Abstract
Biotic transformation of imidacloprid (IMD) has been widely investigated in the environments. However, little was known about IMD degradation via abiotic pathways, such as reactive oxygen species (ROS)-based oxidation processes. Here we systematically investigated the mechanism of hydroxyl radical (•OH) production and the associated IMD degradation in the goethite (α-FeOOH)-based Fenton-like systems. Results showed that IMD can be efficiently degraded in the α-FeOOH/H2O2 systems, with degradation rate exceeded 80% within 48 h. Based on the examination of electron paramagnetic resonance (EPR) and chemical probes, •OH was identified as the key ROS that responsible for IMD degradation. IMD can be decomposed via hydroxylation or removal of -N-NO2 to produce hydroxylated IMD, cyclic urea and 6-chloronicotinic acid, with the associated toxicities also evaluated. In addition, the increasing H2O2 concentration and decreasing solution pH both significantly increased IMD degradation. This study provides theoretical understanding for the implications of soil mineral-based Fenton-like reactions in the abiotic transformation of pesticide pollutants.
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Introduction
With the rapid development of agricultural production, the application of insecticides becomes increasingly extensive in the agricultural fields, especially for neonicotinoid insecticides, the most widely used insecticides in the world (Simon-Delso et al. 2015). As one of the highly effective neonicotinoid insecticides, imidacloprid (IMD) is a synthetic compound with a structure similar to nicotine and it kills insects by affecting their central nervous system (Bass et al. 2015; Schaeffer and Wijntjes 2022). The residual average levels of IMD were documented in the range of < 1 to 10 ng g− 1(Jones et al. 2014, Stewart, Lorenz et al. 2014), and the half-life of IMD was approximated ranged from 3 to > 1000 days (Hladik et al. 2018) in different types soils, such as sandy and silty clay soil (Goulson 2013). It has been reported that microbial processes played an important role in IMD transformation in soil. Specifically, Anhalt et al. found that IMD can be degraded by microorganisms using it as the nitrogen source (Anhalt et al. 2007). Besides, bacterial types also affected the pathways and degradation products of IMD (Akoijam and Singh 2015, Kandil, Trigo et al. 2015). The current studies on the transformation and degradation of IMD are mainly focused on the microbial processes in soil (Hussain et al. 2016, Pang, Lin et al. 2020), and little was known about the kinetics and associated mechanisms to IMD transformation via abiotic pathways, such as reactive oxygen species (ROS)-based oxidation processes.
As one of the most powerful oxidants in natural environment, hydroxyl radical (•OH, Eo=2.8 V) can degrade a wide range of organic pollutants in atmosphere, surface water and soil environments (Oturan and Aaron 2014; Gligorovski et al. 2015), including diethyl phthalate (DEP), 2-chlorobiphenyl (2-CB), etc. (Fang et al. 2013, Chen, Fang et al. 2016, Liu, Yuan et al. 2017, Zeng, Dong et al. 2017, Chen, Fang et al. 2019, Chen, Huang Chen et al. 2021a, b). Since superoxide radical (O2•−) are broadly produced by soil microorganisms (Diaz et al. 2013), the formation of hydrogen peroxide (H2O2) can be accomplished via O2•− protonation and oxidase enzymes mediated by functional microbes (Hayyan et al. 2016). Hence, •OH production through the reactions between H2O2 and catalysts (e.g., Fe2+, Fe (oxyhydr)oxides) via Fenton and Fenton-like mechanisms was an omnipresent phenomenon in soil environments. The traditional Fenton reactions used dissolved Fe2+ and H2O2 to produce •OH and degrade organic pollutants effectively (Dalla Villa and Nogueira 2006, Chen, Wei et al. 2022). Besides, iron-bearing minerals-based heterogeneous Fenton-like reactions were also explored (Garrido-Ramirez et al. 2010), which is capable to degrade organic pollutants effectively within the wide pH range and prevent the precipitation of iron ions (Huang et al. 2001, Matta, Hanna et al. 2007, Pham, Lee et al. 2009). Although papers have reported that Fe bearing mineral-based Fenton-like systems (e.g., Fe-bearing minerals/H2O2) were active to induce the organic pollutants degradation, such as alachlor (Hou et al. 2017), acetamiprid (Mitsika et al. 2013), dimethyl sulphoxide (Wu et al. 2006) etc., current studies are mainly focused on exploring applicable strategies for enhancing the efficiency of ROS formation and contaminants degradation in the goethite/H2O2 systems, such as the introducing hydroxylamine (Hou et al. 2017), and ascorbate (Wang et al. 2021 , Chen et al. 2021a, b). Hence, systematic studies involving organic contaminants degradation in the goethite/H2O2 systems are still needed, especially the degradation of organic contaminants that rarely reported. Besides, imidacloprid (IMD) is one of the highly effective neonicotinoid insecticides with production of ten thousands of tons per year (Bass et al. 2015). Many studies have reported the microbial degradation of IMD in soil environments (Hussain et al. 2016, Pang, Lin et al. 2020), whereas its transformation via abiotic pathways, such as reactive oxygen species (ROS)-based oxidation processes, was rather limited. Accordingly, our study was conducive to predicting the abiotic degradation of IMD in soil environments through iron bearing mineral-based Fenton-like reactions.
Accordingly, goethite was selected as the model iron-bearing mineral to examine IMD degradation during Fenton-like reactions. Based on this, our study mainly aims to investigate the mechanisms of •OH formation and IMD degradation by goethite-based Fenton-like reactions, and examine the effect of associated environmental factors. The obtained results will be conducive to understanding the kinetics and mechanisms of •OH-mediated abiotic transformation of pesticide pollutants in soil environments.
Materials and Methods
Chemicals and Materials
Imidacloprid (IMD, ≥ 98%) was purchased from Sigma-Aldrich (USA). Sodium hydroxide (NaOH, 97%), sulfuric acid (H2SO4, 98%), potassium titanium oxalate (C4H2K2O10Ti, 98%), potassium hydroxide(KOH, 85%), ferric nitrate nonahydrate (Fe(NO3)3·9H2O, 98%), tert-butanol (TBA, 99%) were obtained from China National Medicines Corporation Ltd. (Beijing, China). Hydrogen peroxide (H2O2, 30%), benzoic acid (BA, 99.5%), and p-hydroxybenzoic acid (p-HBA, 99.5%) were provided by Nanjing Chemical Reagents Co., Ltd. (Nanjing, China). 5, 5-dimethyl-1-pyrroline N-oxide (DMPO, 97%) and HPLC grade methanol were supplied by J&K Scientific Ltd., China (Shanghai).
Synthesis of Goethite
Goethite (α-FeOOH) was synthesized based on the well-established method (Shuai et al. 2019). Briefly, 30 mL 5 M KOH was added to 1.5 L 0.1 M Fe(NO3)3 solution with pH adjusted to 12.0. The suspension was placed in an oven at 70C for 40 h, and then cooled to room temperature. After that, the suspension was put into 3 K Dalton dialysis bags in ultrapure water bath for 3 days with continuous stirring, and the ultrapure water was renewed three times daily. Finally, the obtained solids were poured into glass vials and freeze-dried to gain α-FeOOH particles. The obtained α-FeOOH samples were characterized by transmission electron microscopy (TEM, JEM-2100 F) and X-ray diffraction (XRD, Ultima IV, Japan; Fig. S1).°
Experimental Procedure
Degradation experiments were performed in 40 mL glass vials, which were placed in a constant temperature shaker (150 rpm, 25 \(\pm\)2 °C) for oscillation reaction. Typical experimental suspensions were consisted of different contents of α-FeOOH, H2O2 and 10 µM IMD, using 0.1 M H2SO4 and NaOH to adjust the solution pH. All experiments were performed in triplicates with standard deviations reported. At predetermined time intervals, a certain volume of suspension was withdrawn and mixed with 50% methanol to quench the reaction. Then, the suspension was filtered with 0.22 μm PTFE membrane for IMD analysis. Benzoic acid (BA) was added to probe the produced •OH via formation of hydroxybenzoic acid (HBA) without IMD addition. The concentration of p-hydroxybenzoic acid (p-HBA) was analyzed to quantify the •OH accumulation with the conversion factor of 5.87 (Chen et al. 2021). The effects of α-FeOOH dosages (0.5-5 g L−1), H2O2 concentration (0.2-2 mM) and pH (3.0–11.0) on IMD degradation were also performed under same conditions. All experiments were conducted in triplicates, with mean values and standard errors reported.
Analytical Methods
The concentrations of IMD, BA and p-HBA were analyzed by HPLC (Agilent 1200, USA) equipped with a Supelcosil LC-18 column (25 cm×4.6 mm) and a diode-array detector (DAD). The mobile phase was consisted of 60% ultrapure water and 40% methanol at a flow rate of 1.0 mL min− 1 for IMD analysis. The detection wavelength of DAD was at 270 nm. The mobile phase was consisted of 35% methanol and 65% phosphate buffer (0.1%) at a flow rate of 1.0 mL min− 1 for BA and p-HBA analyses. The detection wavelength of DAD was at 254 and 300 nm. The LODs of BA and IMD were 25 and 91 nM, respectively. The recovery of IMD was in the range of 91.0-99.5%, with standard deviation in the range of 0.7–6.1%. The IMD products were identified by liquid chromatographic time-of-flight mass spectrometer (LC-TOF-MS, AB SCIEX, USA).
H2O2 concentration was analyzed based on the potassium titanium oxalate method and detect the H2O2 concentration by spectrophotometer (UV 2700, Shimadzu, Japan) at 400 nm wavelength (Pham et al. 2009). The •OH production was examined using an electron paramagnetic resonance (EPR, Bruker E500-9.5/12) with 0.1 M 5, 5-dimethyl-1-pyrroline N-oxide (DMPO) as the trapping agent. The operational condition of EPR was set at X-band with a microwave power of 6.33 mW, modulation frequency of 100 kHz, resonance frequency of 9.42 GHz, and modulation amplitude of 1.0 G.
Results and Discussion
IMD Degradation in the α-FeOOH/H2O2 Systems
The degradation kinetics of IMD (10 µM) were firstly examined in the α-FeOOH/H2O2 systems (Fig. 1a). The IMD concentration negligibly changed with α-FeOOH alone, which indicated that IMD was relatively stable in the presence of α-FeOOH. The IMD concentration decreased by approximated 20% within 48 h in the presence of H2O2, suggesting that IMD was oxidized by H2O2. However, IMD degradation exceeded 80% within 48 h in the α-FeOOH/H2O2 system, indicating IMD degradation was greatly enhanced due to the Fenton-like reaction between α-FeOOH and H2O2.
The IMD degradation of were well fitted with the pseudo first-order kinetics, with the results shown in Fig. 1b. The degradation rate constant (kobs) of IMD was 0.035 \(\pm\)(9.1 \(\times\)10− 4) h− 1 in the α-FeOOH and H2O2 system, which was much higher than that of α-FeOOH (2.2 ± 1.5 × 10− 4 h− 1) and H2O2(6.9 ± 0.2 × 10− 3 h− 1) alone. These results further demonstrated that IMD degradation was significantly enhanced in the α-FeOOH and H2O2 system. Meanwhile, the amount of dissolved Fe3+ was measured by O-phenanthroline colorimetry (Fang et al. 2013), and results showed that the dissolved Fe3+ concentration was undetectable after reaction. Hence, IMD degradation was mainly induced by the heterogeneous Fenton processes rather than homogeneous reactions (Lin et al. 2014).
Mechanism of IMD Degradation in The α-FeOOH and H2O2 System
The Identification of Key ROS
To investigate key ROS in the α-FeOOH/H2O2 system, EPR examination was applied with DMPO as trapping agent (Fang et al. 2013). The signals of free radical formation in the α-FeOOH/H2O2 system was measured at different times (Fig. 2a). As shown in Fig. 2a, there are strong 4-fold characteristic peaks with an intensity ratio of 1:2:2:1, which was the characteristic signal of DMPO-OH (Zhou et al. 2018). This result indicated the •OH signal production in the α-FeOOH/H2O2 system. The DMPO-OH signal was slightly increased at 48 h versus that at 5 min, suggesting •OH production was sustained during reaction. The TBA was further added to reaction system as the scavenger of •OH. Results showed that IMD degradation was significantly inhibited (<1%) with addition of TBA, further indicating that the produced •OH was responsible for IMD degradation.
The •OH formation was further quantified with BA (Fig. 2c), which showed that 630.2 µM •OH was accumulated within 48 h. Besides, correlation analyses between •OH accumulation and IMD concentration was performed in Fig. 2d. Results showed that IMD concentration was negatively correlated (R2\(=\)0.90) with •OH accumulation. These combined results demonstrated that •OH was the key ROS for IMD degradation in the α-FeOOH/H2O2 system.
The Proposed Degradation Pathways of IMD Induced by •OH
The total of five products of IMD were identified after •OH oxidation (Fig. S2), including the hydroxylated IMD, cyclic urea and 6-chloronicotinic acid, etc. Accordingly, IMD degradation pathways were proposed based on the identified products and previous studies (Malato et al. 2001, Wang, Shu et al. 2022). As shown in Fig. S3, there are two main pathways for IMD degradation, showing that IMD was hydroxylated by •OH to produced products I and II. Meanwhile, the removal of -N-NO2 from IMD can generate productsIII and IV. Finally, all intermediate products were converted into 6-chloronicotinic acid.
To evaluate the ecological risk of IMD and its products, ECOSAR program was used to predict the toxicity of IMD and its products. Table S1 shows that the median lethal concentration (LC50), median effect concentration (EC50) and chronic value (ChV) of 4-hydroxy derivative for fish and green algae exceed 100 mg/L, which indicated that 4-hydroxy derivative was lower toxicity than IMD. The LC50 of cyclic urea for daphnia was 39.68 mg/L, and the EC50 of cyclic urea for green algae was 0.02 mg/L. Besides, the ChV of cyclic urea for fish, daphnia and green algae were 0.94, 9.64, 0 mg/L, respectively. Additionally, the LC50 of 6-chloronicontic acid for fish and daphnia were 21.09, 12.8 mg/L, and the ChV of 6-chloronicontic acid for fish and daphnia were 10.89, 0.69 mg/L respectively. The LC50, EC50 and ChV of parameters of cyclic urea and 6-chloronicontic acid were lower than those of IMD, which indicated that these two products were much more toxic than IMD. Therefore, the toxicity of IMD intermediate products increased or decreased depending on its structures.
Effects of Environmental Factors on IMD Degradation
α-FeOOH Dosages
The effect of α-FeOOH dosages on IMD degradation were investigated under ambient conditions (Fig. S4a). Results showed that IMD degradation increased from 65 to 80% with α-FeOOH dosages increasing from 0.5 to 1 g L− 1, and changed negligibly at 2 g L− 1. With α-FeOOH dosage increased to 5 g L− 1, IMD degradation efficiency declined to 60%. Correspondingly, the kobs value increases from 2.2 ± 0.1 × 10− 2 h− 1(0.5 g L− 1) to 3.1 ± 0.1 × 10− 2 h− 1(1 g L− 1), but then gradually decreased to 1.7 ± 0.1 × 10− 2 h− 1 at 5 g L− 1(Fig. S4b). These combined results further indicated that 1 g L− 1 of α-FeOOH was the optimal dosage for IMD degradation. These results might be mainly because that increasing dosages of α-FeOOH was contributed to producing more •OH (Le-Tuan et al. 2012, Lin, Ma et al. 2014). But large amounts of α-FeOOH adsorbed more surface Fe3+ and consequently induced more HO2• production via H2O2 decomposition (Eqs. 1 and 2) (Usman et al. 2022), which finally inhibited IMD degradation.
Effect of pH
The effect of pH (3.0–11.0) on IMD degradation was further investigated in the α-FeOOH/H2O2 system (Fig. S5a). Results showed that IMD degradation rate significantly decreased from 80 to 15% with pH increasing from 3.0 to 11.0. Correspondingly, the kobs decreased from 2.9 ± 0.0 × 10− 2 h− 1 to 3.0 ± 0.4 × 10− 3 h− 1(Fig. S5b), indicating IMD degradation was intensively inhibited under neutral and alkaline conditions. Two possible reasons might be responsible for this phenomenon. Firstly, lower pH was conducive to activating more H2O2 to produce more •OH (Burbano et al. 2005). However, H2O2 was easily decomposed into H2O and O2 under alkaline conditions, which inhibited •OH production (Buthiyappan et al. 2016, Zong, Xu et al. 2020). Another probable reason was probably due to the changed surface charge of α-FeOOH, with point of zero charge (pHpzc) of 7.7 (Nezamzadeh-Ejhieh and Amiri 2013). When pH is higher than pHpzc(Lin and Gurol 1998), the surface of α-FeOOH is negatively charged (Nezamzadeh-Ejhieh and Zabihi-Mobarakeh 2014). Hence, H2O2 decomposition was increasingly impeded with the increase of pH due to the repellency between H2O2 and negatively charged surface. Consequently, •OH production was significantly declined and induced less IMD degradation.
H2O2 Concentration
Figure S6a shows the effect of H2O2 concentrations on IMD degradation. The degradation efficiency increased from 30 to 80% with the H2O2 concentration increased from 0.2 to 2 mM. Meanwhile, kobs values also increased from 6.5 ± 0.5 × 10− 3 h− 1 to 2.8 ± 0.1 × 10− 2 h− 1(Fig. S6b), which indicated that the increased H2O2 concentration enhanced IMD degradation. Previous studies also documented that increased H2O2 concentration was contributed to •OH production (Fang et al. 2018, Wang, Ding et al. 2020), which was responsible for the enhanced IMD degradation. Meanwhile, H2O2 concentration also decreased during reaction (Fig. S7a,b), indicating the decomposition of H2O2 for •OH production. These combined results demonstrated that the increased H2O2 concentration was conducive to IMD degradation in the α-FeOOH/H2O2 system.
Conclusion
This study systematically investigated the processes and mechanisms of •OH production and associated IMD degradation in the α-FeOOH/H2O2 systems. Results showed that the lower pH and increasing H2O2 concentration significantly improved IMD degradation. The •OH was key ROS in the α-FeOOH/H2O2 system as demonstrated by EPR and chemical probes, which was responsible for the proposed initial hydroxylation products and following degradation of IMD. IMD can be decomposed via hydroxylation or removal of -N-NO2 to produce hydroxylated IMD, cyclic urea and 6-chloronicotinic acid. The toxicities of these intermediates increased or decreased depended on the properties of organic compounds. All these results provides theoretical understanding to α-FeOOH-based Fenton-like reactions that responsible for the abiotic transformation of pesticide pollutants, like IMD.
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Acknowledgements
This work was supported by the Anhui Province Natural Science Foundation (2208085MD87), the National Natural Science Foundation of China (no. 42107382) and the Natural Science Foundation of Jiangsu Province (BK20200323).
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Ye, B., Cui, H., Chen, N. et al. A Mechanistic Study of Goethite-Based Fenton-Like Reactions for Imidacloprid Degradation. Bull Environ Contam Toxicol 110, 57 (2023). https://doi.org/10.1007/s00128-023-03696-7
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DOI: https://doi.org/10.1007/s00128-023-03696-7