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The arrows in Fig. 1 indicate the direction of magnetization of magnets.
The strength and direction of magnetization of the magnet blocks are measured using a Helmholtz coil system.
Figure 14a d demonstrates the change in the magnetic image depending on the direction of magnetization of a thin section.
Application of an external field changes the direction of magnetization of part or all of the domains, setting up a net magnetization parallel to the field.
From studying the direction of magnetization of many rocks, geologists know that such reversals occur, without a discernible pattern, at intervals that range from tens of thousands of years to millions of years, though they are still uncertain about the mechanisms responsible.
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It was long recognized that the directions of magnetization of many rocks do not correspond to the present direction of the geomagnetic field at their sites; but not until the 1950s was there sufficient paleomagnetic data to suggest that the poles had moved in a systematic way over the surface of the Earth.
Fig. 4. Equal area projections of the directions of magnetization of the high- and low-temperature components for samples from cores AVL1 and AVL2.
Because spinels are cubic in structure, with no preferred direction of magnetization, they are "soft" magnetically; i.e., it is relatively easy to change the direction of magnetization through the application of an external magnetic field.
One of such features is a topological charge which characterized a direction of magnetization vector M → reversal in the center of magnetic structure.
The Earth's magnetic field aligns the grains, yielding a preferred direction of magnetization.
It is found that the stiffness is improved by stacking the magnet in the special combination of different radial cum axial direction of magnetization.
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