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Environmental Processes
Rapid Hydrolysis of Penicillin Antibiotics Mediated by Adsorbed Zinc on Goethite Surfaces Feng Sheng, Jingyi Ling, Chao Wang, Xin Jin, Xueyuan Gu, Hong Li, Jiating Zhao, Yujun Wang, and Cheng Gu Environ. Sci. Technol., Just Accepted Manuscript • DOI: 10.1021/acs.est.9b02666 • Publication Date (Web): 16 Aug 2019 Downloaded from pubs.acs.org on August 16, 2019
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Rapid Hydrolysis of Penicillin Antibiotics Mediated by Adsorbed Zinc on Goethite Surfaces
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Feng Sheng1, Jingyi Ling1, Chao Wang1, Xin Jin1, Xueyuan Gu1, Hong Li2, Jiating Zhao2, Yujun Wang3, Cheng Gu1*
4 5 6
1State
Environment, Nanjing University, Nanjing 210023, P.R. China
7 8
Key Laboratory of Pollution Control and Resource Reuse, School of the
2CAS
Key Laboratory for Biological Effects of Nanomaterials and Nanosafety,
9
HKU-IHEP Joint Laboratory on Metallomics, Institute of High Energy Physics,
10
Chinese Academy of Sciences, Beijing 100049, P.R. China
11 12
3State
Key Laboratory of Soil and Sustainable Agriculture, Institute of Soil
Science, Chinese Academy of Sciences, Nanjing 210008, P. R. China
13 14
*To whom correspondence should be addressed
15
Cheng Gu
16
Professor
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School of the Environment
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Nanjing University
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Nanjing, Jiangsu, 210023
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P. R. China
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Phone/Fax: +86-25-89680636
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E-mail:
[email protected] 1
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TOC Art
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Abstract
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The soil environment is an important sink for penicillin antibiotics released from
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animal manure and wastewater, but the mineral-catalyzed transformation of
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penicillins in soil has not been well studied. To simulate this environmental process,
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we systematically investigated the behavior of penicillin G and amoxicillin, the two
32
most widely-used penicillin antibiotics, in the presence of goethite and metal ions.
33
The results demonstrated that Zn ion significantly promoted the hydrolysis of
34
penicillins in goethite suspensions, as evidenced by the degradation rate nearly three
35
orders of magnitude higher than that of the non-Zn-containing control. Spectroscopic
36
analysis indicated that the specific complexation between penicillins, adsorbed Zn and
37
goethite was responsible for the enhanced degradation. Metastable interactions,
38
involving hydrogen bonds between carbonyl groups in the β-lactam ring and the
39
double/triple hydroxyl groups on goethite surface, and coordination bonding between
40
carboxyl groups and surface irons, were proposed to stabilize the ternary reaction
41
intermediates. Moreover, the surface zinc-hydroxide might act as powerful
42
nucleophile to rapidly rupture the β-lactam ring in penicillins. This study is among the
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first to identify the synergic roles of Zn ion and goethite in facilitating penicillin
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degradation and provides insights for β-lactam antibiotics to assess their
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environmental risk in soil.
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Introduction
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Recently, the widespread antibiotics in aquatic and soil environments have raised
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a worldwide concern, as the overuse of antibiotics leads to the emergence of resistant
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bacteria problem threatening human health.1-3 The β-lactam antibiotics are the most
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frequently used antibiotics, making up over 50% of the total worldwide antibiotic
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consumption.4,5 Among them, the usage of penicillins accounts for the major
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consumption of β-lactam antibiotics.6 Previous study indicated that penicillin
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antibiotics could be degraded through hydrolysis, photolysis and biological reactions
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in the aqueous environment, where the occurrence of penicillin antibiotics is relatively
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low ranging from 3 to 200 ng L-1 in wastewater effluent and surface water.7 The
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metal-assisted degradation of penicillin antibiotics in the presence of Zn2+,8 Cu2+,9
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Mn2+,10 Fe3+ 4 and Cd2+
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carbonyl and amino functional groups in penicillins account for the strong tendency to
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complex with metal ions, which in turn significantly influences the stability of the
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β-lactam ring.4 For example, coordination between Zn2+ and penicillins could stabilize
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the tetrahedral intermediate generated from OH- attack on β-lactam ring and promote
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their degradations.8 Previous studies further indicated that different metal ions
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exhibited different enhancement for the degradation of penicillin antibiotics due to the
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different sites of metal-ion coordination.12 Compared to aqueous phase reactions, few
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studies have investigated the transformation of penicillin antibiotics in soil.
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Nonetheless, the intense veterinary usage of penicillins in livestock and the
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subsequent application of antibiotic-containing animal manure on agricultural fields
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has been widely reported in solution phase. The carboxyl,
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as fertilizer have led to the release of considerable amounts of antibiotics into the
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soil.13,14 According to the previous literatures, microbial-involved hydrolysis reaction
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in soil environment is deemed as the main degradation pathway for penicillins.15-18 A
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recent study found that amoxicillin could still be quickly degraded in sterilized soil,14
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suggesting that abiotic degradation of penicillins might also play an essential role in
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soil environment. Furthermore, the different physicochemical characteristics of
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penicillins, such as their solubility, speciation and octanol-water partitioning
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coefficient (KOW), as well as the properties of the soil, including the pH, water content
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and microbial activity, could also affect degradation.7,13 The low KOW values of
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penicillins (0.87–1.83)1 would hinder their association with the organic components
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of soil, whereas soil minerals, e.g., iron oxides, clays and manganese oxides, may
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provide matrices to form surface complexes with penicillin functional groups.19,20
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Goethite is a common mineral, which is ubiquitously distributed in soils and
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sediments.21 Due to its unique surface structure, goethite is able to strongly adsorb
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several antibiotics in soil and subsequently catalyze their transformation.22-26 For
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instance, Zhang and Huang found that fluoroquinolone antimicrobials could be
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strongly adsorbed onto goethite accompanied by the slow oxidation process.2
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Furthermore, goethite mineral usually coexists with various heavy metals in natural
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soil.27 According to the prior studies, goethite particles were considered as the
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potential sink for many cations (Cu, Mn, Ni and Zn)28 and Zn-bound goethite was also
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observed in natural loess soil.29,30 The typical concentrations of Zn in agricultural
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soils were reported to range from 52.17 to 227 mg kg-1.31-33 Even higher 5
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concentrations of Zn could be detected in industrial polluted soils.27 Therefore, the
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coexistence of metals and goethite could be ubiquitous in natural soil, which might
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significantly affect the migration and transformation of organic and inorganic
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contaminants on goethite surface.34-38 Gräfe et al. investigated the co-sorption of
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arsenate and zinc ion in soil, and found that the adsorption of arsenate on ferrihydrite
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increased by ~5 times in the presence of zinc via the formation of surface precipitate
97
[Zn2(AsO4)OH].27 In addition, the study of Gu et al. revealed that copper ion was able
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to enhance the adsorption of ciprofloxacin on goethite surface by forming
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goethite-copper-ciprofloxacin ternary complex.25
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So far, few studies have comprehensively examined the reactions of penicillin
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antibiotics in metal/goethite systems. Thus, the objectives of this study were to
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identify the surface-mediated reaction of penicillins on goethite in the presence of
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common metal ions, and to elucidate the mechanism underlying the rapid hydrolysis
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of penicillin determined in a Zn/goethite system. The analyses were performed using
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Fourier transform infrared (FTIR) and Zn K-edge X-ray absorption near edge
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structure (Zn K-edge XANES) spectrometry. To our knowledge, this study is among
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the first to demonstrate the synergetic effects of Zn ion and goethite on catalyzing
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hydrolysis of penicillin antibiotics under mild conditions. As such, these new findings
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contribute to a better understanding of the environmental persistence and
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transformation of not only penicillins but also many other β-lactam antibiotics in soil.
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Materials and Methods
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Chemicals. Chemicals used in this study were described in the Supporting
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Information. Goethite was synthesized following the method of Zhao et al26 and the
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details were also shown in the Supporting Information.
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Degradation and Adsorption Experiments. Three buffers, MES (10 mM, pH
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5.5 and 6.5), HEPES (10 mM, pH 7, 7.5 and 8) and CHES (10 mM, pH 9 and 10),
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were selected due to their previously reported negligible effects on the interactions
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between contaminants and minerals.9,39 These buffers were prepared by dissolving the
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required amounts of reagents and then adjusting the solution pH by the addition of 1
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M HCl or 1 M NaOH. To exclude the effects of organic buffers and glass bottles,
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control experiments were conducted and the detailed information was listed in
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Supporting Information. The results (Figure S1-S3) indicated that neither organic
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buffers nor glass bottles had effects on the degradation process. Before the reaction,
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the colloid solution (100 mL) containing goethite (0.02 to 0.5 g L-1), Zn ion (1 to 50
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µM) and different buffer (MES, HEPES or CHES, 10 mM) was thoroughly mixed
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using magnetic stirring bar at 200 rpm in an amber glass vial (100 mL) for 2 h. Our
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preliminary results (Figure S4) indicated that the adsorption of Zn, Co, Ni, Cu and Pb
128
on goethite could reach equilibrium within 2 h. The reaction temperature was at 20 ±
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2 °C, and the variation of pH was controlled within 0.1 units. The initial concentration
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of antibiotics was 50 µM in the reaction vial. To initiate the reaction, 1 mL antibiotic
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solution (5 mM) was spiked into the reaction solution (100 mL). At predetermined
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time interval, 1 mL suspension was sampled and transferred to a tube prefilled with 7
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0.1 mL EDTA solution (0.2 M). Then the residual antibiotic was extracted by shaking
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for 5 min, and filtered through a 0.22 µm PTFE membrane. The recovery rates of PG
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and AMX with EDTA extraction were detected as 103-104% and 99-103%,
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respectively. The adsorption of penicillins on goethite was proven to be negligible in
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Zn/goethite system (Figure S5, S6). Similar experiments were conducted for Co, Ni,
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Cu and Pb ions. A pseudo-first-order kinetics model was used to fit the degradation
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kinetics and then the rate constant (k, min-1) was calculated.4,10 Calculation details of
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the pseudo-first order degradation constant were involved in Supporting Information.
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The degradation of penicillin antibiotics under anoxic condition was also conducted
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by purging N2 during the whole reaction period. A quenching experiment, in which
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isopropanol (100 mM) was added as a radical scavenger, was conducted to investigate
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the potential involvement of hydroxyl radicals in the reaction. All the experiments
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were conducted in triplicate.
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We also tested the adsorption of Zn on goethite at different concentrations of Zn
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and goethite at pH 7 under the same reaction conditions. Before the analysis, the
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samples were centrifuged at 4,000 g for 20 min and filtered through a 0.22 µm
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cellulose acetate membrane. The Zn2+ concentration in solution was finally
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determined by inductively coupled plasma-optical emission spectroscopy (ICP-OES,
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PQ 9000, Jena, Germany) after the sample was acidified with 6 M HNO3 (10 µL).
152 153 154
Analytical Methods. The details of analytical methods of penicillin antibiotics were described in Supporting Information. Spectroscopic Analysis. IR spectra were obtained by FTIR spectroscopy 8
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(Bruker Tensor 27, Germany), using a system equipped with an attenuated total
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reflection (ATR) ZnSe crystal flow cell. In this study, H2O was replaced by D2O to
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eliminate the disturbance due to the strong H-O-H bending absorption at ~1640
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cm-1.17 To investigate the interaction between AMX and goethite in the presence of
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Zn, 1 mL of 4 g L-1 goethite suspension in D2O was initially spread on the cell and
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dried at 40 °C in a vacuum oven overnight to form a uniform goethite coating. The IR
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spectra were then collected as below. Firstly, 1 mL NaCl solution (10 mM, in D2O)
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was added into the coated cell and then 20 µL Zn2+ solution (5 mM, in D2O) was
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applied. After equilibrium of Zn on goethite for 2 h, the background spectrum for
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each sample was collected. Subsequently, 0.1 mL AMX stock solution (5 mM in
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D2O) was spiked into the cell and IR spectra were continuously collected every 10
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min in the range of 1000 to 2000 cm-1 with a resolution of 4 cm-1 and total scan of 64
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within 30 min. The pD of the solution was adjusted to 7.0 ± 0.1 by addition of 1 M
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DCl or 1 M NaOD. Similarly, the FTIR spectra of control groups, including AMX
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solution alone, AMX/Zn, and AMX/goethite systems, were obtained for comparison.
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The zinc species adsorbed on goethite were characterized by Zn K-edge XANES
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experiment conducted on the BL14W beamline at Shanghai synchrotron radiation
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facility. The energy of synchrotron was performed at 3.5 GeV and the current was
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between 150 and 200 mA. Franklinite (ZnFe2O4), smithsonite (ZnCO3), willenite
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(Zn2SiO4), Zn(OH)2 and ZnO were served as the reference compounds. The
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suspension sample, consisting of goethite, NaCl and Zn with the final concentrations
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of 5 g L-1, 10 mM and 10 mM, was firstly prepared. Then the system pH was adjusted 9
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to 5.5, 7 and 10 by addition of HCl (1 M) and NaOH (1 M). After the pH was
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stabilized for 48 h, the suspension was centrifuged at 4000 g for 30 min and the
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sludge paste was collected to mount in a thin plastic sample holder covered with
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Kapton tape. The Zn K-edge (9659 eV) was carried out with a Si (111) crystal
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monochromator, and the Athena program was used for data processing.
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Results and Discussion
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Enhanced Degradation of Penicillins on Goethite in the Presence of
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Different Metals. The degradation of PG in the presence of goethite was negligible
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(< 4%) at neutral solution (pH = 7) within 48 h (Figure S7). However, when metal
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ions were present, the degradation rates were significantly enhanced, following the
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order: Zn > Co > Ni ≈ Cu ≈ Pb (Figure 1a). Especially for Zn, the degradation rate (k
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= 1.14 h-1) increased ~3 orders of magnitude higher than the control sample with PG
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and goethite (k = 0.001 h-1). The enhancement of PG degradation by Zn in the
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presence of goethite was also observed at lower PG concentration (Figure S8). The
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study by Gu et al. showed the enhanced adsorption of ciprofloxacin in ternary
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complexation of Cu/goethite/ciprofloxacin.25 However, in our penicillin/Zn/goethite
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system, the adsorption of penicillins on goethite was negligible (Figure S5, S6).
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Previous studies also indicated that metals (Cu, Zn, Co, et. al.) could facilitate the
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degradation of penicillin antibiotics via forming the metal/antibiotics complexes in
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homogeneous solution, while the rates followed a different pattern as Cu > Zn > Ni ≈
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Co.27,35 In homogeneous metal-catalyzed degradation, the aqueous metal ions (e.g. 10
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Zn2+, Co2+, Fe3+) could coordinate with the functional groups in penicillin molecules
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to stabilize the tetrahedral intermediate generated from H2O and OH- attack on the
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beta-lactam ring.10 Moreover, the prominent mechanism for penicillin degradation in
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the presence of Cu2+ was attributed to Cu-complex oxidation process.9 Therefore, the
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discrepancy probably reflected the difference in the mechanism of PG degradation in
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metal/goethite vs. aqueous system. Since Zn exhibited the most significant effect, we
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would focus on the catalytic degradation of penicillins in the coexistence of Zn ion
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including adsorbed and aqueous Zn, and goethite suspension (Zn/goethite system) to
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explore the underlying mechanism in the following study. Degradations of three
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analogous penicillins (6-APA, AMP and AMX) were also conducted in Zn/goethite
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system, which had the same basic structure as PG but different substituted groups in
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the branched chain (Figure 2). As a result, compared to the control groups (Figure
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S9), the prominent enhancements for degradation of all four penicillins in Zn/goethite
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system were observed (Figure 1b), and the calculated pseudo-first-order degradation
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constants of PG, AMP, AMX and 6-APA were 1.14, 0.516, 0.438 and 0.174 h-1,
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respectively. The different degradation behaviors of these penicillin antibiotics were
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consistent with their susceptibility to the nucleophilic attack, which was mainly
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attributed to the inherent strain in β-lactam ring.12 As the structural hydrogen in
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penicillins was substituted by the electron-donating groups (amino and hydroxyl
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groups), the torsional rotation of β-lactam ring might decrease, subsequently
218
enhancing the stability.35 The penicillin antibiotics could be rapidly degraded in
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Zn/goethite system, and the ternary interactions between penicillin antibiotics, 11
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goethite and Zn ion might account for this degradation.
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The degradation of penicillin antibiotics via hydrolysis and oxidation reactions
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mediated by transition metals or minerals has been widely reported.3,9,19,39 To obtain
223
insights into the mechanism of penicillin degradation in Zn/goethite system, we
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conducted anoxic and radical quenching experiments with two typical penicillins (PG
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and AMX) and identified the reaction products arising from their degradation. As
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shown in Figure S10, neither oxygen nor isopropanol had a significant effect on the
227
degradation, indicating that penicillin degradation did not involve oxygen or hydroxyl
228
radicals. The analysis of degradation products demonstrated that the hydrolysis
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products of AMX and PG differed in their retention times but had the same molecular
230
weights as 383 (365 + 18) for AMX and 352 (334 + 18) for PG (Figure S11).40
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According to the mass spectra, the major degradation products were confirmed to be
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the two amoxicilloic acid isomers for AMX, and two penicilloic acid isomers for PG
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(Figure S11), which were widely reported as the major hydrolysis products of PG and
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AMX.4 Whereas, the absence of oxidation products with molecular weights of 381
235
(AMX, 365 + 16) and 350 (PG, 334 + 16) indicated the absence of the oxidation
236
reaction
237
demonstrated that only hydrolysis degradation of penicillin antibiotics occurred, when
238
Zn2+ or Fe3+ ions existed in solution.4,8,10 Therefore, the coexistence of Zn and
239
goethite catalyzes the rapid degradation of penicillins dominantly via hydrolysis
240
rather than oxidation. Interestingly, the degradations of both AMX and PG were
241
completely suppressed by addition of EDTA (Figure S10), which could be explained
in
the
AMX(PG)/Zn/goethite
system.
Similarly,
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by the strongly competitive complexation of EDTA against penicillins for the reactive
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sites in Zn/goethite system. Hence, the primary interaction between penicillin
244
antibiotics and Zn/goethite is prerequisite for the hydrolysis reaction.
245
Furthermore, the effects of Zn concentration, goethite dosage and system pH on
246
AMX and PG hydrolysis were also investigated. As shown in Figure 3, PG was more
247
facile to undergo hydrolysis than AMX in Zn/goethite system, in agreement with the
248
regular hydrolysis pattern in homogeneous solution.4,40 The hydrolysis rates of both
249
AMX and PG increased with the increasing dosage of adsorbed Zn. Moreover, the
250
remarkable correlation between hydrolysis rates (k, min-1) and amounts of adsorbed
251
Zn (Figure 3a) suggested that the degradation of AMX (R2 = 0.94, p < 0.01) and PG
252
(R2 = 0.96, p < 0.01) was dependent on the adsorbed Zn rather than the aqueous Zn. In
253
addition, less enhancement for both PG and AMX degradation was observed with
254
high adsorbed Zn (>24 mg g-1, Figure 3a). As the initial concentration of Zn ion
255
was >30 µM, nearly maximum adsorption capacity (24 mg g-1) on goethite (50 mg
256
L-1) could be achieved (Figure S12a). Meanwhile, the Zn ion in solution also
257
significantly increased (Figure S12b), which would complex with penicillins in
258
homogenous solution and prevent the formation of ternary intermediate. This result
259
further confirmed the important role of adsorbed Zn species in penicillin hydrolysis in
260
Zn/goethite system. Similarly, Figure S13 showed that the rates of AMX and PG
261
hydrolysis also increased as more goethite was added, presumably due to the creation
262
of additional reactive sites for hydrolysis as Zn ions were increasingly adsorbed.
263
However, the excessive goethite (dosage above 0.2 g L-1) slightly suppressed both 13
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AMX and PG hydrolysis in Figure S13. When the amount of goethite was over 0.2 g
265
L-1, all the Zn ions were adsorbed, and the excessive goethite could compete against
266
Zn species to form the reactive ternary complex, finally resulting in the decreased
267
rates of hydrolysis.4 Moreover, system pH also played an essential role in hydrolysis
268
with the optimal condition at pH 8.5 (Figure 3b). As the pH changed from 5.5 to 10, a
269
few parameters in penicillin/Zn/goethite system would be altered, including the
270
adsorption amount of Zn, species of adsorbed Zn and penicillin antibiotics, and
271
surface charge of goethite. Specifically, due to the multiple pKa values of AMX (2.4,
272
7.4 and 9.6) and PG (2.7),41 AMX would exist as zwitterion AMX, AMX- and
273
AMX2-, whereas anionic PG- was the dominant species of PG in this pH range (Figure
274
S14). Compared to PG hydrolysis, the similar trend for AMX degradation was
275
observed (Figure 3b), suggesting that the varied charge of AMX might have little
276
influence on its hydrolysis process. Figure 3b also showed that the adsorption of Zn
277
ion on goethite reached the maximum at pH 8.5, since higher pH promoted the
278
deprotonation of the active surface and the surface-mediated hydrolysis of Zn.42 As
279
the pH increased to 8.5, the increased amounts of adsorbed Zn would provide more
280
reactive sites and penicillin hydrolysis would be accelerated.43 However, at a pH >
281
8.5, the surface charge of goethite would alter from positive to negative, as the point
282
of zero charge (pHPZC) of goethite was measured as ~9 (Figure S19). The electrostatic
283
repulsion between negatively charged goethite and penicillin molecules would
284
strongly inhibit their interactions, finally suppressing the hydrolysis process. In
285
addition, as the change of system pH, the speciation of adsorbed Zn also changed. 14
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However, it is quite difficult to distinguish the importance between the speciation of
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adsorbed Zn and the adsorption amount for the enhanced hydrolysis of penicillin,
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since the two variables changed simultaneously. More discussion for the reactive Zn
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species on goethite surface was provided below.
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FTIR and Zn K-edge XANES Analysis. In this study, FTIR spectroscopy was
291
applied to investigate the interactions between penicillin antibiotics and Zn/goethite.
292
Due to the low absorption intensity of PG, AMX served as the model compound
293
(Figure S15). As shown in Figure 4, the absorption bands of AMX solution at 1766,
294
1674, 1602, 1518, 1457, 1402 and 1268 cm-1 referred to the stretching vibration of
295
ketone in β-lactam ring (νC=O), stretching vibration of ketone in amide bond (νC=O,
296
amide),
297
phenolic hydroxyl (νOH), bending vibration of C-N-C in amide group (νC-N-C,
298
symmetric stretching vibration of carboxyl (νCOOs) and bending vibration of C-N in
299
β-lactam ring (νC-N), respectively. The FTIR spectra of AMX binding to the sole Zn
300
ion (Figure 4a), goethite (Figure 4b) and coexistence of Zn and goethite (Figure 4c)
301
were also recorded for comparison. It was reported that the difference Δν (Δν = νCOOas
302
- νCOOs) between asymmetric and symmetric stretching vibrations of carboxyl could
303
be used to identify the binding mode of the carboxylic group with metals.25 When the
304
Δν of the free carboxyl was greater than that of the carboxyl-metal coordination, it
305
suggested a bidentate complex in carboxyl-metal chelate, otherwise a monodentate
306
complex.
307
asymmetric stretching vibration of carboxyl (νCOOas), stretching vibration of amide),
At pD 7.0, the Δν of AMX/Zn (232 cm-1) was greater than that of AMX (201 15
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cm-1), indicating a monodentate complex between the carboxylic group and Zn ion in
309
solution (Figure 4a). Together with the blue shift of C-N group from 1269 to 1283
310
cm-1 in β-lactam ring and red shift of carboxyl group from 1402 to 1372 cm-1,
311
aqueous Zn ion was indicated to complex with AMX via carboxyl group and ternary
312
nitrogen, which was in good agreement with a previous study.4 Furthermore, the
313
slight red shifts (4 and 3 cm-1) at 1518 and 1457 cm-1 in AMX/Zn system suggested
314
that the active coordination sites of AMX might also involve the phenolic hydroxyl
315
and amide nitrogen. However, the absence of an obvious change at 1766 cm-1 ruled
316
out the coordination of carbonyl group in β-lactam ring with aqueous Zn ion (Figure
317
4a).
318
In contrary, unlike AMX/Zn system, the carbonyl bonds in both β-lactam ring
319
and amide group shifted to 1752 and 1656 cm-1 upon the interaction with goethite,
320
respectively (Figure 4b). These widened and red-shifted peaks in AMX/goethite
321
system evidenced the formation of hydrogen bonds between carbonyl groups and
322
hydroxyl groups on goethite surface.25,44,45 Furthermore, the decreased Δν (191 cm-1)
323
in AMX/goethite system supported the bidentate coordination between carboxylic
324
group and surface iron, which was different from the monodentate complex in
325
AMX/Zn system. The unchanged absorption at 1268 cm-1 indicated that the C-N
326
group in β-lactam ring was not involved in the interaction between AMX and goethite
327
(Figure 4b).
328
The coordination bonds between the goethite surface and the β-lactam ring
329
determined for AMX/Zn/goethite were confirmed by the similarities of peak shifts 16
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compared with the AMX/goethite and AMX/Zn systems (Figure 4c). Among them,
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carboxyl group of AMX on Zn/goethite preferentially formed the bidentate complex
332
with surface iron rather than Zn species, evidenced by the less Δν of AMX (190 cm-1).
333
The coordination of AMX in Zn/goethite system was further confirmed at different Zn
334
concentrations. As shown in Figure 4d, the absorption peaks of AMX at 1752 and
335
1658 cm-1 did not increase accordingly, suggesting that the carbonyl groups were
336
primarily coordinated with goethite. Meanwhile, the increasing intensity of IR peak at
337
1272 cm-1 supported the coordination between Zn species and nitrogen in β-lactam
338
ring. In addition, the increase in the Δν of AMX from 176 cm−1 to 193 cm−1 was
339
consistent with a change in AMX complexation, from a bidentate ligand with surface
340
iron to a monodentate ligand with the excess of Zn species. Together with all the
341
evidence above, we could conclude that the specific interactions in AMX/Zn/goethite
342
system involved: (i) the coordination between adsorbed Zn species and nitrogen in
343
β-lactam ring, (ii) bidentate coordination between carboxyl group and surface iron,
344
and (iii) hydrogen bonds between carbonyl groups and surface hydroxyl groups.
345
Therefore, the enhancement of AMX hydrolysis can be mostly attributed to the
346
specific ternary coordination between AMX and Zn/goethite. A similar mechanism
347
for the abiotic hydrolysis of penicillins in Zn2+/tris(hydroxymethyl)aminomethane
348
(Zn2+/Tris) system was also reported.43 The chelating effect of Tris in a ternary
349
coordination of penicillin/Zn2+/Tris was shown to be responsible for stabilization,
350
with the Zn-bound hydroxyl group of Tris serving as a powerful nucleophile to attack
351
the β-lactam carbonyl group. An analogous mechanism was described for hydrolytic 17
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in metallo-β-lactamase enzymes,41 in which two dominant metals were located in
353
their active sites. One is essential for catalysis and the other for stabilizing the
354
reaction intermediate.15-18,46 In AMX/Zn/goethite system, the abundance of hydroxyl
355
groups on the crystallographic surface of goethite offer the sufficient reactive sites to
356
form hydrogen and coordination bonds, which in turn stabilize the ternary
357
intermediates. The positive correlation between the degradation rates (k, min-1) and
358
amounts of adsorbed Zn (R2>0.94, Figure 3a) suggests that the adsorbed Zn species
359
may act as the strong nucleophile to attack the β-lactam ring, leading to rapid
360
cleavage of the C-N bond. In contrary, in penicillin/goethite system, the complexation
361
forms between carbonyl group and surface hydroxyl group without a powerful
362
nucleophile on the reactive site. In this case, H2O or OH- in solution acts as the weak
363
nucleophile, which would explain the slow hydrolysis measured at neutral pH (Figure
364
S9). Similarly, the slow hydrolysis in penicillin/Zn system is attributed to the low
365
concentrations of stabilizer. In summary, the enhanced hydrolysis determined in
366
penicillin/Zn/goethite system can be attributed to the synergistic effects of both
367
goethite surface and adsorbed Zn species. Furthermore, goethite surface may offer
368
sufficient reaction sites to concentrate both nucleophile and penicillin molecule,
369
thereby increasing the possibility of their direct contact.
370
Since the hydrolysis reaction was strongly affected by the species of adsorbed
371
Zn, we analyzed the morphology of Zn at different pH values using Zn K-edge
372
XANES analysis. As shown in Figure 5, the normalized absorptions could be fitted by
373
standard references, including franklinite, smithsonite, willenite, Zn(OH)2 and ZnO at 18
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pH 5.5, 7 and 10 (Figure S16). According to the linear combination fitting shown in
375
Table 1, franklinite was the predominant Zn species at pH 5.5 (41.4%), followed by
376
Zn(OH)2 (26.8%). As the pH increased to 7, 61.5% of the adsorbed Zn species was in
377
the form of Zn(OH)2, while ZnO accounted for 67.3% of the Zn species and Zn(OH)2
378
decreased to 7.1% at pH 10 on the goethite surface (Table 1). Based on these results,
379
hydrolysis reaction is mostly related to the Zn adsorption in the presence of
380
zinc-hydroxide species such as Zn(OH)2, which could mediate the rapid hydrolysis of
381
penicillin antibiotics. Similarly, in homogeneous Zn/penicillin reaction, zinc-bound
382
hydroxyls could act as the main nucleophile to catalyze the hydrolysis of penicillins.43
383
In summary, Zn ion can interact with goethite surface in penicillin/Zn/goethite
384
system. The pKa of Zn-bound water decreases via polarization effect to form the
385
adsorbed zinc-hydroxides on goethite surface, which act as the Lewis acid to complex
386
with functional groups in penicillin.43 The generation of zinc-hydroxide would
387
account for its role as the main nucleophile in penicillin hydrolysis.
388
Effects of Different Surface Hydroxyl Groups on Penicillin Hydrolysis.
389
Based on the FTIR results (Figure 4), the hydrogen bonds between the surface
390
hydroxyl groups and AMX are crucial for hydrolysis. However, three different
391
hydroxyl groups, including singly (≡FeOH), doubly (≡Fe2OH) and triply (≡Fe3OH)
392
coordinated forms, co-exist on goethite surface.47 To differentiate the effects of
393
different hydroxyl groups on hydrolysis reaction, goethite surface was modified by
394
phosphate or fluoride following the Wei’s method (Supporting Information).48
395
Excessive Na2HPO4 (1 mM) and NaF (10 mM) were utilized in modification to 19
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ensure the complete OH-substitution on surface. After modification, hydroxyl groups
397
were coordinated by fluoride or phosphate, as the hydroxyl stretching vibration (3132
398
cm-1) for both phosphate and fluoride modified goethite underwent the remarkable red
399
shifts (4 cm-1) in Figure S17.49,50 However, previous study indicated that fluoride and
400
phosphate ions preferentially exchanged with singly coordinated hydroxyls, while the
401
doubly and triply coordinated groups remained intact.47 Therefore, the modification
402
mainly changed the singly coordinated hydroxyls, rather than the doubly or triply
403
complexed counterparts. Interestingly, as shown in Figure S18, phosphate modified
404
goethite exhibited the strong inhibition for AMX hydrolysis, while the negligible
405
effect was observed for fluoride modification. In the reaction solution, neither
406
phosphate nor fluoride ion was detected (data not shown), suggesting that the
407
disturbance of aqueous phosphate or fluoride ion on the adsorption of Zn could be
408
excluded. Our results demonstrate that lack of singly coordinated hydroxyls in
409
fluoride modified goethite does not result in the remarkable decrease of hydrolysis
410
rate, indicating that the carbonyl group in β-lactam ring might prefer to complex with
411
doubly and triply coordinated hydroxyl groups to form the surface hydrogen bond.
412
The inhibition by phosphate modified goethite might be explained by the change of
413
surface charge on goethite. After phosphate modification, the pHPZC of goethite
414
decreased from 9.2 to 6.7, while the change of pHPZC for fluoride modified goethite
415
(8.9) was negligible (Figure S19). The repulsions between negatively charged AMX
416
and phosphate modified goethite would obstruct the coordination at pH 7, finally
417
inhibiting the AMX hydrolysis. Therefore, the doubly or triply coordinated hydroxyl 20
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groups on goethite surface might be the dominant sites for penicillin complexation.
419
Environmental Significance
420
This study demonstrates that penicillin antibiotics can be rapidly hydrolyzed in a
421
Zn/goethite system under environmentally relevant conditions (neutral pH, room
422
temperature and environmental concentration). The enhanced hydrolysis is likely due
423
to the synergetic effects of goethite and the adsorbed Zn species, in which goethite
424
stabilizes the reaction intermediates and zinc-hydroxide acts as a powerful
425
nucleophile. This finding reveals a new abiotic degradation route for penicillin
426
antibiotics, and thereby improves the understanding of environmental fate for both
427
penicillin antibiotics and their transformation products in soil. Moreover, the
428
degradation mechanism may be also relevant to the hydrolysis of other β-lactam
429
antibiotics (e.g. cephalosporins and monobactams) in the environmental matrices,
430
containing metal ions and minerals, which would provide valuable information for
431
developing abiotic degradation strategies for antibiotics. More importantly, our results
432
suggest that the potential effects of naturally occurring ions (K+, Ca2+, Na+ and heavy
433
metals) on the adsorption and transformation processes of common antibiotics in soil
434
should not be ignored and need more investigations in future researches.
435
Acknowledgements
436
This work was financially supported by National Science Foundation of China
437
(21777066), the Natural Science Foundation of Jiangsu Province (BK20170634) and
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the Collaborative Innovation Center for Regional Environmental Quality.
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Supporting Information Available
440
Parameters of HPLC and HPLC-QTOF-MS methods for 6-APA, PG, AMP and
441
AMX antibiotics; degradation of PG in the presence of goethite in control treatment;
442
degradation of 6-APA, PG, AMP and AMX antibiotics in control treatments;
443
degradation of AMX and PG with quenching reagents or under ambient and anoxic
444
conditions; AMX and PG degradation products analysis by HPLC-QTOF-MS ;
445
degradation of PG and AMX in different concentration of goethite; distribution
446
fractions of PG and AMX molecules in pH (1 ~ 12); different molecular structures of
447
PG and AMX; Zn K-edge XANES spectra of standard reference compounds; FTIR
448
spectra of goethite, phosphate-modified and fluoride-modified goethite; hydrolysis of
449
AMX with original and different modified goethite; zeta potentials of original and
450
different modified goethite from pH 5.5 to 10.
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References
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alga-containing water environment: a mechanism and kinetic study. Environ. Sci. Pollut. R. 2019, 26, 9184-9192. 2.
Zhang, H.; Huang, C. H. Adsorption and oxidation of fluoroquinolone antibacterial agents and
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Kümmerer, K. Antibiotics in the aquatic environment - A review Part II. Chemosphere 2009, 75,
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Hydrolysis vs oxidation. J. Hazard. Mater. 2017, 335, 117-124. 5.
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Shannon, M. M.; Jeffrey L. U.; Amy L. T.; Richard J. W. pH and temperature effects on the
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dinuclear zinc(II) complexes: Functional mimics of metallo-β-lactamases. J. Am. Chem. Soc. 2000, 122, 6411-6422. 19. Hsu, M. H.; Kuo, T. H.; Chen, Y. E.; Huang, C. H.; Hsu, C. C.; Lin, A. Y. C. Substructure reactivity affecting the manganese dioxide oxidation of cephalosporins. Environ. Sci. Technol. 2018, 52, 9188-9195. 20. Pan, M.; Chu, L. M. Fate of antibiotics in soil and their uptake by edible crops. Sci. Total. Environ. 2017, 599-600, 500-512. 21. Liu, Q.; Li, X.; Tang, J.; Zhou, Y.; Lin, Q.; Xiao, R.; Zhang, M. Characterization of goethite-fulvic acid composites and their impact on the immobility of Pb/Cd in soil. Chemosphere 2019, 222, 556-563. 22. Xu, J.; Marsac, R.; Costa, D.; Cheng, W.; Wu, F.; Boily, J. F.; Hanna, K. Co-binding of pharmaceutical compounds at mineral surfaces: Molecular investigations of dimer formation at goethite/water interfaces. Environ. Sci. Technol. 2017, 51, 8343-8349. 23. Krumina, L.; Lyngsie, G.; Tunlid, A.; Persson, P. Oxidation of a dimethoxyhydroquinone by ferrihydrite and goethite nanoparticles: Iron reduction versus surface catalysis. Environ. Sci. Technol. 2017, 51, 9053-9061. 24. Benacherine, M. E. M.; Debbache, N.; Ghoul, I.; Mameri, Y. Heterogeneous photoinduced degradation of amoxicillin by goethite under artificial and natural irradiation. J. Photoch. Photobio. A. 2017, 335, 70-77. 25. Gu, X.; Tan, Y.; Tong, F.; Gu, C. Surface complexation modeling of coadsorption of antibiotic ciprofloxacin and Cu(II) and onto goethite surfaces. Chem. Eng. J. 2015, 269, 113-120. 26. Zhao, Y.; Geng, J.; Wang, X.; Gu, X.; Gao, S. Adsorption of tetracycline onto goethite in the presence of metal cations and humic substances. J. Colloid Interf. Sci. 2011, 361, 247-251. 27. Carabante, I.; Grahn, M.; Holmgren, A.; Kumpiene, J.; Hedlund, J. Influence of Zn(II) on the adsorption of arsenate onto ferrihydrite. Environ. Sci. Technol. 2012, 46, 13152-13159. 28. Wei B. G.; Yang L. S. A review of heavy metal contaminations in urban soils, urban road dusts and agricultural soils from China. Microchem. J. 2010, 94, 99-107. 29. Singh, B. and Gilkes, R. J. Properties and distribution of iron oxides and their association with minor elements in the soils of south-western Australia. J. Soil Sci. 1992, 43, 77-78. 30. Manceau, A.; Tamura, N.; Celestre, R. S.; MAcdowell, A. A.; Geoffroy, N.; Sposito, G.; Padmore, H. A. Molecular-scale speciation of Zn and Ni in soil ferromanganese nodules from loess soils of the Mississippi Basin. Environ. Sci. Technol. 2003, 37, 75-80. 31. Pan, L. B.; Ma, J.; Wang, X. L.; Hou, H. Heavy metals in soils from a typical county in Shanxi Province, China: Levels, sources and spatial distribution. Chemosphere 2016, 148, 248-254. 32. Holmgren, G. G. S.; Meyer, R. L.; Chaney, R. L.; Daniels R. B. Cadmium, lead, zinc, copper and nickel in agricultural soils of the United States of America. J. Environ. Qual. 1993, 22, 335-348. 33. Facchinelli., A.; Sacchi., E.; Mallen., L. Multicariate statistical and GIS-based approach to identify heavy metal sources in soils. Environ. Pollut. 2001, 114, 313-324. 34. Forbes, E. A.; Posner, A. M.; Quirk, J. P. The specific adsorption of divalent Cd, Co, Cu, Pb, and Zn on goethite. J. Soil Sci. 1976, 27, 154-166. 35. Buerge-Weirich, D.; Hari, R.; Xue, H.; Behra, P.; Sigg, L. Adsorption of Cu, Cd and Ni on goethite in the presence of natural groundwater ligands. Environ. Sci. Technol. 2002, 36, 328-336. 36. Swedlund, P. J.; Webster, J. G.; Miskelly, G. M. Goethite adsorption of Cu(II), Pb(II), Cd(II), and Zn(II) in the presence of sulfate: Properties of the ternary complex. Geochim. Cosmochim. Ac. 2009, 24
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73, 1548-1562. 37. Alcacio, T. E.; Hesterberg, D.; Chou, J. W.; Martin, J. D.; Beauchemin, S.; Sayers, D. E. Molecular scale characteristics of Cu(II) bonding in goethite-humate complexes. Geochim. Cosmochim. Ac. 2001, 65, 1355-1366. 38. Grossl, P. R.; Sparks, D. L.; Ainsworth, C. C. Rapid kinetics of Cu(II) adsorption/desorption on goethite. Environ. Sci. Technol. 1994, 28, 1422-1429. 39. Chen, J.; Sun, P.; Zhang, Y.; Huang, C. H. Multiple roles of Cu(II) in catalyzing hydrolysis and oxidation of β-lactam antibiotics. Environ. Sci. Technol. 2016, 50, 12156-12165. 40. Hirte, K.; Seiwert, B.; Schüürmann, G.; Reemtsma, T. New hydrolysis products of the beta-lactam antibiotic amoxicillin, their pH-dependent formation and search in municipal wastewater. Water Res. 2016, 88, 880-888. 41. Vijaya Bhaskar Reddy, A.; Yusop, Z.; Jaafar, J.; Jamil, N. H.; Majid, Z. A.; Aris, A. B. Development and validation of capillary electrophoresis method for simultaneous determination of six pharmaceuticals in different food samples combining on-line and off-line sample enrichment techniques. Food Anal. Method. 2018, 11, 533-545. 42. Mustafa, G.; Singh, B.; Kookana, R. S. Cadmium adsorption and desorption behaviour on goethite at low equilibrium concentrations: Effects of pH and index cations. Chemosphere 2004, 57, 1325-1333. 43. Diaz, N.; Sordo, T. L.; Suarez, D.; Mendez, R.; Martin-Villacorta, J. Zn2+ catalysed hydrolysis of β-lactams: Experimental and theoretical studies on the influence of the β-lactam structure. New J. Chem. 2004, 28, 15-25. 44. Fang, Y.; Zhou, W.; Tang, C.; Huang, Y.; Johnson, D. M.; Ren, Z. J.; Ma, W. Brönsted catalyzed hydrolysis of microcystin-LR by siderite. Environ. Sci. Technol. 2018, 52, 6426-6437. 45. Paul, T.; Machesky, M. L.; Strathmann, T. J. Surface complexation of the zwitterionic fluoroquinolone antibiotic ofloxacin to nano-anatase TiO2 photocatalyst surfaces. Environ. Sci. Technol. 2012, 46, 11896-11904. 46. Hu, Z.; Periyannan, G.; Bennett, B.; Crowder, M. W. Role of the Zn1 and Zn2 sites in metallo-β-lactamase L1. J. Am. Chem. Soc. 2008, 130, 14207-14216. 47. Ding, X.; Song, X.; Boily, J. F. Identification of fluoride and phosphate binding sites at FeOOH surfaces. J. Phys. Chem. C 2012, 116, 21939-21947. 48. Li, W.; Zhang, S.; Shan, X. Q. Surface modification of goethite by phosphate for enhancement of Cu and Cd adsorption. Colloid. Surface. A 2007, 293, 13-19. 49. Wei, S.; Tan, W.; Zhao, W.; Yu, Y.; Liu, F.; Koopal, L. K. Microstructure, interaction mechanisms and stability of binary systems containing goethite and kaolinite. Soil Sci. Soc. Am. J. 2012, 76, 389-398. 50. Weckler, B.; Lutz, H. D. Lattice vibration spectra. Part XCV. Infrared spectroscopic studies on the iron oxide hydroxides goethite(α) akaganéite(β) lepidocrocite(γ) and feroxyhite(δ). Eur. J. Solid State Inorg. Chem. 1998, 35, 531-544.
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578
Table 1 Relative proportion of Zn species on goethite at different pH values (5.5,
579
7 and 10) as determined by Zn XANES linear combination fitting (%) Sample
Franklinite
Smithsonite
Willenite
Zn(OH)2
ZnO
R-factor
pH 5.5
41.4
11.4
21.3
26.8
NA
0.0025
pH 7.0
10.4
4.9
23.2
61.5
NA
0.0014
pH 10
10.6
NA
15.0
7.1
67.3
0.0024
580
Franklinite: ZnFe2O4, Smithsonite: ZnCO3, Willenite: Zn2SiO4.
581
NA: Not available.
582
R-factor: Residual factor.
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Figure legends
585
Figure 1. (a) Degradation kinetics of PG in the presence of goethite and different
586
metal ions, including Co2+, Ni2+, Cu2+, Pb2+ and Zn2+; (b) Degradation kinetics of
587
6-APA, PG, AMP and AMX in the presence of goethite and Zn ion. The initial
588
concentrations of penicillin antibiotic, goethite, metal salt were 50 µM, 50 mg L-1 and
589
3 µM, respectively. The reaction pH was controlled at 7.0 ± 0.1 by 10 mM HEPES
590
buffer.
591
Figure 2. Molecular structures of 6-APA, PG, AMP and AMX.
592
Figure 3. (a) The degradation constants (k, min-1) of PG (red) and AMX (black)
593
plotted against the adsorption amounts of Zn ion (mg g-1) on goethite. The linear
594
fitting equations, determination coefficient (R2) and significance (p) were shown.
595
Reaction pH was controlled at 7.0 ± 0.1 by 10 mM HEPES. (b) Degradation constants
596
(k, min-1) of PG and AMX plotted against the different pH values (black). Adsorption
597
amounts of Zn on goethite plotted against the different pH values (blue). The initial
598
concentrations of Zn, AMX, PG and goethite were 3 µM, 50 µM, 50 µM and 50 mg
599
L-1, respectively. The pH values ranged from 5.5-9.5 were stabilized in 10 mM MES,
600
HEPES and CHES buffers.
601
Figure 4. ATR-FTIR spectra of (a) AMX in Zn solution; (b) AMX on goethite film;
602
(c) AMX on goethite film in the presence of Zn. The spectra were recorded every 10
603
min within 30 min. (d) FTIR spectra of AMX on goethite film with different initial Zn
604
concentrations (1, 10 and 100 µM) after 30 min equilibrium. The ionic strength and
605
pD were 10 mM NaCl and 7.0 ± 0.1, respectively. The initial concentration of AMX
606
was 500 µM. The spectrum of AMX (5 mM) in D2O at pD 7.0 was shown in black
607
line.
608
Figure 5. Zn K-edge XANES spectra of adsorbed Zn species on goethite at different
609
pH of 5.5, 7.5 and 10. Normalized absorption and fitting absorption at different pH
610
were represented in solid line and dots, respectively.
27
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612
613 614
Figure 1
615
28
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616 617
Figure 2
618
29
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619
620 621
Figure 3
622 623
30
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625
31
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627 628
Figure 4
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630 631 632 633
Figure 5
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