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The First Atomic Bomb Test in 1945 Created an Entirely New Material
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The First Atomic Bomb Test in 1945 Created an Entirely New Material

Wired · May 17, 2026, 9:30 AM

Key takeaways

  • The term “clathrates” denotes materials characterized by a “cage-like” structure that traps other atoms and molecules inside, giving them unique properties.
  • To discover the new material, researchers focused on trinitite, a silicate glass containing rare metallic phases.
  • The new material, the researchers say, formed spontaneously during a nuclear explosion.

Why this matters: a development in AI with implications for how people work, create, and decide.

The new material is a clathrate made of calcium, copper, and silicon .Luca Bindi/Università di Firenze Comment Loader Save Story Save this story Comment Loader Save Story Save this story During the Trinity nuclear test on July 16, 1945, in the New Mexico desert—the world's very first test of an atomic bomb—a new material spontaneously formed. It was discovered only recently, by an international research team coordinated by geologist Luca Bindi at the University of Florence, which identified the novel clathrate based on calcium, copper, and silicon. It's a material never before observed either in nature or as an artificial compound created in the laboratory.

The term “clathrates” denotes materials characterized by a “cage-like” structure that traps other atoms and molecules inside, giving them unique properties. Of great technological interest, these materials are being studied for various applications ranging from energy conversion (as thermoelectric materials capable of transforming heat into electricity) to the development of new semiconductors, to gas storage and hydrogen for future energy technologies.

To discover the new material, researchers focused on trinitite, a silicate glass containing rare metallic phases. Using some techniques like x-ray diffraction, the team was able to identify a type I clathrate based on calcium, copper, and silicon within a tiny copper-rich metal droplet embedded in a sample of red trinitite.

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