ferromagnetische

Ferromagnetic, or in German Ferromagnetische, describes materials in which the magnetic moments of atoms tend to align parallel to each other due to the quantum mechanical exchange interaction. This spontaneous alignment can persist after an external magnetic field is removed, below a characteristic temperature called the Curie temperature. Above this temperature, thermal fluctuations disrupt the alignment and the material becomes paramagnetic.

In most ferromagnets the magnetization is organized into domains, regions where moments are aligned in the same direction. The overall magnetization of a sample depends on the relative orientation of these domains. Domain walls separate differently aligned regions, and the movement or reorientation of these walls under an applied field gives rise to magnetic hysteresis—the history-dependent response that is central to many applications.

Common ferromagnetic elements include iron, nickel, and cobalt, together with numerous alloys and compounds. Notable hard ferromagnets (permanent magnets) include NdFeB and SmCo magnets, while soft ferromagnets with low coercivity are used in transformers and inductors. Variants such as ferrimagnetic and antiferromagnetic materials exhibit related, but distinct, forms of magnetic ordering.

Properties of ferromagnetic materials include high saturation magnetization, significant remanence after the external field is removed, and varying coercivity. These characteristics enable a range of applications in data storage, electric motors, sensors, and magnetic refrigeration. Research continues to explore new ferromagnetic materials, tuning of Curie temperatures, and technologies such as spintronics and permanent-magnet alternatives.