and the sorption kinetics data of TYL on MS and MSF well fits the pseudo-second-order kinetics model and the sorption isotherms data well fits the linear model. Moreover, the sorption thermodynamics of TYL on MSF and MS indicate that a high temperature could favor the sorption of TYL on MS and MSF. In addition, the sorption of TYL on MS and MSF can be affected by pH and ionic strength of the solution. The sorption mechanisms of TYL on MS mainly involve electrostatic interactions and hydrophobic interactions, whereas electrostatic interactions, H bonding, hydrophobic interactions and surface complexation play a primal role in the sorption of TYL on MSF.
Currently, many scholars have studied the removal of antibiotics from water, and the main methods for the removal of antibiotics include sorption, photodegradation, biodegradation and oxidation.1 Sorption, due to its simplicity, eco-friendliness and high efficiency, is one of the most important methods for antibiotics removal.8 Jia et al.9 reported oxytetracycline sorption on maize-straw-derived biochar, and their results showed that the sorption of oxytetracycline on biochar is highly pH-dependant and that surface complexation, π–π interaction and metal bridging were the most important sorption mechanisms. Zheng et al.10 studied sulfamethoxazole (SMX) sorption on biochars produced at 300–600 °C, and their results showed that biochars have the potential for remediation of soil or water containing sulfonamides in a wide range of pH and that hydrophobic interaction, π–π electron donor–acceptor interaction and pore-filling were the most important sorption mechanisms. Pezoti et al.11 reported NaOH-activated carbon of high surface area, which was produced from guava seeds, as an adsorbent for amoxicillin removal, and their results showed that the high-efficiency of the modified guava seeds for amoxicillin sorption was predominantly due to chemisorption. However, the process used to prepare biochars is mainly pyrolysis, which wastes lots of energy. Renewable agricultural residues are produced in huge quantities as waste, and their storage and management create environmental problems.12 Maize straw is very common in China and might be valuable for biomass production. However, it has not been paid much attention for the removal of antibiotics, which makes use of some of the more environmentally friendly ways that it can be modified.13
At present, there are many reports on the sorption of pollutants by modified biomass, for example Zhang et al.14 investigated the use of hexadecyl trimethyl ammonium bromide (HTAB) to modify rice straw by the grafting method. Zhou et al.15 reported novel carboxylate-rich wheat straw through surface graft modification for the efficient separation of Ce(III) from wastewater. However, the use of chemical methods to modify straw is not very good, since they are likely to produce secondary pollution. Goethite (a-FeOOH) is one of the most common and stable crystalline iron oxide in sediments and natural systems.16 This mineral has a relatively high surface area and high reactivity, which could be suitable for the sorption and deactivation of pesticides, nutrients, and hazardous compounds in natural conditions and might greatly affect the distribution and transport of contaminants in the environment.17 Previous studies have shown that goethite has the capacity to adsorb antibiotics, therefore the capacity of tylosin on biomass will be improved by using goethite to modify straw biomass, and not produce secondary pollution.4
In this study, the aim was to find an efficient method for TYL removal from aqueous solution by goethite modified maize straw, and understand the contribution of complexes on the aqueous solution fate of TYL and assess the sorption behavior and mechanism of TYL on complexes accurately. The influences of solution chemical factors (pH and ionic strength) on the sorption of TYL on straw biomass and goethite complexes are systematically investigated.
Goethite was synthesized according to the method introduced by Brigante et al.18 In brief, 5 M KOH was added to 0.5 M Fe(NO3)3 until a red colloid was generated. The resulting ferrihydrite dispersion was aged at 60 °C in a capped Teflon container for 60 h and then it was washed with double distilled deionized (DDI) water until the supernatant reached a pH close to the point of zero charge. Furthermore, the dispersion was freeze-dried to obtain a dry powder.
The MS–goethite (MSF) complexes were synthesized according to Guo et al.17 with minor modification. Briefly, 0.8 g bulk MS was added to 300 mL distilled water, and the suspension was sonicated for 10 min. Then, 0.8 g FeOOH was added to the suspension, and the suspension was successively sonicated for 30 min and stirred for 3 h. Then the mixture solution was poured into a Teflon crucible and placed inside an autoclave at 120 °C for 3 h, after which the suspensions were centrifuged at 3500 rpm for 30 min, then dried at 50 °C.19
Fourier transform infrared (FTIR) spectra were recorded with KBr pellets in the mid-infrared region using a Nicolet 6700 Infrared Detector (Thermo Fisher Scientific, USA). The constituents of the samples were identified using an X-ray powder diffractometer (XRD) (XD-2X/M4600, Beijing Purkinje General Instrument Co., Ltd, China). During the analysis, the samples were scanned from 20 to 70° at a speed of 4° min−1 using Cu Ka radiation at 40 kV. The microscopic features of the materials were recorded with an environmental scanning electron microscope (SEM) (XL-30-ESEM, Philips, Netherlands). X-ray photoelectron spectroscopy (XPS) data were obtained with an XSAM-800 spectrometer to study the elemental compositions. The point of zero charge (PZC) was measured by potentiometric titrations at three KCl concentrations.
Sorption isotherm experiments for TYL were conducted at 25 ± 2 °C by adding adsorbent to 15 mL solutions with initial concentrations of TYL of 1 ppm, 5 ppm, 10 ppm, 20 ppm and 30 ppm with the adsorbent dosage of 0.02 g, 0.03 g, 0.03 g, 0.05 g and 0.07 g, respectively. The mixed solutions were shaken at a speed of 150 rpm for 12 h. After the sorption, the samples were collected in a pre-weighed 1.5 mL amber glass vial and filtered through a 0.45 μm membrane filter, and analyzed for the TYL concentration. Each concentration level, including blanks, was run in three parallels.
The pH effect experiments were carried out by adding a mass of 0.03 g sorbent to 25 mL solutions containing TYL with the initial concentration of 10 ppm. The mixed solutions were shaken at a speed of 150 rpm for 12 h. The solution pH was adjusted to different values between 3.0 and 11.0 using potassium hydroxide and HNO3 solution. After the sorption, the samples were filtered through a 0.45 μm membrane filter and analyzed, and each concentration level, including blanks, was run in three parallels.
For ionic strength experiments, a series of 10 ppm TYL solutions were prepared with ionic strengths from 0 to 0.1 M KNO3. The other sorption procedures were the same as that in the above pH effect experiments.
![]() | (1) |
![]() | (2) |
The rate parameter ki for intraparticle diffusion model can be defined as:
qt = kit0.5 + constant | (3) |
The experimental isotherm data of TYL was correlated by the linear, Freundlich and Langmuir equations, which can be written as follows:2,7
qe = kdCe | (4) |
qe = kfCen | (5) |
![]() | (6) |
The thermodynamic parameters (ΔH0, ΔS0, and ΔG0) can be determined from the temperature dependence. Free energy changes (ΔG0) are calculated from the following equations:
ΔG0 = −RT![]() ![]() | (7) |
![]() | (8) |
The values of ΔS0 were calculated from:
![]() | (9) |
Fig. 2 shows the X-ray diffractogram of the FeOOH, MS and MSF samples. The peak coincidence and the absence of extra peaks in the experimental diffractogram indicate that the studied FeOOH sample was a well-crystallized goethite, and that no other crystalline phases were detected by XRD. The goethite characteristic peaks are located at 20.92, 32.66, 35.96 and 53.06.18 Strong diffraction peaks are observed at the 2θ of 15.60 and 22.23 for MS. After combining MS and FeOOH, all the peaks of the as-prepared MS and FeOOH were still observed, although the intensity of the reflection peaks at the 2θ of 15.60 decreased, which imply that the MSF complexes retained the composition of both MS and FeOOH. This result indicates that the crystal structure of goethite was not changed after modification with MS.21
Fig. 3 shows the FTIR spectra of the FeOOH, MS and MSF samples. For the goethite spectrum, the two index peaks at 3400 and 3150 cm−1 are assigned to the –OH vibration which is related to non-stoichiometric hydroxyl units (excess water) in the goethite structure. The band at 1634 cm−1 is assigned to the water bending vibration. The strong absorption peaks at 890 cm−1 and 790 cm−1 are caused by the in-plane bending of the surface hydroxyl of Fe–O–Fe, and 638 cm−1 is due to Fe–O stretching.18,22 For the MS spectrum, the band at 3450 cm−1 is assigned to the O–H stretching vibration of water or H-bonded hydroxyl groups. The band at 2920 cm−1 is assigned to –CH2 stretching. The bands at 1640 and 1380 cm−1 in the spectra MS and MSF can be assigned to CO axial deformation (aldehyde, lactone, ketone and carboxyl groups) and to oxygen functionalities such as highly conjugated C
O stretching or C–O stretching in carboxyl groups, respectively. The peaks at 1560, 1510 and 1460 cm−1 are characteristic bonds of aromatic compounds, which represent the C
O and C
C stretching of conjugated ketones and quinines and aromatic skeletal C, respectively. The bands at 1160 cm−1 can be attributed to the C–O stretching vibration. The peak at around 890 cm−1 is assigned to –OH stretching.9,11 However, compared with the spectra of MS and FeOOH, the only difference in the MSF spectrum is that it has no band at 3150 cm−1. These results confirm that the addition of FeOOH has no effect on the crystal structure of MS. It is also indicated that the binding of FeOOH to the MS surface is mainly through ligand exchange.21
More quantitative information with respect to the chemical composition and functional groups were extracted from the XPS analysis. Fig. 4a shows the XPS spectra of MS and MSF, in which MS shows two dominant peaks at 286 and 533 eV, which correspond to the C1s and O1s bands, respectively. The MSF spectrum shows the same peaks in addition to a third peak at 726 eV, which corresponds to the Fe2p band. As shown in Fig. 4b, for the O1s spectra of MS and MSF, the peaks at 532.79 eV and 531.81 eV, respectively, correspond to the double bond of oxygen, and these peaks confirm the existence of carbonyl and carboxyl groups. The peaks at 534.54 eV and 533.46 eV can be attributed to the single bond of oxygen, and these peaks confirm the existence of epoxy and hydroxyl. However, the XPS spectrum of MSF exhibits a peak at 529.97 eV, which is attributed to the O ion in goethite. As shown in Fig. 4c, the XPS spectrum of MS exhibits three peaks at 284.57 eV, 286.08 eV and 287.34 eV, which are attributed to the CC bond, C–O bond and C
O bond, respectively.23,24 Compared with MS, MSF only has two peaks at 284.6 eV and 286.76 eV, and it is also observed that MSF has no C
O bond at 287.34 eV. Fig. 4d shows the XPS spectra of MSF, in which the peaks at 713.29 eV and 725.99 eV are due to the 2p3/2 and 2p1/2 transitions in goethite, respectively.25
Fig. 5 shows the relationship between zeta potential and pH, and the iso-electric points (IEPs) of MS and MSF. The results indicate that the IEPs of MS and MSF approximately occur in the pH of 2.4 and 6.3, respectively. The IEPs of MSF are higher than that of MS, which suggest that the goethite modification caused MS to have more negative charge due to the introduction of a large amount of goethite.
Conditions | qe exp (mg kg−1) | Pseudo-first-order | Pseudo-second-order | ||||
---|---|---|---|---|---|---|---|
qe (mg kg−1) | k1 (1/h) | R2 | qe (mg kg−1) | k2 × 10−4 (g μg−1 h−1) | R2 | ||
MS | 1527 | 532 | 0.899 | 0.770 | 1530 | 26.07 | 0.999 |
MSF | 2765 | 1867 | 0.962 | 0.793 | 2795 | 6.38 | 0.999 |
To reveal the relative contribution of surface and intraparticle diffusion to the entire kinetic sorption process, the experimental data were fitted with the intraparticle diffusion model. Intraparticle diffusion is presumed to be the rate-controlling step if the simulation curve is linear and the plot passes through origin. As seen from Fig. 7, the fact that the model curves did not pass through the origin with positive intercepts (C ≠ 0) indicates that both surface sorption and intra-particle diffusion contribute to the actual sorption process of TYL on MS and MSF.26 Subsequently, three successive sorption mechanisms were postulated to fit a linear model, as seen in Fig. 7. The first stage, in which about 68–80% of TYL is adsorbed on MS and MSF, is attributed to the occupation of exterior activated sites by various physicochemical interactions (such as hydrophobic interactions, covalent forces, and van der Waals forces). Moreover, the thickness of the boundary layer (C) for MS and MSF in this stage is more conspicuous, which indicates that surface sorption plays an important role for TYL sorption on MS and MSF. In the second stage, only 20–25% of the TYL adsorbed on the sorbents slowly diffused from liquid film into the microporous surface. In the third stage, the intra-particle diffusion rate was obviously lower than the former stage of surface diffusion due to the diameter of the micropore which was relatively small compared to the larger size of the TYL molecule.21
Conditions | Henry model | Freundlich model | Langmuir model | |||||
---|---|---|---|---|---|---|---|---|
kd (L kg−1) | R2 | n | kf (mg kg−1) (mg L)−n | R2 | qm (mg kg−1) | b | R2 | |
MS | 31.4 | 0.987 | 0.705 | 72.2 | 0.963 | 497.5 | 0.218 | 0.959 |
MSF | 125.2 | 0.998 | 0.694 | 281.9 | 0.966 | 1596.9 | 0.293 | 0.954 |
The linear isotherm characteristic suggests an apparent partition of organic pollutants between the two phases of the solids and the solution.2 It can be seen from Table 2 that the sorption data could be fitted well by the linear model (R2 = 0.987 for MS and R2 = 0.998 for MSF), and the kd were 31.4 and 125.2 (L kg−1) for TYL sorption on MS and MSF, respectively. In this matter, our results are in agreement with the studies investigating the sulfadimethoxine and sulfaguanidine sorption behavior on natural soils.27
The Freundlich model is a nonlinear sorption model, which suggests the heterogeneity of the surface and the exponential distribution of sites and their energies.28 It can be seen from Table 2 that the sorption data also could be fitted well by the Freundlich model (R2 = 0.963 for MS and R2 = 0.966 for MSF). The n values were below 1, which suggest a decreasing sorption tendency with an increase in initial concentration. This might be because the high energy sites of MS and MSF were occupied firstly, followed by the lower energy sites, which is an observation characteristic of heterogeneous media.29 The nonlinearity of the sorption behaviors indicates specific interactions with functional groups on MS and MSF.27 The kf for the Freundlich model obtained in this study were 72.2 and 281.9 (mg kg−1) (mg L)−n for MS and MSF, respectively, which indicate that the sorption capacity of TYL on MSF is larger than MS (Table 3).
Conditions | Henry model | Freundlich model | Langmuir model | ||||||
---|---|---|---|---|---|---|---|---|---|
kd (L kg−1) | R2 | n | kf (μg g−1) (mg L)−n | R2 | qm (mg kg−1) | b | R2 | ||
MSF | 15 °C | 75.8 | 0.987 | 0.711 | 183 | 0.978 | 1313 | 0.194 | 0.959 |
25 °C | 123.3 | 0.998 | 0.703 | 278 | 0.971 | 1694 | 0.254 | 0.953 | |
35 °C | 148.9 | 0.994 | 0.627 | 424 | 0.986 | 2005 | 0.387 | 0.975 | |
MS | 15 °C | 19.3 | 0.996 | 0.768 | 37 | 0.973 | 369 | 0.130 | 0.973 |
25 °C | 31.5 | 0.996 | 0.723 | 71 | 0.982 | 552 | 0.187 | 0.978 | |
35 °C | 39.0 | 0.962 | 0.678 | 121 | 0.999 | 862 | 0.198 | 0.993 |
The Langmuir model suggests that uptake occurs on the homogeneous surface by monolayer sorption without interaction between the sorbed molecules.30 It assumes uniform sorption energies onto the surface and no transmigration of sorbate in the surface.2,31 It is clear from Table 2 that the saturate sorption amount of tetracycline on MS and MSF was 497.5 and 1596.9 mg kg−1, respectively. However, the suitability of the use of the Langmuir isotherm to describe the sorption behavior of the investigated TYL can be explained either by the low concentrations used in the experiments or probably by the homogeneity of the interaction sites.27 Nevertheless, the fitting to the Langmuir equation yielded results (R2 = 0.959 for MS and R2 = 0.954 for MSF) not as good as that obtained with the linear model and the Freundlich model mentioned above.
The thermodynamic parameters (ΔH0, ΔS0, and ΔG0) calculated by eqn (7)–(9) are shown in Table 4. It can be seen that the value of kd increased with an increase in temperature. Since the plot of lnk versus 1/T is linear for TYL and SMT (Fig. 10), the related thermodynamic parameters, such as ΔH0 and ΔS0, are available.21 The increased ΔG0 with increasing TYL sorption illustrates that the driving force of sorption decreased due to the occupation of the high energy sorption sites. The highest negative ΔG0 values were found for TYL at the same temperature, which suggest that the sorption potential for TYL was the largest at this temperature. The positive ΔH0 values for TYL indicate that sorption of TYL on MSF and MS was endothermic and associated with an entropy driven process (ΔS0 > 0). Changes in ΔH0 may indicate the binding mechanisms including physisorption (ΔH0 < 40 kJ mol−1) and chemisorption (ΔH0 > 40 kJ mol−1). Thus, TYL sorption onto MS can be mainly attributed to physisorption and TYL sorption onto MSF can be mainly attributed to chemisorption. Another thermodynamic parameter, entropy ΔS0, was used to evaluate the randomness of the system. The sorption of TYL disrupts the hydration shell around MS and MSF, thus leading to increased randomness for the TYL–water–MS/MSF system (ΔS0 > 0). For the TYL–water–MSF system with a higher ΔS0 than the TYL–water–MS system, more energy is needed to regain its original entropy state and TYL sorption onto MSF can be mainly attributed to chemisorption.4,21
Sample | ln![]() |
Temperature (°C) | ΔG0 (kJ mol−1) | ΔH0 (kJ mol−1) | ΔS0 (J mol−1 K−1) |
---|---|---|---|---|---|
MSF | 4.32 | 15 | −17.9 | 41.9 | 155.2 |
4.81 | 25 | −23.2 | |||
5.01 | 35 | −28.5 | |||
MS | 2.96 | 15 | −8.62 | 29.3 | 76.4 |
3.45 | 25 | −10.1 | |||
3.67 | 35 | −13.6 |
The effect of ionic strength as indicated by KNO3 concentration on TYL sorption is shown in Fig. 12. The sorption of TYL decreased as ionic strength increased. The observed inverse relationship between the amount of sorbed TYL and ionic strength suggests that K+ might have competed with TYL for sorption sites,9,33 which suggests that there might exist surface complexation between TYL and MSF.21 The surface of goethite contains active hydroxyl groups, which can adsorb organic pollutants in the form of complexation. A similar interaction was also identified between goethite with TYL and ciprofloxacin.6,34 The sorption mechanisms of TYL on MS and MSF are shown in Fig. 13.
This journal is © The Royal Society of Chemistry 2016 |