Why do ferrofluids move towards regions with higher magnetic field gradients?

  • Thread starter styleworker
  • Start date
  • Tags
    Convection
In summary, the conversation discusses the physics behind ferrofluids and how they behave in the presence of temperature and magnetic field gradients. The speaker explains that when a constant external magnetic field is applied, the magnetization gradient and magnetic field gradient are in opposite directions, resulting in a rise in the density of magnetic field lines. The mathematical solution for this phenomenon is given, but the speaker is looking for a physical explanation.
  • #1
styleworker
4
0
Hello!

I'm currently reading papers about ferrofluids and trying to understand the physics behind this topic.

I do understand, that if we consider a vertikal temperature gradient, we get a antiparallel magnetization gradient. The ferrofluid with a the higher magnetization will move to the area with higher magnetic field, if we have applied an external magnetic field gradient.

But if we consider a constant external magnetic field, the magnetization gradient induces a antiparallel magnetic field gradient. As far as I know, ferrofluids are superparamagnetic and therefore density of magnetic field lines will rise. So, in my mind, the magnetic field gradient has to be in the same direction as the magnetization gradient for a constant external magnetic field.
Here you can see an illustration of the above example: http://www.mpipks-dresden.mpg.de/~adlange/research.html#thermomagnetic"

Can somebody explain this phenomena?
 
Last edited by a moderator:
Physics news on Phys.org
  • #2
The mathematical solution is actually easy:

[itex]div\vec{B}=0[/itex]

with

[itex]\vec{B}= \mu_0(\vec{M}+\vec{H})[/itex]
[itex]\vec{H}=\begin{pmatrix} 0 \\ 0 \\ H_z \end{pmatrix} ,\vec{M}=\begin{pmatrix} 0 \\ 0 \\ M_z \end{pmatrix}[/itex]

we get

[itex]\frac{dH}{dz} = -\frac{dM}{dz}[/itex]

But the physical explanation?!
 

FAQ: Why do ferrofluids move towards regions with higher magnetic field gradients?

What is thermomagnetic convection?

Thermomagnetic convection is a phenomenon that occurs when a fluid is subjected to a magnetic field and a temperature gradient, causing the fluid to flow due to the interaction between thermal and magnetic forces.

What are the applications of thermomagnetic convection?

Thermomagnetic convection has various applications in industrial processes such as materials processing, crystal growth, and heat transfer enhancement. It also has potential uses in geophysics and astrophysics for studying convection in planetary cores.

How does thermomagnetic convection differ from regular convection?

Thermomagnetic convection differs from regular convection in that it is driven by both thermal and magnetic forces, whereas regular convection is only driven by temperature differences. Additionally, thermomagnetic convection can occur in electrically conducting fluids, while regular convection can occur in any fluid.

What factors affect the strength of thermomagnetic convection?

The strength of thermomagnetic convection is affected by the strength of the magnetic field, the temperature gradient, the properties of the fluid (such as its electrical conductivity and viscosity), and the geometry of the system in which it is occurring.

How is thermomagnetic convection relevant to Earth's magnetic field?

Thermomagnetic convection plays a crucial role in the generation and maintenance of Earth's magnetic field. It is believed that the convection of the liquid iron in the outer core, combined with the Earth's rotation, is responsible for the geodynamo that generates the magnetic field.

Back
Top