Research news on remanent magnetism

Remanent magnetism, or remanence, is the magnetization that persists in a material after an external magnetic field is removed. It arises from the alignment and pinning of magnetic domains, controlled by factors such as crystal anisotropy, domain-wall energetics, and microstructural defects. In rock and mineral systems, remanent magnetism (including thermal, chemical, and depositional remanent magnetization) records the direction and intensity of past geomagnetic fields, enabling quantitative paleomagnetic and tectonic reconstructions. The magnitude and stability of remanent magnetism depend on grain size, composition, temperature history, and time-dependent relaxation processes such as viscous remanent magnetization.

When Earth's magnetic field took its time flipping

Earth's magnetic field is generated by the churn of its liquid nickel-iron outer core, but it is not a constant feature. Every so often, the magnetic north and south poles swap places in what are called geomagnetic reversals, ...

Reading the moon's diary, one speck of dust at a time

Magnetism on the moon has always been a bit confusing. Remote sensing probes have noted there is some magnetic signature, but far from the strong cocoon that surrounds Earth itself. Previous attempts to detect it in returned ...

Molten Martian core could explain red planet's magnetic quirks

Like Earth, Mars once had a strong magnetic field that shielded its thick atmosphere from the solar wind. But now only the magnetic imprint remains. What's long baffled scientists, though, is why this imprint appears most ...

Chang'e-6 farside basalts reveal a reinforced lunar dynamo

The evolution of the lunar dynamo is crucial for understanding the moon's deep interior structure, thermal history, and surface environment. A study by Chinese scientists conducted paleomagnetic analyses on basalts returned ...