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Published on: July 14, 2021
Testing the mean magnetization approximation, dimensionless and scaling numbers in magnetorheology
José Antonio Ruiz-López1, Juan Carlos Fernández-Toledano, Roque Hidalgo-Alvarez
1Department of Applied Physics, Faculty of Sciences, University of Granada, C/Fuentenueva s/n, 18071-Granada, Spain. jvicente@ugr.es.
The mean magnetization approximation is validated for inverse ferrofluids across broad conditions. However, for conventional magnetorheological fluids, its applicability is limited to magnetic saturation or infinite dilution scenarios.
Area of Science:
- Magnetorheology
- Soft Matter Physics
- Materials Science
Background:
- The mean magnetization (MM) approximation simplifies particle behavior in magnetorheological fluids.
- This approximation treats particles as effective dipole moments, crucial for theoretical and simulation studies.
- Mathematical justification for the MM approximation's widespread use is often lacking.
Purpose of the Study:
- To rigorously test the validity of the mean magnetization approximation.
- To evaluate the approximation's applicability across diverse magnetic field strengths and particle concentrations.
- To compare the MM approximation's performance in conventional magnetorheological fluids (CMRFs) and inverse ferrofluids (IFFs).
Main Methods:
- Experimental investigations
- Theoretical analysis
- Computational simulations
Main Results:
- The MM approximation is found to be highly applicable in IFFs up to 265 kA m⁻¹ field strengths and 20 vol% particle loadings.
- For CMRFs, the MM approximation is valid only under conditions of magnetic saturation.
- In CMRFs, the approximation is also applicable in the limit of infinite dilution.
Conclusions:
- The MM approximation offers a reliable framework for IFFs within tested parameters.
- The MM approximation's utility in CMRFs is significantly constrained, requiring specific conditions for accuracy.
- This study clarifies the scope and limitations of the MM approximation in magnetorheology.
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