Stefano
Econdi
ab,
Chiara
Bisio
*ac,
Fabio
Carniato
c,
Stefano
Marchesi
c,
Geo
Paul
c,
Elisabetta
Gargani
d,
Ilaria
Cutino
d,
Alessandro
Caselli
b and
Matteo
Guidotti
*a
aCNR-Istituto di Scienze e Tecnologie Chimiche “Giulio Natta”, Via C. Golgi 19, Milan, Italy. E-mail: matteo.guidotti@cnr.it; chiara.bisio@uniupo.it
bDipartimento di Chimica, Università degli Studi di Milano, Via C. Golgi 19, Milan, Italy
cDipartimento di Scienze e Tecnologie Avanzate, Università del Piemonte Orientale, Via T. Michel, Alessandria, Italy
dConsiglio per la Ricerca in agricoltura e l'analisi dell'Economia Agraria CREA– Centro di ricerca Difesa e Certificazione DC, Florence, Italy
First published on 22nd May 2024
A set of organic/inorganic layered materials was obtained by functionalizing a montmorillonite-containing bentonite natural clay with linear aliphatic C6 or C7 aldehydes through a cost-effective and technologically simple incipient-wetness deposition method. The solids were investigated by means of a multi-technique approach (X-ray powder diffraction, XRPD, scanning electron microscopy, SEM, Fourier-transform infrared spectroscopy, FT-IR, thermogravimetric analysis, TGA, elemental analysis and solid-state nuclear magnetic resonance, ssNMR) to clarify the nature of the deposited organic species and the mode of interaction between the aldehyde and the clay. Since both natural clays and short-chain linear aldehydes find application as alternative strategies in the control of the olive fruit fly, Bactrocera oleae, the hybrid layered materials were tested under real-life conditions and their insect-inhibiting capability was evaluated in open-field trials on olive tree orchards in Tuscany, Central Italy. Specific tests were conducted to evaluate the resistance of the solids to weathering and their capability to provide a constant and long-lasting release of the bioactive ingredient. Aldehyde-containing bentonite clays have shown promising performance in controlling B. oleae infestation (with up to 86–95% reduction of affected olive fruits) in open-field trials across two years in two locations with different pedological and meteo-climatic characteristics.
Fig. 1 Chemical structures of dimethoate (1), deltamethrin (2), lambda-cyhalothrin (3), acetamiprid (4), phosmet (5), and Spinosad (6). |
Nevertheless, all these insecticides have also shown adverse effects on various non-target animals including mammals, birds, fish, bees and, in general, the environment.10,11 Moreover, their extensive and long use has facilitated the development of insecticide resistance,5,12–14 with a negative impact on beneficial entomofauna15,16 and on the quality of olive oil.17
Therefore, the implementation of innovative and environmentally friendly control methods for this pest has gained significant attention. This interest has grown, especially after the years 2014, 2016, and 2019, when Southern European olive oil production suffered substantial losses in both quality and quantity.18 Furthermore, the recent ban by the European Union on the use of dimethoate in olive crops starting in October 2020 has accelerated the need for alternative strategies.19 These strategies increasingly emphasize the integration of various control methods that meet four main criteria: toxicological safety, environmental selectivity, pest control efficiency and economic sustainability. To prevent or mitigate the effects of fruit fly infestation, various inorganic solids can be applied to olive trees. Many of these systems meet the stringent requirements necessary for use in organic agriculture. Phyllosilicate clays and zeolites of natural origin have often shown interesting features in the protection of crops from pests and diseases.20–24 This is attributed to their negligible toxicological impact, environmental compatibility and remarkable physico-chemical characteristics, in terms of cation-exchange capability and sorption properties. Finely ground mineral clays are indeed able to form a homogeneous particle film on plant leaves and tissues, hence acting as a viable strategy for controlling the infestation of parasitic species.20–22 Analogously, zeolites can be successfully used in agriculture and find application in the reduction of heat stress and sunburn for crops, enhancement of photosynthetic processes and, especially, for their fungicidal and insecticidal properties.25 From the perspective of the most common mineral species used for these purposes, two solids are mainly reported: montmorillonite, with the average composition (Na,Ca)0.3(Al,Mg)2Si4O10(OH)2·n(H2O), that is the main phyllosilicate clay in the natural commercial solid called bentonite, and clinoptilolite, that is a natural-origin zeolite having the minimum formula (Ca,Na,K)2–3Al3(Al,Si)2Si13O36·12(H2O), with a two-dimensional channel system (parallel to a and c axes) with openings in the range of 0.40–0.72 nm.26 Both montmorillonite clay and clinoptilolite zeolite can readily act as adsorbents and ion exchangers.
Considering these properties, clays and zeolites have successfully found application in the protection of olive crops from olive fly as alternatives to conventional agrochemicals. They feature an indirect repellant action against B. oleae, as the inorganic material does not kill the parasite but, rather, negatively affects the recognition of the olive tree and fruit by the adult insect. In fact, when the plant surface is treated with a thin layer of solid, the visual, tactile and olfactive signals by which the fly can recognize the optimal location for egg deposition are masked or scrabbled and this leads to a disorienting action for the insect. Micronized zeolites or clays, in fact, create uniform films, which do not interfere with the metabolic lifecycle of plants but, in contrast, enhance their resistance to external pests and disease.25–27 In addition, these solids, as adsorbing materials, are able to capture water molecules from the surface of leaves and fruits (drying effect), hindering the growth of fungi, larvae and other undesired parasitic species.25
Moreover, such a covering layer helps in protecting the plant from adult insects and other phytophagous arthropods, since the colouring and the microscopic surface structure of leaves and fruits are altered.28,29 Then, the high adsorption capability of zeolites and clays makes them ideal materials for the targeted and controlled release of agrochemicals, semiochemicals and vegetable extracts useful in the protection of crops from pests. Agrochemicals can be deposited, inserted and/or chemisorbed on or in the pore network of zeolitic solids and rock powder or within the interlayer spaces of phyllosilicate clays, thus reducing the amount of active ingredients with a neat benefit in terms of environmental impact, frequency of treatments and amounts of chemicals used.30,31
In line with our ongoing research on aluminosilicate minerals as host plant masking solids,32 these previous attempts prompted us to design a novel class of composite oxidic materials capable of hosting an organic bioactive compound that can effectively disrupt the host-plant selection process of B. oleae adults, featuring a targeted, constant and mild release of the active species for a long-term treatment of the olive fruits. Several studies have demonstrated that medium-chain linear aliphatic aldehydes, specifically n-hexanal, n-heptanal, (E)-hex-2-enal and (E)-hept-2-enal, exhibit clear repellent and/or signalling activity against pests and parasitic organisms affecting crops.33 In particular, these C7 and C6 aldehydes are effective semiochemicals and interfering agents against the olive fly, Bactrocera oleae, and are increasingly being applied for the protection of olive crops.34–37 This includes their deposition and immobilization within lamellar solids in benchmark supports, such as synthetic saponite clays.38
The present study aims at designing and preparing a composite organic/inorganic (oxidic) layered material capable of accommodating a bioactive compound that is active in disrupting the host-plant selection process of B. oleae adults featuring a targeted, smooth and constant release of the bioactive species over time for a long-term treatment of the olive fruits. To this aim, a series of solids inducing an interference activity on the infestations of B. oleae have been prepared. The materials are based on an inorganic support, namely a bentonite clay (mainly composed of montmorillonite) of natural origin. The solids were used either in their native state or after the deposition of a bioactive principle based on organic compounds. The solids were fully characterized by a multi-technique approach (XRPD, SEM, FT-IR, TGA, CHN, elemental metal analysis and solid-state NMR) in order to understand the specific interaction between the aldehyde and the clay and to evaluate the release capability and the stability of the organic species in the materials under ambient conditions.
Finally, the solids were tested under real-life conditions and their insect-inhibiting capability was evaluated in open-field trials on olive tree orchards in Tuscany, Central Italy.
• Bentonite Gl obalfeed AR (Ben; 50 kg batch no. 3101204) is a montmorillonite-containing natural mineral clay, kindly obtained from Laviosa Chimica Mineraria SpA, Livorno, Italy. Its elemental composition, expressed as % m/m, is: Na2O (0.40%), MgO (2.28%), Al2O3 (14.18%), SiO2 (72.32%), P2O5 (0.03%), K2O (1.87%), CaO (0.91%), TiO2 (0.26%), MnO (0.03%) and Fe2O3 (2.33%). The specific surface area of the Ben sample is 114 m2 g−1, calculated from N2 physisorption analyses at 77 K using the Brunauer–Emmett–Teller (BET) model. When Ben was used in its pristine state, it was pretreated as follows: an aliquot of 240 g of Ben was dried in an oven at 110 °C for 3 h and then cooled down for 30 min under anhydrous conditions. Aldehyde-containing solids were prepared by an incipient wetness approach. Linear saturated or unsaturated aldehydes were used, namely: n-hexanal (C6AN; Sigma Aldrich, ≥97%), n-heptanal (C7AN; Sigma Aldrich, ≥95%), (E)-hex-2-enal (C6EN; Tokyo Chemical Industry Ltd, ≥97%), (E)-hept-2-enal (C7EN; TCI, ≥95%). The main physical properties (boiling point, vapour pressure and water solubility) of the organic compounds used in this work are summarised in Table S1.† The support material Ben, after being pre-treated, was placed in contact with a 150 mL solution of the desired aldehyde (15 mL or 13 mL for C7AN or C7EN and for C6AN or C6EN, respectively) in petroleum ether 40/60 (Sigma Aldrich). The solution was gently poured onto the clay and the impregnated solid was thoroughly mixed. It was then left to dry under a fume cupboard for at least 14 h to allow the complete evaporation of all the impregnation solution. The final solid was stored under anhydrous conditions. Five materials were obtained accordingly: Ben (native state), BenC6AN (Ben + n-hexanal), BenC7AN (Ben + n-heptanal), BenC6EN (Ben + (E)-hex-2-enal) and BenC7EN (Ben + (E)-hept-2-enal).
• Zeolite clinoptinolite (Zeo, batch: 014/2018) is a natural mineral zeolite, kindly obtained from Biohelp Your Planet Srl (Tarquinia, Italy), used in its native state (Zeo) as a reference material in open-field trials. Its elemental composition, expressed as % m m−1, is: Na2O (0.1–0.5%), MgO (0.9–1.2%), Al2O3 (10–12%), SiO2 (62–65%), P2O5 (0.02–0.05%), K2O (2.5–3.8%), CaO (2.4–3.7%), Cr2O3 (0–0.01%), MnO (0–0.08%) and Fe2O3 (0.7–1.9%).
Absorbance FT-IR spectra were recorded using a FT-IR FTS-60 (Bio-Rad) spectrophotometer with a liquid nitrogen-cooled MCT (mercury telluride and cadmium) detector. Variable-temperature experiments were carried out on a Bruker Equinox 55 spectrometer in the range 4000–400 cm−1 with a resolution of 4 cm−1 using a dedicated apparatus and all thermal treatments (from 30 to 500 °C) were performed in situ. Infrared spectra of pure liquid aldehydes were collected at room temperature by using a cell for liquid samples.
Thermogravimetric analysis was carried out with a TGA 7HT (PerkinElmer) instrument connected to a TAC 7/DX PerkinElmer controller. The temperature program covered the range from 50 °C to 950 °C (with an increase of 3 °C min−1), using extra-pure air as the analysis gas and nitrogen as the purge gas.
X-ray powder (XRPD) diffractograms were collected on unoriented ground powders with a ThermoARL X'TRA-048 powder diffractometer (Thermo Fisher Scientific, Waltham, MA, USA) with Cu-Kα1 (λ = 1.54062 Å) monochromatic radiation. Diffractograms were recorded at room temperature (RT) in the 5°–80° 2θ range with a step size of 0.02° and a rate of 1.0° min−1. The X-ray profiles at low angles (2–8° and 3–10° 2θ) were collected with narrower slits and at a rate of 0.25° min−1.
Solid-state NMR (ssNMR) spectra were acquired on a Bruker Avance III 500 spectrometer equipped with a wide bore 11.74 T magnet and a 4 mm triple resonance probe. Powdered samples were packed on a zirconia rotor and spun at a magic angle spinning (MAS) rate of 10–15 kHz at 298 K. 1D experiments such as 1H MAS and ECHO MAS NMR were conducted using a radio-frequency field of 100 kHz. The relaxation delay d1 between accumulations was 5 s. A rotor-synchronized spin-echo sequence was applied to record the 1H ECHO MAS NMR spectra with a delay time τ of 2010 ms. All chemical shifts were reported on the δ scale and externally referenced to tetramethylsilane at 0 ppm.
Scanning electron microscopy (SEM) images were collected on a Philips/FEI Quanta 200 Environmental SEM (ESEM) using a tungsten filament as an electron source (200 keV) and a back-scattering detector operating at low vacuum. A conductive coating of gold (sputtering thickness of 10 nm) by low-pressure plasma was deposited on samples, previously placed on carbon grids, to avoid the presence of electronically charged insulating particles under the electron beam.
The structural features of bentonite before and after impregnation with the aldehydes were investigated by X-ray powder diffraction (XRPD). The pristine Ben sample shows the typical crystallographic reflexes of the montmorillonite phase,39 which represents the main component in the X-ray pattern (Fig. 3A). No other relevant crystalline components were revealed by XRPD analysis. When the pristine Ben sample was directly impregnated with the aldehydes, the intense and very well resolved (001) signal slightly shifted towards lower d-spacing values (Fig. 3B, b–d and Table 1), with a small broadening and reduction in intensity of the reflection in general.
Sample | d (001) spacing [nm] |
---|---|
Ben | 1.499 |
BenC6AN | 1.475 |
BenC6EN | 1.461 |
BenC7AN | 1.452 |
BenC7EN | 1.448 |
This behaviour suggests that the impregnation of both saturated and unsaturated aliphatic aldehydes during the preparation steps does not lead to any evident expansion of the d-spacing between the TOT layers of the clay. Rather, since Ben can absorb up to 4.5 wt% of physisorbed water under open-air conditions (as from TGA analysis, see Fig. S4a†), the small, but non-negligible, decrease of d(001) spacing observed in the hybrid materials (Table 1) can be associated with the removal of water molecules during the thermal pretreatment before the impregnation step.
By elemental C,H,N analysis, the changes in carbon content and thus the organic fraction deposited onto the solids were determined.
The pristine bentonite clay, Ben, contains a minimal amount of carbon (0.17%), likely due to inorganic carbonate species, since the material is of mineral origin (Table 2). Upon aldehyde adsorption, there is a significant increase in carbon content, which is clear evidence that the deposition of organic species was successful. The contribution to the carbon content by potential residues of petroleum ether solvent (used for aldehyde deposition) is negligible (as shown in the fourth entry of Table 2 (C: 0.09%), where the pristine bentonite was treated with petroleum ether alone in the absence of aldehydes). In this case, values of hydrogen content are not meaningful because the solid could not be dried in an oven due to the volatility of the aldehyde. Therefore, the presence of absorbed water from atmospheric moisture cannot be excluded or properly monitored.
Ben | BenC6AN | BenC7AN |
---|---|---|
C: 0.17% | C: 2.99% | C: 3.66% |
H: 1.21% | H: 1.35% | H: 1.48% |
N: 0.19% | N: 0.04% | N: 0.01% |
Ben (treated with solvent) | BenC6EN | BenC7EN |
---|---|---|
C: 0.09% | C: 2.86% | C: 3.82% |
H: 1.31% | H: 1.34% | H: 1.43% |
N: 0.03% | N: 0.00% | N: 0.00% |
The mass percentage of the deposited aldehyde in the materials was calculated taking into account the initial carbon present in the pristine bentonite. The calculation was iterated until convergence, adjusting the initial mass of the bentonite support by subtracting the calculated mass of the adsorbed aldehyde. Aldehyde contents were the following:
n-hexanal in BenC6AN = 3.93 wt%; n-heptanal in BenC7AN = 4.75 wt%; (E)-hex-2-enal in BenC6EN = 3.75 wt%; (E)-hept-2-enal in BenC7EN = 4.67 wt%
The solids subjected to the weathering tests underwent elemental C,H,N analysis to determine the residual content of aldehyde species. Bentonite clays containing saturated aldehydes exhibit good resistance to leaching compared to the ones containing unsaturated aldehydes (Table 3) and 75% to 60% of hexanal and heptanal were still found in the solid at the end of the test. Conversely, in the clays containing unsaturated aldehydes, a significant decrease in carbon content was observed, with only 30% to 6% of the original hexenal or heptenal left on the solid. Since no detectable presence of aldehydes was revealed by GC-FID analysis in the aqueous phase, the bioactive species was likely displaced from the solid directly into vapour form without dissolving in the washout medium, with the solubility of these aldehydes in water being indeed scarce (vs. Table S1†).
BenC6AN | BenC6AN (W) | BenC6AN (WH+) |
---|---|---|
C: 2.64% | C: 1.99% | C: 1.54% |
H: 1.49% | H: 1.43% | H: 1.38% |
N: 0.04% | N: 0.03% | N: 0.01% |
BenC7AN | BenC7AN (W) | BenC7AN (WH+) |
---|---|---|
C: 3.66% | C: 2.38% | C: 2.43% |
H: 1.48% | H: 1.45% | H: 1.33% |
N: 0.00% | N: 0.07% | N: 0.08% |
BenC6EN | BenC6EN (W) | BenC6EN (WH+) |
---|---|---|
C: 2.86% | C: 0.19% | C: 0.30% |
H: 1.34% | H: 1.43% | H: 1.18% |
N: 0.00% | N: 0.00% | N: 0.04% |
BenC7EN | BenC7EN (W) | BenC7EN (WH+) |
---|---|---|
C: 3.82% | C: 1.16% | C: 1.03% |
H: 1.43% | H: 1.27% | H: 1.22% |
N: 0.00% | N: 0.00% | N: 0.00% |
Weathering tests using simulated rainwater have underscored the fair robustness of the hybrid organic/inorganic layered solids, especially the ones containing saturated aldehydes, against weathering under harsh conditions, simulated by a full immersion in aqueous medium for 30 min.
From the carbon content profile over time, in terms of controlled smooth release of the bioactive ingredient, the most promising type of material is the one containing saturated aldehydes, i.e. BenC6AN and BenC7AN (Fig. 4). Conversely, in line with the observations after weathering tests (see above), with unsaturated aldehydes, especially in BenC6EN, the carbon content of the organic ingredient fell below the reliable quantification limit for the instrument after ca. 4 weeks. For this reason, the C,H,N elemental analysis measurements was terminated on the 39th day for BenC6EN and BenC7EN. Such further observation suggests that a different mode of interaction between the aldehyde and the bentonite support takes place, moving from saturated aldehydes to unsaturated ones.
In Fig. S3,† the total weight of the solid for BenC6AN is constantly monitored and reported with the relative humidity of the day of the measurement (thus mimicking a real open-field exposure to summer weather). It is evident that the total weight of the clay material is mainly governed by the amount of humidity taken or released, on a daily basis, under ambient conditions. The gradual loss of the bioactive aldehyde, conversely, is negligible under these conditions with respect to the oscillations of the overall weight.
From these observations, it can be concluded that the layered solids containing saturated aldehydes were more gently released over time compared to the ones containing unsaturated aldehydes. The saturated aldehyde-containing bentonite systems are therefore promising candidates to ensure a constant and long-lasting release of the bioactive ingredient into the surrounding atmosphere up to 60 days after deposition. Such behaviour is a critical feature when envisaging the use of these layered solids in open-field trials.
Fig. 5 1H MAS (A) and ECHO (B) NMR spectra of BenC6AN (a), BenC7AN (b), BenC6EN (c), BenC7EN (d) and Ben (e) samples. |
Fig. 6 TGA (blue curve) and DTG (red curve) profiles of the pristine Ben material. Analysis conditions: 50–750 °C range; 3 °C min−1; extra-pure air. |
An analogous behaviour is recorded for the aldehyde-containing materials (BenC6AN; Fig. 7A and BenC7AN; Fig. 7B). Compared to pristine bentonite, however, the weight loss between 120 °C and 520 °C ca. is due to the evaporation/degradation of the aldehyde. Actually, aldehyde-bentonite composites contain a lower amount of water, as they are carefully dried at 110 °C prior to the impregnation of aldehydes. Because of the deposited organic species, their surface becomes more hydrophobic than the pristine Ben solid. A remarkably low amount of physisorbed water is therefore observed in the initial part of the TGA profile between 50 °C and 130 °C in Fig. 7. The different degradation temperatures of the aldehyde are attributed to its different locations within the material. The weight loss at lower temperatures is likely due to the fraction of aldehyde loosely adsorbed mainly on the external surface of the bentonite. The second weight loss at higher temperatures (250–350 °C) is caused by the degradation of the intercalated aldehyde fraction, which is delayed under harsher conditions, thanks to the protective and thermal stability effect of the clay structure on the organic additive.38,46 Eventually, structural collapse above 600 °C is always present (Fig. 7A and B). When computing the mass losses, the materials containing aldehydes exhibit a larger mass loss than the pristine Ben clay (Fig. S4†), expressed as:
ΔmBen = 4.57 wt%; ΔmBenC6AN = 8.31 wt%; ΔmBenC7AN = 9.00 wt% |
ΔBenC6AN = 3.74 wt%; ΔmBenC7AN = 4.43 wt%. |
Fig. 7 TGA (solid blue curve) and DTG (dashed red curve) profiles of BenC6AN (A) and BenC7AN (B) materials. Analysis conditions: 50–750 °C range; 3 °C min−1; extra-pure air. |
A band located at 1690 cm−1 or 1680 cm−1 for BenC6AN and BenC7AN, respectively, is visible in Fig. 8 and 9 and is attributed to the presence of the aldehydic carbonyl group. Interestingly, this band is shifted by 40 cm−1 and 50 cm−1 compared to the carbonyl stretching band of the free aldehydes in the liquid state (Fig. S5A†). This shift is therefore indicative of the weakening of the double bond, resulting in lower wavenumbers of νCO absorption. Such observation suggests that the interaction between the aldehydes and the support is not a simple physisorption impregnation but, rather, a chemisorption interaction involving strong bonds between the δ− oxygen of the aldehyde carbonyl group and the δ+ Lewis acid sites on the clay, between the lamellae, at their edge and/or on their external surface (Fig. 10). In all these parts of the layered material, a relevant number of δ+ interaction sites are indeed present and it is increased by the presence of a good fraction of transition metal heteroatoms (e.g. Ti, Mn, Fe; see the Experimental details section) dispersed throughout the natural clay.
Fig. 10 A schematic depiction of the possible interaction between the clay and the bioactive aldehydes. |
By recording FT-IR spectra at variable temperatures (from 30 to 500 °C), a gradual elimination of adsorbed water from the clays was observed, with a clear diminution of the bands at 3500–3200 cm−1 and 1640 cm−1 (Fig. S6 and S7†). Accordingly, the bands attributed to the presence of the aldehyde decreased with increasing temperature. Nevertheless, a non-negligible presence of low-intensity bands due to the organic species (in the range 3000–2800 cm−1) was detected even up to 500 °C. This is a further clue to the remarkable role of the montmorillonite structure in stabilizing a noteworthy fraction of the aldehyde within its interlayer spaces.46,50
This set of data confirms that organic aldehyde compounds are present on the bentonite-based materials (as shown by ssNMR too) and are bound to the clay support via dispersion and specific dipole–dipole interactions.38 These specific interactions account for the robustness against weathering and leaching in aqueous solutions and the long-lasting smooth release of the bioactive ingredient into the surrounding atmosphere over time.
During the 2019 campaign, there was a medium-high level of infestation in the olive groves. All treated trees showed a lower infestation percentage than the control ones in all observations (T1, T2 and T3) (Fig. 12). Zeo achieved a very good performance in terms of infestation abatement, much more than in the trials of the previous year (cf.Fig. 11). In general, the good effectiveness of aldehyde-containing clay materials was confirmed in this year's trial too and, in particular, excellent results were observed with BenC7AN, which, at the end of the campaign (early October), had a total infestation rate of only 1%. The results for the clays containing unsaturated aldehydes are quite uniform and good as well. Conversely, the result shown after the third treatment with BenC6AN is unexpectedly scarce, at least in this specific trial and under the tested pedological and meteo-climatic conditions. The factors governing the olive fly infestation are indeed multifaceted and a unique explanation for their value is not available at the moment.
Footnote |
† Electronic supplementary information (ESI) available. See DOI: https://doi.org/10.1039/d4dt00705k |
This journal is © The Royal Society of Chemistry 2024 |