Strontium-90 is with cesium-137 a major radioactive product of nuclear fission. After the explosion of an atomic bomb or within a nuclear reactor, it is abundant: 5.8% of uranium-235 fissions produces this radioelement. There was mention of strontium-90 during testing atomic bombs in the atmosphere of the 1960s. It was also widespread in accidents like those of the Techa River, Chernobyl and recently Fukushima.
Chemically, strontium is close to calcium in the Mendeleev classification. Like calcium, when absorbed, it is preferably fixed in the bone mass. It emits only beta radiation with a short range, which makes it harmful if swallowed or inhaled. In this case, it may be the source of bone cancers and leukaemias if the spinal cord is involved.
In food, milk and calcium-rich cheese favour strontium. At sea, strontium will be fixed more on oyster and mussels, crab and shrimp shells, fish bones and scales than in fish flesh. Strontium remains generally at low levels in aquatic organisms.
Strontium-90 does not emit gamma rays. Owing to the absence of very characteristic energy rays which would sign its presence, strontium-90 presence is difficult to identify. This absence of gamma rays also means reduced external exposures. One can tread without excessive risks ground contaminated by strontium-90 ...
Strontium-90 is less dispersed than cesium after reactor accidents because it is significantly less volatile, as has been observed in Chernobyl. Mobility and transfer into the environment however remain poorly understood.
Strontium transport by surface water and groundwater has been studied in the Chernobyl zone where large amounts of radioactive materials were found buried in a sand layer of 5 to 7 meters thick lying in a stagnant phreatic table. On the vertical, strontium 90 has contaminated ground water at around 10 kilobecquerels per litre (kBq / l). Tens of meters away, this contamination falls to about 0.1 kBq / l. In this situation, the migration of strontium-90 with water appeared to have been slow.
In Fukushima The strontium 90 issue has come up in the fall of 2013 near Fukushima after leaks of contaminated water that was stored in tanks. While a cesium decontamination of water was in place since 2011, that of strontium was not yet operational. Strontium-90 was present in water stored on the site, part of which was spilled mainly in March-April 2011 in the coastal zone.
The lifespan of strontium-90 is long on a human scale with a radioactive half-life of 28.79 years, close to that of cesium-137. In a first step it decays into Ytrium-90, which being instable itself becomes Zirconium-90 after a few tens of hours.
The energy available in the two decays in cascade is high, 2736 keV, the two beta electrons emitted taking on average half this amount. They dissipate locally their energy as heat after a short course in matter. Thereby, strontium-90 radiates a relatively large amount of heat : 0.91 watt per gram.
This energy release has led to the use of strontium-90 in the former Soviet Union for thermoelectric generators called RTG for supplying energy and electricity to a thousand beacons and unmanned lighthouses in the remote Siberian north. Such sources were much cheaper than plutonium-238 sources embarked for distant space missions of NASA.
The substantial heat released by strontium decays intervenes in the management of high level radioactive waste. When a vitrified waste package is produced at the La Hague plant, a quarter of the heat released - 500 watts - is due to strontium decay. This heat release requires many years of cooling before burying these waste packages in a deep geological repository. However at the time scale of such geological storages, the radioactivity and the heat release by strontium-90 decline by large amounts : they are divided by 11 within a century, by 1380 in three centuries..
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