Zinc oxide (ZnO) nanoparticles may provide a more soluble and plant available source of Zn in Zn fertilizers due to their greater reactivity compared to equivalent micron- or millimetre-sized (bulk) particles. However, the effect of soil on solubility, spatial distribution and speciation of ZnO nanoparticles has not yet been investigated. In this study, we examined the diffusion and solid phase speciation of Zn in an alkaline calcareous soil following application of nanoparticulate and bulk ZnO coated fertilizer products (monoammonium phosphate (MAP) and urea) using laboratory-based x-ray techniques and synchrotron-based μ-x-ray fluorescence (μ–XRF) mapping and absorption fine structure spectroscopy (μ–XAFS). Mapping of the soil-fertilizer reaction zones revealed that most of the applied Zn for all treatments remained on the coated fertilizer granule or close to the point of application after five weeks of incubation in soil. Zinc precipitated mainly as scholzite (CaZn2(PO4)2.2H2O) and zinc ammonium phosphate (Zn(NH4)PO4) species at the surface of MAP granules. These reactions reduced dissolution and diffusion of Zn from the MAP granules. Although Zn remained as zincite (ZnO) at the surface of urea granules, limited diffusion of Zn from ZnO-coated urea granules was also observed for both bulk and nanoparticulate ZnO treatments. This might be due to either the high pH of urea granules, which reduced solubility of Zn, or aggregation (due to high ionic strength) of released ZnO nanoparticles around the granule/point of application. The relative proportion of Zn(OH)2 and ZnCO3 species increased for all Zn treatments with increasing distance from coated MAP and urea granules in the calcareous soil. When coated on macronutrient fertilizers, Zn from ZnO nanoparticles (without surface modifiers) was not more mobile or diffusible compared to bulk forms of ZnO. The results also suggest that risk associated with the presence of ZnO NPs in calcareous soils would be the same as bulk sources of ZnO.
Citation: Milani N, Hettiarachchi GM, Kirby JK, Beak DG, Stacey SP, McLaughlin MJ (2015) Fate of Zinc Oxide Nanoparticles Coated onto Macronutrient Fertilizers in an Alkaline Calcareous Soil. PLoS ONE 10(5): e0126275. https://doi.org/10.1371/journal.pone.0126275
Academic Editor: Yogendra Kumar Mishra, Institute for Materials Science, GERMANY
Received: November 7, 2014; Accepted: March 31, 2015; Published: May 12, 2015
This is an open access article, free of all copyright, and may be freely reproduced, distributed, transmitted, modified, built upon, or otherwise used by anyone for any lawful purpose. The work is made available under the Creative Commons CC0 public domain dedication
Data Availability: All relevant data are available in the manuscript and its Supporting Information files.
Funding: Use of the Advanced Photon Source was supported by the U.S. Department of Energy, Office of Science, Office of Basic Energy Sciences, under Contract No. DE-AC02-06CH11357 (http://science.energy.gov/). The funders had no role in study design, data collection and analysis, decision to publish, or preparation of the manuscript.
Competing interests: The authors have declared that no competing interests exist.
Zinc (Zn) deficiency is one of the most common micronutrient problems that adversely affects agricultural production, particularly in alkaline calcareous soils . Calcareous soils constitute a major resource for agricultural use, mainly localized in arid or Mediterranean environments of the world . The most important soil parameters that limit Zn availability to plants in calcareous soils are the alkaline pH, which reduces Zn solubility, and the high calcium carbonate (CaCO3) content, which can adsorb and precipitate Zn [3, 4]. Inorganic sources of Zn such as zinc oxides (ZnO) and zinc sulphates (ZnSO4 H2O or ZnSO4 7H2O) are commonly being used as Zn fertilizers to correct Zn deficiency in soils . The effectiveness of applied Zn fertilizers is strongly correlated with the solubility of the Zn source [6, 7], which is heavily influenced by the properties of the soil to which it is applied.
Solubility and dissolution kinetics of particles depend on their surface area. Therefore, the rate and extent of dissolution is greater for nanoparticles compared to bulk materials  due to their smaller particle sizes, higher specific surface area and an increased proportion of reactive surface atoms [9, 10]. It follows then, that the use of zinc oxide nanoparticles (ZnO NPs) in Zn fertilizers may increase Zn dissolution and consequently its bioavailability in problematic soils, such as calcareous soils. Diffusion of dissolved Zn is the main mechanism for the movement of Zn from fertilizer to the plant roots following the dissolution process . A small increase in the diffusion radius of Zn in soil following the application of ZnO NPs may also considerably increase the volume of the Zn-enriched soil and the subsequent availability of Zn fertilizer to plants. Therefore, use of nanoparticulate sources of Zn in Zn fertilizers may increase Zn use efficiency and reduce the quantity and frequency of Zn fertilizer application.
Despite the benefits speculated for the application of ZnO NPs as a source of Zn in soil, nanoparticles are unlikely to remain in their original form following incubation in soils . Soil components will inevitably interact with released ZnO nanoparticles in the soil and affect the spatial distribution and speciation of added Zn. Although application of ZnO NPs as a source of Zn aims to optimize efficiency of applied Zn fertilizer, it is the fate and behaviour of ZnO NPs in soils that will ultimately determine its effectiveness and/or environmental risk (e.g. increased mobility and toxicity of ZnO NPs). The chemical and physical behaviour of soluble and bulk sources of Zn in soils have been widely investigated [13–18]. There is limited understanding of the fate and transformations of ZnO NPs in natural soils, especially calcareous soils. Scheckel et al. (2010)  examined the reactions of nanoparticulate ZnO with suspensions of kaolin and found that nanoparticles transformed very rapidly (~1 day) to soluble and sorbed Zn. However, no comparison was made with bulk-sized ZnO particles. A previous study showed that the kinetic of Zn dissolution from ZnO coated fertilizers in a porous media was not affected by the size of ZnO particles used for coating . However, in natural soil environments soil properties such as presence of organic materials in soil, the ionic strength of soil solution, soil pH and minerals type and content can affect mobility and bioavailability of ZnO nanoparticles . The information on the reactions and solid phase speciation of Zn following the addition of ZnO NPs to soils is of vital importance for a realistic assessment of potential effectiveness and/or adverse effects of using ZnO nanoparticle-coated fertilizers in Zn deficient soils.
Although the complexity of soil systems and heterogeneity at the micro-scale were previously obstacles in solid phase speciation of soils, synchrotron based x-ray absorption spectroscopy (XAS) techniques have provided an excellent research tool for in situ investigations at the molecular level of the solid phase speciation of elements such as Zn in soil environments [22–24]. The sensitivity of μ-focused XAS techniques in the complex local micro-structural environment of the element of interest and low detection limits give them an advantage over other physical techniques . Synchrotron x-ray florescence (XRF) analysis also allows quantitative distribution mapping of several elements simultaneously and with high resolution, in complex environmental systems .
The aim of this study was to examine the diffusion and solid phase speciation of Zn in an alkaline calcareous soil following application of nanoparticulate and bulk ZnO coated fertilizer products (monoammonium phosphate (MAP) and urea). A fertilizer diffusion cell method and synchrotron-based μ-x-ray fluorescence (μ–XRF) mapping and absorption fine structure spectroscopy (μ–XAFS) were used to examine the diffusion and speciation of Zn treatments in the selected calcareous soil. The information will be used to assess the efficacy and environmental risk of ZnO NP coated fertilisers in calcareous soils.
Materials and Methods
Characterisation of ZnO particles and preparation of coated fertilizers
Commercial ZnO nanoparticle powder was purchased from Nanostructure & Amorphous Material Inc. (Houston, USA) with a nominal particle size of 20 nm. Bulk ZnO powder (99.9%, nominal diameter < 1 μm) was purchased from Sigma-Aldrich (Sydney, Australia). Surface capping agents or modifiers were not present on ZnO particles. The methods used to characterize primary nanoparticulate and bulk ZnO particles and their findings can be found in Milani et al. (2012) . The ZnO powders were examined using transmission electron microscopy (TEM; Phillips CM200, Edindhoven, The Netherlands) (Fig 1) and x–ray diffraction (XRD) (PANalytical X’Pert Pro, Almelo, The Netherlands) techniques. The XRD patterns were used to confirm the presence of ZnO in samples and to estimate crystallite size of particles. The Brunauer-Emmett-Teller (BET) surface area equation  after liquid N2 adsorption (Quanta Chrome, USA) was used to determine specific surface area of particles. The crystallite structure determined using XRD patterns showed that the ZnO NPs were exclusively composed of zincite (zinc oxide), while the XRD pattern of bulk ZnO revealed a dominant presence of zincite crystals along with minor amounts of hydrozincite. The crystallite size estimates of ZnO NPs based on the Sherrer equation using full width at half maximum of the XRD pattern and BET-N2 analysis suggested that the size of ZnO NPs are consistent with the nominal size provided by the manufacturer (20 nm). BET-N2 analysis on ZnO powders resulted in surface areas equal to 31 m2g-1 and 12 m2g-1 for ZnO NPs and bulk ZnO, respectively.
The monoammonium phosphate (MAP- Mosaic Co., Plymouth, USA) and commercial urea fertilizer granules were coated with ZnO powders using the method described in Milani et al. (2012) . The four coated fertilizer treatments were MAP granules coated with nanoparticulate ZnO (NanoMAP), MAP granules coated with bulk ZnO (BulkMAP), urea granules coated with ZnO NPs (NanoUrea) and urea granules coated with bulk ZnO (BulkUrea).
The distribution of ZnO powders on the surface of the coated fertilizer granules was investigated using scanning electron microscopy (SEM; Philips XL30 field emission SEM, Eindhoven, The Netherlands). Fertilizer granules with/without ZnO coating were cross sectioned, coated with carbon and gold to reduce static electric charge accumulation and finally mounted onto aluminium specimen holders for SEM analysis. Elemental compositions of selected points of interest at the surface of fertilizer granules as well as the points in the core of the granules (after fracture) were examined using integrated energy dispersive X-ray analysis (EDXA; Genesis EDX Spectrometer system, NJ, USA). Mineralogy of the coated fertilizer granules was investigated using XRD analysis. The methods used and their findings can be found in Milani et al. (2012) . In summary, SEM images illustrated a nearly homogeneous distribution of the coating at the surface of the fertilizer granules (Fig 2 and Fig 3). The EDXA spectra of MAP granules coated with ZnO powders showed that the coatings of granules mainly consisted of phosphorus (P), Zn and oxygen (O) followed by nitrogen (N), whereas the elemental composition of inner granule were predominantly P, O and N (S1, S2 and S3 Figs). The elemental composition at the surface of commercial urea fertilizers and the core of urea granules coated with ZnO mainly consisted of N and O (S4 and S5 Figs). The surface of urea granules coated with ZnO predominantly contained Zn followed by O (S5 and S6 Figs). Mineralogical characterization using XRD patterns showed dominant and intense peaks of zinc ammonium phosphate (Zn(NH4)PO4) for coated MAP fertilizers and a small amount of zincite. In contrast, XRD patterns of coated urea granules revealed the Zn as the mineral zincite at the surface of the fertilizer granule. The XRD patterns showed that ZnO NPs at the surface of urea granules had a similar crystallite size (20–30 nm) to the added primary ZnO NPs.
Synchrotron based μ-XRF mapping and μ-XAFS data collection and analysis
Zinc distribution from ZnO-coated fertilizers in an alkaline calcareous soil was investigated following their incubation in soil using μ-XRF mapping. Solid phase speciation of selected points on, or adjacent to, the incubated fertilizer granules in the soil was also studied using μ-XAFS. The fertilizer diffusion protocol developed by Hettiarachchi et al. (2008)  was adopted for use in this study. A highly calcareous sandy loam soil [Sodic Calcixerept ] was collected from upper Eyre Peninsula, South Australia to be used in the experiment. Selected physical and chemical properties of the soil are presented in Table 1.
Four experimental cells (5 cm long x 5 cm wide x 0.5 cm deep Plexiglass holders with 25 mm diameter circular Kapton windows at the top) were uniformly packed with 17 g of slightly wetted soil and further wetted to 60% of its maximum water holding capacity  by adding ultra-pure deionised water. The cells were equilibrated for 24 hr and then one coated MAP granule or 5 coated urea granules were placed into the centre of each experimental cell close to the Kapton window (centre top). Experimental cells were then incubated in a temperature controlled environment at 25°C for five weeks under aerobic condition. The individual cells were weighed and sufficient ultrapure deionised water added during the experiment to maintain the soils at 60% of maximum water holding capacity.
The μ-XRF mapping and μ- XAFS data collection were performed at beamline 13-BM-D (GeoSoilEnviro Consortium of Advanced Radiation Sources), at the Advanced Photon Source at Argonne National Laboratory, Argonne, IL. The electron storage ring is operated at 7 GeV and 13-BM is a bending magnet beamline equipped with a Si (111) monochromator with an energy range of 6–28 keV. Experimental cells containing fertilizer-incubated soils were mounted onto the sample stage on the rotation axis of an x-y-θ stepping motor stage with the side containing Kapton x-ray window facing the beam. The incident x-ray beam was focused to a 50 μm spot size to assess elemental distribution in the soil as a function of distance from point of fertilizer granule application. The μ-XRF mapping data was collected at ambient temperature using a solid-state energy-dispersive x-ray detector that allowed simultaneous detection of fluorescence signals from multiple elements. At each position, the fluorescence signal from a given element was proportional to the integrated number of atoms of that element along each transect of synchrotron beam. Florescence data were collected for a 7000 by 4800 μm area for the soil sample treated with NanoMAP granules, a 7000 by 5000 μm area for the soil sample treated NanoUrea and a 5000 by 2950 μm area for soil sample treated with BulkUrea fertilizer granules (The μ-XRF map for the soil treated with BulkMAP fertilizer granule was previously collected by Hettiarachchi et al., 2008). Micro-XRF maps for Ca, Cu, Fe, Mn, Ti and Zn were collected. Micro-XRF maps of Ca and Ti were used to identify the location of fertilizer granules in petri dishes. For each μ-XRF map, 2 or 3 points of interest (determined based on highest relative intensity) were identified for μ–XAFS speciation analysis.
The μ- XAFS spectra of selected points were collected from 150 eV below to 640 eV above the K-edge of Zn (9659 eV) in fluorescence mode using a 13-element Ge solid-state detector. Three replicate scans from selected points on each fertilizer treatments as well as unexposed fertilizer granules were collected. In addition, μ- XAFS of ZnO powders and standard Zn compounds were collected in the same mode (fluorescence) and scan conditions, after diluting standard compounds using boron nitride (BN) to bring concentration of Zn in each Zn standard to approximately 0.5%. Zn standard compounds included ZnSO4.7H2O, Zn(OH)2, Zn(NH4)PO4.6H2O, smithonite (ZnCO3), zincite (ZnO), hydrozincite (Zn5(CO3)2(OH)6), scholzite (CaZn2(PO4)2.2H2O), franklinite (Zn0.6Mn0.3(II)Fe0.1(II)Fe1.5(III)Mn0.5(III)O4), hopeite (Zn3(PO4)2.4H2O), willemite [Zn2(SiO4)], ferrihydrite (Fe5HO8.4H2O)-adsorbed Zn and calcite-adsorbed Zn.
The collected μ-XAFS spectra were analysed using the Athena software package . Replicate scans of each sample were aligned using a reference spectrum (Zn foil, 7659 eV) and then averaged into a final spectrum for each sample. Averaged spectra were background-corrected and normalized. Linear combination fitting (LCF) operations were also performed using Athena. Since the accuracy of the LCF species identified is limited by the choice of standard compounds and the presence of impure minerals in soil , a combination of techniques (x-ray spectroscopic, microscopic and diffraction) were used to identify the reaction products of unexposed fertilizers and validate the reaction product identification.
Results and Discussions
Zinc diffusion and spatial distribution
Micro-XRF maps showing spatial distribution of Zn on and around coated fertilizer granules incubated in the soil can be found in Fig 4. The μ–XRF map of the NanoMAP granule revealed that most of the fertilizer Zn remained at the surface of the granule after five weeks of incubation. The observed high intensity of elements on one side of the MAP granule (Fig 4A) may be due to the granule being partially covered with soil and the fluorescent signal being lost in the concealed regions. Moreover, an artifact caused by the offset of the x-ray beam angle on the curved granule might have resulted in a higher intensity of elements in one side of the granule. The μ–XRF maps of Zn treatments for the coated urea granules can be found in Fig 4B and Fig 4C. Although complete dissolution of urea granules made it difficult to recognize their accurate position or size in the scanned region, dashed areas illustrate the likely original location of the coated urea granules in the scanned area of experimental cells found via overlapping maps of different elements. As observed for MAP granules, Zn released from the coating of urea granules mainly remained close to the application point of granules.
The colour scheme represents white-yellow for high concentrations and blue-black for low concentrations of the elements. The dashed area represent the probable location of the fertilizer granules in the soil sample and the marked points in Zn Kα map indicate the locations for which μ-XAS spectra were collected.
Limited diffusion of Zn from coated fertilizers may be due to reactions of ZnO NPs at the surface of granule, mass flow of water in soil towards the fertilizer granules or pH effects. Transformation of nanoparticulate ZnO in the coating of MAP granules to zinc phosphate-like species may have hindered expected diffusion of ZnO NPs in the calcareous soil. This process resulted in the same restricted Zn diffusion which was previously reported for commercial Zn-enriched MAP granules (with Zn incorporated throughout the granule) [22, 30]. Although ZnO in the coating of urea granules did not transform to other Zn species, aggregation of released ZnO NPs around the granule due to high pH and ionic strength would be expected in soil solution adjacent to the dissolved urea granule. This process may have reduced dissolution and subsequent diffusion of Zn in the soil.
Mass flow of water from the soil towards the hygroscopic fertilizer granule in the opposite direction to Zn diffusion could be a probable mechanism restricting Zn diffusion the same way as it was earlier reported for restricted diffusion of phosphorus in a highly calcareous soil . Acidity produced by the fertilizer granule may also affect the solubility, speciation and diffusion of Zn in the soil. Suspensions of coated urea fertilizer granules in ultra-pure deionised water (Millipore) had a pH of ca.7.5 whereas pH of coated MAP suspension was ca. 4.8 . Therefore, solubility and reaction products of Zn from the coating of MAP and urea granules in the soil would be affected by the acidity produced by the fertilizer granule. The initial neutral to alkaline pH in the soil around coated urea granules may have reduced solubility of ZnO NPs. In comparison, MAP fertilizer granules reduced the pH of the environment adjacent to the granule . Despite this decrease in soil pH which may promote dissolution of ZnO to Zn2+, the large pH buffering capacity of the alkaline calcareous soil may limit the solubility and diffusion of Zn around the MAP granules. Moreover, phosphate dissolved from the MAP granule could rapidly reduce the release of Zn2+ as a result of precipitation of Zn phosphate-like species adjacent to the MAP granule .
Solid phase speciation of Zn
The Zn K-edge XAFS spectra collected from unexposed fertilizer granules as well as selected points of interest on, or adjacent to, the MAP and urea fertilizer granules incubated in the calcareous soil were analysed using Linear Combination Fitting (LCF) method. The Zn K-edge XAFS spectra and fitted lines can be found in Fig 5. The resultant Zn speciation for each point based on the LCF method is listed in Table 2.
Similar Zn speciation was found for unexposed NanoMAP and BulkMAP granules which was predominantly scholzite (more than 60%), followed by Zn(NH4)PO4 and Zn(OH)2. Minor amount of zincite was found in unexposed ZnO-coated MAP granules suggested transformations of ZnO as a result of the reactions with phosphate in MAP fertilizer granules during the manufacturing process. The x-ray diffraction patterns identified Zn(NH4)PO4 as the major Zn species at the surface of unexposed MAP fertilizers. According to the μ-XAFS analysis, the major Zn species present were scholzite (CaZn2(PO4)2 2H2O) and Zn(OH)2-like species. Considering that the XRD technique provides information on the structure of crystalline substances , these results suggest that scholzite and Zn(OH)2 identified using μ-XAFS technique were in amorphous or poorly crystalline forms which were not detected by XRD. The Zn species found in unexposed urea granules coated with ZnO NPs was exclusively zincite (ZnO). Unexposed urea granules coated with bulk ZnO contained minor amounts (7%) of hydrozincite (Zn5(CO3)2(OH)6) in addition to zincite species (Table 2) which can be attributed to the minor amounts of hydrozincite in bulk ZnO powder. Zinc oxide particles coated at the surface of urea granules may also transform to hydrozincite species at the atmospheric partial pressure of CO2 (10–3.5) during coating and handling processes .
A comparison of μ-XAFS spectra of the points of interest at the surface of coated MAP granules incubated in soil and unexposed MAP fertilizer granules indicated a reduction in the proportion of scholzite species and increase in the percentage of Zn(NH4)PO4 species with incubation in soil (Table 2). For example, μ-XAFS at point P1 at the surface of a NanoMAP granule incubated in soil (Fig 4A), showed Zn speciation to be 43% Zn(NH4)PO4 and 47% scholzite. On the other hand, the relative proportion of Zn(NH4)PO4 and scholzite were 23% and 62% at the surface of an unexposed NanoMAP granule, respectively (Table 2). The same trend was observed for BulkMAP granules where the relative proportion of Zn(NH4)PO4 increased from 19% at the surface of unexposed BulkMAP granules to 48% at the surface of granules incubated in the soil; and the percentage of scholzite decreased from 63% in unexposed BulkMAP granules to 34% at point P1 at the surface of BulkMAP granules incubated in the soil (Table 2). The solubility constant for scholzite (log Ksp = -9.46) and Zn(NH4)PO4 (log Ksp = -12.4; Degryse et al., unpublished data) at 0.00038 atm pressure for CO2(g) (which is the probable CO2 pressure for calcareous soils) indicate that Zn(NH4)PO4 is more soluble (less stable) than scholzite in the experimental conditions investigated. An enhanced percentage of more soluble Zn species suggests dissolution of Zn at the surface of incubated MAP granules and re-precipitation in the ion saturated region immediately at the surface of the fertilizer. With increasing distance from the coated MAP granules, significant amounts of Zn carbonate species were identified (Table 2). Solid phase speciation at points P2, adjacent to the NanoMAP (Fig 4A) and BulkMAP granules incubated in the soil indicated Zn species to be 46% and 25% smithonite (ZnCO3), respectively (Table 2). Earlier investigations of the reaction products of ZnSO4 plus ammonium phosphate (NH4H2PO4) in calcareous soils has also confirmed formation of Zn(NH4)PO4, Zn3(PO4)2.4H2O and ZnCO3 species using XRD analysis . In a synchrotron-based study, the dominant Zn species around a Zn-incorporated MAP granule in a calcareous soil were identified to be scholzite followed by minor amounts of willemite and zincite .
Zinc speciation at the surface of unexposed NanoUrea and BulkUrea granules consisted of 100% and 93% zincite, respectively (Table 2). However, solid phase speciation of points P1 and P2, at the point of application of the NanoUrea granules (Fig 4B), revealed formation of Zn(OH)2 species due to dissolution of ZnO NPs. The relative percentage of Zn species present as Zn(OH)2 increased to a dominant 89% at P3 (Fig 4B) which was the furthest point collected away from the NanoUrea granules in soil. In contrast, a combination of zincite, Zn(OH)2 and smithonite species were found for selected points in the soil incubated with BulkUrea fertilizer granules (Table 2). Gimbert et al. (2007) reported limited dissolution or partitioning of ZnO NPs in a suspension of an alkaline soil using flow field-flow fractionation. In contrast, our results suggested significant changes in Zn solid phase speciation of ZnO particles at the points on, or adjacent to, the coated urea granules due to dissolution of ZnO particles and re-precipitation of Zn(OH)2 and ZnCO3 species (Table 2). The stability of ZnO NPs in the Gimbert et al. experiment may be due the presence of a dispersant which could have educed/eliminated the dissolution and re-precipitation reactions of ZnO NPs in the soil suspension over the two weeks period of the experiment .
Investigations of the solid phase speciation of Zn added to calcareous soils have shown the importance of adsorption reactions on Fe- and Al-oxides at low added Zn concentrations [15, 39]. At elevated added concentrations of Zn in alkaline soils, adsorption sites can be saturated and chemical precipitation of Zn as Zn(OH)2, ZnCO3 and hydrozincite (Zn5(CO3)2(OH)6) are favoured over adsorption [13, 15]. In this study, significant amounts of Zn(OH)2 and ZnCO3 species were found at points on, or adjacent to, the coated urea fertilizer granules (Table 2). This suggests the formation of a Zn-rich region adjacent to the fertilizer granule due to dissolution of ZnO coated at the surface of the granule. High Zn concentrations in the vicinity of coated fertilizer granules likely favour precipitation reactions over adsorption reactions and therefore adsorbed Zn species were not detected by solid phase speciation of Zn in this soil. Hettiarachchi et al. (2008) also reported the absence, or very insignificant amounts, of adsorbed Zn species around the MAP-Zn granules in a calcareous soil .
The μ-XANES spectra region of selected points for the soil treated with MAP and urea granules are shown in Fig 6. Careful visual observations of the μ-XANES spectra in Fig 6 together with the μ-XRF maps in Fig 4 suggested that μ-XAFS spectra of NanoUrea P1 and P2 might have been affected by self-absorption effects. Although the highest concentration of Zn was assumed to be ca.1000 mg kg-1 for MAP-Zn granules , it is possible that these two spots were more concentrated than 1000 mg kg-1. Therefore, it should be noted that the conclusion that these spots were zincite and/or zinc hydroxide is tentative. Self- absorption effects were not observed for all other points including NanoUrea P3. Visual observation of MAP spectra demonstrated similar Zn speciation for MAP granules treated with bulk ZnO or ZnO NPs. Spectra of urea granules illustrated more obvious changes in the shape and structure in comparison to the spectra collected from MAP treatments, indicating greater reactivity of Zn species at the surface of urea granules.
This study provides better understanding of the diffusion and transformation process of ZnO nanoparticles coated onto macronutrient fertilizers in situ in soil. It also highlights changes in solid phase speciation of Zn from ZnO nanoparticles associated with macronutrient fertilizers in a natural soil environment. Micro–XRF mapping showed that diffusion of Zn from the coated granules was highly restricted, irrespective of whether the bulk or nanoparticulate forms of ZnO was used. The μ-XAFS data suggested that ZnO-coated MAP and urea fertilizer granules produce different reaction products following incubation in the calcareous soil used. Chemical reactions of Zn sources with phosphate species in the MAP granule affected the solid phase speciation of Zn in the soil. Transformation of ZnO to Zn(NH4)PO4 and scholzite species in coated MAP granules hindered expected high solubility of nanoparticulate ZnO. Although ZnO particles remained as zincite at the surface of coated urea granules, high pH and ionic strength in soil solutions from hydrolysis of urea would have promoted aggregation of any ZnO NPs released from the granules and masked the effect of particle size on solubility and mobility of ZnO particles. Therefore, significant greater dissolution of ZnO NPs was not observed for NanoUrea granules compared to BulkUrea granules as was anticipated based on theoretical considerations .These results are in agreement with our previous study on dissolution kinetics of the same fertilizer granules in porous media, which showed size of ZnO particles did not affect solubility and dissolution kinetics of Zn from coated fertilizer granules . Similar dissolution rate and equilibrium solubility for bulk and nanoparticulate ZnO due to aggregation of ZnO NPs was previously reported . Our study suggests that the application of ZnO NPs (without surface modifiers) rather than bulk forms of ZnO as a micronutrient coating for urea or MAP appears to offer little benefit in terms of Zn dissolution and diffusion in calcareous soils. However, from an ecotoxicological point of view the risks associated with the presence of ZnO NPs in soils would be the same as bulk sources of ZnO.
S1 Dataset. Micro-x-ray absorption fine structure (μ-XAFS) data for zinc standards and treatments used in the experiment.
S1 Fig. The SEM-EDXA analysis of the surface of a commercial mono ammonium phosphate (MAP) fertiliser granule.
This figure shows (a) scanning electron microscopy (SEM) image of the surface of commercial mono ammonium phosphate (MAP) fertiliser granule used in the experiment and (b) EDXA spectrum that is collected from the point at the surface of the granule indicated by a cross on the SEM image. Elemental composition of the point of interest is reported in the table.
S2 Fig. The SEM-EDXA analysis of a cross sectioned MAP granule coated with ZnO nanoparticles in backscattered mode.
The figure illustrates (a) coated area (left) and inner granule (right) as well as the spots from which EDXA spectra were collected. EDXA spectra collected from spot 1 (b) and spot 2 (c) and their elemental compositions are also reported.
S3 Fig. The SEM-EDXA analysis of a cross sectioned MAP granule coated with bulk ZnO.
The figure shows (a) scanning electron microscopy image of a cross sectioned MAP granule coated with bulk ZnO particles illustrating inner granule and coated surface of BulkMAP granule. The EDXA spectra collected from (b) spot 1 at the surface of coated granule and (c) spot 2 located in the core of granule as well as elemental composition at these points are shown.
S4 Fig. The SEM-EDXA analysis of the surface of commercial urea granule.
The figure illustrates (a) SEM image of the surface of commercial urea granule which was used in the experiment and (b) EDXA spectra collected from the point specified using a cross on the SEM image and elemental composition of the scanned point of interest.
S5 Fig. The SEM-EDXA analysis of a cross-sectioned urea granule coated with bulk ZnO.
The figure shows (a) the scanning electron microscopy image of a cross sectioned urea granule coated with bulk ZnO particles. The dark grey area at the right side of the image shows inner granule. Distribution of bulk ZnO particles at the surface of the granule can be observed at the left side of the image. The EDXA spectra collected from (b) points of interest at the surface of granule (spot1) and (c) inner granule (spot 2) to identify elemental compositions at these points.
S6 Fig. The SEM-EDXA analysis of a urea granule coated with ZnO nanoparticles.
The figure illustrates (a) SEM image of the surface of a urea granule coated with ZnO nanoparticles. The EDXA collected from (b) spot 1 and (c) spot 2 and the elemental compositions of aforementioned points of interest are reported in tables.
The authors would like to thank Dr Peter Self for assistance with TEM-EDXA and SEM-EDXA imaging and analysis, Mark Raven for XRD analysis, Dr Mathew Newville for XAS data collection, Dr Sola Ajiboye for providing XAS spectra of some Zn standards, Drs Geert Cornelis and Fien Degryse for their advice to improve the manuscript.
‡ The U.S. EPA has not subjected this manuscript to internal policy review. Therefore, the research results presented herein do not necessarily reflect Agency policy. Mention of trade names of commercial products and companies does not constitute endorsement or recommendation for use.
Conceived and designed the experiments: NM GMH MJM JKK SPS. Performed the experiments: NM GMH MJM JKK. Analyzed the data: NM GMH DGB. Contributed reagents/materials/analysis tools: NM GMH DGB MJM JKK SPS. Wrote the paper: NM GMH DGB MJM JKK SPS.
- 1. Takkar PN, Walker CD. The Distribution and Correction of Zinc Deficiency. In: Robson AD, editor. Zinc in Soils and Plants. Development in plant and soil science. 55. Dordrecht; Boston Kluwer Academic Publishers; 1993. pp. 151–166.
- 2. FAO. Land and Plant Nutrient Management. ProSoil-Problem soil database Rome: FAO/AGL; 2000. Available from: http://www.fao.org/ag/agl/agll/nrdb/links.jsp?lang=en.
- 3. Alloway BJ. Soil factors associated with zinc deficiency in crops and humans. Environ Geochem Health. 2009; 31(5):537–48. pmid:19291414
- 4. Rashid A, Ryan J. Micronutrient constraints to crop production in soils with Mediterranean-type characteristics: A review. J Plant Nutr. 2004; 27(6): 959–75.
- 5. Mortvedt JJ. Crop response to level of water-soluble zinc in granular zinc fertilizers. Fert Res. 1992; 33(3): 249–55.
- 6. Amrani M, Westfall DG, Peterson GA. Influence of water solubility of granular zinc fertilizers on plant uptake and growth. J Plant Nutr. 1999; 22(12): 1815–27.
- 7. Mortvedt JJ. Crop response to applied zinc in ammoniated phosphate fertilizers. J Agric Food Chem. 1968; 16(2): 241–5.
- 8. Borm P, Klaessig FC, Landry TD, Moudgil B, Pauluhn J, Thomas K, et al. Research strategies for safety evaluation of nanomaterials, Part V: Role of dissolution in biological fate and effects of nanoscale particles. Toxicol Sci. 2006; 90(1): 23–32. pmid:16396841
- 9. Nel A, Xia T, Madler L, Li N. Toxic potential of materials at the nanolevel. Science. 2006; 311(5761): 622–7. pmid:16456071
- 10. Wigginton NS, Haus KL, H MF Jr. Aquatic environmental nanoparticles. J Environ Monit. 2007; 9(12): 1306–16. pmid:18049768
- 11. Gangloff WJ, Westfall DG, Peterson GA, Mortvedt JJ. Mobility of organic and inorganic zinc fertilizers in soils. Commun Soil Sci Plant Anal. 2006; 37(1–2): 199–209.
- 12. Lv JT, Zhang SZ, Luo L, Han W, Zhang J, Yang K, et al. Dissolution and microstructural transformation of ZnO nanoparticles under the influence of phosphate. Environ Sci Technol. 2012; 46(13): 7215–21. pmid:22651907
- 13. Saeed M, Fox RL. Relations between suspension pH and zinc solubility in acid and calcareous soils Soil Sci. 1977; 124(4): 199–204.
- 14. Ma YB, Uren NC. Effect of aging on the availability of zinc added to a calcareous clay soil. Nutr Cycling Agroecosyst. 2006; 76(1): 11–8.
- 15. Jacquat O, Voegelin A, Villard A, Marcus MA, Kretzschmar R. Formation of Zn-rich phyllosilicate, Zn-layered double hydroxide and hydrozincite in contaminated calcareous soils. Geochim Cosmochim Acta. 2008; 72(20): 5037–54.
- 16. Voegelin A, Pfister S, Scheinost AC, Marcus MA, Kretzschmar R. Changes in zinc speciation in field soil after contamination with zinc oxide. Environ Sci Technol. 2005; 39(17): 6616–23. pmid:16190219
- 17. Voegelin A, Jacquat O, Pfister S, Barmettler K, Scheinost AC, Kretzschmar R. Time-dependent changes of zinc speciation in four soils contaminated with zincite or sphalerite. Environ Sci Technol. 2011; 45(1): 255–61. pmid:21142002
- 18. Degryse F, Voegelin A, Jacquat O, Kretzschmar R, Smolders E. Characterization of zinc in contaminated soils: complementary insights from isotopic exchange, batch extractions and XAFS spectroscopy. Eur J Soil Sci. 2011; 62(2): 318–30.
- 19. Scheckel KG, Luxton TP, El Badawy AM, Impellitteri CA, Tolaymat TM. Synchrotron speciation of silver and zinc oxide nanoparticles aged in a kaolin suspension. Environ Sci Technol. 2010; 44(4): 1307–12. pmid:20078035
- 20. Milani N, McLaughlin MJ, Stacey SP, Kirby JK, Hettiarachchi GM, Beak DG, et al. Dissolution kinetics of macronutrient fertilizers coated with manufactured zinc oxide nanoparticles. J Agric Food Chem. 2012; 60(16): 3991–8. pmid:22480134
- 21. Cornelis G, Hund-Rinke K, Kuhlbusch T, Van den Brink N, Nickel C. Fate and Bioavailability of Engineered Nanoparticles in Soils: A Review. Crit Rev Environ Sci Technol. 2014; 44(24): 2720–64.
- 22. Hettiarachchi GM, McLaughlin MJ, Scheckel KG, Chittleborough DJ, Newville M, Sutton S, et al. Evidence for different reaction pathways for liquid and granular micronutrients in a calcareous soil. Soil Sci Soc Am J. 2008; 72(1): 98–110.
- 23. Lombi E, Susini J. Synchrotron-based techniques for plant and soil science: opportunities, challenges and future perspectives. Plant Soil. 2009; 320(1–2): 1–35.
- 24. McNear DH, Tappero R, Sparks DL. Shining light on metals in the environment. Elements. 2005; 1(4): 211–6.
- 25. Wang B, Wang Z, Feng WY, Wang M, Hu ZB, Chai ZF, et al. New methods for nanotoxicology: synchrotron radiation-based techniques. Anal Bioanal Chem. 2010; 398(2): 667–76. pmid:20526771
- 26. Brunauer S, Emmett PH, Teller E. Adsorption of gases in multimolecular layers. J Am Chem Soc. 1938; 60(2): 309–19.
- 27. Soil Survey Staff. Keys to Soil Taxonomy. 11th ed. Washington, DC.: USDA-Natural Resources Conservation Service; 2010.
- 28. Brookes PC. Principles and Methodologies of Measuring Microbial Activity and Biomass in Soil. In: Tibbett M, Carter DO, editors. Soil Analysis in Forensic Taphonomy: Chemical and Biological Effects of Buried Human Bodies. Boca Raton, FL: CRC Press; 2008.
- 29. Ravel B, Newville M. ATHENA, ARTEMIS, HEPHAESTUS: data analysis for X-ray absorption spectroscopy using IFEFFIT. J Synchrotron Radiat. 2005; 12: 537–41. pmid:15968136
- 30. Hettiarachchi G, Lombi E, McLaughlin M, Chittleborough D, Johnston C. Chemical behavior of fluid and granular Mn and Zn fertilisers in alkaline soils. Aust J Soil Res. 2010; 48(3): 238–47.
- 31. Hettiarachchi GM, Lombi E, McLaughlin MJ, Chittleborough D, Self P. Density changes around phosphorus granules and fluid bands in a calcareous soil. Soil Sci Soc Am J. 2006; 70(3): 960–6.
- 32. Lombi E, McLaughlin MJ, Johnston C, Armstrong RD, Holloway RE. Mobility and lability of phosphorus from granular and fluid mnoammonium phosphate differs in a calcareous soil. Soil Sci Soc Am J. 2004; 68(2): 682–9.
- 33. Bertrand I, McLaughlin M, Holloway R, Armstrong R, McBeath T. Changes in P bioavailability induced by the application of liquid and powder sources of P, N and Zn fertilizers in alkaline soils. Nutr Cycling Agroecosyst. 2006; 74(1): 27–40.
- 34. Harris W, White GN. X-ray diffraction techniques for soil mineral identification. In: Ulery AL, Drees LR, editors. Methods of Soil Analysis Part 5 Mineralogical Methods. 5. Madison, WI: Soil Science Society of America; 2008. pp. 81–116.
- 35. Vagvolgyi V, Hales M, Martens W, Kristof J, Horvath E, Frosts RL. Dynamic and controlled rate thermal analysis of hydrozincite and smithsonite. J Therm Anal Calorim. 2008; 92(3): 911–6.
- 36. Nriagu JO. Formation and stability of base metal phosphate in soils and sediments. In: Nriagu JO, Moore PB, editors. Phosphate Minerals. Berlin: Springer-Verlag; 1984. pp. 318–29.
- 37. Kalbasi M, Racz GJ, Lewenrudgers LA. Reaction-products and solubility of applied zinc compounds in some Manitoba soils. Soil Sci. 1978; 125(1): 55–64.
- 38. Gimbert LJ, Hamon RE, Casey PS, Worsfold PJ. Partitioning and stability of engineered ZnO nanoparticles in soil suspensions using flow field-flow fractionation. Environ Chem. 2007; 4(1): 8–10.
- 39. Brummer G, Tiller KG, Herms U, Clayton PM. Adsorption-desorption and/or percipitation-dissolution processes of zinc in soils Geoderma. 1983; 31(4): 337–54.
- 40. Franklin NM, Rogers NJ, Apte SC, Batley GE, Gadd GE, Casey PS. Comparative toxicity of nanoparticulate ZnO, bulk ZnO, and ZnCl2 to a freshwater microalga (Pseudokirchneriella subcapitata): The importance of particle solubility. Environ Sci Technol. 2007; 41(24): 8484–90. pmid:18200883