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

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Ferrofluids exhibit movement toward regions with higher magnetic field gradients due to their superparamagnetic properties. When an external magnetic field is applied, the magnetization gradient causes the ferrofluid to migrate toward areas of increased magnetic field strength. This phenomenon occurs even in the presence of a constant external magnetic field, where the induced magnetization gradient creates an antiparallel magnetic field gradient. The relationship between the magnetic field and magnetization gradients can be mathematically described, but the underlying physical explanation remains complex. Understanding these interactions is crucial for applications in various fields, including engineering and materials science.
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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?
 
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The mathematical solution is actually easy:

div\vec{B}=0

with

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

we get

\frac{dH}{dz} = -\frac{dM}{dz}

But the physical explanation?!
 
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