Researchers discovered a previously unknown metal alloy formed by the 1945 Hiroshima atomic bomb blast.
The alloy was found embedded in small, glass-like beads called hiroshimaites, recovered from the beach sands of Hiroshima Bay.
The discovery was published in Science Advances on July 29.
The alloy formed due to the extreme heat (over 7,000 degrees Celsius) and subsequent ultrafast cooling of urban materials.
Detailed Insights:
The hiroshimaites are glass-like beads that formed when intense heat vaporized building materials, soil, and metals, which then solidified upon falling.
The micrometer-sized metallic grain identified within the beads is a complex mix of iron, chromium, nickel, manganese, molybdenum, silicon, and aluminium.
The unique crystal structure of the alloy is attributed to ultrafast quenching, a process where elements mixed under conditions impossible to replicate normally.
This discovery suggests that high-energy plasma events, like nuclear detonations, can act as natural laboratories for discovering new materials.
The alloy shares characteristics with other unusual high-entropy alloys and quasicrystals.
The research highlights how debris can preserve a "high-resolution record" of the chemical and physical environment during a nuclear event.
Scientific/Technical Concepts Involved:
Hiroshimaites: Small, glass-like beads formed from vaporized materials during the Hiroshima atomic bomb blast.
Ultrafast quenching: A rapid cooling process that can lead to the formation of unique material structures.
High-entropy alloys: Alloys containing multiple elements in near-equimolar ratios, often exhibiting unique properties.
Quasicrystals: Materials with an ordered, but non-periodic, atomic structure, unlike traditional crystals.