Low-background steel

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A body counting room at the Rocky Flats Plant in Denver, Colorado, made entirely from pre-World War II steel Body counting room at Rocky Flats Plant.jpg
A body counting room at the Rocky Flats Plant in Denver, Colorado, made entirely from pre-World War II steel

Low-background steel, also known as pre-war steel [1] and pre-atomic steel, [2] is any steel produced prior to the detonation of the first nuclear bombs in the 1940s and 1950s. Typically sourced from ships (either as part of regular scrapping or shipwrecks) and other steel artifacts of this era, it is often used for modern particle detectors because more modern steel is contaminated with traces of nuclear fallout. [3] [4]

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Steel

Since the end of atmospheric nuclear testing, background radiation has decreased to very near natural levels, [5] making special low-background steel no longer necessary for most radiation-sensitive uses, as brand-new steel now has a low enough radioactive signature that it can generally be used. [6] Some demand remains for the most radiation-sensitive uses, such as Geiger counters and sensing equipment aboard spacecraft. For the most demanding items even low-background steel can be too radioactive and other materials like high purity copper may be used. [4]

In cases where World War II-era shipwrecks in and near the relatively shallow Java Sea and western South China Sea that have been illegally scavenged it has been suggested that the target is low-background steel. [7] Andrew Brockman, a maritime crime researcher and archaeologist, argues that it is more likely to be conventional salvage. [8]

Radionuclide contamination

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. [6] Another source of radioactive contamination was the coating of steel cauldrons in Cobalt-60 in order to monitor wear. [8] Steel that would otherwise be expected to be low background can itself be contaminated due to thorium in welding rods. [4]

World anthropogenic background radiation levels peaked at 0.11  mSv/yr above natural levels in 1963, the year that the Partial Nuclear Test Ban Treaty was enacted. Since then, by about 2008, anthropogenic background radiation has decreased to 0.005 mSv/yr above natural levels. [5]

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<span class="mw-page-title-main">Nuclear and radiation accidents and incidents</span> Severe disruptive events involving fissile or fusile materials

A nuclear and radiation accident is defined by the International Atomic Energy Agency (IAEA) as "an event that has led to significant consequences to people, the environment or the facility." Examples include lethal effects to individuals, large radioactivity release to the environment, or a reactor core melt. The prime example of a "major nuclear accident" is one in which a reactor core is damaged and significant amounts of radioactive isotopes are released, such as in the Chernobyl disaster in 1986 and Fukushima nuclear disaster in 2011.

<span class="mw-page-title-main">Radioactive contamination</span> Undesirable radioactive elements on surfaces or in gases, liquids, or solids

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<span class="mw-page-title-main">Cobalt-60</span> Radioactive isotope of cobalt

Cobalt-60 (60Co) is a synthetic radioactive isotope of cobalt with a half-life of 5.2714 years. It is produced artificially in nuclear reactors. Deliberate industrial production depends on neutron activation of bulk samples of the monoisotopic and mononuclidic cobalt isotope 59
Co
. Measurable quantities are also produced as a by-product of typical nuclear power plant operation and may be detected externally when leaks occur. In the latter case the incidentally produced 60
Co
is largely the result of multiple stages of neutron activation of iron isotopes in the reactor's steel structures via the creation of its 59
Co
precursor. The simplest case of the latter would result from the activation of 58
Fe
. 60
Co
undergoes beta decay to the stable isotope nickel-60. The activated cobalt nucleus emits two gamma rays with energies of 1.17 and 1.33 MeV, hence the overall equation of the nuclear reaction is: 59
27
Co
+ n → 60
27
Co
60
28
Ni
+ e + 2 γ

<span class="mw-page-title-main">Caesium-137</span> Radioactive isotope of caesium

Caesium-137, cesium-137 (US), or radiocaesium, is a radioactive isotope of caesium that is formed as one of the more common fission products by the nuclear fission of uranium-235 and other fissionable isotopes in nuclear reactors and nuclear weapons. Trace quantities also originate from spontaneous fission of uranium-238. It is among the most problematic of the short-to-medium-lifetime fission products. Caesium-137 has a relatively low boiling point of 671 °C (1,240 °F) and easily becomes volatile when released suddenly at high temperature, as in the case of the Chernobyl nuclear accident and with atomic explosions, and can travel very long distances in the air. After being deposited onto the soil as radioactive fallout, it moves and spreads easily in the environment because of the high water solubility of caesium's most common chemical compounds, which are salts. Caesium-137 was discovered by Glenn T. Seaborg and Margaret Melhase.

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<span class="mw-page-title-main">Gamma ray</span> Energetic electromagnetic radiation arising from radioactive decay of atomic nuclei

A gamma ray, also known as gamma radiation (symbol
γ
), is a penetrating form of electromagnetic radiation arising from the radioactive decay of atomic nuclei. It consists of the shortest wavelength electromagnetic waves, typically shorter than those of X-rays. With frequencies above 30 exahertz (3×1019 Hz) and wavelength less than 10 picometer (1×10−11 m) gamma ray photons have the highest photon energy of any form of electromagnetic radiation. Paul Villard, a French chemist and physicist, discovered gamma radiation in 1900 while studying radiation emitted by radium. In 1903, Ernest Rutherford named this radiation gamma rays based on their relatively strong penetration of matter; in 1900 he had already named two less penetrating types of decay radiation (discovered by Henri Becquerel) alpha rays and beta rays in ascending order of penetrating power.

<span class="mw-page-title-main">Lists of nuclear disasters and radioactive incidents</span>

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<span class="mw-page-title-main">Radioactive source</span>

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References

  1. M. Manohari; R. Mathiyarasu; V. Rajagopal; V. Meenakshisundaram; R. Indira (2011). "Calibration of phoswich-based lung counting system using realistic chest phantom". Radiation Protection Dosimetry. 144 (1–4): 427–432.
  2. James Mahaffey. Atomic Awakening: A New Look at the History and Future of Nuclear Power. pp. 226–227.
  3. Aaron, D. Jayne; Berryman, Judith (1997). "Rocky Flats Plant, Emergency Medical Services Facility". U.S. Department of Energy, Office of Legacy Management. HAER No. CO-83-S (Rocky Flats Plant, Building 122). Archived from the original on 8 June 2019.
  4. 1 2 3 Mandelbaum, Ryan F (19 December 2017). "How Physicists Recycled WWII Ships And Artillery To Unlock The Mysteries Of The Universe". Gizmodo. Retrieved 25 May 2023.
  5. 1 2 Sources and Effects of Ionizing Radiation. United Nations Scientific Committee on the Effects of Atomic Radiation (UNSCEAR) (Report). Vol. I. New York: United Nations. 2010 [2008]. p. 6. ISBN   978-92-1-142274-0. UNSCEAR 2008 Report.
  6. 1 2 Adams, Cecil (10 December 2010). "Is steel from scuttled German warships valuable because it isn't contaminated with radioactivity?". The Straight Dope.
  7. "The world's biggest grave robbery: Asia's disappearing WWII shipwrecks". The Guardian.
  8. 1 2 Oelbaum, Jed (10 May 2018). "The Worldwide Scavenger Hunt For Vintage, Low-Radiation Metals". Good.is. Retrieved 27 May 2023.