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Radiocarbon Dating: From Willard Libby's Discovery to Modern Crime Solving

From Baltimore sewage to Nobel Prizes, radiocarbon dating has revolutionized history and forensics. Learn how it works and its impact on our world.

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This image looks like an edited photo in which I can see historical monuments, trees, group of people, board, sculptures, rocks and the sky.

Radiocarbon Dating: From Willard Libby's Discovery to Modern Crime Solving

Chemist Willard Libby's groundbreaking work in the mid-1940s led to the development of radiocarbon dating, a technique that has revolutionized our understanding of history and the environment. His pioneering efforts earned him the 1960 Nobel Prize in Chemistry.

Libby's journey began when he discovered carbon-14 in methane gas from Baltimore sewage. He realised that this radioactive isotope, constantly produced in the atmosphere by cosmic rays, could serve as a 'clock' within living things. Plants and animals absorb carbon-14 while alive, and upon death, it begins to decay at a predictable rate. This decay rate forms the basis of radiocarbon dating.

Modern laboratories, such as Oxford's Radiocarbon Accelerator Unit, have refined this method. They now use advanced mass spectrometers to analyse tiny samples, as small as a few milligrams. This precision has enabled the technique to resolve historical disputes, confirm the age of ancient artifacts, and even identify missing persons like Laura Ann O'Malley.

One notable application is the 'bomb pulse' method. It utilises the spike in carbon-14 levels caused by mid-20th century nuclear testing to precisely date materials from this period. This has proven invaluable in understanding climate change and resolving historical mysteries, such as confirming the age of Britain's oldest known human burial in Wales.

From its inception with Willard Libby's discovery to its current use in advanced laboratories, radiocarbon dating has proven to be an invaluable tool. It has revolutionized our understanding of history, crime identification, and climate change by providing a reliable method to date organic materials across millennia.

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