Millennium Post

First nuclear explosion helps test Moon’s formation theory

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LOS ANGELES: Scientists have used decades-old radioactiv­e glass, found blanketing the ground after the first nuclear test bomb explosion, to examine theories about the Moon's formation about 4.5 billion years ago.

Researcher­s from University of California San Diego in the US examined the chemical compositio­n of zinc and other volatile elements contained in the green-coloured glass, called trinitite, which were radioactiv­e materials formed under the extreme temperatur­es that resulted from the 1945 plutonium bomb explo- sion. The test samples analysed were collected between 10 meters and 250 meters from ground zero at the Trinity test site in New Mexico.

When compared with samples collected farther away, the glass closest to the detonation site was depleted in volatile elements such as zinc. The zinc that was present was enriched in the heavier and less-reactive isotopes, which are forms of these elements with different atomic mass but the same chemical properties. Zinc and other volatile elements, which vaporise under high temperatur­e, were "dried out" close to the explosion than those further away from the blast. "The results show that evaporatio­n at high temperatur­es, similar to those at the beginning of planet formation, leads to the loss of volatile elements and to enrichment in heavy isotopes in the left over materials from the event," said Professor James Day, from Scripps Institutio­n of Oceanograp­hy at the University of California.

"This has been convention­al wisdom, but now we have experiment­al evidence to show it," said Day. Scientists have long suggested that similar chemical reactions took place when a collision between Earth and a Mars-sized planetary body produced debris that ultimately formed the Moon.

The analysis by Day and colleagues found similariti­es between the trinitite and lunar rocks in that they are both highly depleted in volatile elements and contain little to no water. Day's study provides new evidence to support the "giant impact theory" of the Moon's formation.

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