Low-background steel is any steel produced prior to the detonation of the first atomic bombs in the 1940s and 1950s. With the Trinity test and the Atomic bombing of Hiroshima and Nagasaki in 1945, and then subsequent nuclear weapons testing during the early years of the Cold War, background radiation levels increased across the world. Modern steel is contaminated with radionuclides because its production used atmospheric air. Low background steel is so called because it does not suffer from such nuclear contamination. This steel is used in devices that require the highest sensitivity for detecting radionuclides.
From 1856 until the mid 20th century, steel was produced in the Bessemer process where air was forced into Bessemer converters converting the pig iron into steel. By the mid-20th century, many steelworks had switched to the BOS process which uses pure oxygen instead of air. However as both processes use atmospheric gas, they are susceptible to contamination from airborne particulates. Present-day air carries radionuclides, such as cobalt-60, which are deposited into the steel giving it a weak radioactive signature.
World anthropogenic background radiation levels peaked at 0.15 mSv/yr above natural levels in 1963, the year that the Partial Nuclear Test Ban Treaty was enacted. Since then, anthropogenic background radiation has decreased exponentially to 0.005 mSv/yr above natural levels.
However, cobalt-60 still contaminates modern steel because it has been recycled through the scrap metal supply chain.
Devices that require low-background steel include:
- Geiger counters
- Medical apparatus: whole body counting and lung counters
- Scientific equipment: photonics
- Aeronautical and space sensors
As these are detecting radioactive emissions, they require an extremely low radiation environment in order to work correctly. Low background counting chambers are made from low-background steel with extremely heavy radiation shielding. They are used to detect the minutest nuclear emissions.
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The estimated per caput effective dose of ionizing radiation due to global fallout from atmospheric nuclear weapons testing was highest in 1963, at 0.11 mSv/yr, and subsequently fell to its present level of about 0.005 mSv/yr (see figure II). This source of exposure will decline only very slowly in the future as most of it is now due to the long-lived radio-nuclide carbon-14.
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