scholarly journals Size and property bimodality in magnetic nanoparticle dispersions: single domain particles vs. strongly coupled nanoclusters

Nanoscale ◽  
2017 ◽  
Vol 9 (12) ◽  
pp. 4227-4235 ◽  
Author(s):  
E. Wetterskog ◽  
A. Castro ◽  
L. Zeng ◽  
S. Petronis ◽  
D. Heinke ◽  
...  
Nanoscale ◽  
2018 ◽  
Vol 10 (4) ◽  
pp. 2052-2066 ◽  
Author(s):  
Jeppe Fock ◽  
Christoph Balceris ◽  
Rocio Costo ◽  
Lunjie Zeng ◽  
Frank Ludwig ◽  
...  

AC susceptibility (ACS) and optomagnetic (OM) measurements vs. field and frequency allow determination of the bivariate distribution in moment and size. The obtained correlation provides information on the morphology of the magnetic nanoparticles.


2007 ◽  
Vol 308 (2) ◽  
pp. 305-312 ◽  
Author(s):  
S. Dutz ◽  
R. Hergt ◽  
J. Mürbe ◽  
R. Müller ◽  
M. Zeisberger ◽  
...  

Nanoscale ◽  
2021 ◽  
Author(s):  
Christian Appel ◽  
Björn Kuttich ◽  
Tobias Kraus ◽  
Bernd Stühn

Non-polar magnetic nanoparticles exhibit agglomeration upon cooling. This process is followed by in-situ small angle X-ray scattering to assess structural properties of the emerging agglomerates. On the length scale of...


2017 ◽  
Vol 95 (13) ◽  
Author(s):  
F. H. Sánchez ◽  
P. Mendoza Zélis ◽  
M. L. Arciniegas ◽  
G. A. Pasquevich ◽  
M. B. Fernández van Raap

MRS Advances ◽  
2017 ◽  
Vol 2 (49) ◽  
pp. 2669-2674
Author(s):  
B. Dodrill ◽  
P. Ohodnicki ◽  
M. McHenry ◽  
A. Leary

AbstractFirst-order-reversal-curves (FORCs) are an elegant, nondestructive tool for characterizing the magnetic properties of materials comprising fine (micron- or nano-scale) magnetic particles. FORC measurements and analysis have long been the standard protocol used by geophysicists and earth and planetary scientists investigating the magnetic properties of rocks, soils, and sediments. FORC can distinguish between single-domain, multi-domain, and pseudo single-domain behavior, and it can distinguish between different magnetic mineral species [1]. More recently, FORC has been applied to a wider array of magnetic material systems because it yields information regarding magnetic interactions and coercivity distributions that cannot be obtained from major hysteresis loop measurements alone. In this paper, we will discuss this technique and present high-temperature FORC results for two magnetic nanoparticle materials: CoFe nanoparticles dispersed in a SiO2 matrix, and FeCo-based nanocrystalline amorphous/nanocomposites.


Author(s):  
Stuart McKernan ◽  
C. Barry Carter

The determination of the absolute polarity of a polar material is often crucial to the understanding of the defects which occur in such materials. Several methods exist by which this determination may be performed. In bulk, single-domain specimens, macroscopic techniques may be used, such as the different etching behavior, using the appropriate etchant, of surfaces with opposite polarity. X-ray measurements under conditions where Friedel’s law (which means that the intensity of reflections from planes of opposite polarity are indistinguishable) breaks down can also be used to determine the absolute polarity of bulk, single-domain specimens. On the microscopic scale, and particularly where antiphase boundaries (APBs), which separate regions of opposite polarity exist, electron microscopic techniques must be employed. Two techniques are commonly practised; the first [1], involves the dynamical interaction of hoLz lines which interfere constructively or destructively with the zero order reflection, depending on the crystal polarity. The crystal polarity can therefore be directly deduced from the relative intensity of these interactions.


2000 ◽  
Vol 10 (PR5) ◽  
pp. Pr5-271-Pr5-274
Author(s):  
H. Totsuji ◽  
K. Tsuruta ◽  
C. Totsuji ◽  
K. Nakano ◽  
T. Kishimoto ◽  
...  

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