Marco
Sanna Angotzi
ab,
Valentina
Mameli
ab,
Claudio
Cara
ab,
Davide
Peddis
bcd,
Huolin L.
Xin
e,
Claudio
Sangregorio
bfg,
Maria Laura
Mercuri
a and
Carla
Cannas
*ab
aDepartment of Chemical and Geological Sciences, University of Cagliari, S.S. 554 bivio per Sestu, 09042 Monserrato (CA), Italy. E-mail: ccannas@unica.it
bConsorzio Interuniversitario Nazionale per la Scienza e Tecnologia dei Materiali (INSTM), Via Giuseppe Giusti 9, 50121 Firenze (FI), Italy
cDipartimento di Chimica e Chimica Industriale, Università di Genova, Via Dodecaneso, 31, 16131 Genova, Italy
dIstituto di Struttura della Materia, Consiglio Nazionale delle Ricerche, Via Salaria Km 29.300, 00015 Monterotondo Scalo (RM), Italy
eDepartment of Physics and Astronomy, University of California, Irvine, CA 92617, USA
fIstituto di Chimica dei Composti OrganoMetallici-Consiglio Nazionale delle Ricerche (ICCOM-CNR), Via Madonna del Piano 10, 50019 Sesto Fiorentino (FI), Italy
gDepartment of Chemistry “U. Schiff”, University of Florence, Via della Lastruccia 3-13, 50019, Sesto Fiorentino (FI), Italy
First published on 21st January 2021
Multifunctional nano-heterostructures (NHSs) with controlled morphology are cardinal in many applications, but the understanding of the nanoscale colloidal chemistry is yet to be fulfilled. The stability of the involved crystalline phases in different solvents at mid- and high-temperatures and reaction kinetics considerably affect the nucleation and growth of the materials and their final architecture. The formation mechanism of manganese ferrite-based core–shell NHSs is herein investigated. The effects of the core size (8, 10, and 11 nm), the shell nature (cobalt ferrite and spinel iron oxide) and the polarity of the solvent (toluene and octanol) on the dissolution phenomena of manganese ferrite are also studied. Noteworthily, the combined use of bulk (powder X-ray diffraction, 57Fe Mössbauer spectroscopy, and DC magnetometry) and nanoscale techniques (HRTEM and STEM-EDX) provides new insights into the manganese ferrite dissolution phenomena, the colloidal stability in an organic environment, and the critical size below which dissolution is complete. Moreover, the dissolved manganese and iron ions react further, leading to an inverted core–shell in the mother liquor solution, paving the way to novel synthetic pathways in nanocrystal design. The MnFe2O4@CoFe2O4 core–shell heterostructures were also employed as heat mediators, exploiting the magnetic coupling between a hard (CoFe2O4) and a soft phase (MnFe2O4).
In a previous paper,10 spinel ferrite-based core–shell NHSs were efficiently synthesized by an oleate-based solvothermal approach, starting from either cobalt ferrite of different sizes or manganese ferrite as seeds. In the case of manganese ferrite seeds, a slight dissolution was observed, suggesting a peculiar heterostructure formation mechanism. A systematic study on manganese ferrite stability when it is adopted as a seed material for the growth of a spinel ferrite shell is herein presented as a function of core size, chemical nature of the shell, and solvent polarity. Bulk characterization techniques (XRD, ICP, etc.) and transmission electron microscopy probed down to the nanoscale level (HRTEM and STEM-EDX) have been used to get insights into heterostructure formation and spinel ferrite stability. The core–shell systems in which magnetically hard (CoFe2O4) and soft (MnFe2O4) ferrimagnetic materials are coupled are also investigated as heat mediators under the applied alternating magnetic field.
Sample | Seeds (mg) | n-oleatea (mmol) | 1-Pentanol (mL) | Octanol (mL) | Toluene (mL) | Distilled water (mL) | Temperature | Reaction time |
---|---|---|---|---|---|---|---|---|
a Referred to CoII–FeIII oleates for MnA@Co or FeII oleate for all the other samples. | ||||||||
MnA | — | 6 | 10 | 10 | — | 5 | 220 | 10 |
MnB | — | 1.5 | 10 | — | 10 | 5 | 220 | 10 |
MnC | — | 3 | 10 | — | 10 | 5 | 220 | 10 |
Co | — | 6 | 10 | — | 10 | 5 | 220 | 10 |
MnA@Co | 50 | 2 | 10 | — | 10 | 5 | 220 | 10 |
MnA@Fe1 | 50 | 2 | 10 | — | 10 | 5 | 220 | 10 |
MnA@Fe2 | 50 | 2 | 10 | 10 | — | 5 | 220 | 10 |
MnB@Fe | 25 | 1 | 10 | — | 10 | 5 | 220 | 10 |
MnC@Fe | 25 | 1 | 10 | — | 10 | 5 | 220 | 10 |
Hydrophobic nanoparticles were converted to hydrophilic nanoparticles by ligand exchange with PEG-TMS.65 6 mg of inorganic particles was dispersed in 30 mL of hexane containing 0.01% (v/v) acetic acid. Then, 0.5% (v/v) of PEG-TMS was added to the mixture and kept under stirring in a rotating shaker for 72 hours, during which the particles were sedimented. The black-brown precipitate was separated using a magnet and washed three times with hexane to remove all silanes in excess. The product was re-dispersed in distilled water. The concentration of colloidal dispersions was 3.4 mg mL−1 for all the samples.
TEM images were obtained using a JEOL 200CX operating at 160 kV. The particle size distribution was obtained by measuring over 1000 particles with the aid of software Pebbles, setting a spherical shape for the elaboration.69 The volume-weighted particle diameter was calculated as
DTEM_V = DTEMe(3σ2) | (1) |
HRTEM images were acquired using a JEOL JEM 2010 UHR equipped with a 794 slow-scan CCD camera.
EDX measurements were performed on an FEI Talos F200X in the STEM mode using a field-emission gun operating at 200 kV equipped with a four-quadrant 0.9-sr energy-dispersive X-ray spectrometer. The core size and shell thickness were calculated by examining about 20 particles using software ImageJ.
Fourier-Transform Infrared (FT-IR) spectra were recorded in the 400 to 4000 cm−1 range using a Bruker Equinox 55 spectrophotometer. Samples were measured in a KBr pellet. Spectra were processed using OPUS software.
Thermogravimetric Analysis (TGA) curves were obtained using a PerkinElmer STA 6000, in the 25–850 °C range, with a heating rate of 10 °C min−1 under 40 mL min−1 O2 flow.
Room temperature 57Fe Mössbauer spectroscopy was performed on a Wissel spectrometer using the transmission arrangement and a proportional detector LND-45431. An α-Fe foil was used as a standard, and the fitting procedure was done using the NORMOS program to determine the isomer shift, quadrupole splitting, hyperfine field, and full width at half maximum of the signals.
Inductively coupled plasma-optical emission spectroscopy (ICP-OES) was performed on an Agilent 5110 spectrometer. The samples (around 5 mg) were digested by adding 4 mL of concentrated nitric acid (65%) and stirring for 3 hours at 60 °C. The solution was then filtered with 0.20 μm sieves and diluted for analysis. The calibration curve was done with iron, cobalt, and manganese NIST standards in the range 0.1–2 ppm, employing argon (420.067 nm) as the internal standard and using the following wavelengths for the analysis with the coefficient of determination given in brackets: for cobalt, 228.615 nm (R2 = 0.9999), 230.786 nm (R2 = 0.9998), and 237.863 nm (R2 = 0.9999); for iron, 234.350 nm (R2 = 0.9891), 238.204 (R2 = 0.9893), and 259.940 (R2 = 0.9888); for manganese, 257.610 nm (R2 = 0.9996), 259.372 nm (R2 = 0.9995), and 260.568 nm (R2 = 0.9998). For the calculation of the stoichiometry of the shell in the sample MnA@Co, it was assumed that the stoichiometry of the core did not change.
The magnetic properties were studied using a Quantum Design SQUID magnetometer (Hmax = ±55 kOe). Zero field cooled–field cooled (ZFC–FC) protocols were used to record the magnetization versus temperature curves within 5–300 K under different values of magnetic field. The ZFC curve was obtained by heating the sample from 5 to 300 K under a magnetic field after a cooling process under a zero magnetic field. The FC curve was obtained by cooling the sample from 5 to 300 K under a nonzero magnetic field.
Calorimetric estimation of specific absorption rate (SAR) was carried out using a non-adiabatic experimental set-up built at the LAboratorio di Magnetismo Molecolare (LA.M.M.) using a power supply CELESs MP6/400 (FIVES CELES), a water-cooled heating station connected to the power supply, and an induction coil. Heating curves were recorded under a magnetic field of 17 kA m−1 at 183 kHz for 300 s on water colloidal dispersions of the magnetic NPs. The hydrophobic NPs were made hydrophilic by the ligand exchange procedure with PEG-TMS. The concentration of the colloidal dispersion was 3.4 mg mL−1 for all samples. The temperature of the sample was monitored with an optical fiber probe (OPTOCON-FOTEMP) dipped into the solution. The sample holder was surrounded by polystyrene and placed in a glass Dewar, equipped with an ethylene glycol thermostat, to ensure proper thermal insulation. The SAR, i.e., the thermal power per mass unit, values were estimated by a linear curve fitting in the first 20 s of the heating curves (initial slope method).
Sample | Formula | D TEM_V (nm) | σ TEM (%) | D COREEDX (nm) | D XRD (nm) | ε (10−3) | a (Å) | Fe/Mn | Feshell/Fecore |
---|---|---|---|---|---|---|---|---|---|
MnA | Mn0.91Fe2.06O4 | 8.2 | 13 | — | 9.0 (1) | 4.6 (1) | 8.49 (2) | 2.3 | — |
MnA@Co | Mn0.91Fe2.06O4@Co0.98Fe2.02O4 | 11.6 | 9 | 5.2 (7) | 12.5 (1) | 4.2 (1) | 8.441 (1) | 6.3 | 1.7 |
MnA@Fe1 | — | 11.8 | 9 | — | 14.3 (1) | 3.8 (1) | 8.382 (1) | 24.4 | 9.6 |
MnA@Fe1S | — | 6.8 | 12 | — | 7.9 (1) | 6.5 (2) | 8.384 (3) | 12.6 | 4.4 |
MnA@Fe2 | — | 7.5 | 29 | — | 9.6 (1) | 5.2 (2) | 8.393 (2) | 21.1 | 8.1 |
MnB | Mn0.95Fe2.03O4 | 9.7 | 18 | — | 10.6 (1) | 4.0 (1) | 8.493 (1) | 2.1 | — |
MnB@Fe | — | 13.7 | 10 | 6.5 (9) | 13.8 (1) | 4.4 (1) | 8.400 (1) | 11.8 | 4.4 |
MnC | Mn0.87Fe2.09O4 | 11.4 | 13 | — | 13.5 (1) | 3.8 (1) | 8.489 (1) | 2.4 | — |
MnC@Fe | — | 13.5 | 13 | 9.2 (9) | 14.5 (1) | 5.1 (1) | 8.435 (1) | 7.1 | 1.9 |
Co | Co0.95Fe2.03O4 | 11.7 | 12 | — | 14.1 (1) | 3.6 (1) | 8.395 (1) | — | — |
The XRD patterns of MnA, MnB, and MnC displayed in Fig. 1 reveal the typical reflexes of the spinel ferrite phase and the calculated lattice parameter (8.492 ± 0.001 Å) fits well with the manganese ferrite value reported in the literature (8.4990 Å, PDF Card 010-0319). For all samples, microstrain values are in the order of 10−3, in agreement with previous results on spinel ferrite-based heterostructures of similar size and prepared by the oleate-based solvothermal method.43 The particles exhibit a spherical shape and a homogeneous distribution of Fe and Mn (TEM and STEM-EDX chemical mapping in Fig. 1). Similar values of crystallite (DXRD) and particle size (DTEM_V) account for highly crystalline particles, as revealed in the HRTEM images (Fig. 2S‡), which also show the inter-lattice distances typical for spinel ferrites. Moreover, a monolayer of oleate molecules (Fig. 3S and 4S‡) surrounds the particles.10 ICP-OES analysis of samples (Table 2) shows that sub-stoichiometric manganese ferrite (Mn0.91±0.04Fe2.03±0.03O4) is present, similarly to the results already obtained elsewhere.10,63
Interestingly, as it can be seen by the TEM and HRTEM images reported in Fig. 2 and 3, the sample MnA@Co features different morphologies besides spheroidal, in contrast to MnA@Fe1. To better understand these features and study the heterostructure architecture, STEM-EDX chemical mapping was performed on both samples (Fig. 4). For MnA@Fe1, spherical Mn-free iron oxide nanoparticles were formed, suggesting that manganese was completely dissolved. This dissolution effect is visible, to a less extent, also for MnA@Co (Fig. 4), showing a smaller core size than the original MnA (5.2 nm (DCOREEDX) vs. 8.2 nm (DTEM_V); 74% volume reduction) and asymmetric covering of the shell, which indicates an inhomogeneous growth of cobalt ferrite. These results are also confirmed by ICP-OES analysis of samples (Table 2, vide supra). Indeed, while a minimal amount of manganese was revealed in MnA@Fe1 (Fe/Mn = 24.4 and Feshell/Fecore = 9.6), MnA@Co features a stoichiometric cobalt ferrite shell (Mn0.91Fe2.06O4@Co0.98Fe2.02O4). The latter result indicates that the observed dissolution phenomenon involves the whole manganese ferrite phase and did not affect the stoichiometry of cobalt ferrite.
Fig. 3 HRTEM images with inter-lattice distances and Miller's indices for the sample MnA@Co. A red line highlights the defects and edges of the nanocrystals. |
Some authors have reported the observation of dissolution phenomena on colloidal dispersions of nanoparticles subjected to thermal treatment.10,70–75 However, in the case of core–shell nanoparticles, the dependence of the dissolution phenomena on the size and chemical nature of the shell has not been treated so far. Here, the systematic study revealed that manganese dissolution is more evident in shells formed by iron oxide rather than cobalt ferrite. Explaining this difference is rather complex since several phenomena take place simultaneously. The following aspects can play a role: (i) solubility of nanostructured metal oxides (core and shell) at a specific temperature, (ii) stabilities of the metal–oleate complexes, (iii) nucleation and growth kinetics of the shell, and (iv) strength of interaction between the NP surface and oleate molecules.
Different authors take into account the hard/soft acid/base theory,76–78 where carboxylates and MnII/FeIII are classified as hard bases/acids, while CoII and FeII are borderline acids. In this context, MnII/FeIII–oleate complexes should be more stable than CoII/FeII–oleate ones. Nevertheless, this interpretation is contradicted when the hydration enthalpies of aqua ions79 or the solubility products of hydroxides are considered. Indeed, H2O and OH− are hard bases (Table 1S‡), and we should expect stronger bonds with MnII and FeIII, considering the hard–soft properties of metal cations. Actually, for both aqua ions and hydroxides, the stability follows the order FeIII > CoII > FeII > MnII. The softer behavior of MnII can be explained in terms of a larger ionic radius (Table 1S‡), which results in higher polarizability. The lower stability of MnII aqua ions and hydroxides should reflect in the lower stability of manganese ferrite if compared to both cobalt ferrite and iron oxide. This trend could explain the observed dissolution phenomenon for manganese ferrite cores. Moreover, the dependence of dissolution phenomena on the chemical nature of the shell can be justified by the higher stability of the CoII species than the FeII ones, which can be reflected in the nucleation kinetics. Indeed, the presence of manganese ferrite in MnA@Co and its absence in MnA@Fe1 can be caused by a faster nucleation rate of cobalt ferrite than iron oxide, which can grow around manganese ferrite before it is completely dissolved. This hypothesis can be confirmed by considering the nucleation and growth mechanism of single-phase NPs. It has already been observed63 that, under the same synthesis conditions, cobalt ferrite gives rise to larger particles than iron oxide. The fast growth of cobalt ferrite when manganese ferrite dissolves progressively can give rise to the formation of asymmetric core shells in MnA@Co, and in some cases, heterojunctions, instead of core–shell architectures (Fig. 3).
The structural and magnetic properties of MnA, MnA@Fe1, and MnA@Co were studied through 57Fe Mössbauer spectroscopy, at room temperature (RT), and DC magnetometry (Fig. 5). At RT, the sample MnA shows a singlet, accounting for nanoparticles in the superparamagnetic state, having an isomer shift of 0.32 mm s−1, typical of FeIII. In contrast, the sample MnA@Co reveals the presence of two overlapped sextets, caused by spinel ferrite nanoparticles in the blocked state, due both to the larger size of particles and the presence of CoII, that cause an increase of the magnetic spin flipping energy barrier (ΔEa = KV, where K is the anisotropy constant and V the particle volume). The two sextets are derived from FeIII in the octahedral and tetrahedral sites of the spinel ferrite structures, as indicated in Table 2S.‡ In contrast, MnA@Fe1, even though larger than MnA, displays a sharp singlet, due to NPs in the superparamagnetic state, with an isomer shift of 0.41 mm s−1, which indicates the presence of FeIII, even though the higher value could be an indication of the presence of a small fraction of FeII. Therefore, both MnA and MnA@Fe1 display superparamagnetic behavior at 300 K, in contrast to MnA@Co, which reveals ferromagnetic behavior due both to the high anisotropy of CoFe2O4 and the rigid coupling between the two ferrimagnetic phases. This has been confirmed by both the hysteresis loop and DCD curves recorded at 5 K, clearly indicating high anisotropy for the MnA@Co sample (Fig. 5).9,17,80 Field-dependent magnetization curves obtained at 10 K (Fig. 5) show no hysteresis for the MnA and MnA@Fe1 samples, typical of magnetically soft ferrites, and a large hysteresis (Hc = 1.14 T) for MnA@Co, due to the presence of the hard cobalt ferrite. The saturation magnetization values found for the samples reach the maximum for the manganese ferrite sample (Ms = 101 emu g−1), as expected for the values found in the literature,81 and the minimum for MnA@Fe1 (Ms = 87 emu g−1), in agreement with the observed scenario of the absence of manganese ferrite in the latter sample and the predominance of FeIII ions. The ZFC curves (Fig. 5) exhibit, for all samples, a single maximum with the absence of a shoulder, indicating a single-particle population. Moreover, there is no separation of ZFC and FC curves at temperatures higher than Tmax, due to the small difference in blocking temperatures of the particles, as also evidenced by the small size dispersity of samples (9–13%). The blocking temperature (Tb) increases in the order of MnA < MnA@Fe1 < MnA@Co, in line with the particle size and effective anisotropy constant. The flatness of the FC curve, especially for MnA@Fe1, indicates high interparticle interactions. It is worth noting that the single maximum in the ZFC curve and the one-stage hysteresis loop of the field-dependent magnetization curve of MnA@Co are important evidence of a single magnetic response caused by the rigid coupling between cobalt and manganese ferrite.
The samples MnA and MnA@Fe1 were analyzed by 57Fe Mössbauer spectroscopy at low temperatures (LT) also to get insights into the site occupancy (Fig. 5, 6S and Table 3S‡).17,82–85 MnA exhibits an iron site occupancy of 22% and 78% for the tetrahedral and octahedral sites, respectively, which are reflected in the inversion degree value of 0.46, close to the values found in the literature for nanosized manganese ferrite.63 For MnA@Fe1, the site occupancy reached 37% for tetrahedral (Td) and 63% for octahedral (Oh) sites, due to the absence of manganese ferrite and the presence of only iron oxide, as observed from STEM-EDX chemical mapping. The ratio Fe(Oh)/Fe(Td), equal to 1.70, is very close to the theoretical γ-Fe2O3 ratio (1.67),81 indicating that, even though the presence of magnetite cannot be excluded, the sample is manly composed of maghemite.
Since the sample MnA@Fe1 did not evidence the presence of manganese ferrite, neither from STEM-EDX chemical mapping nor from 57Fe Mössbauer spectra, the particles present in the mother liquor of synthesis were analyzed. In fact, after the solvothermal treatment, the system is composed of large particles that were separated by a magnet (MnA@Fe1) and a mother liquor containing clear water and dark organic solvents, where smaller particles are present (MnA@Fe1S). This fraction, commonly discharged, has been collected and washed using the same procedure as for the other samples. The XRD pattern and TEM images of MnA@Fe1S are reported in Fig. 2, while the parameters are presented in Table 2. The sample features a spinel structure and a spheroidal particle shape, but with lower crystallite and particle sizes than both MnA and MnA@Fe1, and a higher microstrain value, probably due to the different formation mechanism. Interestingly, through STEM-EDX analysis (Fig. 4), it is possible to observe the formation of core–shell nanoparticles having iron oxide as the core and a thin layer (∼1 nm) of manganese ferrite as the shell. Therefore, the manganese ferrite that dissolved during the solvothermal synthesis of the core–shell grew around the just-formed iron oxide nanoparticles.
Another core–shell sample, MnA@Fe2, was prepared under the same synthesis conditions as for MnA@Fe1, but changing toluene with octanol, to study the effect of the use of a more polar solvent mixture (octanol and pentanol) on dissolution phenomena, and therefore, on core–shell formation. The as-obtained nanoparticles feature a spinel structure, a spheroidal shape, and a similar lattice parameter as MnA@Fe1 (Fig. 2 and Table 2) but a smaller particle size and a broader size distribution (29%), indicating that octanol is not a suitable solvent for producing high-quality core–shell nanoparticles. The STEM-EDX chemical mapping (Fig. 4) also exhibits, in this case, almost complete dissolution of manganese ferrite, as also evidenced by the ICP-OES data that show a similar content of manganese for MnA@Fe2 if compared with MnA@Fe1 (Fe:Mn = 21.1 and Feshell:Fecore = 8.1).
Similar to MnA@Fe1, MnB@Fe and MnC@Fe also feature larger crystallite and particle sizes and a lower size dispersity than the respective cores, suggesting a homogeneous growth of particles after the second solvothermal treatment. The STEM-EDX chemical mapping image, shown in Fig. 6, indicates the architecture of the core–shell nanoparticles in which, as evidenced above, the dissolution of manganese took place, but to a less extent in comparison with MnA@Fe1 and MnA@Fe2. Indeed, the core size of MnB@Fe decreased from 9.7 nm (DTEM_V) up to 6.5 nm (DCOREEDX; 70% volume reduction, Table 2) with a dispersity of 22% (similar to that of MnB), even though the final core–shell size dispersity is about 10% (σMnB = 18%). Regarding MnC@Fe, the core size decreased from 11.4 nm to 9.2 nm (DCOREEDX), with 47% volume reduction and 14% dispersity (σMnC = 13%). These results indicate that (i) the dissolution of manganese ferrite is size-dependent, and a linear trend has been found between the volume reduction due to dissolution and the DTEM_V of the cores (Fig. 7S‡); (ii) under the synthetic conditions employed, below a critical size (∼8 nm) the manganese dissolution is complete and a theoretical critical size of about 14 nm should be reached to hamper dissolution phenomena; (iii) a size-regularization process took place and led to core–shell nanoparticles with narrow size dispersity (10% and 14%), although the core size and shell thickness dispersity are relatively high. The size dependence on the manganese dissolution is also confirmed also by ICP-OES data, revealing an increase in the manganese content as the particle size increases (Fe/Mn = 24.4, 11.8, and 7.1; Feshell/Fecore = 9.6, 4.4, and 1.9 for MnA@Fe1, MnB@Fe, and MnC@Fe, respectively).
It has lately been demonstrated17,18,87 that the exchange coupling between a hard and a soft magnetic material enhances the heating performance with respect to the corresponding core, but the behavior of a core–shell nanoparticle having a soft core and a hard shell if compared to a hard nanoparticle of the same size led to different results in the literature. Indeed, Zhang et al.88 found better performances for a cobalt ferrite sample of 15 nm than those of MnFe2O4@CoFe2O4 of about 14 nm (core 7 nm) due to the lower anisotropy constant of the first nanoparticles. In contrast, Angelakeris and co-workers,89 comparing CoFe2O4 of 15 nm and a core–shell of 16 nm having a 10 nm MnFe2O4 core and a CoFe2O4 shell, obtained higher heating release for the latter sample, despite the lower saturation magnetization. Again, discording results were discovered when studying the effect of the amount of hard-CoFe2O4 shell in spinel iron oxide@cobalt ferrite systems. In one case, the group of Solopan90 revealed an initial increase and then a decrease when the thickness of the cobalt ferrite shell was increased from 0.1 nm to 1 nm and 2.5 nm. In the second case, a constant gain in the heat loss was found with decreasing cobalt ferrite shell thickness, by Yelenich et al.91 Generally, these studies are conducted in water, but sometimes hydrophobic particles in organic dispersions are analyzed.
In this work, magnetic heat dissipation performances were studied in the aqueous colloidal dispersion, after the ligand exchange reaction of oleate molecules with the PEG-TMS one, to render the nanoparticle surface hydrophilic.65Fig. 7 reports the heating curves obtained for the MnA@Co, Co, and MnC dispersions (Cox = 3.4 mg mL−1) under an alternating magnetic field of 183 kHz and 17 kA m−1 (Table 3). The resultant SAR value of the core–shell nanoparticles (43 W g−1, ILP = 0.81 nH m2 kgox−1) was higher, almost double, than that of the cobalt ferrite sample (24 W g−1, ILP = 0.45 nH m2 kgox−1), while MnC did not heat up at all. These results further confirm the efficiency of magnetic exchange coupling to boost the heat dissipation performances.
Fig. 7 Heating curves of aqueous colloidal dispersions of samples (Cox = 3.4 mg mL−1) at 30 °C. The magnetic field was 183 kHz and 17 kA m−1. |
Sample | D TEM_V (nm) | σ (%) | D DLS (nm) | D (μ2 s−1) | τ B (s) | SAR (W gox−1) | ILP (nH m2 kgox−1) |
---|---|---|---|---|---|---|---|
MnA@Co | 11.6 | 9 | 23(6) | 7.7 | 1.1 × 10−4 | 43(5) | 0.81(9) |
Co | 11.7 | 12 | 33(8) | 3.5 | 1.2 × 10−3 | 24(1) | 0.45(2) |
MnC | 11.4 | 13 | 42(10) | 2.6 | 3.0 × 10−3 | 0 | 0 |
Footnotes |
† The present work is dedicated to Prof. Anna Musinu, on the occasion of her retirement, for her precious and unique contribution to research and teaching activities of the Solid State Chemistry and Nanomaterials Group. |
‡ Electronic supplementary information (ESI) available: Scheme of synthesis. Additional TEM and STEM-EDX figures. FTIR spectra. TGA curves. Rietveld refinements of XRD patterns. Magnetic properties. Magnetic fluid hyperthermia. See DOI: 10.1039/d0na00967a |
This journal is © The Royal Society of Chemistry 2021 |