| Literature DB >> 35343985 |
Lorena Moor1, Subas Scheibler1,2, Lukas Gerken1,2, Konrad Scheffler3,4, Florian Thieben3,4, Tobias Knopp3,4, Inge K Herrmann1,2, Fabian H L Starsich1,2.
Abstract
Signal stability is crucial for an accurate diagnosis via magnetic particle imaging (MPI). However, MPI-tracer nanoparticles frequently agglomerate during their in vivo applications leading to particle interactions altering the signal. Here, we investigate the influence of such magnetic coupling phenomena on the MPI signal. We prepared Zn0.4Fe2.6O4 nanoparticles by flame spray synthesis and controlled their inter-particle distance by varying SiO2 coating thickness. The silica shell affected the magnetic properties indicating stronger particle interactions for a smaller inter-particle distance. The SiO2-coated Zn0.4Fe2.6O4 outperformed the bare sample in magnetic particle spectroscopy (MPS) in terms of signal/noise, however, the shell thickness itself only weakly influenced the MPS signal. To investigate the importance of magnetic coupling effects in more detail, we benchmarked the MPS signal of the bare and SiO2-coated Zn-ferrites against commercially available PVP-coated Fe3O4 nanoparticles in water and PBS. PBS is known to destabilize nanoparticle colloids mimicking in vivo-like agglomeration. The bare and coated Zn-ferrites showed excellent signal stability, despite their agglomeration in PBS. We attribute this to their process-intrinsic aggregated morphology formed during their flame-synthesis, which generates an MPS signal only little affected by PBS. On the other hand, the MPS signal of commercial PVP-coated Fe3O4 strongly decreased in PBS compared to water, indicating strongly changed particle interactions. The relevance of this effect was further investigated in a human cell model. For PVP-coated Fe3O4, we detected a strong discrepancy between the particle concentration obtained from the MPS signal and the actual concentration determined via ICP-MS. The same trend was observed during their MPI analysis; while SiO2-coated Zn-ferrites could be precisely located in water and PBS, PVP-coated Fe3O4 could not be detected in PBS at all. This drastically limits the sensitivity and also general applicability of these commercial tracers for MPI and illustrates the advantages of our flame-made Zn-ferrites concerning signal stability and ultimately diagnostic accuracy.Entities:
Year: 2022 PMID: 35343985 PMCID: PMC9119029 DOI: 10.1039/d1nr08402j
Source DB: PubMed Journal: Nanoscale ISSN: 2040-3364 Impact factor: 8.307
Fig. 1STEM images of as-prepared (a) bare and (b) 70 wt% SiO2-coated Zn0.4Fe2.6O4 nanoparticles. Insets schematically depict characteristic morphology. Table (below) summarizes morphological characteristics of the different prepared particles: crystal sizes (dXRD), geometric mean primary particle sizes of core (dTEM,core), geometrical standard deviations of primary particle sizes of core (σg), geometric means of hydrodynamic diameter (dDLS), ζ-potentials (ζ-pot).
Fig. 2(a) Magnetizations per mass of overall sample as function of applied field. (b) Magnetizations per mass of overall sample as a function of temperature at a constant applied field of 150 mT (i.e. field-cooling curves). Blocking temperatures are indicated by a blue hollow sphere.
Summary of magnetic properties extracted from magnetization and field-cooling curves: saturation magnetizations (Ms) per mass of overall samples and per nominal mass of magnetic core, coercivities (Hc), magnetic susceptibilities (χ), blocking temperatures (TB)
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| [emu gsample−1] | [emu gcore−1] | [mT] | [1/mT] | [K] | |
| Zn0.4Fe2.6O4 – 0 wt% SiO2 | 59 | 59 | 0.86 | 0.03 | 252 |
| Zn0.4Fe2.6O4 – 15 wt% SiO2 | 52.7 | 62 | 0.72 | 0.036 | 227 |
| Zn0.4Fe2.6O4 – 50 wt% SiO2 | 29.7 | 59.4 | 0.31 | 0.047 | 215 |
| Zn0.4Fe2.6O4 – 70 wt% SiO2 | 18.1 | 60.3 | 0.39 | 0.059 | 201 |
Fig. 3MPS results: (a) measured signal as function of time; (b) measured signal as a function of applied field (i.e. point spread function); (c) magnetization as a function of frequency (i.e. magnetic spectrum); (d) magnetization as a function of applied field strength (i.e. hysteresis). Measurements were conducted at 20 mT with a frequency of 26 kHz and at a constant nominal magnetic material concentration of 17 g L−1.
Fig. 4Comparison of signal stability as a function of dispersion medium for synthesized Zn-ferrites and commercial magnetite nanoparticles. Calibration curves for (a) 3rd and (b) 15th harmonic for bare and SiO2-coated (70 wt%) Zn0.4Fe2.6O4, as well as commercial PVP (polyvinylpyrrolidone)-coated Fe3O4, dispersed in H2O (closed symbols) or PBS (open symbols). (c) The slope of the calibration lines as a function of the harmonics for all samples in H2O and PBS. (d) The ratio of the calibration slopes in PBS over H2O for all particles. A value close to 1 indicates a stable signal. Samples were measured at the same overall particle concentrations (core + shell).
Fig. 5Signal stability in vitro. Particles were incubated with cells for 24 h and their concentration and MPS signal after washing were determined. Data is shown for bare and SiO2-coated (70 wt%) Zn0.4Fe2.6O4, as well as commercial PVP-coated Fe3O4 dispersed in H2O (closed symbols) or PBS (open symbols). (a) Ratio of MPS signals predicted at the measured particle concentration through calibration curves and actual measured MPS signal. (b) Error of particle concentration determined via MPS calibration curves.
Fig. 6Influence of dispersion medium on MPI quality of SiO2-coated (70 wt%) Zn0.4Fe2.6O4, as well as commercial PVP-coated Fe3O4, dispersed in H2O or PBS at 17 g L−1. (a) Absolute values of the system matrices at 99.57 kHz. Values are normalized to sample maximum. (b) Signal at the particle location as a function of the signal harmonics. (c) Reconstructed images of all samples. Signals are normalized to sample maximum. Blue square indicates particle location. (d) Ratio of signal measured in H2O over PBS at the particle location as a function of the signal harmonics.