Mysterious magnetism in Apollo moon rocks is natural in origin, new study finds

Lunar samples displayed in the paleomagnetism lab at Stanford. (Image credit: Harry Gregory)

Back in the 1980s, geophysicists analyzing moon rocks brought to Earth during Apollo missions were surprised to find very strong magnetic fields etched onto those samples. The moon is not large enough to power such a field, let alone do so for more than 1.5 billion years. How then, did these lunar samples get magnetized?

The conundrum had previously led a few researchers to suspect other sources of magnetism, including the possibility that the Apollo spacecraft ferrying the samples back home may be responsible. But now, a new study demonstrates that the magnetization preserved in lunar rocks is, in fact, natural in origin — and that spaceflight does not have a significant impact on the force. These findings disprove one of two big oppositions to the theory that the moon powered its own dynamo.

"You want to know that the spacecraft returning your sample is not magnetically frying your rock, essentially," Sonia Tikoo, an assistant professor of geophysics at the Stanford Doerr School of Sustainability and the lead author of the new study, said in a statement.

To arrive at their conclusions, Tikoo and study co-author Ji-In Jung exposed eight moon rock samples from four Apollo missions to magnets that generated magnetic fields with strengths equivalent to those generated onboard a spacecraft. For two days — which replicated a return journey from the moon — the samples were specifically exposed to a field strength of 5 millitesla, which is roughly 100 times stronger than Earth's magnetic field, according to the new study.

Later, the team observed how the "magnetic contamination" decayed and found it could be easily cleaned using standard methods.